Variability of Extreme Temperature in the Arctic - Observation and RCM

This paper discusses results of a simulation with the regional climate model HIRHAM for 1958-2001, driven by the ECMWF reanalysis (ERA40) data over the Arctic domain. The aim is to analyze the ability of the model to capture certain features of climate extremes derived from daily mean, maximum and m...

Full description

Bibliographic Details
Published in:The Open Atmospheric Science Journal
Main Authors: Matthes, Heidrun, Rinke, Annette, Dethloff, Klaus
Format: Article in Journal/Newspaper
Language:English
Published: Bentham Science Publishers Ltd. 2010
Subjects:
Online Access:http://dx.doi.org/10.2174/1874282301004010126
https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.pdf
https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.xml
id crbenthamsciepub:10.2174/1874282301004010126
record_format openpolar
spelling crbenthamsciepub:10.2174/1874282301004010126 2023-11-05T03:39:00+01:00 Variability of Extreme Temperature in the Arctic - Observation and RCM Matthes, Heidrun Rinke, Annette Dethloff, Klaus 2010 http://dx.doi.org/10.2174/1874282301004010126 https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.pdf https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.xml en eng Bentham Science Publishers Ltd. https://creativecommons.org/licenses/by/4.0/legalcode The Open Atmospheric Science Journal volume 4, issue 1, page 126-136 ISSN 1874-2823 Atmospheric Science journal-article 2010 crbenthamsciepub https://doi.org/10.2174/1874282301004010126 2023-10-09T16:43:47Z This paper discusses results of a simulation with the regional climate model HIRHAM for 1958-2001, driven by the ECMWF reanalysis (ERA40) data over the Arctic domain. The aim is to analyze the ability of the model to capture certain features of climate extremes derived from daily mean, maximum and minimum temperatures. For this purpose, a range of climate indices (frost days, cold and warm spell days, growing degree days and growing season length) was calculated from the model output as well as from ERA40 data and region-specific station data for Eastern and Western Russian Arctic for comparison. It is demonstrated that the model captures the main features in the spatial distribution and temporal development of most indices well. Though systematic deviations in the seasonal means occur in various indices (frost days, growing degree days), variability and trends are well reproduced. Seasonal mean patterns in frost days are reproduced best, though the model persistently calculates too many frost days. Seasonal means of cold and warm spell days are reproduced without systematic biases, though deviations occur in summer for cold spells and in spring and summer for warm spells due to an early spring warming in the regional climate model and a low variability of the daily maximum temperature over sea ice. Article in Journal/Newspaper Arctic Sea ice Bentham Science Publishers (via Crossref) The Open Atmospheric Science Journal 4 1 126 136
institution Open Polar
collection Bentham Science Publishers (via Crossref)
op_collection_id crbenthamsciepub
language English
topic Atmospheric Science
spellingShingle Atmospheric Science
Matthes, Heidrun
Rinke, Annette
Dethloff, Klaus
Variability of Extreme Temperature in the Arctic - Observation and RCM
topic_facet Atmospheric Science
description This paper discusses results of a simulation with the regional climate model HIRHAM for 1958-2001, driven by the ECMWF reanalysis (ERA40) data over the Arctic domain. The aim is to analyze the ability of the model to capture certain features of climate extremes derived from daily mean, maximum and minimum temperatures. For this purpose, a range of climate indices (frost days, cold and warm spell days, growing degree days and growing season length) was calculated from the model output as well as from ERA40 data and region-specific station data for Eastern and Western Russian Arctic for comparison. It is demonstrated that the model captures the main features in the spatial distribution and temporal development of most indices well. Though systematic deviations in the seasonal means occur in various indices (frost days, growing degree days), variability and trends are well reproduced. Seasonal mean patterns in frost days are reproduced best, though the model persistently calculates too many frost days. Seasonal means of cold and warm spell days are reproduced without systematic biases, though deviations occur in summer for cold spells and in spring and summer for warm spells due to an early spring warming in the regional climate model and a low variability of the daily maximum temperature over sea ice.
format Article in Journal/Newspaper
author Matthes, Heidrun
Rinke, Annette
Dethloff, Klaus
author_facet Matthes, Heidrun
Rinke, Annette
Dethloff, Klaus
author_sort Matthes, Heidrun
title Variability of Extreme Temperature in the Arctic - Observation and RCM
title_short Variability of Extreme Temperature in the Arctic - Observation and RCM
title_full Variability of Extreme Temperature in the Arctic - Observation and RCM
title_fullStr Variability of Extreme Temperature in the Arctic - Observation and RCM
title_full_unstemmed Variability of Extreme Temperature in the Arctic - Observation and RCM
title_sort variability of extreme temperature in the arctic - observation and rcm
publisher Bentham Science Publishers Ltd.
publishDate 2010
url http://dx.doi.org/10.2174/1874282301004010126
https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.pdf
https://openatmosphericsciencejournal.com/contents/volumes/V4/TOASCJ-4-126/TOASCJ-4-126.xml
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source The Open Atmospheric Science Journal
volume 4, issue 1, page 126-136
ISSN 1874-2823
op_rights https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.2174/1874282301004010126
container_title The Open Atmospheric Science Journal
container_volume 4
container_issue 1
container_start_page 126
op_container_end_page 136
_version_ 1781694792212676608