WEBVTT

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<v ->Good evening.</v>

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Welcome to the annual Seaside Chat Speaker series.

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We will start promptly at 6:30 PM Central Time.

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All right. Good evening.

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We are pleased to have you join us today

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for our annual Seaside Chats Speaker series

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about ocean topics associated with Flower Garden Banks,

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National Marine Sanctuary,

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and the surrounding gulf habitats.

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We are also part

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of the National Marine Sanctuaries Webinar series.

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During the presentation,

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all attendees will be in listen-only mode.

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You are welcome to type questions

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for the presenters into the question box at the bottom

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of the control panel on the right hand side of your screen.

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You may also let us know

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about any technical issues you are having.

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We are monitoring incoming questions and technical issues

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and we'll respond to them as soon as we can.

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In addition, we encourage you to close all other programs

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you may have open on your computer

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or any non webinar tabs on your internet browser.

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This will ensure the best viewing quality for the webinar.

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We are recording the session

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and we'll post the recording

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to the National Marine Sanctuaries

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and Flower Garden Banks National Marine Sanctuary websites

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within a few weeks.

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We will notify registered participants via email

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when these recordings are available.

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And for those of you who are interested, we have a document

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of links to additional resources on today's topic

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in the handout pane of the control panel,

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simply click on this item to download.

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So my name is Taylor Galaviz.

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I am the Constituent Engagement Specialist

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and Acting Education Coordinator

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for Flower Garden Banks National Marine Sanctuary.

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I am facilitating today's webinar from Galveston, Texas.

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Also with me today is Olivia Eisenbach,

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one of our research specialist who will be helping me

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with the backend administration of this webinar.

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So in 1972, the United States ushered in a new era

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of ocean conservation

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by creating the National Marine Sanctuary system.

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Since then, we've grown into a nationwide network

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of 18 national marine sanctuaries

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and two national marine monuments

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that can serve more than 629,000 square miles

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of spectacular ocean and great lakes waters.

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These marine protected areas are similar to national parks,

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but underwater.

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The National Marine Sanctuaries Act gives NOAA the authority

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to designate special marine areas

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such as National Marine Sanctuaries.

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It also mandates that the Office

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of National Marine Sanctuaries conduct research, monitoring,

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resource protection, education, outreach

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and management of America's underwater treasures

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to preserve them for future generations.

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In addition to being places for recreation and research,

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national marine sanctuaries are also living classrooms

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where people can see, touch, learn

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about the nation's great lakes and ocean treasures.

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This webinar series is just one part

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of that national education and outreach effort.

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The Seaside Chat series is hosted

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by Flower Garden Banks National Marine Sanctuary,

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the only national marine sanctuary in the Gulf.

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This sanctuary consists of 17 banks

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or small underwater mountains that are home

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to some of the healthiest coral reefs in the world.

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Amazing algal and sponge communities

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and deeper mesophotic reef habitats featuring an abundance

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of black coral and gorgonians.

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We invite you to learn more about us

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by visiting the sanctuary website at flowergarden.noaa.gov.

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Now to kick us off this evening, I'm gonna give a little bit

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of background over some programs

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that we currently have ongoing within the sanctuary.

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So these banks lie 80 to 125 miles from shore

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and create a chain of protected habitats

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that are both ecologically and economically important

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across the Northwestern Gulf.

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East Flower Garden Bank and West Flower Garden Bank

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were the original parts of the sanctuary

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when it was designated in 1992.

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The coral reefs at East and West Flower Garden Bank

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are some of the healthiest in the world

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surviving at the northern limits of their range.

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These reefs are perched on top of small underwater mountains

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that are brought up from the sea floor into the photic,

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also known as the light zone,

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and provide hard surfaces where coral larvae could settle.

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Far from shore, they thrived unnoticed by humans

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for thousands of years.

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The reefs on top of East and West Flower Garden Banks

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are dominated by large stony corals,

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mostly brain and star corals.

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And of these hard corals that grow

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of there are about 20 species,

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but in the photic or shallow zones there are no soft corals.

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And these are the ones that are flexible,

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sway with the currents, things like sea fans and sea whips.

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And those are gonna be found more

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in the mesophotic habitats, so in the deeper waters.

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In addition, over 52% of the bottom is covered

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in these hard reef building corals.

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This is a phenomenal amount of coral,

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especially at a time when reefs

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around the globe are in decline.

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Another aspect of these coral reefs are their depths.

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The highest point of these reef,

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these reefs are about 55 feet underwater,

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whereas most reefs are shallower

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and may even have corals that reach up to the surface.

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Adding to the intrigue

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of these beautiful healthy coral reefs is the fact

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that they are situated in the middle of one

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of the most active oil fields in the world.

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So if you look at this map, the blue dots are platforms

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and the white dash lines are pipelines

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that are in the immediate vicinity

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of East and West Flower Garden Banks.

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In addition, one platform used to operate

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within the sanctuary boundaries at the southeast edge

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of East Flower Garden Bank.

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This platform called High Island A-389-A was in place

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before the sanctuary was designated

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and is important part for the following discussion.

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All right, so in the midst of all this

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there are these reefs that are still healthy.

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The sanctuary's long-term monitoring program

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helps to look at that.

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So what do we look at?

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What kinds of data do we collect and how do we analyze it?

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So monitoring here actually predates the sanctuary itself.

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It started in 1978 as a regulatory requirement

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by the government agency that we now know

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as the Bureau of Ocean and Energy Management or BOEM

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for the High Island A-389-A platform

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which sat less than a mile from East Flower Garden Bank.

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It was later decided

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that this should become a more long-term effort.

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And in 1988, the Flower Garden Bank's

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long-term monitoring program was established.

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This program was managed by BOEM until 2008

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when the sanctuary research vessel was acquired.

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Since 2009, sanctuary staff

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have managed the monitoring program

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with supporting funds from BOEM.

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So the photo on your screen is from 2011

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and you can see our Research Vessel MANTA is moored

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at East Flower Garden Bank

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with the platform in the distance.

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This platform was decommissioned

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and partially removed in 2018.

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Since it would be impossible

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to survey the entire reef each year

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our long-term monitoring takes place

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within two permanent study sites,

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one at East Flower Garden Bank,

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and one at West Flower Garden Bank.

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Each site is a hundred meters by a hundred meters squared.

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The white boxes on these maps

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show their locations on the reef.

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The study sites were selected as being representative of

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what we might see across most if not all of the reef.

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So what we learn from studying these small areas

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is then extrapolated to represent the entire reef.

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Each year the sides of the study site are marked out

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with a hundred meter measuring tapes,

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which are attached to metal stakes.

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And as you can see here, trumpetfish occasionally

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take advantage of these temporary lines for camouflage.

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A pin at the center of the site allows researchers,

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to divide the site into quadrants,

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which makes it easier to navigate around the site.

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These quadrant lines are referred to as the cross hairs.

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So within the study site

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researchers conduct the following activities:

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random photo transects,

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repetitive photo stations, fish surveys,

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and lobster and urchin surveys.

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So let's start with random transect.

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There are 24 ten meter transects

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that are placed randomly about the reef.

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A diver then uses a camera system mounted on a metal T frame

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to take 17 non-overlapping images

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along a 10 meter transect.

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These images are later evaluated for benthic cover,

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also known as bottom cover,

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percentages of coral, algae ,sponges and substrate.

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Now onto the repetitive photo station.

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So these are identified by metal pins

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that are placed at various locations around the study site

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so that comparative photos can be taken year after year.

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Over the years some of the stations have gone missing

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and some new stations have been established,

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but many of the original stations are still used today.

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So a map of the study site can shows

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the approximate location of each pin

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along with the distances and headings

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from a known point along the line to mark the study site.

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The symbols and colors on the map are used to designate

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different kinds of stations as well as locations

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that may not have been found in the previous years.

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But just because we didn't find a pin one year

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doesn't mean it's not still there.

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Sometimes we'll find it again in the future

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or we can use the photos that we've taken previously

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to help find the stations even if it's been camouflaged,

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damaged or missing.

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These are repetitive photo station images are taken

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using a camera mounted on a longer T frame

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than those that are used for random transects.

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This helps standardize the amount of area

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covered by each photo, which is about five square meters.

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The base of the frame is placed at the pin

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and oriented so that the compass on top is facing north.

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A level on top of the T frame helps the photographer

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get the same angle on the photo from year to year.

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Taking the same image in the same way year after year

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provides a time series for specific sections of the reef.

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Just like with random transects,

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these images are evaluated for benthic cover

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of coral algae, sponges and substrate.

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So I have a question for you all.

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Why do we need photo stations and photo transects

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if they collect the exact same kind of data?

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I'll give you a second to think about it.

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And if you've got anyone in the room with you,

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you may wanna discuss that amongst yourself.

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All right.

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So if you thought to yourself

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or you talked with someone else,

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the repetitive photo stations give us a time series

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for evaluation of the same spots

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over an extended period of time.

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So I'm talking years, even decades.

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These random transects give us a look at a broader spectrum

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of the reef so it can help us kind of fill in the gaps

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where those repetitive photo stations

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are locked into one place.

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All right, now analysis of the data

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included in the long-term monitoring reports

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for East and West Flower Garden Banks and Stetson Bank.

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This includes comparisons to previous data

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so that we can note trends over a longer period of time.

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So please remember that benthic data is

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from random transects and repetitive photo stations

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is just one part of the story.

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We also do fish and invertebrate surveys that is analyzed

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and included in these reports.

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So these science reports can help with management decisions.

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Help us see the bigger picture of the condition

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of the reef over time and identify those long-term trends.

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So the product of long-term monitoring

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is to better understand the overall health of the reef

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and be able to track the effects of bleaching, disease

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and mortality in corals.

