Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations

Snow accumulation measurements from automatic weather stations (AWS) around the Ross Ice Shelf (RIS), Antarctica, are used to provide a new set of ground-based observations which are compared to precipitation from the ECMWF ERA-Interim and NCEP/NCAR Reanalysis-2 datasets. The high temporal resolutio...

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Published in:The Cryosphere
Main Authors: L. Cohen, S. Dean
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/tc-7-1399-2013
https://doaj.org/article/760b8ff207c842fca62727c0c951e61e
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spelling ftdoajarticles:oai:doaj.org/article:760b8ff207c842fca62727c0c951e61e 2023-05-15T13:40:00+02:00 Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations L. Cohen S. Dean 2013-09-01T00:00:00Z https://doi.org/10.5194/tc-7-1399-2013 https://doaj.org/article/760b8ff207c842fca62727c0c951e61e EN eng Copernicus Publications http://www.the-cryosphere.net/7/1399/2013/tc-7-1399-2013.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-7-1399-2013 1994-0416 1994-0424 https://doaj.org/article/760b8ff207c842fca62727c0c951e61e The Cryosphere, Vol 7, Iss 5, Pp 1399-1410 (2013) Environmental sciences GE1-350 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/tc-7-1399-2013 2022-12-31T14:14:07Z Snow accumulation measurements from automatic weather stations (AWS) around the Ross Ice Shelf (RIS), Antarctica, are used to provide a new set of ground-based observations which are compared to precipitation from the ECMWF ERA-Interim and NCEP/NCAR Reanalysis-2 datasets. The high temporal resolution of the AWS snow accumulation measurements allow for an event-based comparison of reanalyses precipitation to the in situ observations. Snow accumulation records from nine AWS provide multiple years of accumulation data between 2008 and 2012 over a relatively large, homogeneous region of Antarctica, and also provide the basis for a statistical evaluation of accumulation and precipitation events. The complex effects of wind on snow accumulation (which can both limit and enhance accumulation) complicate the use of the accumulation measurements, but this analysis shows that they can provide a valuable source of ground-based observations for comparisons to modelled precipitation on synoptic timescales. The analysis shows that ERA-Interim reproduces more precipitation events than NCEP-2, and these events correspond to an average 8.2% more precipitation. Significant correlations between reanalyses and AWS event sizes are seen at several stations and show that ERA-Interim consistently produces larger precipitation events than NCEP-2. Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Ross Ice Shelf The Cryosphere Directory of Open Access Journals: DOAJ Articles Ross Ice Shelf The Cryosphere 7 5 1399 1410
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
L. Cohen
S. Dean
Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Snow accumulation measurements from automatic weather stations (AWS) around the Ross Ice Shelf (RIS), Antarctica, are used to provide a new set of ground-based observations which are compared to precipitation from the ECMWF ERA-Interim and NCEP/NCAR Reanalysis-2 datasets. The high temporal resolution of the AWS snow accumulation measurements allow for an event-based comparison of reanalyses precipitation to the in situ observations. Snow accumulation records from nine AWS provide multiple years of accumulation data between 2008 and 2012 over a relatively large, homogeneous region of Antarctica, and also provide the basis for a statistical evaluation of accumulation and precipitation events. The complex effects of wind on snow accumulation (which can both limit and enhance accumulation) complicate the use of the accumulation measurements, but this analysis shows that they can provide a valuable source of ground-based observations for comparisons to modelled precipitation on synoptic timescales. The analysis shows that ERA-Interim reproduces more precipitation events than NCEP-2, and these events correspond to an average 8.2% more precipitation. Significant correlations between reanalyses and AWS event sizes are seen at several stations and show that ERA-Interim consistently produces larger precipitation events than NCEP-2.
format Article in Journal/Newspaper
author L. Cohen
S. Dean
author_facet L. Cohen
S. Dean
author_sort L. Cohen
title Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
title_short Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
title_full Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
title_fullStr Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
title_full_unstemmed Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
title_sort snow on the ross ice shelf: comparison of reanalyses and observations from automatic weather stations
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/tc-7-1399-2013
https://doaj.org/article/760b8ff207c842fca62727c0c951e61e
geographic Ross Ice Shelf
geographic_facet Ross Ice Shelf
genre Antarc*
Antarctica
Ice Shelf
Ross Ice Shelf
The Cryosphere
genre_facet Antarc*
Antarctica
Ice Shelf
Ross Ice Shelf
The Cryosphere
op_source The Cryosphere, Vol 7, Iss 5, Pp 1399-1410 (2013)
op_relation http://www.the-cryosphere.net/7/1399/2013/tc-7-1399-2013.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-7-1399-2013
1994-0416
1994-0424
https://doaj.org/article/760b8ff207c842fca62727c0c951e61e
op_doi https://doi.org/10.5194/tc-7-1399-2013
container_title The Cryosphere
container_volume 7
container_issue 5
container_start_page 1399
op_container_end_page 1410
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