Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data

ERA-Interim reanalysis data and data of the Hadley Centre Global Environmental Model version 2 (HadGEM2) are compared with continuous meteorological observations of near-surface wind and temperature carried out for more than 30 years at Neumayer station, situated on the Ekström Ice Shelf of Antarct...

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Main Authors: Milan Klöwer, Thomas Jung, Gert König-Langlo, Tido Semmler
Format: Article
Language:English
Published: Borntraeger 2013-12-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/0941-2948/2013/0505
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spelling doaj-845f957c20fd49bc9ed51bf228eb0edd2020-11-24T22:30:24ZengBorntraegerMeteorologische Zeitschrift0941-29482013-12-0122669970910.1127/0941-2948/2013/050582077Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model dataMilan KlöwerThomas JungGert König-LangloTido SemmlerERA-Interim reanalysis data and data of the Hadley Centre Global Environmental Model version 2 (HadGEM2) are compared with continuous meteorological observations of near-surface wind and temperature carried out for more than 30 years at Neumayer station, situated on the Ekström Ice Shelf of Antarctica. Significant temperature correlations between Neumayer climate and the climate of both the interior of the Antarctic continent and oceanic regions north of Neumayer are investigated using observational data and model data. Mean sea level pressure fluctuations at Neumayer can be connected to changes in the Southern Annular Mode (SAM). Shortcomings in the ERA-Interim reanalysis data with spurious trends of up to 7 °C over 31 years are identified at several places in Antarctica. Furthermore, it is shown that katabatic winds in both the ERA-Interim reanalysis data and in the HadGEM2 climate model are underrepresented in frequency and speed, presumably due to the problems in representing topography in these relatively coarse resolution models. This may be one reason for the positive 2m air temperature bias of 3 °C in the models at Neumayer station. The results of this study reemphasize that climatic trends in regions with a low station density can not be assessed solely from model data. Thus, it is absolutely necessary to maintain polar observatories such as Neumayer station to quantify climate change over the Southern Ocean and Antarctica.http://dx.doi.org/10.1127/0941-2948/2013/0505antarcticaclimate modelkatabatic windsneumayerobservationsreanalysissouthern annular mode
collection DOAJ
language English
format Article
sources DOAJ
author Milan Klöwer
Thomas Jung
Gert König-Langlo
Tido Semmler
spellingShingle Milan Klöwer
Thomas Jung
Gert König-Langlo
Tido Semmler
Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
Meteorologische Zeitschrift
antarctica
climate model
katabatic winds
neumayer
observations
reanalysis
southern annular mode
author_facet Milan Klöwer
Thomas Jung
Gert König-Langlo
Tido Semmler
author_sort Milan Klöwer
title Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
title_short Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
title_full Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
title_fullStr Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
title_full_unstemmed Aspects of weather parameters at Neumayer station, Antarctica, and their representation in reanalysis and climate model data
title_sort aspects of weather parameters at neumayer station, antarctica, and their representation in reanalysis and climate model data
publisher Borntraeger
series Meteorologische Zeitschrift
issn 0941-2948
publishDate 2013-12-01
description ERA-Interim reanalysis data and data of the Hadley Centre Global Environmental Model version 2 (HadGEM2) are compared with continuous meteorological observations of near-surface wind and temperature carried out for more than 30 years at Neumayer station, situated on the Ekström Ice Shelf of Antarctica. Significant temperature correlations between Neumayer climate and the climate of both the interior of the Antarctic continent and oceanic regions north of Neumayer are investigated using observational data and model data. Mean sea level pressure fluctuations at Neumayer can be connected to changes in the Southern Annular Mode (SAM). Shortcomings in the ERA-Interim reanalysis data with spurious trends of up to 7 °C over 31 years are identified at several places in Antarctica. Furthermore, it is shown that katabatic winds in both the ERA-Interim reanalysis data and in the HadGEM2 climate model are underrepresented in frequency and speed, presumably due to the problems in representing topography in these relatively coarse resolution models. This may be one reason for the positive 2m air temperature bias of 3 °C in the models at Neumayer station. The results of this study reemphasize that climatic trends in regions with a low station density can not be assessed solely from model data. Thus, it is absolutely necessary to maintain polar observatories such as Neumayer station to quantify climate change over the Southern Ocean and Antarctica.
topic antarctica
climate model
katabatic winds
neumayer
observations
reanalysis
southern annular mode
url http://dx.doi.org/10.1127/0941-2948/2013/0505
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