Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes

Precipitation on Svalbard can generally be linked to the atmospheric circulation in the Northern Atlantic. Using an automated circulation type classification, we show that weather type statistics are well represented in the Max Planck Institute Earth System Model at base resolution (MPI-ESM-LR). For...

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Published in:Atmosphere
Main Authors: Andreas Dobler, Julia Lutz, Oskar Landgren, Jan Erik Haugen
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11121378
https://doaj.org/article/0f6a9fdad216430396837907e26fa4e2
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spelling ftdoajarticles:oai:doaj.org/article:0f6a9fdad216430396837907e26fa4e2 2023-05-15T18:29:21+02:00 Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes Andreas Dobler Julia Lutz Oskar Landgren Jan Erik Haugen 2020-12-01T00:00:00Z https://doi.org/10.3390/atmos11121378 https://doaj.org/article/0f6a9fdad216430396837907e26fa4e2 EN eng MDPI AG https://www.mdpi.com/2073-4433/11/12/1378 https://doaj.org/toc/2073-4433 doi:10.3390/atmos11121378 2073-4433 https://doaj.org/article/0f6a9fdad216430396837907e26fa4e2 Atmosphere, Vol 11, Iss 1378, p 1378 (2020) convection permitting climate modelling COSMO-CLM Svalbard precipitation integrated water vapour projections Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.3390/atmos11121378 2022-12-31T04:52:04Z Precipitation on Svalbard can generally be linked to the atmospheric circulation in the Northern Atlantic. Using an automated circulation type classification, we show that weather type statistics are well represented in the Max Planck Institute Earth System Model at base resolution (MPI-ESM-LR). For a future climate projection following the Representative Concentration Pathway scenario RCP8.5, we find only small changes in the statistics. However, convection permitting simulations with the regional climate model from the Consortium for Small-scale Modeling in climate mode (COSMO-CLM) covering Svalbard at 2.5 km demonstrate an increase in precipitation for all seasons. About 74% of the increase are coming from changes under cyclonic weather situations. The precipitation changes are strongly related to differences in atmospheric conditions, while the contribution from the frequencies of weather types is small. Observations on Svalbard suggest that the general weather situation favouring heavy precipitation events is a strong south-southwesterly flow with advection of water vapour from warmer areas. This is reproduced by the COSMO-CLM simulations. In the future projections, the maximum daily precipitation amounts are further increasing. At the same time, weather types with less moisture advection towards Svalbard are becoming more important. Article in Journal/Newspaper Svalbard Directory of Open Access Journals: DOAJ Articles Svalbard Atmosphere 11 12 1378
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic convection permitting climate modelling
COSMO-CLM
Svalbard
precipitation
integrated water vapour
projections
Meteorology. Climatology
QC851-999
spellingShingle convection permitting climate modelling
COSMO-CLM
Svalbard
precipitation
integrated water vapour
projections
Meteorology. Climatology
QC851-999
Andreas Dobler
Julia Lutz
Oskar Landgren
Jan Erik Haugen
Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
topic_facet convection permitting climate modelling
COSMO-CLM
Svalbard
precipitation
integrated water vapour
projections
Meteorology. Climatology
QC851-999
description Precipitation on Svalbard can generally be linked to the atmospheric circulation in the Northern Atlantic. Using an automated circulation type classification, we show that weather type statistics are well represented in the Max Planck Institute Earth System Model at base resolution (MPI-ESM-LR). For a future climate projection following the Representative Concentration Pathway scenario RCP8.5, we find only small changes in the statistics. However, convection permitting simulations with the regional climate model from the Consortium for Small-scale Modeling in climate mode (COSMO-CLM) covering Svalbard at 2.5 km demonstrate an increase in precipitation for all seasons. About 74% of the increase are coming from changes under cyclonic weather situations. The precipitation changes are strongly related to differences in atmospheric conditions, while the contribution from the frequencies of weather types is small. Observations on Svalbard suggest that the general weather situation favouring heavy precipitation events is a strong south-southwesterly flow with advection of water vapour from warmer areas. This is reproduced by the COSMO-CLM simulations. In the future projections, the maximum daily precipitation amounts are further increasing. At the same time, weather types with less moisture advection towards Svalbard are becoming more important.
format Article in Journal/Newspaper
author Andreas Dobler
Julia Lutz
Oskar Landgren
Jan Erik Haugen
author_facet Andreas Dobler
Julia Lutz
Oskar Landgren
Jan Erik Haugen
author_sort Andreas Dobler
title Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
title_short Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
title_full Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
title_fullStr Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
title_full_unstemmed Circulation Specific Precipitation Patterns over Svalbard and Projected Future Changes
title_sort circulation specific precipitation patterns over svalbard and projected future changes
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/atmos11121378
https://doaj.org/article/0f6a9fdad216430396837907e26fa4e2
geographic Svalbard
geographic_facet Svalbard
genre Svalbard
genre_facet Svalbard
op_source Atmosphere, Vol 11, Iss 1378, p 1378 (2020)
op_relation https://www.mdpi.com/2073-4433/11/12/1378
https://doaj.org/toc/2073-4433
doi:10.3390/atmos11121378
2073-4433
https://doaj.org/article/0f6a9fdad216430396837907e26fa4e2
op_doi https://doi.org/10.3390/atmos11121378
container_title Atmosphere
container_volume 11
container_issue 12
container_start_page 1378
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