The Underwater Photic Environment of a Small Arctic Lake

The underwater light field in a small arctic lake on Victoria Island, Northwest Territories, was examined. Downward radiance was found to be bimodal, with transmission peaks at 480 and 640 nanometres (nm, or .000000001 m). Upward radiance was similar near the surface, with peaks at 480 and 620 nm, b...

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Published in:ARCTIC
Main Authors: Heinermann, P.H., Johnson, L., Ali, M.A.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1990
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64657 2023-05-15T14:19:13+02:00 The Underwater Photic Environment of a Small Arctic Lake Heinermann, P.H. Johnson, L. Ali, M.A. 1990-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657/48571 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657 ARCTIC; Vol. 43 No. 2 (1990): June: 99–200; 129-136 1923-1245 0004-0843 arctic limnology underwater light diurnal variation spectral quality irradiance radiance arctique limnologie lumiere sous-marine variation diurne qualité spectrale info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1990 ftunivcalgaryojs 2022-03-22T21:21:48Z The underwater light field in a small arctic lake on Victoria Island, Northwest Territories, was examined. Downward radiance was found to be bimodal, with transmission peaks at 480 and 640 nanometres (nm, or .000000001 m). Upward radiance was similar near the surface, with peaks at 480 and 620 nm, but became unimodal with depth and shifted to 580 nm near the bottom. Diurnal variation in the underwater downward and upward irradiance of PAR (photosynthetically active radiation) was approximately two orders of magnitude. The spectral quality of light transmission also changed over this 24 hour period. Unimodal transmission of red light occurred in the early morning (1:00 and 5:00) and late evening (22:00), while bimodal transmission of blue-green and red light was observed during the day (9:00-17:30). Kd(Zm), the vertical attenuation coefficient for downward irradiance at the midpoint of the euphotic zone, was relatively insensitive to changes in solar elevation. Diurnal variation in the reflectance of PAR differed from the predicted by previous simulation models, while the inverse relationship between reflectance and the absorption coefficient was in agreement with these same models. Gilvin, humic material-dissolved iron complexes, algal fucoxanthin, chlorophyll a and tripton all contribute to the attenuation of light and are responsible for the unique underwater spectral transmission in Keyhole Lake. Article in Journal/Newspaper Arctic Arctic Arctique* Northwest Territories Victoria Island University of Calgary Journal Hosting Arctic Arctic Lake ENVELOPE(-130.826,-130.826,57.231,57.231) Keyhole ENVELOPE(-67.338,-67.338,-68.785,-68.785) Keyhole Lake ENVELOPE(163.683,163.683,-78.133,-78.133) Lumiere ENVELOPE(-64.033,-64.033,-65.317,-65.317) Northwest Territories ARCTIC 43 2
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic arctic
limnology
underwater light
diurnal variation
spectral quality
irradiance
radiance
arctique
limnologie
lumiere sous-marine
variation diurne
qualité spectrale
spellingShingle arctic
limnology
underwater light
diurnal variation
spectral quality
irradiance
radiance
arctique
limnologie
lumiere sous-marine
variation diurne
qualité spectrale
Heinermann, P.H.
Johnson, L.
Ali, M.A.
The Underwater Photic Environment of a Small Arctic Lake
topic_facet arctic
limnology
underwater light
diurnal variation
spectral quality
irradiance
radiance
arctique
limnologie
lumiere sous-marine
variation diurne
qualité spectrale
description The underwater light field in a small arctic lake on Victoria Island, Northwest Territories, was examined. Downward radiance was found to be bimodal, with transmission peaks at 480 and 640 nanometres (nm, or .000000001 m). Upward radiance was similar near the surface, with peaks at 480 and 620 nm, but became unimodal with depth and shifted to 580 nm near the bottom. Diurnal variation in the underwater downward and upward irradiance of PAR (photosynthetically active radiation) was approximately two orders of magnitude. The spectral quality of light transmission also changed over this 24 hour period. Unimodal transmission of red light occurred in the early morning (1:00 and 5:00) and late evening (22:00), while bimodal transmission of blue-green and red light was observed during the day (9:00-17:30). Kd(Zm), the vertical attenuation coefficient for downward irradiance at the midpoint of the euphotic zone, was relatively insensitive to changes in solar elevation. Diurnal variation in the reflectance of PAR differed from the predicted by previous simulation models, while the inverse relationship between reflectance and the absorption coefficient was in agreement with these same models. Gilvin, humic material-dissolved iron complexes, algal fucoxanthin, chlorophyll a and tripton all contribute to the attenuation of light and are responsible for the unique underwater spectral transmission in Keyhole Lake.
format Article in Journal/Newspaper
author Heinermann, P.H.
Johnson, L.
Ali, M.A.
author_facet Heinermann, P.H.
Johnson, L.
Ali, M.A.
author_sort Heinermann, P.H.
title The Underwater Photic Environment of a Small Arctic Lake
title_short The Underwater Photic Environment of a Small Arctic Lake
title_full The Underwater Photic Environment of a Small Arctic Lake
title_fullStr The Underwater Photic Environment of a Small Arctic Lake
title_full_unstemmed The Underwater Photic Environment of a Small Arctic Lake
title_sort underwater photic environment of a small arctic lake
publisher The Arctic Institute of North America
publishDate 1990
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657
long_lat ENVELOPE(-130.826,-130.826,57.231,57.231)
ENVELOPE(-67.338,-67.338,-68.785,-68.785)
ENVELOPE(163.683,163.683,-78.133,-78.133)
ENVELOPE(-64.033,-64.033,-65.317,-65.317)
geographic Arctic
Arctic Lake
Keyhole
Keyhole Lake
Lumiere
Northwest Territories
geographic_facet Arctic
Arctic Lake
Keyhole
Keyhole Lake
Lumiere
Northwest Territories
genre Arctic
Arctic
Arctique*
Northwest Territories
Victoria Island
genre_facet Arctic
Arctic
Arctique*
Northwest Territories
Victoria Island
op_source ARCTIC; Vol. 43 No. 2 (1990): June: 99–200; 129-136
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657/48571
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64657
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container_volume 43
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