WRF-data analysis at Svalbard 1989-2010
A polaroptimized mesoscale climate model, Polar Weather Research and Forcasting model (WRF), has been used over the Svalbard archipelago for analysing last trends in climate. The climate model has been downscaled by the reanalysis model ERA-Interim to 8 km spatial resolution for the period 1989-2010...
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Uppsala universitet, Institutionen för geovetenskaper
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ndltd-UPSALLA1-oai-DiVA.org-uu-2388122015-11-25T04:54:33ZWRF-data analysis at Svalbard 1989-2010engJörpeland, JonUppsala universitet, Institutionen för geovetenskaper2014A polaroptimized mesoscale climate model, Polar Weather Research and Forcasting model (WRF), has been used over the Svalbard archipelago for analysing last trends in climate. The climate model has been downscaled by the reanalysis model ERA-Interim to 8 km spatial resolution for the period 1989-2010. Annual and seasonal trends for three sites, scattered across the archipelago, were analyzed for three meteorological parameters, temperature, precipitation and wind. An additional lapse rate were calculated for two glaciers at Nordaustlandet. The analyze shows that the Polar-WRF model suggest an significance temperature increase by 0.67-0.82oC. However, changes in precipitation and wind are harder to prove. The calculated annual lapse rate at Nordaustlandet shows an temperature decrease by 4.2-4.6oC. Student thesisinfo:eu-repo/semantics/bachelorThesistexthttp://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-238812Självständigt arbete ; 112application/pdfinfo:eu-repo/semantics/openAccess |
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NDLTD |
language |
English |
format |
Others
|
sources |
NDLTD |
description |
A polaroptimized mesoscale climate model, Polar Weather Research and Forcasting model (WRF), has been used over the Svalbard archipelago for analysing last trends in climate. The climate model has been downscaled by the reanalysis model ERA-Interim to 8 km spatial resolution for the period 1989-2010. Annual and seasonal trends for three sites, scattered across the archipelago, were analyzed for three meteorological parameters, temperature, precipitation and wind. An additional lapse rate were calculated for two glaciers at Nordaustlandet. The analyze shows that the Polar-WRF model suggest an significance temperature increase by 0.67-0.82oC. However, changes in precipitation and wind are harder to prove. The calculated annual lapse rate at Nordaustlandet shows an temperature decrease by 4.2-4.6oC. |
author |
Jörpeland, Jon |
spellingShingle |
Jörpeland, Jon WRF-data analysis at Svalbard 1989-2010 |
author_facet |
Jörpeland, Jon |
author_sort |
Jörpeland, Jon |
title |
WRF-data analysis at Svalbard 1989-2010 |
title_short |
WRF-data analysis at Svalbard 1989-2010 |
title_full |
WRF-data analysis at Svalbard 1989-2010 |
title_fullStr |
WRF-data analysis at Svalbard 1989-2010 |
title_full_unstemmed |
WRF-data analysis at Svalbard 1989-2010 |
title_sort |
wrf-data analysis at svalbard 1989-2010 |
publisher |
Uppsala universitet, Institutionen för geovetenskaper |
publishDate |
2014 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-238812 |
work_keys_str_mv |
AT jorpelandjon wrfdataanalysisatsvalbard19892010 |
_version_ |
1718136699883618304 |