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Fate tracking, which is a technique

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that involves tracking individual coral colonies over time

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to determine their survival, growth, mortality and health,

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especially following disturbances like bleaching or disease

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is something that we're looking at.

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So why does bleaching impact a particular colony over time?

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If disease is present, how fast is it moving

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or has that disease halted?

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And then what is the resistance

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and resilience of these coral colonies?

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Through expanding our technology and methods

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will only increase our understanding

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of the overall health of the reef.

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Help us track the effects of bleaching, disease,

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and mortality, and then understand the percentage

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of individual corals that are affected over time.

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All right, so getting into today's presentation,

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Stitching it Together with Photogrammetry and Photomosaics,

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Tonight we'll discover

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how Flower Garden Banks National Marine Sanctuary

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is evolving 30 years of tradition

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by integrating cutting edge photogrammetry

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into our reef monitoring program.

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Donavon French will share

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how stitching photos into immersive digital models

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provides a massive leap in understanding

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and protecting the sanctuary's coral reefs.

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So Donavon French is a graduate

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of Texas A&amp;M University at Galveston

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with a bachelor of science and marine biology

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and a minor in diving technology and methods.

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Donavon joined the Flower Garden Banks

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National Marine Sanctuary team as a seasonal diver

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in the summer of 2022.

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After the summer research season wrapped, Donavon stayed on

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as a full-time employee to help analyze data

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and our photography lead.

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Since joining the research team,

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Donavon has updated many of the site's camera systems,

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including photogrammetry methods

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00:16:46.080 --> 00:16:48.600
and analyzed many, many coral reef photos

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to support the sanctuary's reef monitoring efforts.

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In addition to his camera and photogrammetry work,

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Donavon is also a NOAA dive master

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and assists the Sanctuary's unit dive supervisor

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00:17:00.600 --> 00:17:03.090
to keep the dive program running smoothly.

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00:17:03.090 --> 00:17:04.920
Donavon has worked as a dive master

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and diving instructor in the Galveston community.

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So Donavon, thank you for sharing your work

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00:17:10.740 --> 00:17:12.843
and experiences with us tonight.

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Are you ready to take over?

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00:17:16.620 --> 00:17:18.540
<v ->Yeah, let's get this started.</v>

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00:17:18.540 --> 00:17:19.410
<v ->Perfect.</v>

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00:17:19.410 --> 00:17:21.100
Let me pull up

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00:17:22.080 --> 00:17:23.943
and change presenters.

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00:17:25.500 --> 00:17:29.490
All right, you should have control of things now.

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00:17:29.490 --> 00:17:30.363
<v ->All right.</v>

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00:17:32.807 --> 00:17:34.557
Let me share my screen. Here we go.

321
00:17:36.120 --> 00:17:36.953
All right.

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00:17:36.953 --> 00:17:37.860
<v ->Looks good to me.</v>
<v ->That coming through?</v>

323
00:17:37.860 --> 00:17:39.480
Awesome.

324
00:17:39.480 --> 00:17:41.160
Well, hello everybody.

325
00:17:41.160 --> 00:17:43.200
Thank you for the introduction Taylor,

326
00:17:43.200 --> 00:17:45.390
and for all the knowledge you were able

327
00:17:45.390 --> 00:17:47.250
to share on our long-term monitoring.

328
00:17:47.250 --> 00:17:48.780
Hopefully I could take it from here.

329
00:17:48.780 --> 00:17:51.270
And as mentioned, I'm Donavon French,

330
00:17:51.270 --> 00:17:52.770
this is Stitching It Together:

331
00:17:52.770 --> 00:17:56.733
Photogrammetry and Photosmosaics, Seaside Chats, 2026.

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00:17:58.260 --> 00:17:59.093
All right.

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00:18:00.090 --> 00:18:03.426
So to start us off, what is photogrammetry?

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00:18:03.426 --> 00:18:06.450
Well, photogrammetry is actually a pretty broad thing

335
00:18:06.450 --> 00:18:08.790
to talk about, but it could boil down

336
00:18:08.790 --> 00:18:12.900
to a method in technology that is used to create

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00:18:12.900 --> 00:18:16.350
two or three dimensional models out of a series

338
00:18:16.350 --> 00:18:19.260
of overlapping 2-D data, such as images

339
00:18:19.260 --> 00:18:22.680
or some other kind of data, which could be, you know,

340
00:18:22.680 --> 00:18:26.460
radar, sonar, lidar, others.

341
00:18:26.460 --> 00:18:29.460
One that you could think of is Google Maps and Google Earth.

342
00:18:29.460 --> 00:18:33.630
So it's a series of satellite images that have been used

343
00:18:33.630 --> 00:18:35.280
to create one large map

344
00:18:35.280 --> 00:18:38.460
that we can interpret on how to get places.

345
00:18:38.460 --> 00:18:40.110
So in this image here,

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00:18:40.110 --> 00:18:44.310
here I am under the blue dot at NOAA Flower Garden's Office.

347
00:18:44.310 --> 00:18:47.250
And if you have look at this image, you know,

348
00:18:47.250 --> 00:18:50.310
it just looks like a nice normal image.

349
00:18:50.310 --> 00:18:54.570
However, if we zoom out to a nice chunk of Galveston,

350
00:18:54.570 --> 00:18:56.523
you might notice a couple things.

351
00:18:57.810 --> 00:18:59.700
There's a couple blocky textures,

352
00:18:59.700 --> 00:19:03.000
this is from where they have merged images

353
00:19:03.000 --> 00:19:05.220
and there's also some lines of

354
00:19:05.220 --> 00:19:08.583
where they have combined overlapping scans.

355
00:19:10.830 --> 00:19:14.370
And then as mentioned, we could also use photogrammetry

356
00:19:14.370 --> 00:19:16.950
to create three dimensional models of structures

357
00:19:16.950 --> 00:19:18.810
or places of interests,

358
00:19:18.810 --> 00:19:22.500
which in particular makes it popular in archeology.

359
00:19:22.500 --> 00:19:25.050
So you could create a model of a dig site

360
00:19:25.050 --> 00:19:29.280
or in some cases underwater objects such as shipwrecks.

361
00:19:29.280 --> 00:19:32.073
Objects that will degrade over time.

362
00:19:33.240 --> 00:19:36.690
This is useful because we can create a snapshot of a place

363
00:19:36.690 --> 00:19:41.130
and time that we can use to measure objects in both scale

364
00:19:41.130 --> 00:19:43.140
as well as their change over time

365
00:19:43.140 --> 00:19:47.940
if we compare models taken at different points.

366
00:19:47.940 --> 00:19:50.760
Because this is frequently used

367
00:19:50.760 --> 00:19:55.603
in the Great Lakes sanctuaries such as Thunder Bay.

368
00:19:56.850 --> 00:19:58.140
And this is where I'm actually gonna

369
00:19:58.140 --> 00:19:59.730
kind of start our story today.

370
00:19:59.730 --> 00:20:04.620
So I was trained in June of 2024 up at Thunder Bay.

371
00:20:04.620 --> 00:20:07.290
I traveled up to Alpena, Michigan on the shores

372
00:20:07.290 --> 00:20:10.020
of Lake Huron for a photogrammetry workshop

373
00:20:10.020 --> 00:20:11.460
that was with the NOAA Dive Center

374
00:20:11.460 --> 00:20:14.190
as well as the Thunder Bay research team.

375
00:20:14.190 --> 00:20:16.260
Thunder Bay National Marine Sanctuary is home

376
00:20:16.260 --> 00:20:18.630
to nearly a hundred historic shipwrecks

377
00:20:18.630 --> 00:20:21.113
and is a hotspot for American, Canadian

378
00:20:21.113 --> 00:20:24.330
and even global shipping history.

379
00:20:24.330 --> 00:20:28.140
And in this workshop we went in less than two weeks

380
00:20:28.140 --> 00:20:31.050
from shooting practice drive models on land

381
00:20:31.050 --> 00:20:32.950
to smaller models in under diving tank

382
00:20:33.900 --> 00:20:36.840
to shooting historic shipwrecks out in the field.

383
00:20:36.840 --> 00:20:39.690
This was also a great chance for me to expand myself

384
00:20:39.690 --> 00:20:42.270
as a diver as I learned how to use a drysuit

385
00:20:42.270 --> 00:20:43.470
because as you can imagine,

386
00:20:43.470 --> 00:20:44.910
the waters up there are quite cold,

387
00:20:44.910 --> 00:20:46.983
anywhere from 60 to 50 degrees.

388
00:20:48.840 --> 00:20:52.770
So to start off, we kind of got familiar

389
00:20:52.770 --> 00:20:55.470
with our cameras using their tank.

390
00:20:55.470 --> 00:20:58.680
It's a retired water tank that they just now use

391
00:20:58.680 --> 00:21:02.760
for diving, outreach events, using ROVs,

392
00:21:02.760 --> 00:21:04.290
anything such as this.

393
00:21:04.290 --> 00:21:08.490
And these two photos on the left is Stephanie Gandulla.

394
00:21:08.490 --> 00:21:11.820
She I believe is their research protection specialist

395
00:21:11.820 --> 00:21:13.140
up at Thunder Bay.

396
00:21:13.140 --> 00:21:15.150
And then on the right is Phil Hartmeyer

397
00:21:15.150 --> 00:21:17.940
who is now part of NOAA Ocean Exploration.

398
00:21:17.940 --> 00:21:20.220
And they're both holding two of the cameras

399
00:21:20.220 --> 00:21:22.890
that we were using during this class.

