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Processes in GeoMedia—Volume VITrends in Barents and Kara Sea Areas from Reanalysis Data

Processes in GeoMedia—Volume VI: Trends in Barents and Kara Sea Areas from Reanalysis Data [In the work, the change of number of the extreme winds, turbulent stresses and heat fluxes in the Arctic zone are studied using the reanalysis data Arctic System Reanalysis version 2 (ASRv2) in the period 2000–2016. A decrease in the number of extreme winds in the central and western part of the Barents Sea and an increase in the coastal area and in the northern part of the Barents Sea and in the Kara Sea according to the obtained maps for the tilt angle of linear trends is observed. It is shown that the main contribution to the change in the number of occurrences of extreme winds is made by the winter season.] http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png

Processes in GeoMedia—Volume VITrends in Barents and Kara Sea Areas from Reanalysis Data

Part of the Springer Geology Book Series
Editors: Chaplina, Tatiana

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Publisher
Springer International Publishing
Copyright
© The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerland AG 2023
ISBN
978-3-031-16574-0
Pages
73 –77
DOI
10.1007/978-3-031-16575-7_8
Publisher site
See Chapter on Publisher Site

Abstract

[In the work, the change of number of the extreme winds, turbulent stresses and heat fluxes in the Arctic zone are studied using the reanalysis data Arctic System Reanalysis version 2 (ASRv2) in the period 2000–2016. A decrease in the number of extreme winds in the central and western part of the Barents Sea and an increase in the coastal area and in the northern part of the Barents Sea and in the Kara Sea according to the obtained maps for the tilt angle of linear trends is observed. It is shown that the main contribution to the change in the number of occurrences of extreme winds is made by the winter season.]

Published: Jan 1, 2023

Keywords: Reanalysis; Polar low; Extreme winds; Turbulent stress; Heat fluxes; Barents Sea

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