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Soil drought and circulation types in a longitudinal transect over central Europe

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F21%3A00542138" target="_blank" >RIV/86652079:_____/21:00542138 - isvavai.cz</a>

  • Alternative codes found

    RIV/68378289:_____/21:00533689 RIV/62156489:43210/21:43918455 RIV/00216224:14310/21:00120773

  • Result on the web

    <a href="https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.6883" target="_blank" >https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.6883</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/joc.6883" target="_blank" >10.1002/joc.6883</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Soil drought and circulation types in a longitudinal transect over central Europe

  • Original language description

    Among the variables that can be employed to characterize agricultural drought, soil drought is of particular importance. This contribution uses gridded soil-drought values calculated from the SoilClim model for the 1961-2019 period to analyse soil drought episodes (based on the 10th percentile) in four lowlands, relatively homogeneous regions in central Europe that provide a longitudinal transect over central Europe. These areas are predominantly located at altitudes of below 400 m asl and include central Bohemia, southern Moravia and an adjacent part of Slovakia, southern Slovakia and eastern Slovakia. The results indicate that, after 1990, such episodes occurred largely in the summer half-year (April-September), accompanied by an increasing linear trend in the 1961-2019 period, while the situation was reversed in the winter half-year (October-March). Selected drought episodes are further divided into three phases (Phase I origin, Phase II course, Phase III end) and investigated separately in terms of precipitation and objective classification of circulation types based on flow strength, direction and vorticity. Decreases in the frequency of precipitation-rich cyclonic and the directional types associated with higher daily precipitation totals, together with increases in precipitation-poor anticyclonic types, were responsible for soil-drought Phases I and II, with the opposite pertaining to Phase III. Differences in the effects of circulation types on precipitation and soil-drought occurrence were considerable, particularly for central Bohemia compared with the other three regions. The results obtained are also discussed with respect to data uncertainty and their broader spatiotemporal context.

  • 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

    <a href="/en/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    International Journal of Climatology

  • ISSN

    0899-8418

  • e-ISSN

    1097-0088

  • Volume of the periodical

    41

  • Issue of the periodical within the volume

    JAN

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    17

  • Pages from-to

    "E2834"-"E2850"

  • UT code for WoS article

    000580674600001

  • EID of the result in the Scopus database

    2-s2.0-85093513350