Studying Summer Season Drought in Western Russia

During the 2010 summer, a severe drought impacted Western Russia, including regions surrounding Moscow and Belgorod (about 700 km south of Moscow). The drought was accompanied by high temperatures. Moscow recorded 37.8°C (100°F) for the first time in over 130 years of record keeping. The record heat...

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Main Authors: Anthony R. Lupo, Igor I. Mokhov, Yury G. Chendev, Maria G. Lebedeva, Mirseid Akperov, Jason A. Hubbart
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2014/942027
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author Anthony R. Lupo
Igor I. Mokhov
Yury G. Chendev
Maria G. Lebedeva
Mirseid Akperov
Jason A. Hubbart
author_facet Anthony R. Lupo
Igor I. Mokhov
Yury G. Chendev
Maria G. Lebedeva
Mirseid Akperov
Jason A. Hubbart
author_sort Anthony R. Lupo
collection DOAJ
description During the 2010 summer, a severe drought impacted Western Russia, including regions surrounding Moscow and Belgorod (about 700 km south of Moscow). The drought was accompanied by high temperatures. Moscow recorded 37.8°C (100°F) for the first time in over 130 years of record keeping. The record heat, high humidity, dry weather, and smoke from forest fires caused increased human mortality rates in the Moscow region during the summer. The excessive heat and humidity in Western Russia were the result of atmospheric blocking from June through mid-August. The NCAR-NCEP reanalyses were used to examine blocking in the Eastern European and Western Russia sector during the spring and summer seasons from 1970 to 2012. We found that drier years were correlated with stronger and more persistent blocking during the spring and summer seasons. During these years, the Moscow region was drier in the summer and Belgorod during the spring seasons. In the Moscow region, the drier summers were correlated with transitions from El Niño to La Niña, but the opposite was true in the Belgorod region. Synoptic flow regimes were then analyzed and support the contention that dry years are associated with more blocking and El Niño transitions.
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spelling doaj-art-c287abc0fa9e4a42bd9ee293143d75e52025-02-03T05:49:37ZengWileyAdvances in Meteorology1687-93091687-93172014-01-01201410.1155/2014/942027942027Studying Summer Season Drought in Western RussiaAnthony R. Lupo0Igor I. Mokhov1Yury G. Chendev2Maria G. Lebedeva3Mirseid Akperov4Jason A. Hubbart5Department of Soil, Environmental, and Atmospheric Science, 302 E Anheuser Busch Natural Resources Building, University of Missouri-Columbia, Columbia, MO 65211, USAA.M. Obukhov Inst. of Atmospheric Physics, Russian Academy of Sciences, 3 Pyzhevsky, Moscow 119017, RussiaNatural Resources Management and Land Cadastre (Yu. Chendev), Faculty of Mining and Natural Resources Management, 85 Pobeda Street Building No. 14, Floor 2, Room 2-11, Belgorod 308015, RussiaNatural Resources Management and Land Cadastre (Yu. Chendev), Faculty of Mining and Natural Resources Management, 85 Pobeda Street Building No. 14, Floor 2, Room 2-11, Belgorod 308015, RussiaA.M. Obukhov Inst. of Atmospheric Physics, Russian Academy of Sciences, 3 Pyzhevsky, Moscow 119017, RussiaDepartment of Soil, Environmental, and Atmospheric Science, 302 E Anheuser Busch Natural Resources Building, University of Missouri-Columbia, Columbia, MO 65211, USADuring the 2010 summer, a severe drought impacted Western Russia, including regions surrounding Moscow and Belgorod (about 700 km south of Moscow). The drought was accompanied by high temperatures. Moscow recorded 37.8°C (100°F) for the first time in over 130 years of record keeping. The record heat, high humidity, dry weather, and smoke from forest fires caused increased human mortality rates in the Moscow region during the summer. The excessive heat and humidity in Western Russia were the result of atmospheric blocking from June through mid-August. The NCAR-NCEP reanalyses were used to examine blocking in the Eastern European and Western Russia sector during the spring and summer seasons from 1970 to 2012. We found that drier years were correlated with stronger and more persistent blocking during the spring and summer seasons. During these years, the Moscow region was drier in the summer and Belgorod during the spring seasons. In the Moscow region, the drier summers were correlated with transitions from El Niño to La Niña, but the opposite was true in the Belgorod region. Synoptic flow regimes were then analyzed and support the contention that dry years are associated with more blocking and El Niño transitions.http://dx.doi.org/10.1155/2014/942027
spellingShingle Anthony R. Lupo
Igor I. Mokhov
Yury G. Chendev
Maria G. Lebedeva
Mirseid Akperov
Jason A. Hubbart
Studying Summer Season Drought in Western Russia
Advances in Meteorology
title Studying Summer Season Drought in Western Russia
title_full Studying Summer Season Drought in Western Russia
title_fullStr Studying Summer Season Drought in Western Russia
title_full_unstemmed Studying Summer Season Drought in Western Russia
title_short Studying Summer Season Drought in Western Russia
title_sort studying summer season drought in western russia
url http://dx.doi.org/10.1155/2014/942027
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