Atmospheric Circulation as a Factor Contributing to Increasing Drought Severity in Central Europe
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F20%3A00532371" target="_blank" >RIV/68378289:_____/20:00532371 - isvavai.cz</a>
Alternative codes found
RIV/86652079:_____/20:00533145 RIV/00020699:_____/21:N0000006
Result on the web
<a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2019JD032269" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2019JD032269</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2019JD032269" target="_blank" >10.1029/2019JD032269</a>
Alternative languages
Result language
angličtina
Original language name
Atmospheric Circulation as a Factor Contributing to Increasing Drought Severity in Central Europe
Original language description
Long‐lasting and severe droughts seriously threaten agriculture, ecosystems, and society. Summer 2018 in central Europe was characterized by unusually persistent heat and drought, causing substantial economic losses, and became a part of a several years long dry period observed across this region. This study assesses the magnitude of the recent drought within a long‐term context and links the increased drought severity to changes in atmospheric circulation. Temporal variability of drought conditions since the late 19th century was analyzed at seven long‐term stations distributed across the Czech Republic using the Palmer Drought Severity Index and the Standardized Precipitation Evaporation Index. The Palmer Z Index and a variation of the Standardized Precipitation Evaporation Index were used to study rapidly emerging short‐term droughts and to link these episodes to atmospheric circulation. Changes in circulation were analyzed through circulation types calculated from flow strength, direction and vorticity in mean sea level pressure data from the National Centers for Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) reanalysis for 1948–2018. Increasing drought severity across the Czech Republic with record‐low values of the drought indices during 2015–2018 was found. The trend was distinctive in both vegetation (April–September) and cold (October–March) periods. The tendency toward more severe droughts in recent decades was linked to changes in frequency of dry and wet circulation types, highlighting the important role of atmospheric circulation in regional climate. It remains an open question whether the significantly increasing frequency of dry circulation types in the vegetation period is related to climate change, or rather represents multidecadal climate variability.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10509 - Meteorology and atmospheric sciences
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Geophysical Research: Atmospheres
ISSN
2169-897X
e-ISSN
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Volume of the periodical
125
Issue of the periodical within the volume
18
Country of publishing house
US - UNITED STATES
Number of pages
17
Pages from-to
e2019JD032269
UT code for WoS article
000576404200015
EID of the result in the Scopus database
2-s2.0-85091456365