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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

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • 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

  • 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