Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode

Understanding the linkages between the Arctic and mid-latitudes is important to motivate improvements in the NWP capabilities in the Arctic. Recent studies have suggested that Arctic teleconnections affect the weather of the mid-latitudes on timescales relevant for medium-range weather forecasting....

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Main Author: Day, Jonathan
Format: Lecture
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://doi.org/10.5281/zenodo.3548339
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spelling ftzenodo:oai:zenodo.org:3548339 2024-09-09T19:17:55+00:00 Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode Day, Jonathan 2019-09-10 https://doi.org/10.5281/zenodo.3548339 unknown Zenodo https://zenodo.org/communities/applicate https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.3548338 https://doi.org/10.5281/zenodo.3548339 oai:zenodo.org:3548339 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/lecture 2019 ftzenodo https://doi.org/10.5281/zenodo.354833910.5281/zenodo.3548338 2024-07-25T17:10:51Z Understanding the linkages between the Arctic and mid-latitudes is important to motivate improvements in the NWP capabilities in the Arctic. Recent studies have suggested that Arctic teleconnections affect the weather of the mid-latitudes on timescales relevant for medium-range weather forecasting. In this study, we use several numerical experimentation approaches with a state-of-the-art global opera- tional numerical weather prediction system to investigate this idea further. Focusing on boreal winter, we investigate whether the influence of the Arctic on mid-latitude weather, and the impact of the current Arctic observing system on the skill of medium-range weather forecasts in the mid-latitudes is more pronounced in certain flow regimes. Using so called Observing System Experiments, we demonstrate that removing in-situ or satellite observations from the data assimilation system, used to create the initial conditions for the forecasts, deteriorates mid-latitude synoptic forecast skill in the medium-range, particularly over northern Asia. By looking at the day-to-day variations in the linkages, we find that this deterioration is largest during Scandinavian Blocking episodes. The mechanisms behind the impact is 1) enhanced error growth in the European-Arctic sector of the Atlantic, as a result of increased baroclinicity in the region, and 2) high amplitude planetary waves allow errors to propagate from the Arctic into mid-latitudes. These conclusions are corroborated by numerical experimentation in which the Arctic is relaxed towards the best estimate of the atmospheric state. We also demonstrate that the linkage is enhanced during the Scandinavian blocking regime through a diagnostic analysis spanning several winters of the ERA5 reanalysis and reforecasts. Lecture Arctic Zenodo Arctic
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Understanding the linkages between the Arctic and mid-latitudes is important to motivate improvements in the NWP capabilities in the Arctic. Recent studies have suggested that Arctic teleconnections affect the weather of the mid-latitudes on timescales relevant for medium-range weather forecasting. In this study, we use several numerical experimentation approaches with a state-of-the-art global opera- tional numerical weather prediction system to investigate this idea further. Focusing on boreal winter, we investigate whether the influence of the Arctic on mid-latitude weather, and the impact of the current Arctic observing system on the skill of medium-range weather forecasts in the mid-latitudes is more pronounced in certain flow regimes. Using so called Observing System Experiments, we demonstrate that removing in-situ or satellite observations from the data assimilation system, used to create the initial conditions for the forecasts, deteriorates mid-latitude synoptic forecast skill in the medium-range, particularly over northern Asia. By looking at the day-to-day variations in the linkages, we find that this deterioration is largest during Scandinavian Blocking episodes. The mechanisms behind the impact is 1) enhanced error growth in the European-Arctic sector of the Atlantic, as a result of increased baroclinicity in the region, and 2) high amplitude planetary waves allow errors to propagate from the Arctic into mid-latitudes. These conclusions are corroborated by numerical experimentation in which the Arctic is relaxed towards the best estimate of the atmospheric state. We also demonstrate that the linkage is enhanced during the Scandinavian blocking regime through a diagnostic analysis spanning several winters of the ERA5 reanalysis and reforecasts.
format Lecture
author Day, Jonathan
spellingShingle Day, Jonathan
Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
author_facet Day, Jonathan
author_sort Day, Jonathan
title Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
title_short Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
title_full Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
title_fullStr Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
title_full_unstemmed Increased Arctic influence on the mid-latitude flow during Scandinavian Blocking episode
title_sort increased arctic influence on the mid-latitude flow during scandinavian blocking episode
publisher Zenodo
publishDate 2019
url https://doi.org/10.5281/zenodo.3548339
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation https://zenodo.org/communities/applicate
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https://doi.org/10.5281/zenodo.3548338
https://doi.org/10.5281/zenodo.3548339
oai:zenodo.org:3548339
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.354833910.5281/zenodo.3548338
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