Open AccessCzasowa zmienność i przestrzenne zróżnicowanie ewapotranspiracji w zlewni nizinnej rzeki Łasicy
Author(s) -
Urszula Somorowska
Publication year - 2021
Publication title -
prace i studia geograficzne
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.106
H-Index - 10
eISSN - 2543-7313
pISSN - 0208-4589
DOI - 10.48128/pisg/2021-66.3-03
Subject(s) - evapotranspiration , environmental science , precipitation , hydrology (agriculture) , water balance , water cycle , vegetation (pathology) , growing season , dry season , drainage basin , physical geography , forestry , geography , agronomy , ecology , meteorology , geology , medicine , geotechnical engineering , cartography , pathology , biology
Accurate quantification of evapotranspiration is necessary for understanding the water cycle at a local scale. At catchment scale, evapotranspiration might be approximated using remote sensing data useful in spatialtemporal analyses. In this study, the long-term and seasonal variability of evapotranspiration in the Łasica River catchment in the years 2003–2020 was assessed on the basis of data acquired from the SSEBop project (Operational Simplified Surface Energy Balance). Additionally, using the index of precipitation utilization (WWO), the degree of precipitation consumption for the water demands of plants was determined. The highest evapotranspiration occurs in forest areas, slightly lower in marshy belts covered with meadow vegetation, and the lowest in agricultural areas and anthropogenically transformed areas. The spatial differentiation of evapotranspiration is particularly marked during the growing season, from April to October. Mean annual evapotranspiration sum is 403 mm, of which 96% falls on the growing season. Extremely low annual ET sums occurred in 2015 (329 mm), 2019 (342 mm) and 2003 (384 mm), while particularly high – in 2010 (455 mm) and 2013 (447 mm). In dry years, WWO is even 71–77%, while in particularly wet years, WWO is much lower and amounts to 54–58%.