Modeled underwater light during Polar Night.

Underwater light intensity plotted as scalar irradiance (E o irradiance on a point from all directions weighted equally). Light values were derived from radiative transfer model results of diffuse skylight irradiance measured at Rijpfjorden, Svalbard (80° 37.79N 22° 4.14E) at solar noon on January 1...

Full description

Bibliographic Details
Main Authors: Jonathan H. Cohen (7958483), Kim S. Last (11581392), Corie L. Charpentier (3200505), Finlo Cottier (749186), Malin Daase (471602), Laura Hobbs (9152223), Geir Johnsen (257802), Jørgen Berge (235355)
Format: Still Image
Language:unknown
Published: 2021
Subjects:
Online Access:https://doi.org/10.1371/journal.pbio.3001413.g004
Description
Summary:Underwater light intensity plotted as scalar irradiance (E o irradiance on a point from all directions weighted equally). Light values were derived from radiative transfer model results of diffuse skylight irradiance measured at Rijpfjorden, Svalbard (80° 37.79N 22° 4.14E) at solar noon on January 15, 2016, then propagated through the water column (bold black line showing irradiance as a function of depth). The dotted vertical line denotes the visual sensitivity threshold for T . inermis (1% of V max for subjective midnight V- log I ). Dashed vertical lines show thresholds for light-mediated processes in a range of other taxa: entrainment of circadian rhythms in fruit flies [ 53 ] and mice [ 55 ]; 1% of V max from V- log I for Antarctic fish Pagothenia [ 56 ]. Depth-stratified abundance of T . inermis at Rijpforden (06:30 on January 14, 2016) is plotted as bubbles of proportional size. For data, see S2 Data .