400
00:21:22.890 --> 00:21:26.160
On those arms you see the white little cylinders,

401
00:21:26.160 --> 00:21:28.110
those are the strobes that allow us

402
00:21:28.110 --> 00:21:30.930
to get a little extra light while we're underwater.

403
00:21:30.930 --> 00:21:34.560
And a big lens in the middle is actually a housing

404
00:21:34.560 --> 00:21:37.590
that will keep the camera safe underwater

405
00:21:37.590 --> 00:21:40.530
as it's just kind of a normal DSLR camera

406
00:21:40.530 --> 00:21:42.960
that you'll use here on land.

407
00:21:42.960 --> 00:21:47.910
So to start off, for my first water bottle,

408
00:21:47.910 --> 00:21:50.280
we just used a ladder that we tossed it into the tank

409
00:21:50.280 --> 00:21:53.940
and I like to think it was so good, I got two ladders.

410
00:21:53.940 --> 00:21:56.490
However, my instructor, he was less impressed.

411
00:21:56.490 --> 00:21:59.130
We figured out this was an error in my processing

412
00:21:59.130 --> 00:22:00.603
so we tried again.

413
00:22:01.770 --> 00:22:03.393
And you know what they say?

414
00:22:04.560 --> 00:22:06.090
If you don't succeed, try again.

415
00:22:06.090 --> 00:22:08.933
And you may just end up with what looks like a real ladder.

416
00:22:10.350 --> 00:22:13.380
But this is where I want to get into showing you

417
00:22:13.380 --> 00:22:16.290
some of the shipwrecks that we were able to shoot.

418
00:22:16.290 --> 00:22:19.233
So I'm gonna go ahead and share a video.

419
00:22:29.610 --> 00:22:30.780
All right.

420
00:22:30.780 --> 00:22:32.220
Now should be showing a video.

421
00:22:32.220 --> 00:22:36.120
This is of the shallow NEW ORLEANS.

422
00:22:36.120 --> 00:22:38.140
It's one of the earliest shipwrecks

423
00:22:39.090 --> 00:22:42.150
in the Thunder Bay National Marine Sanctuary.

424
00:22:42.150 --> 00:22:45.240
And let's see, is it going through?

425
00:22:45.240 --> 00:22:48.150
Yes, my apologies.

426
00:22:48.150 --> 00:22:49.023
First video.

427
00:22:49.920 --> 00:22:51.030
Yeah.

428
00:22:51.030 --> 00:22:53.460
It's one of the earliest shipwrecks in Thunder Bay

429
00:22:53.460 --> 00:22:55.260
sinking in 1849.

430
00:22:55.260 --> 00:22:57.690
It was a wooden side wheel steamboat

431
00:22:57.690 --> 00:23:00.240
that was about 180 feet long,

432
00:23:00.240 --> 00:23:03.690
which now sits in only about 15 feet of water.

433
00:23:03.690 --> 00:23:06.450
Because of that it's a popular stop for kayakers,

434
00:23:06.450 --> 00:23:08.600
divers, divers and even glass bottom boats.

435
00:23:13.470 --> 00:23:16.862
We'll move on to next one.

436
00:23:16.862 --> 00:23:21.227
And we have here the E.B. ALLEN.

437
00:23:22.530 --> 00:23:23.363
Oh.

438
00:23:29.100 --> 00:23:32.070
So this is the E.B. ALLEN, which I shot with a member

439
00:23:32.070 --> 00:23:33.330
of the Thunder Bay research team

440
00:23:33.330 --> 00:23:35.250
that was learning alongside me.

441
00:23:35.250 --> 00:23:37.710
The E.B. ALLEN a wooden two mass schooner,

442
00:23:37.710 --> 00:23:40.170
which collided heavily

443
00:23:40.170 --> 00:23:42.570
or collided in a heavy fog

444
00:23:42.570 --> 00:23:45.420
into another ship called NEWSBOY.

445
00:23:45.420 --> 00:23:49.500
Newsboy tore a hole in the portside hull

446
00:23:49.500 --> 00:23:53.370
of the E.B. ALLEN, but thankfully the NEWSBOY stayed intact

447
00:23:53.370 --> 00:23:55.170
and was actually able to rescue everybody

448
00:23:55.170 --> 00:23:56.970
that was aboard at the E.B. ALLEN.

449
00:23:56.970 --> 00:23:59.280
And now sits in about a hundred feet of water

450
00:23:59.280 --> 00:24:01.563
with its hull mostly intact.

451
00:24:07.200 --> 00:24:10.470
And parts of its deck are still there.

452
00:24:10.470 --> 00:24:12.300
This was one of my coldest dives while I was there.

453
00:24:12.300 --> 00:24:14.700
It was only about above 50 degrees.

454
00:24:14.700 --> 00:24:17.580
And as you notice as we're coming over to the port side,

455
00:24:17.580 --> 00:24:19.890
it's kind of got this reddish orange markings.

456
00:24:19.890 --> 00:24:22.650
That's actually kind of more what the shipwreck color is,

457
00:24:22.650 --> 00:24:24.720
the greenish bluish hues.

458
00:24:24.720 --> 00:24:26.850
It's just because of the depth of the water.

459
00:24:26.850 --> 00:24:30.840
And this is kind of a highlight that came of the strobes

460
00:24:30.840 --> 00:24:34.320
that we were using while photographing this wreck.

461
00:24:34.320 --> 00:24:36.060
So we kind of got a little too close there

462
00:24:36.060 --> 00:24:38.400
so the color became uneven.

463
00:24:38.400 --> 00:24:41.010
And this was just kind of a learning moment for us

464
00:24:41.010 --> 00:24:44.523
as we were, you know, just learning to do photogrammetry.

465
00:24:45.600 --> 00:24:48.783
We'll move to our last and final wreck.

466
00:24:50.580 --> 00:24:51.413
All right.

467
00:24:59.490 --> 00:25:00.323
All right.

468
00:25:00.323 --> 00:25:02.523
And here this is my last one to share today.

469
00:25:03.510 --> 00:25:05.850
This was one of the last models I actually shot

470
00:25:05.850 --> 00:25:06.900
while I was up in Thunder Bay

471
00:25:06.900 --> 00:25:10.800
and it's by far one of my most successful ones.

472
00:25:10.800 --> 00:25:12.420
I also shot it with the same member

473
00:25:12.420 --> 00:25:15.270
of the research team as the E.B. ALLEN.

474
00:25:15.270 --> 00:25:16.800
So this is the D.M. WILSON.

475
00:25:16.800 --> 00:25:18.570
It was a wooden bulk freighter

476
00:25:18.570 --> 00:25:21.180
that primarily shipped coal.

477
00:25:21.180 --> 00:25:25.230
It sunk when it sprang a leak on its way to Milwaukee.

478
00:25:25.230 --> 00:25:26.880
The crew was able to be rescued

479
00:25:26.880 --> 00:25:29.400
and the WILSON was able to be taken into tow.

480
00:25:29.400 --> 00:25:33.150
However, 10 days later the WILSON broke up at a gale of wind

481
00:25:33.150 --> 00:25:37.980
and now is where it rests today in the sanctuary.

482
00:25:37.980 --> 00:25:40.680
So as I mentioned on the E.B. ALLEN,

483
00:25:40.680 --> 00:25:43.680
you will notice this one's much more even in color.

484
00:25:43.680 --> 00:25:46.110
It doesn't get some of those strange artifacts

485
00:25:46.110 --> 00:25:47.760
from using the lighting.

486
00:25:47.760 --> 00:25:50.462
So that was just something where, you know,

487
00:25:50.462 --> 00:25:52.350
we're learning over time

488
00:25:52.350 --> 00:25:53.880
and that's part of why I say

489
00:25:53.880 --> 00:25:56.913
I think this is one of my best models I shot on that trip.

490
00:25:58.800 --> 00:26:00.670
We'll go ahead and move back

491
00:26:05.100 --> 00:26:06.450
to my screen.

492
00:26:06.450 --> 00:26:07.533
Yep, here we go.

493
00:26:08.640 --> 00:26:09.810
All right.

494
00:26:09.810 --> 00:26:11.220
So after that it was kind of

495
00:26:11.220 --> 00:26:13.473
Goodbye Alpena, Hello Flower Gardens!

496
00:26:14.520 --> 00:26:17.760
Right after the trip it was right into the field season

497
00:26:17.760 --> 00:26:20.850
for the East and West Bank Long-term Monitoring.

498
00:26:20.850 --> 00:26:22.920
However, I thought this was a great chance

499
00:26:22.920 --> 00:26:24.510
to test out some of my new skills

500
00:26:24.510 --> 00:26:25.740
in the Flower Gardens coral.

501
00:26:25.740 --> 00:26:27.003
So let me show you some of the models

502
00:26:27.003 --> 00:26:28.383
that I was able to make.

503
00:26:30.150 --> 00:26:32.670
We will do our first video here.

504
00:26:32.670 --> 00:26:34.113
one moment please.

505
00:26:40.410 --> 00:26:41.732
Let's see, that is the wrong one.

506
00:26:41.732 --> 00:26:42.732
It's my bad.

507
00:26:44.673 --> 00:26:45.506
Here we go.

508
00:26:50.040 --> 00:26:50.873
All right.

509
00:26:50.873 --> 00:26:52.890
So this is just a small scale model

510
00:26:52.890 --> 00:26:55.290
that I made out of a brain coral

511
00:26:55.290 --> 00:26:57.480
from the East Flower Garden Bank study site.

512
00:26:57.480 --> 00:26:58.830
The main colony there in the center

513
00:26:58.830 --> 00:27:00.780
is only about a meter across

514
00:27:00.780 --> 00:27:02.250
and it's surrounded by other species

515
00:27:02.250 --> 00:27:03.933
of corals and sponge colonies.

