Supplemental Figure 1: Descent Rate & Volume Sampled

The UVP descends through the water column taking photographs at a rate of 20Hz. Each UVP image captures an 18.8cm x 18.8cm x 3.11cm FOV. This creates the potential for overlap of images, capturing multiple instances of one individual

These figures show the raw descent rates of all cast and the volume sampled in 1-m bins. These also display the potential for overlap, however - it is impossible to truly know if overlap occured from this data because the pressure sensor on the UVP has a specificity of 10cm.

Code
rm(list = ls())
library(EcotaxaTools)
library(ggplot2)
library(cowplot)

dr_plot <- readRDS('../Output/supp_fig_01_descent-rates.rds')
vol_plot <- readRDS('../Output/supp_fig_01_vol-sampled.rds')

dr_dat <- readRDS('../Output/data_supp_01_descent-averages.rds')
vol_dat <- readRDS('../Output/data_supp_01_voldata.rds')
Code
plot_grid(dr_plot, vol_plot)


The UVP was lowered at a slower rate from 0-200m than it was from 200-1000m. The average descent rate (0.653 m/s) in the top 200m of the water column was just above the rate at which overlap is likely (0.622 m/s). Additionally, in the top 200m, there are more images taken (a higher volume sampled) than would be possible if no overlap occurred. This indicates that overlap is either occurring or the UVP is moving horizontally in the water column. In all likelihood both of these are a possibility considering ship-drift. In the mesopelagic, overlap is much less likely because the UVP descends at a much faster rate (average 1.099 m/s). The impact of duplicate images are investigated here