Transparency of Antarctic ice-covered lakes to solar UV radiation

Depth profiles of solar ultraviolet radiation (UVR), photosynthetically available radiation (PAR), and related variables were measured beneath the thick, permanent ice cover of four lakes in the McMurdo Dry Valleys (77’S, 162”E). These lakes span a range of phytoplankton c centrations (0.1-10 pg Chl...

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Main Authors: Warwick F. Vincent, Rowena Rae, Isabelle Laurion, John C. Priscu
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1247
http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.517.1247 2023-05-15T13:56:38+02:00 Transparency of Antarctic ice-covered lakes to solar UV radiation Warwick F. Vincent Rowena Rae Isabelle Laurion John C. Priscu The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1247 http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1247 http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf text ftciteseerx 2016-01-08T09:55:13Z Depth profiles of solar ultraviolet radiation (UVR), photosynthetically available radiation (PAR), and related variables were measured beneath the thick, permanent ice cover of four lakes in the McMurdo Dry Valleys (77’S, 162”E). These lakes span a range of phytoplankton c centrations (0.1-10 pg Chl a liter-l) butreceive little input of chromophoric dissolved organic matter (CDOM) from their barren, polar desert catchments. The diffuse atten-uation coefficients fordownwelling radiation (K,) in the upper water column of the lakes were at or below those for clear natural waters elsewhere, with minimum values in Lake Vanda of 0.080 (305 nm), 0.055 (320 nm), 0.036 (340 nm), 0.023 (380 nm) and 0.034 (PAR) m-l. The attenuation lengths (l/K,) for these lakes and for a set of high latitude lakes in the northern hemisphere (tundra nd boreal forest catchments) showed a close log-log rela-tionship with dissolved organic arbon (DOC) concentrations (r * L 0.90; n = 20); dry valley lakes were at the high transparency end of this polar-subpolar continuum. Phytoplankton exposure to UVR relative toPAR is known to rise steeply with decreasing DOC in the concentration range 2-4 g m-3; the addition of the dry valley lakes data shows the continuation of this upward, markedly nonlinear t end at lower DOC concentrations. Calculation of the biologically effective UVR dosage rate for the upper phytoplankton community of Lake Vanda indicated that sufficient UVR penetrates hrough the 3.5-m-thick la e ice to cause inhibition of algal growth. These results show Text Antarc* Antarctic McMurdo Dry Valleys polar desert Tundra Unknown Antarctic Four Lakes ENVELOPE(-126.826,-126.826,54.858,54.858) Lake Vanda ENVELOPE(161.600,161.600,-77.517,-77.517) McMurdo Dry Valleys Vanda ENVELOPE(161.550,161.550,-77.533,-77.533)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Depth profiles of solar ultraviolet radiation (UVR), photosynthetically available radiation (PAR), and related variables were measured beneath the thick, permanent ice cover of four lakes in the McMurdo Dry Valleys (77’S, 162”E). These lakes span a range of phytoplankton c centrations (0.1-10 pg Chl a liter-l) butreceive little input of chromophoric dissolved organic matter (CDOM) from their barren, polar desert catchments. The diffuse atten-uation coefficients fordownwelling radiation (K,) in the upper water column of the lakes were at or below those for clear natural waters elsewhere, with minimum values in Lake Vanda of 0.080 (305 nm), 0.055 (320 nm), 0.036 (340 nm), 0.023 (380 nm) and 0.034 (PAR) m-l. The attenuation lengths (l/K,) for these lakes and for a set of high latitude lakes in the northern hemisphere (tundra nd boreal forest catchments) showed a close log-log rela-tionship with dissolved organic arbon (DOC) concentrations (r * L 0.90; n = 20); dry valley lakes were at the high transparency end of this polar-subpolar continuum. Phytoplankton exposure to UVR relative toPAR is known to rise steeply with decreasing DOC in the concentration range 2-4 g m-3; the addition of the dry valley lakes data shows the continuation of this upward, markedly nonlinear t end at lower DOC concentrations. Calculation of the biologically effective UVR dosage rate for the upper phytoplankton community of Lake Vanda indicated that sufficient UVR penetrates hrough the 3.5-m-thick la e ice to cause inhibition of algal growth. These results show
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Warwick F. Vincent
Rowena Rae
Isabelle Laurion
John C. Priscu
spellingShingle Warwick F. Vincent
Rowena Rae
Isabelle Laurion
John C. Priscu
Transparency of Antarctic ice-covered lakes to solar UV radiation
author_facet Warwick F. Vincent
Rowena Rae
Isabelle Laurion
John C. Priscu
author_sort Warwick F. Vincent
title Transparency of Antarctic ice-covered lakes to solar UV radiation
title_short Transparency of Antarctic ice-covered lakes to solar UV radiation
title_full Transparency of Antarctic ice-covered lakes to solar UV radiation
title_fullStr Transparency of Antarctic ice-covered lakes to solar UV radiation
title_full_unstemmed Transparency of Antarctic ice-covered lakes to solar UV radiation
title_sort transparency of antarctic ice-covered lakes to solar uv radiation
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1247
http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf
long_lat ENVELOPE(-126.826,-126.826,54.858,54.858)
ENVELOPE(161.600,161.600,-77.517,-77.517)
ENVELOPE(161.550,161.550,-77.533,-77.533)
geographic Antarctic
Four Lakes
Lake Vanda
McMurdo Dry Valleys
Vanda
geographic_facet Antarctic
Four Lakes
Lake Vanda
McMurdo Dry Valleys
Vanda
genre Antarc*
Antarctic
McMurdo Dry Valleys
polar desert
Tundra
genre_facet Antarc*
Antarctic
McMurdo Dry Valleys
polar desert
Tundra
op_source http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.1247
http://www.aslo.org/lo/toc/vol_43/issue_4/0618.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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