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Atmospheric conditions controlling extreme summertime evapotranspiration in Poland (central Europe)

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  • Paweł Bogawski

    (Adam Mickiewicz University
    Adam Mickiewicz University)

  • Ewa Bednorz

    (Adam Mickiewicz University)

Abstract

Extremely high evapotranspiration may constitute a threat to agriculture and to water storage, supply, management and quality. To better understand the occurrence of high evapotranspiration, our goals were to (1) document the synoptic conditions favorable for extreme evapotranspiration and (2) determine the anomalies in the factors that directly affect extremely high evapotranspiration on a daily scale. We calculated the daily reference evapotranspiration (ET0; June–August, 1971–2010) for 31 stations in Poland using the FAO-56 Penman–Monteith method and identified the days with the highest ET0 values (>90th percentile). For these days, we calculated the sea level pressure (SLP), the 500 hPa geopotential heights (z500), the air temperature at 850 hPa (t850) and the amount of precipitable water. We detected a correlation between the air pressure field and high ET0 values (r > 0.4, p

Suggested Citation

  • Paweł Bogawski & Ewa Bednorz, 2016. "Atmospheric conditions controlling extreme summertime evapotranspiration in Poland (central Europe)," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 81(1), pages 55-69, March.
    • Handle: RePEc:spr:nathaz:v:81:y:2016:i:1:d:10.1007_s11069-015-2066-2
    DOI: 10.1007/s11069-015-2066-2
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    2. Urszula Somorowska, 2022. "Changes in Terrestrial Evaporation across Poland over the Past Four Decades Dominated by Increases in Summer Months," Resources, MDPI, vol. 11(1), pages 1-17, January.

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