2022
Long-term changes in drought indices in eastern and central Europe
JAAGUS, Jaak; Anto AASA; Svetlana ANISKEVICH; Boris BOINCEAN; Roxana BOJARIU et. al.Basic information
Original name
Long-term changes in drought indices in eastern and central Europe
Authors
JAAGUS, Jaak (233 Estonia); Anto AASA (233 Estonia); Svetlana ANISKEVICH (428 Latvia); Boris BOINCEAN (498 Republic of Moldova); Roxana BOJARIU (642 Romania); Agrita BRIEDE (428 Latvia); Irina DANILOVICH (112 Belarus); Fernando Dominguez CASTRO (724 Spain); Alexandru DUMITRESCU (642 Romania); Martin LABUDA (703 Slovakia); Lívia LABUDOVÁ (703 Slovakia); Krista LÕHMUS (233 Estonia); Viktar MELNIK (112 Belarus); Kiira MÕISJA (233 Estonia); Rita PONGRACZ (348 Hungary); Vera POTOPOVÁ (203 Czech Republic); Ladislava ŘEZNÍČKOVÁ (203 Czech Republic, guarantor, belonging to the institution); Egidijus RIMKUS (440 Lithuania); Inna SEMENOVA (804 Ukraine); Edvinas STONEVIČIUS (440 Lithuania); Petr ŠTĚPÁNEK (203 Czech Republic); Miroslav TRNKA (203 Czech Republic); Sergio M VICENTE-SERRANO (724 Spain); Joanna WIBIG (616 Poland) and Pavel ZAHRADNÍČEK (203 Czech Republic)
Edition
International Journal of Climatology, Wiley, 2022, 0899-8418
Other information
Language
English
Type of outcome
Article in a journal
Field of Study
10509 Meteorology and atmospheric sciences
Country of publisher
United States of America
Confidentiality degree
is not subject to a state or trade secret
References:
Impact factor
Impact factor: 3.900
RIV identification code
RIV/00216224:14310/22:00124951
Organization unit
Faculty of Science
UT WoS
000665698900001
EID Scopus
2-s2.0-85108430611
Keywords in English
atmospheric evaporative demand; central and eastern Europe; drought; SPEI; SPI; trend analysis
Tags
Tags
International impact, Reviewed
Changed: 18/1/2022 17:04, Mgr. Marie Novosadová Šípková, DiS.
Abstract
In the original language
This study analyses long-term changes in drought indices (Standardised Precipitation Index—SPI, Standardised Precipitation–Evapotranspiration Index—SPEI) at 1 and 3 months scales at 182 stations in 11 central and eastern European countries during 1949–2018. For comparative purposes, the necessary atmospheric evaporative demand (AED) to obtain SPEI was calculated using two methods, Hargreaves-Samani (SPEIH) and Penman-Monteith (SPEIP). The results show some relevant changes and tendencies in the drought indices. Statistically significant increase in SPI and SPEI during the cold season (November–March), reflecting precipitation increase, was found in the northern part of the study region, in Estonia, Latvia, Lithuania, northern Belarus and northern Poland. In the rest of study domain, a weak and mostly insignificant decrease prevailed in winter. Summer season (June–August) is characterized by changes in the opposite sign. An increase was observed in the north, while a clear decrease in SPEI, reflecting a drying trend, was typical for the southern regions: the Czech Republic, Slovakia, Hungary, Romania, Moldova and southern Poland. A general drying tendency revealed also in April, which was statistically significant over a wide area in the Czech Republic and Poland. Increasing trends in SPI and SPEI for September and October were detected in Romania, Moldova and Hungary. The use of SPEI instead of SPI generally enhances drying trends.