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The compound nature of soil temperature anomalies at various depths in the Czech Republic

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F21%3A00546603" target="_blank" >RIV/68378289:_____/21:00546603 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/86652079:_____/21:00549164 RIV/60460709:41210/21:88354

  • Výsledek na webu

    <a href="https://link.springer.com/article/10.1007%2Fs00704-021-03787-7" target="_blank" >https://link.springer.com/article/10.1007%2Fs00704-021-03787-7</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00704-021-03787-7" target="_blank" >10.1007/s00704-021-03787-7</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    The compound nature of soil temperature anomalies at various depths in the Czech Republic

  • Popis výsledku v původním jazyce

    For the first time, this study analyzed the changes in observed soil temperature anomalies in detail at five stratified depths over various time scales in the Czech Republic. From 2000 to 2020, data from 49 weather stations were used, which also incorporated a unique 69-year series of soil temperature measurements from the Doksany station, where measurements have been obtained since 1952. First, climatological statistics for the observed soil temperatures at various depths and time scales were calculated. Second, a comprehensive analysis of soil temperature trends and their links with atmospheric variables was performed. Third, daily soil temperature anomalies (DSTs) at various depths were calculated through the use of standardized values (z‐DST scores). To demonstrate that precipitation triggered a drop in DSTs, we also applied a quantile-based analysis to rainfall-DST-coupled datasets. Compound air–soil heat events in the warm half-years were quantified. Finally, three critical soil temperature thresholds were established, and three minimum soil temperature, namely, lower than − 3 °C, − 5 °C, and − 7 °C were designated as being critical for wheat plants with low, moderate, and high frost tolerance, respectively. We found that the effects from soil warming at all depths and seasons have increased and that the risk of critical winter soil temperatures that cause stress-induced damage in wheat surprisingly increased over the study period. The risk of winterkill is between 28 and 39% in most wheat-planting areas. The most frequent intense long-lasting heat waves occurred in the postheading stage of winter wheat.

  • Název v anglickém jazyce

    The compound nature of soil temperature anomalies at various depths in the Czech Republic

  • Popis výsledku anglicky

    For the first time, this study analyzed the changes in observed soil temperature anomalies in detail at five stratified depths over various time scales in the Czech Republic. From 2000 to 2020, data from 49 weather stations were used, which also incorporated a unique 69-year series of soil temperature measurements from the Doksany station, where measurements have been obtained since 1952. First, climatological statistics for the observed soil temperatures at various depths and time scales were calculated. Second, a comprehensive analysis of soil temperature trends and their links with atmospheric variables was performed. Third, daily soil temperature anomalies (DSTs) at various depths were calculated through the use of standardized values (z‐DST scores). To demonstrate that precipitation triggered a drop in DSTs, we also applied a quantile-based analysis to rainfall-DST-coupled datasets. Compound air–soil heat events in the warm half-years were quantified. Finally, three critical soil temperature thresholds were established, and three minimum soil temperature, namely, lower than − 3 °C, − 5 °C, and − 7 °C were designated as being critical for wheat plants with low, moderate, and high frost tolerance, respectively. We found that the effects from soil warming at all depths and seasons have increased and that the risk of critical winter soil temperatures that cause stress-induced damage in wheat surprisingly increased over the study period. The risk of winterkill is between 28 and 39% in most wheat-planting areas. The most frequent intense long-lasting heat waves occurred in the postheading stage of winter wheat.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10509 - Meteorology and atmospheric sciences

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2021

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Theoretical and Applied Climatology

  • ISSN

    0177-798X

  • e-ISSN

    1434-4483

  • Svazek periodika

    146

  • Číslo periodika v rámci svazku

    3-4

  • Stát vydavatele periodika

    AT - Rakouská republika

  • Počet stran výsledku

    19

  • Strana od-do

    1257-1275

  • Kód UT WoS článku

    000702607500003

  • EID výsledku v databázi Scopus

    2-s2.0-85116292851