(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642
Snowfall was measured at 11 sites in the McMurdo Dry Valleys to determine its magnitude, its temporal changes, and spatial patterns. Annual values ranged from 3 to 50 mm water equivalent with the highest values nearest the coast and decreasing inland. A particularly strong spatial gradient exists in...
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ftdatacite:10.1594/pangaea.809526 2023-05-15T13:56:05+02:00 (Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 Fountain, Andrew G Nylen, Thomas H Monaghan, Andrew J Basagic, Hassan J Bromwich, David H 2010 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.809526 https://doi.pangaea.de/10.1594/PANGAEA.809526 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1002/joc.1933 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Event label Latitude of event Longitude of event Device type DATE/TIME Accumulation of snow in water equivalent per year Unmanned weather station/meteorological observation International Polar Year 2007-2008 IPY Supplementary Dataset dataset Dataset 2010 ftdatacite https://doi.org/10.1594/pangaea.809526 https://doi.org/10.1002/joc.1933 2021-11-05T12:55:41Z Snowfall was measured at 11 sites in the McMurdo Dry Valleys to determine its magnitude, its temporal changes, and spatial patterns. Annual values ranged from 3 to 50 mm water equivalent with the highest values nearest the coast and decreasing inland. A particularly strong spatial gradient exists in Taylor Valley, probably resulting from local uplift conditions at the coastal margin and valley topography that limits migration inland. More snow occurs in winter near the coast, whereas inland no seasonal pattern is discernable. This may be due, again, to local uplift conditions, which are common in winter. We find no influence of the distance to the sea ice edge. Katabatic winds play an important role in transporting snow to the valley bottoms and essentially double the precipitation. That much of the snow accumulation sublimates prior to making a hydrologic contribution underscores the notion that the McMurdo Dry Valleys are indeed an extreme polar desert. : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 Dataset Antarc* Antarctica International Polar Year IPY McMurdo Dry Valleys polar desert Sea ice DataCite Metadata Store (German National Library of Science and Technology) McMurdo Dry Valleys Taylor Valley ENVELOPE(163.000,163.000,-77.617,-77.617) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Device type DATE/TIME Accumulation of snow in water equivalent per year Unmanned weather station/meteorological observation International Polar Year 2007-2008 IPY |
spellingShingle |
Event label Latitude of event Longitude of event Device type DATE/TIME Accumulation of snow in water equivalent per year Unmanned weather station/meteorological observation International Polar Year 2007-2008 IPY Fountain, Andrew G Nylen, Thomas H Monaghan, Andrew J Basagic, Hassan J Bromwich, David H (Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
topic_facet |
Event label Latitude of event Longitude of event Device type DATE/TIME Accumulation of snow in water equivalent per year Unmanned weather station/meteorological observation International Polar Year 2007-2008 IPY |
description |
Snowfall was measured at 11 sites in the McMurdo Dry Valleys to determine its magnitude, its temporal changes, and spatial patterns. Annual values ranged from 3 to 50 mm water equivalent with the highest values nearest the coast and decreasing inland. A particularly strong spatial gradient exists in Taylor Valley, probably resulting from local uplift conditions at the coastal margin and valley topography that limits migration inland. More snow occurs in winter near the coast, whereas inland no seasonal pattern is discernable. This may be due, again, to local uplift conditions, which are common in winter. We find no influence of the distance to the sea ice edge. Katabatic winds play an important role in transporting snow to the valley bottoms and essentially double the precipitation. That much of the snow accumulation sublimates prior to making a hydrologic contribution underscores the notion that the McMurdo Dry Valleys are indeed an extreme polar desert. : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 |
format |
Dataset |
author |
Fountain, Andrew G Nylen, Thomas H Monaghan, Andrew J Basagic, Hassan J Bromwich, David H |
author_facet |
Fountain, Andrew G Nylen, Thomas H Monaghan, Andrew J Basagic, Hassan J Bromwich, David H |
author_sort |
Fountain, Andrew G |
title |
(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
title_short |
(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
title_full |
(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
title_fullStr |
(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
title_full_unstemmed |
(Table 1) Snow accumulation in the McMurdo Dry Valleys, supplement to: Fountain, Andrew G; Nylen, Thomas H; Monaghan, Andrew J; Basagic, Hassan J; Bromwich, David H (2010): Snow in the McMurdo Dry Valleys, Antarctica. International Journal of Climatology, 30(5), 633-642 |
title_sort |
(table 1) snow accumulation in the mcmurdo dry valleys, supplement to: fountain, andrew g; nylen, thomas h; monaghan, andrew j; basagic, hassan j; bromwich, david h (2010): snow in the mcmurdo dry valleys, antarctica. international journal of climatology, 30(5), 633-642 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.809526 https://doi.pangaea.de/10.1594/PANGAEA.809526 |
long_lat |
ENVELOPE(163.000,163.000,-77.617,-77.617) |
geographic |
McMurdo Dry Valleys Taylor Valley |
geographic_facet |
McMurdo Dry Valleys Taylor Valley |
genre |
Antarc* Antarctica International Polar Year IPY McMurdo Dry Valleys polar desert Sea ice |
genre_facet |
Antarc* Antarctica International Polar Year IPY McMurdo Dry Valleys polar desert Sea ice |
op_relation |
https://dx.doi.org/10.1002/joc.1933 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.809526 https://doi.org/10.1002/joc.1933 |
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1766263322693337088 |