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: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/cli10090133
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spelling ftmdpi:oai:mdpi.com:/2225-1154/10/9/133/ 2023-08-20T04:08:23+02:00 Compound Extremes of Air Temperature and Precipitation in Eastern Europe Elena Vyshkvarkova Olga Sukhonos agris 2022-09-05 application/pdf https://doi.org/10.3390/cli10090133 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/cli10090133 https://creativecommons.org/licenses/by/4.0/ Climate; Volume 10; Issue 9; Pages: 133 compound extremes temperature precipitation Eastern Europe trends teleconnection patterns Text 2022 ftmdpi https://doi.org/10.3390/cli10090133 2023-08-01T06:21:34Z 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. Text North Atlantic North Atlantic oscillation MDPI Open Access Publishing Climate 10 9 133
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic compound extremes
temperature
precipitation
Eastern Europe
trends
teleconnection patterns
spellingShingle compound extremes
temperature
precipitation
Eastern Europe
trends
teleconnection patterns
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/cli10090133
op_coverage agris
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Climate; Volume 10; Issue 9; Pages: 133
op_relation https://dx.doi.org/10.3390/cli10090133
op_rights https://creativecommons.org/licenses/by/4.0/
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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