516
00:27:07.620 --> 00:27:09.720
You'll notice I'd like the shipwreck models

517
00:27:09.720 --> 00:27:11.400
with a whole in the model.

518
00:27:11.400 --> 00:27:14.130
This is due to the complexity of the reef

519
00:27:14.130 --> 00:27:16.050
as it's kind of hard for the computer

520
00:27:16.050 --> 00:27:17.490
to model all those crevices.

521
00:27:17.490 --> 00:27:21.180
And it's even harder for me as a photographer to shoot them.

522
00:27:21.180 --> 00:27:24.240
because of this shooting 3-D models of the reef is much more

523
00:27:24.240 --> 00:27:27.480
of a time investment than it is for the shipwrecks.

524
00:27:27.480 --> 00:27:28.500
And it's also, you know,

525
00:27:28.500 --> 00:27:30.900
something we kind of kept in mind going forward.

526
00:27:34.860 --> 00:27:37.083
Go ahead and move to the next one.

527
00:27:51.210 --> 00:27:52.050
All right.

528
00:27:52.050 --> 00:27:54.380
Next one is of a much larger...

529
00:27:55.327 --> 00:27:56.160
Are we good?

530
00:27:59.880 --> 00:28:01.773
<v Taylor>You're good now. Sorry.</v>

531
00:28:01.773 --> 00:28:03.120
<v ->Okay, perfect.</v>

532
00:28:03.120 --> 00:28:05.610
This next one is of a much larger model

533
00:28:05.610 --> 00:28:07.320
or it's a much larger model

534
00:28:07.320 --> 00:28:09.330
of what I've been calling a coral island.

535
00:28:09.330 --> 00:28:11.640
It's about 10 meters in length

536
00:28:11.640 --> 00:28:15.180
and it's just a patch of reef that's in the middle

537
00:28:15.180 --> 00:28:19.280
of a larger sand batch at the west study site.

538
00:28:40.860 --> 00:28:41.820
Additional lighting,

539
00:28:41.820 --> 00:28:45.240
however, it didn't quite work out how I hoped.

540
00:28:45.240 --> 00:28:46.890
The white light from the strobes was able

541
00:28:46.890 --> 00:28:48.870
to bring back some of the orange and reds

542
00:28:48.870 --> 00:28:51.990
of the sponge colonies and others.

543
00:28:51.990 --> 00:28:55.653
However, you'll notice it still kind of favors the blue.

544
00:29:00.570 --> 00:29:03.030
This is because the cameras that we're using

545
00:29:03.030 --> 00:29:04.498
for this underwater photometry

546
00:29:04.498 --> 00:29:09.498
have a very wide field of view.

547
00:29:09.570 --> 00:29:10.920
Think like a (indistinct)

548
00:29:10.920 --> 00:29:12.300
kind of action camera.

549
00:29:12.300 --> 00:29:15.690
The wide lens allows me to collect a large area.

550
00:29:15.690 --> 00:29:17.430
However, that doesn't always mean

551
00:29:17.430 --> 00:29:20.550
that area is gonna be evenly illuminated by the strobe.

552
00:29:20.550 --> 00:29:23.970
So what we kind learned as a takeaway was

553
00:29:23.970 --> 00:29:27.870
that strobes kinda add an unnecessary complexity

554
00:29:27.870 --> 00:29:30.873
that the software is not necessarily gonna handle well.

555
00:29:35.670 --> 00:29:36.543
We'll go back.

556
00:29:38.190 --> 00:29:39.023
There we go.

557
00:29:46.110 --> 00:29:46.943
Okay.

558
00:29:46.943 --> 00:29:49.410
So after the field season, we took to figuring out

559
00:29:49.410 --> 00:29:51.600
okay, what would implementing photogrammetry look like

560
00:29:51.600 --> 00:29:52.770
in our long-term monitoring

561
00:29:52.770 --> 00:29:54.870
and would it even be kind of worth our time?

562
00:29:54.870 --> 00:29:58.050
So we kind of broke it down by the strengths and weaknesses.

563
00:29:58.050 --> 00:29:59.160
So kind of starting off

564
00:29:59.160 --> 00:30:00.930
with some of the strengths we noticed.

565
00:30:00.930 --> 00:30:03.230
It's big kind of draw is that we are able size

566
00:30:04.110 --> 00:30:06.450
it's scale and size, coral colonies at a level

567
00:30:06.450 --> 00:30:09.900
that we are not able to do or can't do

568
00:30:09.900 --> 00:30:12.690
with our other photography methods.

569
00:30:12.690 --> 00:30:15.330
The photogrammetry methods are pretty easy to learn

570
00:30:15.330 --> 00:30:18.030
so it should be pretty easy for the rest of my team

571
00:30:18.030 --> 00:30:20.340
to pick up pretty quickly.

572
00:30:20.340 --> 00:30:22.110
And we already had some partners

573
00:30:22.110 --> 00:30:25.050
that were doing photogrammetry work already

574
00:30:25.050 --> 00:30:26.350
within the Flower Gardens.

575
00:30:28.200 --> 00:30:31.590
So weaknesses though, it's got lower resolution of anything

576
00:30:31.590 --> 00:30:32.940
that's kind of not a coral.

577
00:30:32.940 --> 00:30:37.650
So the sponges and algaes are kind of harder to identify.

578
00:30:37.650 --> 00:30:41.130
As I mentioned, we found that it's a large time investment

579
00:30:41.130 --> 00:30:44.220
for complete 3-D models of the reef

580
00:30:44.220 --> 00:30:47.100
as well as if we were gonna go with strobes,

581
00:30:47.100 --> 00:30:50.553
it would add some unneeded complexity with little benefit.

582
00:30:51.420 --> 00:30:56.420
So as a solution we would focus just on 2-D mosaics,

583
00:30:57.000 --> 00:31:02.000
focus just on the corals and maybe try to (indistinct)

584
00:31:03.150 --> 00:31:05.070
for more data compatibility.

585
00:31:05.070 --> 00:31:09.540
So as a program, we're always trying to look on ways

586
00:31:09.540 --> 00:31:11.220
to fill our gaps in our monitoring,

587
00:31:11.220 --> 00:31:14.130
and one that we've been wanting to improve is our assessment

588
00:31:14.130 --> 00:31:15.840
of disease on the corals.

589
00:31:15.840 --> 00:31:17.973
And the methods that we have now,

590
00:31:20.610 --> 00:31:23.790
while they can relay some of the information on disease

591
00:31:23.790 --> 00:31:27.360
that's not their primary or even secondary use case,

592
00:31:27.360 --> 00:31:30.090
but photogrammetry would be probably a great way

593
00:31:30.090 --> 00:31:31.200
to fill this gap.

594
00:31:31.200 --> 00:31:35.640
So we decided as a goal, let's use the ability

595
00:31:35.640 --> 00:31:40.050
to size corals within the photogrammetry photomosaics

596
00:31:40.050 --> 00:31:42.210
to accurately assess the coverage

597
00:31:42.210 --> 00:31:44.970
and impact of disease on corals

598
00:31:44.970 --> 00:31:46.563
at the east and west bank,

599
00:31:49.230 --> 00:31:52.470
sorry at the East and West Flower Garden Banks to a level

600
00:31:52.470 --> 00:31:54.620
that we haven't previously been able to do.

601
00:31:55.650 --> 00:31:58.263
So what does that look like for us?

602
00:31:59.940 --> 00:32:03.060
In our case, we are going to take a series

603
00:32:03.060 --> 00:32:06.750
of top-down images to create 2-D models of areas

604
00:32:06.750 --> 00:32:09.403
of the coral reef, creating what's sometimes called

605
00:32:09.403 --> 00:32:13.110
a photomosaic or just a mosaic for short.

606
00:32:13.110 --> 00:32:16.020
We do this by first creating a 3-D model

607
00:32:16.020 --> 00:32:18.450
and then squishing it down into a 2-D image

608
00:32:18.450 --> 00:32:21.130
that we're able to size the corals

609
00:32:22.050 --> 00:32:24.840
and the other subjects that are within it.

610
00:32:24.840 --> 00:32:27.360
So here's that model from earlier.

611
00:32:27.360 --> 00:32:29.850
And on the left here, just a nice image of,

612
00:32:29.850 --> 00:32:31.770
but however, if we were to squash it down

613
00:32:31.770 --> 00:32:34.840
from a top point of view, you get an output

614
00:32:36.291 --> 00:32:38.133
of photomosaic here on the right.

615
00:32:40.590 --> 00:32:43.293
And that leads me to my next video.

616
00:32:48.450 --> 00:32:49.350
Which is...

617
00:33:01.326 --> 00:33:03.180
All right, so it leads me to this one here.

618
00:33:03.180 --> 00:33:05.670
So in a field season of 2025,

619
00:33:05.670 --> 00:33:10.200
we started our random photomosaics on our reef wide scale.

620
00:33:10.200 --> 00:33:14.700
These models are of random points across the coral reef cap

621
00:33:14.700 --> 00:33:19.700
at predetermined but random directions to avoid any bias.

622
00:33:20.610 --> 00:33:23.880
Each model is of a 15 by 2 meter area,

623
00:33:23.880 --> 00:33:25.890
which was marked out by scale bars

624
00:33:25.890 --> 00:33:27.633
and a 15 meter measuring tape.

625
00:33:29.730 --> 00:33:33.180
The area captured is a little bit larger than

626
00:33:33.180 --> 00:33:36.360
that study area so that we can make sure

627
00:33:36.360 --> 00:33:39.810
that we properly capture the area we want

628
00:33:39.810 --> 00:33:43.203
and we can always trim it down in post-processing.

