Compound Extremes of Air Temperature and Precipitation in Eastern Europe

The spatial distribution of compound extremes of air temperature and precipitation was studied over the territory of Eastern Europe for the period 1950–2018. Using daily data on air temperature and precipitation, we calculated the frequency and trends of the four indices—cold/dry (CD), cold/wet (CW)...

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Published in:Climate
Main Authors: Elena Vyshkvarkova, Olga Sukhonos
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2022
Subjects:
Q
Online Access:https://doi.org/10.3390/cli10090133
https://doaj.org/article/a314775927564d138e7997001295cdbe
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spelling ftdoajarticles:oai:doaj.org/article:a314775927564d138e7997001295cdbe 2023-05-15T17:33:19+02:00 Compound Extremes of Air Temperature and Precipitation in Eastern Europe Elena Vyshkvarkova Olga Sukhonos 2022-09-01T00:00:00Z https://doi.org/10.3390/cli10090133 https://doaj.org/article/a314775927564d138e7997001295cdbe EN eng MDPI AG https://www.mdpi.com/2225-1154/10/9/133 https://doaj.org/toc/2225-1154 doi:10.3390/cli10090133 2225-1154 https://doaj.org/article/a314775927564d138e7997001295cdbe Climate, Vol 10, Iss 133, p 133 (2022) compound extremes temperature precipitation Eastern Europe trends teleconnection patterns Science Q article 2022 ftdoajarticles https://doi.org/10.3390/cli10090133 2022-12-30T19:58:07Z The spatial distribution of compound extremes of air temperature and precipitation was studied over the territory of Eastern Europe for the period 1950–2018. Using daily data on air temperature and precipitation, we calculated the frequency and trends of the four indices—cold/dry (CD), cold/wet (CW), warm/dry (WD) and warm/wet (WW). The connection between these indices and large-scale patterns in the ocean–atmosphere system, such as the North Atlantic Oscillation (NAO), the East Atlantic (EA) and Scandinavia (SCAND) patterns, was also studied. The positive and statistically significant trends in the region were observed for the warm extremes (especially the WW index) in all seasons, with maximum values in the winter season, while negative trends were obtained for the cold extremes. The NAO index has a strong positive and statistically significant correlation with the warm compound indices (WD and WW) in the northern part of Eastern Europe in winter like the EA pattern, but with smaller values. The spatial distribution of the correlation coefficients between compound extremes and the SCAND index in the winter season is opposite to the correlation coefficients with the NAO index. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Climate 10 9 133
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic compound extremes
temperature
precipitation
Eastern Europe
trends
teleconnection patterns
Science
Q
spellingShingle compound extremes
temperature
precipitation
Eastern Europe
trends
teleconnection patterns
Science
Q
Elena Vyshkvarkova
Olga Sukhonos
Compound Extremes of Air Temperature and Precipitation in Eastern Europe
topic_facet compound extremes
temperature
precipitation
Eastern Europe
trends
teleconnection patterns
Science
Q
description The spatial distribution of compound extremes of air temperature and precipitation was studied over the territory of Eastern Europe for the period 1950–2018. Using daily data on air temperature and precipitation, we calculated the frequency and trends of the four indices—cold/dry (CD), cold/wet (CW), warm/dry (WD) and warm/wet (WW). The connection between these indices and large-scale patterns in the ocean–atmosphere system, such as the North Atlantic Oscillation (NAO), the East Atlantic (EA) and Scandinavia (SCAND) patterns, was also studied. The positive and statistically significant trends in the region were observed for the warm extremes (especially the WW index) in all seasons, with maximum values in the winter season, while negative trends were obtained for the cold extremes. The NAO index has a strong positive and statistically significant correlation with the warm compound indices (WD and WW) in the northern part of Eastern Europe in winter like the EA pattern, but with smaller values. The spatial distribution of the correlation coefficients between compound extremes and the SCAND index in the winter season is opposite to the correlation coefficients with the NAO index.
format Article in Journal/Newspaper
author Elena Vyshkvarkova
Olga Sukhonos
author_facet Elena Vyshkvarkova
Olga Sukhonos
author_sort Elena Vyshkvarkova
title Compound Extremes of Air Temperature and Precipitation in Eastern Europe
title_short Compound Extremes of Air Temperature and Precipitation in Eastern Europe
title_full Compound Extremes of Air Temperature and Precipitation in Eastern Europe
title_fullStr Compound Extremes of Air Temperature and Precipitation in Eastern Europe
title_full_unstemmed Compound Extremes of Air Temperature and Precipitation in Eastern Europe
title_sort compound extremes of air temperature and precipitation in eastern europe
publisher MDPI AG
publishDate 2022
url https://doi.org/10.3390/cli10090133
https://doaj.org/article/a314775927564d138e7997001295cdbe
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Climate, Vol 10, Iss 133, p 133 (2022)
op_relation https://www.mdpi.com/2225-1154/10/9/133
https://doaj.org/toc/2225-1154
doi:10.3390/cli10090133
2225-1154
https://doaj.org/article/a314775927564d138e7997001295cdbe
op_doi https://doi.org/10.3390/cli10090133
container_title Climate
container_volume 10
container_issue 9
container_start_page 133
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