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

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  • Paweł Bogawski
  • Ewa Bednorz

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 (ET 0 ; June–August, 1971–2010) for 31 stations in Poland using the FAO-56 Penman–Monteith method and identified the days with the highest ET 0 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 ET 0 values (r > 0.4, p > 0.001) in northeast Poland; positive anomalies in SLP, z500 and t850 were documented on days with high ET 0 . Substantial anomalies were also observed in the factors that directly affect evapotranspiration, i.e., sunshine duration and air temperature (positive) and relative humidity (negative). The conditions favorable for high ET 0 events are characteristic of anticyclonic weather, so when an anticyclone center is near northeast Poland, high evapotranspiration can be expected. Copyright The Author(s) 2016

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  • 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:p:55-69
    DOI: 10.1007/s11069-015-2066-2
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    References listed on IDEAS

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    1. Sentelhas, Paulo C. & Gillespie, Terry J. & Santos, Eduardo A., 2010. "Evaluation of FAO Penman-Monteith and alternative methods for estimating reference evapotranspiration with missing data in Southern Ontario, Canada," Agricultural Water Management, Elsevier, vol. 97(5), pages 635-644, May.
    2. Paweł Bogawski & Ewa Bednorz, 2014. "Comparison and Validation of Selected Evapotranspiration Models for Conditions in Poland (Central Europe)," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 28(14), pages 5021-5038, November.
    3. Goyal, R. K., 2004. "Sensitivity of evapotranspiration to global warming: a case study of arid zone of Rajasthan (India)," Agricultural Water Management, Elsevier, vol. 69(1), pages 1-11, September.
    4. Brunella Bonaccorso & David Peres & Antonino Cancelliere & Giuseppe Rossi, 2013. "Large Scale Probabilistic Drought Characterization Over Europe," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 27(6), pages 1675-1692, April.
    5. Ali-Akbar Sabziparvar & H. Tabari & A. Aeini & M. Ghafouri, 2010. "Evaluation of Class A Pan Coefficient Models for Estimation of Reference Crop Evapotranspiration in Cold Semi-Arid and Warm Arid Climates," Water Resources Management: An International Journal, Published for the European Water Resources Association (EWRA), Springer;European Water Resources Association (EWRA), vol. 24(5), pages 909-920, March.
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    Cited by:

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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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