629
00:33:44.100 --> 00:33:47.550
The methods that we're using are of an adapted version

630
00:33:47.550 --> 00:33:48.990
of our partners methods

631
00:33:48.990 --> 00:33:51.780
over at the National Coral Reef Monitoring Program.

632
00:33:51.780 --> 00:33:54.690
So we benefit from not having to reinvent the wheel

633
00:33:54.690 --> 00:33:56.130
when it comes to developing

634
00:33:56.130 --> 00:33:58.560
what we wanted to do and how we collect our data.

635
00:33:58.560 --> 00:34:02.103
And we can also now share our data between our programs.

636
00:34:03.210 --> 00:34:08.010
This model here that you're looking at is from East Bank

637
00:34:08.010 --> 00:34:10.590
and it shows the 3-D model that was used

638
00:34:10.590 --> 00:34:13.470
before we created the photomosaic,

639
00:34:13.470 --> 00:34:17.100
and it was shot by Aaron Bouwkamp over at Moody Gardens

640
00:34:17.100 --> 00:34:18.960
who was part of the crews

641
00:34:18.960 --> 00:34:21.180
that collected all these photomosaics

642
00:34:21.180 --> 00:34:23.163
as part of our continued partnership.

643
00:34:24.870 --> 00:34:27.453
All right. I'll hop back to my slides.

644
00:34:34.650 --> 00:34:35.800
All right. There we go.

645
00:34:37.140 --> 00:34:40.770
All right. So overall I'd say the cruise was a success.

646
00:34:40.770 --> 00:34:43.860
However, just like any first run, it did have its flaws.

647
00:34:43.860 --> 00:34:45.600
One of our cameras refused to work

648
00:34:45.600 --> 00:34:48.630
after it shot its first model.

649
00:34:48.630 --> 00:34:49.920
The camera wasn't damaged,

650
00:34:49.920 --> 00:34:52.680
the underwater housing would compress oddly

651
00:34:52.680 --> 00:34:54.480
so some of the buttons couldn't be used

652
00:34:54.480 --> 00:34:57.210
and we ended up only having one camera for the trip,

653
00:34:57.210 --> 00:34:58.740
however, we made the best of it.

654
00:34:58.740 --> 00:35:01.713
So all in all we collected 22 mosaics in total.

655
00:35:03.150 --> 00:35:06.330
This here is a photomosaic that was produced

656
00:35:06.330 --> 00:35:08.280
from the trip at West Bank.

657
00:35:08.280 --> 00:35:11.310
You can see the tape measure at the top.

658
00:35:11.310 --> 00:35:14.730
This lets the divers note the length of the area

659
00:35:14.730 --> 00:35:16.920
that they need to be photographing.

660
00:35:16.920 --> 00:35:20.460
And then in the top left you can see a clipboard.

661
00:35:20.460 --> 00:35:23.070
This clipboard is used underwater by the diver

662
00:35:23.070 --> 00:35:25.560
to record some information about the site,

663
00:35:25.560 --> 00:35:28.680
such as depth of certain points, who's taking the photos,

664
00:35:28.680 --> 00:35:32.070
what site it is, what compass headings being used,

665
00:35:32.070 --> 00:35:35.340
and other kind of useful data like that.

666
00:35:35.340 --> 00:35:39.480
Then in the bottom left, that little rectangle there,

667
00:35:39.480 --> 00:35:41.671
that's one of our scale bars.

668
00:35:41.671 --> 00:35:45.840
The software can actually use these scale bars

669
00:35:45.840 --> 00:35:50.250
to help build the 3D model in the photomosaic

670
00:35:50.250 --> 00:35:54.534
as references as it's stitching everything together.

671
00:35:54.534 --> 00:35:58.380
You'll see the circles there, they're kind of odd shapes.

672
00:35:58.380 --> 00:36:02.250
That's because the software has a internal

673
00:36:02.250 --> 00:36:06.150
kind of protocol to self-analyze the image

674
00:36:06.150 --> 00:36:09.480
and find those so I don't have to put them in myself.

675
00:36:09.480 --> 00:36:11.030
It's a little time saver there.

676
00:36:13.560 --> 00:36:16.680
So once we've built the models

677
00:36:16.680 --> 00:36:19.560
and we've made the photomosaic, what's next?

678
00:36:19.560 --> 00:36:21.150
Well, to analyze each mosaic,

679
00:36:21.150 --> 00:36:23.220
we're using the software called TagLab.

680
00:36:23.220 --> 00:36:28.220
It's an automation tool that allows us to segment the mosaic

681
00:36:29.130 --> 00:36:30.993
into different coral colonies.

682
00:36:31.950 --> 00:36:35.940
Seen here each colony has been segmented out, colored,

683
00:36:35.940 --> 00:36:39.003
whereas each color is a different species of coral.

684
00:36:40.110 --> 00:36:42.060
Once we've labeled the corals,

685
00:36:42.060 --> 00:36:44.250
the software will spit out a spreadsheet

686
00:36:44.250 --> 00:36:47.670
with the total coverage areas of each individual colony.

687
00:36:47.670 --> 00:36:49.470
And we do this twice actually.

688
00:36:49.470 --> 00:36:52.440
The first time we do it with all of the corals

689
00:36:52.440 --> 00:36:54.630
and we capture the entire coral.

690
00:36:54.630 --> 00:36:56.430
And then the second time we segment

691
00:36:56.430 --> 00:36:59.040
only the disease areas of the coral.

692
00:36:59.040 --> 00:37:02.700
We do this so that we can compare the data

693
00:37:02.700 --> 00:37:04.830
and find out what's the percentages

694
00:37:04.830 --> 00:37:06.903
of the coral coverage that is diseased.

695
00:37:08.370 --> 00:37:10.650
And this year this is kind of the main benefit

696
00:37:10.650 --> 00:37:12.720
of using our photomosaics.

697
00:37:12.720 --> 00:37:14.580
Our other photogrammetry methods

698
00:37:14.580 --> 00:37:16.980
like the random transect and repetitive quadrats,

699
00:37:16.980 --> 00:37:20.860
they don't have a way to size the corals or disease

700
00:37:22.980 --> 00:37:26.370
and rely on other ways to derive coverages.

701
00:37:26.370 --> 00:37:29.460
Whereas the photomosiacs can give us accurate numbers

702
00:37:29.460 --> 00:37:32.583
every time that we can use within our monitoring.

703
00:37:36.270 --> 00:37:38.790
From there it's a lot of spreadsheet math

704
00:37:38.790 --> 00:37:39.960
to figure out the rest.

705
00:37:39.960 --> 00:37:41.970
I'll spare you most of the boring details,

706
00:37:41.970 --> 00:37:46.050
but we get a couple important values.

707
00:37:46.050 --> 00:37:50.010
As of right now, the 2025 field season data

708
00:37:50.010 --> 00:37:51.360
is still in processing.

709
00:37:51.360 --> 00:37:54.033
So the data in front of you is from early testing.

710
00:37:55.380 --> 00:37:56.530
So don't look too deep.

711
00:37:57.750 --> 00:37:59.460
The total coverage area...

712
00:37:59.460 --> 00:38:00.293
Sorry.

713
00:38:00.293 --> 00:38:02.280
The first of these values that we get

714
00:38:02.280 --> 00:38:05.070
is the total coverage area for each coral species.

715
00:38:05.070 --> 00:38:08.340
This is similar to what our random transects give us.

716
00:38:08.340 --> 00:38:11.793
And if all goes right, this data should be roughly the same.

717
00:38:12.720 --> 00:38:14.700
This data point kind of serves as a test

718
00:38:14.700 --> 00:38:16.860
or insurance that we know that

719
00:38:16.860 --> 00:38:19.380
what we're doing in these photogrammetry methods

720
00:38:19.380 --> 00:38:22.923
is true to life and is in line with our other methods.

721
00:38:26.070 --> 00:38:28.260
The next kind of value is we get ratios

722
00:38:28.260 --> 00:38:32.370
on healthy to disease individual colonies for species.

723
00:38:32.370 --> 00:38:35.640
So think every, for every X colonies

724
00:38:35.640 --> 00:38:37.890
you get Y that are diseased.

725
00:38:37.890 --> 00:38:39.930
This will highlight any species of coral

726
00:38:39.930 --> 00:38:42.510
that may or may not have a lot of mortality,

727
00:38:42.510 --> 00:38:46.650
but it's possibly more susceptible to catching it.

728
00:38:46.650 --> 00:38:49.410
And lastly, we get the percentage

729
00:38:49.410 --> 00:38:53.043
of disease coverage per species overall.

730
00:38:54.030 --> 00:38:56.550
This will highlight which coral species are being

731
00:38:56.550 --> 00:38:59.610
impacted the most and may be suffering the most mortality

732
00:38:59.610 --> 00:39:01.200
of all of the coral species.

733
00:39:01.200 --> 00:39:03.480
And it'll give us a number that we can use

734
00:39:03.480 --> 00:39:06.270
to track over time to assess the intensity

735
00:39:06.270 --> 00:39:07.773
of the disease on the reef.

736
00:39:08.880 --> 00:39:11.610
So for now, we're gonna continue processing

737
00:39:11.610 --> 00:39:14.043
but hopefully we'll have more to share soon.

738
00:39:15.900 --> 00:39:20.730
So now I've kinda shown you what we're doing with it now,

739
00:39:20.730 --> 00:39:21.840
where can we go with this?

740
00:39:21.840 --> 00:39:24.360
How can we expand our photogrammetry methods

741
00:39:24.360 --> 00:39:26.040
in the future for our monitoring?

742
00:39:26.040 --> 00:39:28.170
So there's a couple ways.

