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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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 |
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Open Polar |
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MDPI Open Access Publishing |
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ftmdpi |
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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 |
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133 |
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1774720613955403776 |