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
Main Authors: L. Cohen, S. Dean
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/7/1399/2013/tc-7-1399-2013.pdf
id doaj-760b8ff207c842fca62727c0c951e61e
record_format Article
spelling doaj-760b8ff207c842fca62727c0c951e61e2020-11-24T21:10:24ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242013-09-01751399141010.5194/tc-7-1399-2013Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stationsL. CohenS. DeanSnow 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.http://www.the-cryosphere.net/7/1399/2013/tc-7-1399-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Cohen
S. Dean
spellingShingle L. Cohen
S. Dean
Snow on the Ross Ice Shelf: comparison of reanalyses and observations from automatic weather stations
The Cryosphere
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
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2013-09-01
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.
url http://www.the-cryosphere.net/7/1399/2013/tc-7-1399-2013.pdf
work_keys_str_mv AT lcohen snowontherossiceshelfcomparisonofreanalysesandobservationsfromautomaticweatherstations
AT sdean snowontherossiceshelfcomparisonofreanalysesandobservationsfromautomaticweatherstations
_version_ 1716756623001649152