743
00:39:28.170 --> 00:39:32.100
For one, we can intensify any of our fate tracking

744
00:39:32.100 --> 00:39:33.483
or fate studies.

745
00:39:35.580 --> 00:39:37.683
Think the repetitive quadrats.

746
00:39:38.610 --> 00:39:40.050
However, if we switch this

747
00:39:40.050 --> 00:39:41.910
over to something like photogrammetry,

748
00:39:41.910 --> 00:39:44.940
it can give us more detailed and numeric information

749
00:39:44.940 --> 00:39:46.800
as to the size of the coral,

750
00:39:46.800 --> 00:39:48.090
which can be used to track

751
00:39:48.090 --> 00:39:50.490
how much the coral has grown over time,

752
00:39:50.490 --> 00:39:52.260
how much has been lost if.

753
00:39:52.260 --> 00:39:53.940
It does have disease, you know,

754
00:39:53.940 --> 00:39:56.100
what is the rate of that disease progressing

755
00:39:56.100 --> 00:39:57.930
or not progressing?

756
00:39:57.930 --> 00:40:00.120
How well has it recovered?

757
00:40:00.120 --> 00:40:03.840
It also could be used to track how much of the colony

758
00:40:03.840 --> 00:40:06.840
and surrounding reef has been lost to bio erosion.

759
00:40:06.840 --> 00:40:09.360
In particular the dissolving

760
00:40:09.360 --> 00:40:12.393
of coral skeleton from ocean acidification.

761
00:40:14.400 --> 00:40:18.210
We can also use it for coral demographic studies.

762
00:40:18.210 --> 00:40:23.160
So this would collect data on the size,

763
00:40:23.160 --> 00:40:25.287
density, abundance and details such as bleaching

764
00:40:25.287 --> 00:40:29.130
and disease of corals tracked in a tracked area

765
00:40:29.130 --> 00:40:31.200
or a random area reef.

766
00:40:31.200 --> 00:40:34.860
Now this isn't too far off from what we're doing now,

767
00:40:34.860 --> 00:40:38.370
however, it's far more expansive and intensive

768
00:40:38.370 --> 00:40:40.140
from a processing side.

769
00:40:40.140 --> 00:40:42.200
So because of that...

770
00:40:43.740 --> 00:40:45.330
Or sorry.

771
00:40:45.330 --> 00:40:48.540
And this is actually how the National Coral Reef Monitoring

772
00:40:48.540 --> 00:40:52.140
program is using photogrammetry.

773
00:40:52.140 --> 00:40:56.133
And because of that and our shared compatibility of data,

774
00:40:58.170 --> 00:41:02.500
the data that we're producing could retroactively be seen

775
00:41:03.960 --> 00:41:05.660
to track the corals in such a way.

776
00:41:06.750 --> 00:41:09.120
The next thing we could do is we could collect larger areas

777
00:41:09.120 --> 00:41:13.140
of data so we could photograph the entire study site

778
00:41:13.140 --> 00:41:15.530
for a year to year model for us to use

779
00:41:15.530 --> 00:41:17.010
as well as our partners.

780
00:41:17.010 --> 00:41:20.010
And this has actually been done previously

781
00:41:20.010 --> 00:41:22.203
by Arc Gleason in 2019.

782
00:41:23.610 --> 00:41:28.140
So in front of you on the right you have all four quadrants

783
00:41:28.140 --> 00:41:30.180
of the study site at east

784
00:41:30.180 --> 00:41:34.200
and then on the left is the southwest quadrant

785
00:41:34.200 --> 00:41:37.020
where each one of those numbers is actually

786
00:41:37.020 --> 00:41:40.323
one of our repetitive photo stations.

787
00:41:41.400 --> 00:41:44.850
So having this larger data set would not only benefit us,

788
00:41:44.850 --> 00:41:48.453
but also could be useful data to pass off to partners.

789
00:41:50.100 --> 00:41:54.210
And lastly, to move away from our scientific methods,

790
00:41:54.210 --> 00:41:56.640
we could create more outreach material,

791
00:41:56.640 --> 00:41:58.980
things like maps of areas of the reef

792
00:41:58.980 --> 00:42:02.010
for recreational divers to reference in dive planning.

793
00:42:02.010 --> 00:42:06.677
Or even models of areas for 3-D virtual reality

794
00:42:07.530 --> 00:42:09.330
so that anybody could dive the reef.

795
00:42:11.160 --> 00:42:13.980
But yeah, that's pretty much all I have for you guys today.

796
00:42:13.980 --> 00:42:15.840
I wanna thank you guys for coming.

797
00:42:15.840 --> 00:42:18.180
I hope you guys enjoyed the show.

798
00:42:18.180 --> 00:42:21.570
I wanna give a special thanks out to Thunder Bay

799
00:42:21.570 --> 00:42:24.090
National Marine Sanctuary and the NOAA Dive Center

800
00:42:24.090 --> 00:42:26.160
for putting on that awesome workshop

801
00:42:26.160 --> 00:42:29.700
and allowing me to bring this knowledge down to my team.

802
00:42:29.700 --> 00:42:31.260
And then I also want to thank my team

803
00:42:31.260 --> 00:42:34.080
and our frequent partners for helping me implement this

804
00:42:34.080 --> 00:42:36.780
and taking it where it is now.

805
00:42:36.780 --> 00:42:39.990
And then of course I wanna thank all of you guys.

806
00:42:39.990 --> 00:42:43.980
This is your sanctuary and it's great to see you all enjoy

807
00:42:43.980 --> 00:42:47.700
and engage with it and it is the reason why we're here

808
00:42:47.700 --> 00:42:50.280
and able to share this with y'all.

809
00:42:50.280 --> 00:42:52.367
So yeah, back to you Taylor.

810
00:42:53.955 --> 00:42:54.788
<v ->Awesome.</v>

811
00:42:54.788 --> 00:42:55.930
Thank you so much Donavon

812
00:42:56.790 --> 00:42:59.370
for sharing your knowledge and your journey

813
00:42:59.370 --> 00:43:01.173
and how you've gotten to this point.

814
00:43:02.400 --> 00:43:05.610
We do have some questions coming in the chat.

815
00:43:05.610 --> 00:43:09.600
So right now is a great time that if you have a question

816
00:43:09.600 --> 00:43:11.250
that you've been wanting to ask,

817
00:43:11.250 --> 00:43:13.277
leave that in the question box

818
00:43:13.277 --> 00:43:16.680
and we'll get to as many questions as we can.

819
00:43:16.680 --> 00:43:19.920
And for those questions that we can't get to,

820
00:43:19.920 --> 00:43:23.850
we do send out an email later on answering those questions.

821
00:43:23.850 --> 00:43:27.300
So Donavon, if you're up for it, I got some questions.

822
00:43:27.300 --> 00:43:28.133
<v ->Let's do it.</v>

823
00:43:29.800 --> 00:43:32.790
<v ->Okay, so first question is</v>

824
00:43:32.790 --> 00:43:35.790
from a viewer who wants to know

825
00:43:35.790 --> 00:43:40.140
on your E.B. ALLEN video there were some white patches.

826
00:43:40.140 --> 00:43:42.180
Could you kind of go back to that video

827
00:43:42.180 --> 00:43:44.340
and explain it to everyone?

828
00:43:44.340 --> 00:43:46.220
<v ->Yeah, let's open it back up.</v>

829
00:43:51.556 --> 00:43:53.223
All right. E.B. ALLEN.

830
00:44:00.690 --> 00:44:01.523
All right, there we go.

831
00:44:01.523 --> 00:44:02.820
I got the video going for you guys.

832
00:44:02.820 --> 00:44:05.850
So yeah, those dark, those whites...

833
00:44:05.850 --> 00:44:06.870
Sorry, lemme back up.

834
00:44:06.870 --> 00:44:10.230
Those white patches are actually areas

835
00:44:10.230 --> 00:44:14.610
where the cameras weren't really able to collect data,

836
00:44:14.610 --> 00:44:15.443
I guess.

837
00:44:15.443 --> 00:44:18.930
Those would be like kind of black parts of the images.

838
00:44:18.930 --> 00:44:20.073
They would be shadows.

839
00:44:20.910 --> 00:44:22.230
As I mentioned this,

840
00:44:22.230 --> 00:44:24.300
this reef is down at about a hundred feet

841
00:44:24.300 --> 00:44:26.820
so it gets pretty dark down there

842
00:44:26.820 --> 00:44:29.130
and that ends up for, you know,

843
00:44:29.130 --> 00:44:31.980
not creating a perfect model.

844
00:44:31.980 --> 00:44:34.950
If we wanted to rectify this,

845
00:44:34.950 --> 00:44:37.860
we would probably do a lot more dives on this site.

846
00:44:37.860 --> 00:44:41.073
Unfortunately I think we were only able to do two.

847
00:44:42.090 --> 00:44:44.910
So what you see is kind of what we were able to collect.

848
00:44:44.910 --> 00:44:48.720
But if we spent more time at this shipwreck,

849
00:44:48.720 --> 00:44:51.120
took more photos, did more passes,

850
00:44:51.120 --> 00:44:55.083
we could create a more fleshed out model.

851
00:45:01.980 --> 00:45:04.440
<v ->Thanks for answering that for us.</v>

852
00:45:04.440 --> 00:45:06.060
All right, next question.

853
00:45:06.060 --> 00:45:09.120
So I know you talked about how strobes

854
00:45:09.120 --> 00:45:10.740
will affect the color of things

855
00:45:10.740 --> 00:45:13.740
and sometimes how close you get affects the colors.

856
00:45:13.740 --> 00:45:17.340
Do you do any post-processing color correction

857
00:45:17.340 --> 00:45:20.883
or do you just mainly focus on what the strobes provide you?

