Overview
We would like to formally evaluate two questions: the first centers around evaluating / optimizing ROV field methods sampling design, and the second revoles around evaluating methods of data interpolation to create spatial layers from our ROV-derived benthic community data. To evaluate both of these questions we will utilize empirical data to simulate sugar kelp across a seascape of depth, and we'll use empirical ROV transects to evaluate how well our surveys captured simulated sugar kelp pattern.
In summer 2025 our team conducted 23 perpendicular ROV transects offshore of Centennial Park in Elliott Bay, Seattle, with each transect starting at a depth of approximately 16m depth and terminating at a depth of approximately 1m depth. As you can see below, summer 2025 we completed 23 of these two perpendicular transects offshore of Centennial Park in Elliott Bay, Seattle, and we split these into two halves (to test the ability to differentiate two "sub-regions" of interpolated layers).
The intent with these perpendicular transects was to capture pattern across depth, i.e., capture the lack of sugar kelp at 16m, and then its emergence towards around 9m, and peak density around 6m.
As noted above, we'd ultimate like to be able to extract empirical sugar kelp data from all our spatially explicit survey photos and use those data to interpolate and create ArcGIS layers for, in this case, sugar kelp. First however, we need to better understand the relationship between the number of ROV transects completed, and the ability to generate minimally effective interpolated layers.
Files / data available
We have the following information:
percent-cover_abundances.csv contains earlier Port of Seattle survey data with sugar kelp information across a broad depth gradient
GLMM.R contains initial code used to conduct generalized linear mixed effects modeling
Extract_Cent_1.tif contains depth information for the sampling region shown above (left)
perpendicular_transects.csv contains ROV telemetry information (including lat/lon) for our 2025 perpendicular transects
nestled within our standard repo structure:
- data - raw data input
- results - files resulting from analyses here
- code - scripts utilized
- figs - output figures, files
Proposed approach
Subsequent empirical step
Now that we have workflows to process imagery at scale (via https://github.com/Seattle-Aquarium/underwater-auto-image-encoder) and can extract Toolbox data at scale, a separate and subsequent Issue will follow utilizing real-world sugar kelp values that have been extracted from the real images. To provide a speedy initial investigation, we will rely upon unverified Toolbox output, i.e., we will not review the model's predictions via Kelp Quest, and will instead simply apply the algorithm and analyze the output.
Overview
We would like to formally evaluate two questions: the first centers around evaluating / optimizing ROV field methods sampling design, and the second revoles around evaluating methods of data interpolation to create spatial layers from our ROV-derived benthic community data. To evaluate both of these questions we will utilize empirical data to simulate sugar kelp across a seascape of depth, and we'll use empirical ROV transects to evaluate how well our surveys captured simulated sugar kelp pattern.
In summer 2025 our team conducted 23 perpendicular ROV transects offshore of Centennial Park in Elliott Bay, Seattle, with each transect starting at a depth of approximately 16m depth and terminating at a depth of approximately 1m depth. As you can see below, summer 2025 we completed 23 of these two perpendicular transects offshore of Centennial Park in Elliott Bay, Seattle, and we split these into two halves (to test the ability to differentiate two "sub-regions" of interpolated layers).
The intent with these perpendicular transects was to capture pattern across depth, i.e., capture the lack of sugar kelp at 16m, and then its emergence towards around 9m, and peak density around 6m.
As noted above, we'd ultimate like to be able to extract empirical sugar kelp data from all our spatially explicit survey photos and use those data to interpolate and create ArcGIS layers for, in this case, sugar kelp. First however, we need to better understand the relationship between the number of ROV transects completed, and the ability to generate minimally effective interpolated layers.
Files / data available
We have the following information:
percent-cover_abundances.csvcontains earlier Port of Seattle survey data with sugar kelp information across a broad depth gradientGLMM.Rcontains initial code used to conduct generalized linear mixed effects modelingExtract_Cent_1.tifcontains depth information for the sampling region shown above (left)perpendicular_transects.csvcontains ROV telemetry information (including lat/lon) for our 2025 perpendicular transectsnestled within our standard repo structure:
Proposed approach
sugar_kelpwithin percent-cover_abundances via GLMM and extract the probability function.Subsequent empirical step
Now that we have workflows to process imagery at scale (via https://github.com/Seattle-Aquarium/underwater-auto-image-encoder) and can extract Toolbox data at scale, a separate and subsequent Issue will follow utilizing real-world sugar kelp values that have been extracted from the real images. To provide a speedy initial investigation, we will rely upon unverified Toolbox output, i.e., we will not review the model's predictions via Kelp Quest, and will instead simply apply the algorithm and analyze the output.