Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008
In this study, we present the winter time surface energy balance at a polygonal tundra site in northern Siberia based on independent measurements of the net radiation, the sensible heat flux and the ground heat flux from two winter seasons. The latent heat flux is inferred from measurements of the a...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.789131 2024-09-30T14:31:47+00:00 Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 Langer, Moritz Westermann, Sebastian Muster, Sina Piel, Konstanze Boike, Julia LATITUDE: 72.376480 * LONGITUDE: 126.489230 * DATE/TIME START: 2007-10-01T00:00:00 * DATE/TIME END: 2009-03-01T00:00:00 * MINIMUM HEIGHT above ground: 2 m * MAXIMUM HEIGHT above ground: 2 m 2012 text/tab-separated-values, 87932 data points https://doi.pangaea.de/10.1594/PANGAEA.789131 https://doi.org/10.1594/PANGAEA.789131 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.789131 https://doi.org/10.1594/PANGAEA.789131 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Langer, Moritz; Westermann, Sebastian; Muster, Sina; Piel, Konstanze; Boike, Julia (2011): The surface energy balance of a polygonal tundra site in northern Siberia – Part 2: Winter. The Cryosphere, 5, 509-524, https://doi.org/10.5194/tc-5-509-2011 Arctic Calculated DATE/TIME Ground heat flux Heat latent sensible HEIGHT above ground latent heat flux Long-wave downward radiation longwave radiation Long-wave upward radiation MULT Multiple investigations Net radiation Net radiometer Kipp & Zonen NR Lite Radiometer CNR 1 Samoylov_Island Samoylov Island Lena Delta Siberia sensible heat flux Short-wave downward (GLOBAL) radiation shortwave radiation Short-wave upward (REFLEX) radiation Time in days dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.78913110.5194/tc-5-509-2011 2024-09-11T00:15:18Z In this study, we present the winter time surface energy balance at a polygonal tundra site in northern Siberia based on independent measurements of the net radiation, the sensible heat flux and the ground heat flux from two winter seasons. The latent heat flux is inferred from measurements of the atmospheric turbulence characteristics and a model approach. The long-wave radiation is found to be the dominant factor in the surface energy balance. The radiative losses are balanced to about 60 % by the ground heat flux and almost 40 % by the sensible heat fluxes, whereas the contribution of the latent heat flux is small. The main controlling factors of the surface energy budget are the snow cover, the cloudiness and the soil temperature gradient. Large spatial differences in the surface energy balance are observed between tundra soils and a small pond. The ground heat flux released at a freezing pond is by a factor of two higher compared to the freezing soil, whereas large differences in net radiation between the pond and soil are only observed at the end of the winter period. Differences in the surface energy balance between the two winter seasons are found to be related to differences in snow depth and cloud cover which strongly affect the temperature evolution and the freeze-up at the investigated pond. Dataset Arctic lena delta The Cryosphere Tundra Siberia PANGAEA - Data Publisher for Earth & Environmental Science Arctic ENVELOPE(126.489230,126.489230,72.376480,72.376480) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Arctic Calculated DATE/TIME Ground heat flux Heat latent sensible HEIGHT above ground latent heat flux Long-wave downward radiation longwave radiation Long-wave upward radiation MULT Multiple investigations Net radiation Net radiometer Kipp & Zonen NR Lite Radiometer CNR 1 Samoylov_Island Samoylov Island Lena Delta Siberia sensible heat flux Short-wave downward (GLOBAL) radiation shortwave radiation Short-wave upward (REFLEX) radiation Time in days |
spellingShingle |
Arctic Calculated DATE/TIME Ground heat flux Heat latent sensible HEIGHT above ground latent heat flux Long-wave downward radiation longwave radiation Long-wave upward radiation MULT Multiple investigations Net radiation Net radiometer Kipp & Zonen NR Lite Radiometer CNR 1 Samoylov_Island Samoylov Island Lena Delta Siberia sensible heat flux Short-wave downward (GLOBAL) radiation shortwave radiation Short-wave upward (REFLEX) radiation Time in days Langer, Moritz Westermann, Sebastian Muster, Sina Piel, Konstanze Boike, Julia Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
topic_facet |
Arctic Calculated DATE/TIME Ground heat flux Heat latent sensible HEIGHT above ground latent heat flux Long-wave downward radiation longwave radiation Long-wave upward radiation MULT Multiple investigations Net radiation Net radiometer Kipp & Zonen NR Lite Radiometer CNR 1 Samoylov_Island Samoylov Island Lena Delta Siberia sensible heat flux Short-wave downward (GLOBAL) radiation shortwave radiation Short-wave upward (REFLEX) radiation Time in days |
description |
In this study, we present the winter time surface energy balance at a polygonal tundra site in northern Siberia based on independent measurements of the net radiation, the sensible heat flux and the ground heat flux from two winter seasons. The latent heat flux is inferred from measurements of the atmospheric turbulence characteristics and a model approach. The long-wave radiation is found to be the dominant factor in the surface energy balance. The radiative losses are balanced to about 60 % by the ground heat flux and almost 40 % by the sensible heat fluxes, whereas the contribution of the latent heat flux is small. The main controlling factors of the surface energy budget are the snow cover, the cloudiness and the soil temperature gradient. Large spatial differences in the surface energy balance are observed between tundra soils and a small pond. The ground heat flux released at a freezing pond is by a factor of two higher compared to the freezing soil, whereas large differences in net radiation between the pond and soil are only observed at the end of the winter period. Differences in the surface energy balance between the two winter seasons are found to be related to differences in snow depth and cloud cover which strongly affect the temperature evolution and the freeze-up at the investigated pond. |
format |
Dataset |
author |
Langer, Moritz Westermann, Sebastian Muster, Sina Piel, Konstanze Boike, Julia |
author_facet |
Langer, Moritz Westermann, Sebastian Muster, Sina Piel, Konstanze Boike, Julia |
author_sort |
Langer, Moritz |
title |
Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
title_short |
Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
title_full |
Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
title_fullStr |
Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
title_full_unstemmed |
Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, October 2007 to March 2008 |
title_sort |
heat fluxes and surface radiation measurements from samoylov island, lena delta, siberia, october 2007 to march 2008 |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.789131 https://doi.org/10.1594/PANGAEA.789131 |
op_coverage |
LATITUDE: 72.376480 * LONGITUDE: 126.489230 * DATE/TIME START: 2007-10-01T00:00:00 * DATE/TIME END: 2009-03-01T00:00:00 * MINIMUM HEIGHT above ground: 2 m * MAXIMUM HEIGHT above ground: 2 m |
long_lat |
ENVELOPE(126.489230,126.489230,72.376480,72.376480) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic lena delta The Cryosphere Tundra Siberia |
genre_facet |
Arctic lena delta The Cryosphere Tundra Siberia |
op_source |
Supplement to: Langer, Moritz; Westermann, Sebastian; Muster, Sina; Piel, Konstanze; Boike, Julia (2011): The surface energy balance of a polygonal tundra site in northern Siberia – Part 2: Winter. The Cryosphere, 5, 509-524, https://doi.org/10.5194/tc-5-509-2011 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.789131 https://doi.org/10.1594/PANGAEA.789131 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.78913110.5194/tc-5-509-2011 |
_version_ |
1811636153471729664 |