858
00:45:21.780 --> 00:45:23.880
<v ->So with what we're doing now,</v>

859
00:45:23.880 --> 00:45:27.300
and I'll actually kind of pull back up the video

860
00:45:27.300 --> 00:45:29.610
from earlier 'cause I think it might do a great job

861
00:45:29.610 --> 00:45:30.443
of showing this.

862
00:45:31.500 --> 00:45:32.333
Let's see.

863
00:45:40.474 --> 00:45:41.307
Here we go.

864
00:45:41.307 --> 00:45:44.310
Okay, so what you're seeing here,

865
00:45:44.310 --> 00:45:47.610
we actually don't use any strobes in this process.

866
00:45:47.610 --> 00:45:52.610
The cameras have a way of white balancing that can kind of

867
00:45:53.280 --> 00:45:57.540
push out some of that blue light

868
00:45:57.540 --> 00:46:01.740
and kind of level itself to kind of pull out the reds

869
00:46:01.740 --> 00:46:03.210
and oranges and yellows

870
00:46:03.210 --> 00:46:05.913
of what the camera is able to receive.

871
00:46:06.810 --> 00:46:09.780
Because of that, we don't have as much of a need

872
00:46:09.780 --> 00:46:11.163
to use strobes.

873
00:46:12.510 --> 00:46:16.980
Now does that mean the corals and the algaes

874
00:46:16.980 --> 00:46:19.740
and everything you're seeing in this model are true to life?

875
00:46:19.740 --> 00:46:21.120
Not quite.

876
00:46:21.120 --> 00:46:23.790
There is a certain amount of,

877
00:46:23.790 --> 00:46:25.110
I don't wanna say guessing,

878
00:46:25.110 --> 00:46:28.740
but it lacks, the camera is taking photos

879
00:46:28.740 --> 00:46:31.260
that it lacks information of.

880
00:46:31.260 --> 00:46:33.900
So we don't necessarily do anything

881
00:46:33.900 --> 00:46:35.190
as far as post-processing,

882
00:46:35.190 --> 00:46:38.340
but the camera itself is doing a lot of processing

883
00:46:38.340 --> 00:46:40.740
of the photos there in the moment

884
00:46:40.740 --> 00:46:42.930
to create something that's, you know,

885
00:46:42.930 --> 00:46:44.523
not just a wash of blue.

886
00:46:45.510 --> 00:46:47.940
I hope that answers your question.

887
00:46:47.940 --> 00:46:49.830
Feel free to, you know, shoot another one

888
00:46:49.830 --> 00:46:52.950
and I'm more than happy to talk about this later

889
00:46:52.950 --> 00:46:54.333
in a follow up.

890
00:46:56.400 --> 00:46:57.960
<v ->Thanks Donavon.</v>

891
00:46:57.960 --> 00:46:59.580
I think we had a really interesting question

892
00:46:59.580 --> 00:47:03.510
that maybe you have to think about a little bit.

893
00:47:03.510 --> 00:47:08.510
But when you're taking these images

894
00:47:08.640 --> 00:47:09.870
over and over and over again,

895
00:47:09.870 --> 00:47:13.290
I'm sure that like fish swim in the way

896
00:47:13.290 --> 00:47:16.800
or maybe an urchins like hanging out,

897
00:47:16.800 --> 00:47:21.800
do you have to remove those like movable objects,

898
00:47:22.110 --> 00:47:26.700
I guess, those animals that aren't corals

899
00:47:26.700 --> 00:47:27.660
or sponges or algae,

900
00:47:27.660 --> 00:47:29.670
do you have to remove them from process

901
00:47:29.670 --> 00:47:31.920
or do you just avoid them altogether?

902
00:47:31.920 --> 00:47:33.820
<v ->So that's actually a great question.</v>

903
00:47:34.740 --> 00:47:38.880
So when we're doing this process,

904
00:47:38.880 --> 00:47:42.060
ideally we're not photographing a location once,

905
00:47:42.060 --> 00:47:44.220
we're photographing it a couple of times.

906
00:47:44.220 --> 00:47:47.670
So if a fish kind of swims over an area

907
00:47:47.670 --> 00:47:49.860
but then kind of continues to move on,

908
00:47:49.860 --> 00:47:51.930
the software is gonna, you know, see that fish

909
00:47:51.930 --> 00:47:53.520
and be like, I don't know what this is,

910
00:47:53.520 --> 00:47:55.830
and it'll just kind of throw that out

911
00:47:55.830 --> 00:47:57.960
and it'll continue as normal.

912
00:47:57.960 --> 00:48:00.727
However, for something like an urchin or even,

913
00:48:00.727 --> 00:48:04.380
you know, if a fish kind of stays in the same spot,

914
00:48:04.380 --> 00:48:06.780
if you pass over that multiple times

915
00:48:06.780 --> 00:48:08.880
and it gets the same kind of data points,

916
00:48:08.880 --> 00:48:11.100
you can actually get some creatures

917
00:48:11.100 --> 00:48:13.233
in your mosaics and in your models.

918
00:48:18.690 --> 00:48:19.793
<v ->Very cool.</v>

919
00:48:19.793 --> 00:48:23.400
Because I know whenever I use even just our photo mats

920
00:48:23.400 --> 00:48:26.257
that are of the reef bottom kids are like,

921
00:48:26.257 --> 00:48:28.950
"Where are the fish? Where are the fish?"

922
00:48:28.950 --> 00:48:30.720
So that's very interesting.

923
00:48:30.720 --> 00:48:32.370
All right.

924
00:48:32.370 --> 00:48:37.050
So how long will it take to process

925
00:48:37.050 --> 00:48:39.540
like all of the photogrammetry that you did

926
00:48:39.540 --> 00:48:40.830
for this past field season?

927
00:48:40.830 --> 00:48:44.310
How long do you think that that processing will take?

928
00:48:44.310 --> 00:48:46.050
<v ->That's a great question that, you know,</v>

929
00:48:46.050 --> 00:48:47.730
I wish I had a crystal ball

930
00:48:47.730 --> 00:48:50.250
that could even tell me the answer

931
00:48:50.250 --> 00:48:52.720
since this is kind of a new thing

932
00:48:53.596 --> 00:48:54.780
we're not a hundred percent sure,

933
00:48:54.780 --> 00:48:59.780
but I believe quite firmly

934
00:48:59.790 --> 00:49:01.500
that we'll have it finished

935
00:49:01.500 --> 00:49:05.250
before the start of this field season for 2026.

936
00:49:05.250 --> 00:49:07.623
So within the next coming month.

937
00:49:12.870 --> 00:49:14.112
<v ->Do you think there's a plan</v>

938
00:49:14.112 --> 00:49:16.770
to continue doing photogrammetry every single year?

939
00:49:16.770 --> 00:49:19.050
Just like how we do our other photo stations?

940
00:49:19.050 --> 00:49:22.380
<v ->Yeah, so this year actually NCRMP is coming to our site</v>

941
00:49:22.380 --> 00:49:27.380
and so us as Flower Gardens won't be shooting our models,

942
00:49:27.480 --> 00:49:30.930
but we'll be assisting in taking theirs,

943
00:49:30.930 --> 00:49:34.630
and we'll use the models that they get

944
00:49:36.120 --> 00:49:38.913
on those crews to process them that way.

945
00:49:46.362 --> 00:49:47.195
All right.

946
00:49:47.195 --> 00:49:48.540
Thank you everyone for all the questions.

947
00:49:48.540 --> 00:49:51.906
There's so many that I'm having to like pick around

948
00:49:51.906 --> 00:49:54.171
and see what we can answer live.

949
00:49:54.171 --> 00:49:57.840
Okay Donavon, we have a quite a few questions about software

950
00:49:57.840 --> 00:50:01.380
and what software we use

951
00:50:01.380 --> 00:50:03.510
to analyze these photos

952
00:50:03.510 --> 00:50:05.604
or to analyze the photogrammetry

953
00:50:05.604 --> 00:50:06.437
and photomosaics.

954
00:50:18.060 --> 00:50:19.860
Can you hear me Donavon?

955
00:50:19.860 --> 00:50:21.630
<v ->Yep, you were chopping up there for a moment,</v>

956
00:50:21.630 --> 00:50:23.193
but I think we're good now.

957
00:50:24.150 --> 00:50:25.710
<v ->Okay. Yeah.</v>

958
00:50:25.710 --> 00:50:27.390
There was a couple questions about

959
00:50:27.390 --> 00:50:31.050
what software we use to process

960
00:50:31.050 --> 00:50:34.143
to stitch together everything to do the photogrammetry.

961
00:50:36.690 --> 00:50:40.473
<v ->Yeah, so let's go back to this one.</v>

962
00:50:41.670 --> 00:50:46.670
Yeah, so the main programs that we're using are,

963
00:50:46.770 --> 00:50:48.683
well, okay to build the model

964
00:50:48.683 --> 00:50:51.660
it's called Agisoft Metashape.

965
00:50:51.660 --> 00:50:54.000
This is kind of become the gold standard

966
00:50:54.000 --> 00:50:57.393
for underwater photogrammetry.

967
00:51:00.840 --> 00:51:04.830
I am not too versed in why that is, but at least for,

968
00:51:04.830 --> 00:51:07.170
you know, on my side of things, we're using it

969
00:51:07.170 --> 00:51:10.860
because there's already a ton of documentation out there.

970
00:51:10.860 --> 00:51:12.860
So if I got a problem, you know, there's

971
00:51:23.490 --> 00:51:24.850
probably a forum or even a

972
00:51:26.000 --> 00:51:26.833
(indistinct)

973
00:51:26.833 --> 00:51:29.670
that has answered another program.

