Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation

Diverse and severe weather conditions and rapid climate change rates in the Arctic emphasize the need for high-resolution climatic and environmental data that cannot be obtained from the scarce observational networks. This study presents a new detailed hydrometeorological dataset for the Russian Arc...

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Published in:Atmosphere
Main Authors: Vladimir Platonov, Mikhail Varentsov
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12030350
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/3/350/ 2023-08-20T04:03:55+02:00 Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation Vladimir Platonov Mikhail Varentsov agris 2021-03-08 application/pdf https://doi.org/10.3390/atmos12030350 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos12030350 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 3; Pages: 350 COSMO-CLM COSMO regional climate modeling Arctic climate extreme climate statistics verification hindcast long-term hydrometeorological dataset Text 2021 ftmdpi https://doi.org/10.3390/atmos12030350 2023-08-01T01:13:48Z Diverse and severe weather conditions and rapid climate change rates in the Arctic emphasize the need for high-resolution climatic and environmental data that cannot be obtained from the scarce observational networks. This study presents a new detailed hydrometeorological dataset for the Russian Arctic region, obtained as a long-term hindcast with the nonhydrostatic atmospheric model COSMO-CLM for the 1980–2016 period. The modeling workflow, evaluation techniques, and preliminary analysis of the obtained dataset are discussed. The model domain included the Barents, Kara, and Laptev Seas with ≈12-km grid spacing. The optimal model setup was chosen based on preliminary simulations for several summer and winter periods with varied options, and included the usage of ERA-Interim reanalysis data as forcing data, the new model version 5.05 with so-called ICON-based physics, and a spectral nudging technique. The wind speed and temperature climatology in the new COSMO-CLM dataset closely agreed with the ERA-Interim reanalysis, but with detailed spatial patterns. The added value of the higher-resolution COSMO-CLM data with respect to the ERA-Interim was most pronounced for higher wind speeds during downslope windstorms with the influence of mountain ranges on the temperature patterns, including surface temperature inversions. The potential applications and plans of further product development are also discussed. Text Arctic Climate change laptev MDPI Open Access Publishing Arctic Atmosphere 12 3 350
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic COSMO-CLM
COSMO
regional climate modeling
Arctic climate
extreme climate statistics
verification
hindcast
long-term hydrometeorological dataset
spellingShingle COSMO-CLM
COSMO
regional climate modeling
Arctic climate
extreme climate statistics
verification
hindcast
long-term hydrometeorological dataset
Vladimir Platonov
Mikhail Varentsov
Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
topic_facet COSMO-CLM
COSMO
regional climate modeling
Arctic climate
extreme climate statistics
verification
hindcast
long-term hydrometeorological dataset
description Diverse and severe weather conditions and rapid climate change rates in the Arctic emphasize the need for high-resolution climatic and environmental data that cannot be obtained from the scarce observational networks. This study presents a new detailed hydrometeorological dataset for the Russian Arctic region, obtained as a long-term hindcast with the nonhydrostatic atmospheric model COSMO-CLM for the 1980–2016 period. The modeling workflow, evaluation techniques, and preliminary analysis of the obtained dataset are discussed. The model domain included the Barents, Kara, and Laptev Seas with ≈12-km grid spacing. The optimal model setup was chosen based on preliminary simulations for several summer and winter periods with varied options, and included the usage of ERA-Interim reanalysis data as forcing data, the new model version 5.05 with so-called ICON-based physics, and a spectral nudging technique. The wind speed and temperature climatology in the new COSMO-CLM dataset closely agreed with the ERA-Interim reanalysis, but with detailed spatial patterns. The added value of the higher-resolution COSMO-CLM data with respect to the ERA-Interim was most pronounced for higher wind speeds during downslope windstorms with the influence of mountain ranges on the temperature patterns, including surface temperature inversions. The potential applications and plans of further product development are also discussed.
format Text
author Vladimir Platonov
Mikhail Varentsov
author_facet Vladimir Platonov
Mikhail Varentsov
author_sort Vladimir Platonov
title Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
title_short Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
title_full Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
title_fullStr Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
title_full_unstemmed Introducing a New Detailed Long-Term COSMO-CLM Hindcast for the Russian Arctic and the First Results of Its Evaluation
title_sort introducing a new detailed long-term cosmo-clm hindcast for the russian arctic and the first results of its evaluation
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12030350
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
laptev
genre_facet Arctic
Climate change
laptev
op_source Atmosphere; Volume 12; Issue 3; Pages: 350
op_relation Climatology
https://dx.doi.org/10.3390/atmos12030350
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12030350
container_title Atmosphere
container_volume 12
container_issue 3
container_start_page 350
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