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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: Cohen, L., Dean, S.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-7-1399-2013
https://tc.copernicus.org/articles/7/1399/2013/
id ftcopernicus:oai:publications.copernicus.org:tc19382
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:tc19382 2023-05-15T13:54:27+02:00 Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations Cohen, L. Dean, S. 2018-09-27 application/pdf https://doi.org/10.5194/tc-7-1399-2013 https://tc.copernicus.org/articles/7/1399/2013/ eng eng doi:10.5194/tc-7-1399-2013 https://tc.copernicus.org/articles/7/1399/2013/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-7-1399-2013 2020-07-20T16:25:21Z 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. Text Antarc* Antarctica Ice Shelf Ross Ice Shelf Copernicus Publications: E-Journals Ross Ice Shelf The Cryosphere 7 5 1399 1410
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
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 Text
author Cohen, L.
Dean, S.
spellingShingle Cohen, L.
Dean, S.
Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
author_facet Cohen, L.
Dean, S.
author_sort Cohen, L.
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
publishDate 2018
url https://doi.org/10.5194/tc-7-1399-2013
https://tc.copernicus.org/articles/7/1399/2013/
geographic Ross Ice Shelf
geographic_facet Ross Ice Shelf
genre Antarc*
Antarctica
Ice Shelf
Ross Ice Shelf
genre_facet Antarc*
Antarctica
Ice Shelf
Ross Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-7-1399-2013
https://tc.copernicus.org/articles/7/1399/2013/
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
_version_ 1766260374568435712