974
00:51:29.670 --> 00:51:32.250
But for analyzing the photomosaics,

975
00:51:32.250 --> 00:51:37.250
what they've been produced as mentioned in the presentation,

976
00:51:37.740 --> 00:51:39.120
we're using TagLab, which is

977
00:51:39.120 --> 00:51:42.693
what creates these nice colorful segmented images.

978
00:51:44.610 --> 00:51:47.250
And it uses a lot of automation

979
00:51:47.250 --> 00:51:49.800
to kind of streamline what we're doing.

980
00:51:49.800 --> 00:51:54.600
The idea of segmenting corals from photos is not new,

981
00:51:54.600 --> 00:51:57.390
but this software has allowed us to kind of step back

982
00:51:57.390 --> 00:52:01.260
into that and do it on a time scale that is, you know,

983
00:52:01.260 --> 00:52:05.853
much faster than what was previously.

984
00:52:08.310 --> 00:52:09.143
Yeah.

985
00:52:13.800 --> 00:52:16.710
<v ->Gotcha. Thanks for that explanation, Donavon.</v>

986
00:52:16.710 --> 00:52:18.240
<v ->So this is gonna be our last question</v>

987
00:52:18.240 --> 00:52:20.220
and I think it's a good one.

988
00:52:20.220 --> 00:52:24.120
So what do you see as the biggest barriers,

989
00:52:24.120 --> 00:52:26.010
either technical or otherwise

990
00:52:26.010 --> 00:52:29.490
that prevent photogrammetry collection with ROVs

991
00:52:29.490 --> 00:52:33.450
or through autonomous surface vehicles?

992
00:52:33.450 --> 00:52:35.190
Do you think it's more the human desire

993
00:52:35.190 --> 00:52:36.870
to collect the data firsthand

994
00:52:36.870 --> 00:52:41.870
or the marine robotic tools too expensive or hard to use?

995
00:52:42.000 --> 00:52:43.800
Do you have any thoughts about that?

996
00:52:44.760 --> 00:52:48.870
<v ->Ooh, that's a great question.</v>

997
00:52:48.870 --> 00:52:50.820
I wouldn't say I'm the most verse to answer it,

998
00:52:50.820 --> 00:52:52.830
but I definitely have my opinions.

999
00:52:52.830 --> 00:52:56.613
I mean, as a scuba diver, I prefer my hands, you know.

1000
00:52:58.350 --> 00:53:01.770
Robots are great, they have their place for me

1001
00:53:01.770 --> 00:53:05.973
as someone who's got two thumbs and can get underwater.

1002
00:53:07.410 --> 00:53:10.770
I have much more of an ability to adapt and change

1003
00:53:10.770 --> 00:53:13.200
what I'm doing underwater versus something

1004
00:53:13.200 --> 00:53:16.770
that has been set up before it gets in the water.

1005
00:53:16.770 --> 00:53:20.520
But also when it comes to ROVs and stuff,

1006
00:53:20.520 --> 00:53:21.600
they're also the future.

1007
00:53:21.600 --> 00:53:24.660
I say that, but they are.

1008
00:53:24.660 --> 00:53:27.900
There are already some autonomous vehicles

1009
00:53:27.900 --> 00:53:30.630
that you can send into the water.

1010
00:53:30.630 --> 00:53:35.490
And they have special software

1011
00:53:35.490 --> 00:53:37.747
that you can actually use to say,

1012
00:53:37.747 --> 00:53:40.170
"Hey, go image this part of the reef."

1013
00:53:40.170 --> 00:53:44.880
and it'll go and do it, which is spectacular.

1014
00:53:44.880 --> 00:53:47.520
It's a much more risk averse way

1015
00:53:47.520 --> 00:53:49.710
to collect data versus diving.

1016
00:53:49.710 --> 00:53:52.650
And it's also a bit more time efficient of course,

1017
00:53:52.650 --> 00:53:54.660
because you don't have to wait for divers to, you know,

1018
00:53:54.660 --> 00:53:57.810
come up, spend some time on the surface, go back down.

1019
00:53:57.810 --> 00:54:00.190
You should just keep tossing that robot

1020
00:54:05.370 --> 00:54:06.778
back into the water.

1021
00:54:06.778 --> 00:54:07.611
<v ->Yeah.</v>

1022
00:54:07.611 --> 00:54:11.356
<v ->But I hear things every now and then, so yeah.</v>

1023
00:54:11.356 --> 00:54:12.189
<v ->Thank you, Donavon.</v>

1024
00:54:12.189 --> 00:54:13.050
Sorry, I thought you stopped talking

1025
00:54:13.050 --> 00:54:14.400
and then I talked over you.

1026
00:54:16.318 --> 00:54:17.151
<v ->All good.</v>

1027
00:54:17.151 --> 00:54:18.900
<v ->Again, thank you so much</v>

1028
00:54:18.900 --> 00:54:21.390
for doing this program this evening.

1029
00:54:21.390 --> 00:54:24.210
Thanks for spending your evening with us.

1030
00:54:24.210 --> 00:54:28.323
I'm gonna go ahead and take back being presenter.

1031
00:54:34.080 --> 00:54:35.103
All right.

1032
00:54:36.117 --> 00:54:40.420
And also a big thank you to our audience

1033
00:54:41.430 --> 00:54:42.870
for being here today

1034
00:54:42.870 --> 00:54:47.190
because without you guys, we would not be here.

1035
00:54:47.190 --> 00:54:49.560
So thank you for attending

1036
00:54:49.560 --> 00:54:52.590
Stitching It Together Photogrammetry and Photomosaics.

1037
00:54:52.590 --> 00:54:54.510
This is just the first presentation

1038
00:54:54.510 --> 00:54:58.530
in the 2026 Flower Garden Banks Seaside Chat series.

1039
00:54:58.530 --> 00:55:00.630
So be sure to sign up for the next presentation,

1040
00:55:00.630 --> 00:55:02.580
which is on February 18th,

1041
00:55:02.580 --> 00:55:04.470
and you'll learn more about

1042
00:55:04.470 --> 00:55:07.050
how successful partnerships work together

1043
00:55:07.050 --> 00:55:10.173
to remove marine debris from within the sanctuary.

1044
00:55:18.390 --> 00:55:20.250
As we mentioned earlier, we will do our best

1045
00:55:20.250 --> 00:55:23.940
to answer the remaining questions that were not answered

1046
00:55:23.940 --> 00:55:27.570
during the webinar live and we'll email out those responses.

1047
00:55:27.570 --> 00:55:30.240
For those of you who would like to learn more on their own,

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00:55:30.240 --> 00:55:32.820
we've provided a document full of resources

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00:55:32.820 --> 00:55:34.860
in the handouts pane of the control panel.

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00:55:34.860 --> 00:55:36.570
And if you haven't downloaded that yet,

1051
00:55:36.570 --> 00:55:38.340
now would be a great time.

1052
00:55:38.340 --> 00:55:41.040
As always, we welcome your feedback and questions

1053
00:55:41.040 --> 00:55:43.020
and you can submit those by replying

1054
00:55:43.020 --> 00:55:45.900
to the follow-up email you receive after the webinar

1055
00:55:45.900 --> 00:55:50.343
or emailing us at flowergarden@noaa.gov.

1056
00:55:51.810 --> 00:55:53.880
Today's presentation has also been part

1057
00:55:53.880 --> 00:55:56.730
of the National Marine Sanctuary Webinar series.

1058
00:55:56.730 --> 00:55:59.430
While Seaside Chats just last one month,

1059
00:55:59.430 --> 00:56:02.700
our national webinar series continues throughout the year

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00:56:02.700 --> 00:56:04.470
to provide you with educational

1061
00:56:04.470 --> 00:56:07.560
and scientific expertise, resources,

1062
00:56:07.560 --> 00:56:10.620
and training to support ocean and climate literacy.

1063
00:56:10.620 --> 00:56:12.660
Be sure to check out the website for recordings

1064
00:56:12.660 --> 00:56:15.990
of past webinars and a schedule of what's to come.

1065
00:56:15.990 --> 00:56:17.820
As a reminder, we will share a recording

1066
00:56:17.820 --> 00:56:20.550
of this webinar via the National Marine Sanctuaries

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00:56:20.550 --> 00:56:23.643
and Flower Garden Banks National Marine Sanctuary Websites.

1068
00:56:24.930 --> 00:56:28.034
Following this webinar, attendees will receive a PDF copy

1069
00:56:28.034 --> 00:56:31.410
of a certificate of attendance that provides documentation

1070
00:56:31.410 --> 00:56:33.690
for one hour of professional development

1071
00:56:33.690 --> 00:56:35.610
for today's presentation.

1072
00:56:35.610 --> 00:56:39.180
This includes our Texas CPE provider number

1073
00:56:39.180 --> 00:56:41.700
for those of you who are Texas educators.

1074
00:56:41.700 --> 00:56:43.980
If you are an educator outside of Texas,

1075
00:56:43.980 --> 00:56:45.300
please use this certificate

1076
00:56:45.300 --> 00:56:48.540
to help get your hours approved in your district.

1077
00:56:48.540 --> 00:56:50.400
If you require additional information,

1078
00:56:50.400 --> 00:56:54.757
please contact us at flowergarden@noaa.gov.

1079
00:56:54.757 --> 00:56:58.260
Following this, there will also be a short evaluation

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00:56:58.260 --> 00:57:00.840
that should only take about three minutes to complete.

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00:57:00.840 --> 00:57:04.023
We greatly appreciate any feedback you are willing to share.

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00:57:05.700 --> 00:57:08.040
Thank you once again for joining us this evening

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00:57:08.040 --> 00:57:11.073
and we look forward to seeing you in the future.

