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Seasonally contrasting responses of evapotranspiration to warming and elevated CO 2 in a semiarid grassland
Author(s) -
Sorokin Y.,
Zelikova T. J.,
Blumenthal D.,
Williams D. G.,
Pendall E.
Publication year - 2017
Publication title -
ecohydrology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.982
H-Index - 54
eISSN - 1936-0592
pISSN - 1936-0584
DOI - 10.1002/eco.1880
Subject(s) - evapotranspiration , environmental science , growing season , precipitation , climate change , vapour pressure deficit , transpiration , grassland , global warming , dry season , atmospheric sciences , vegetation (pathology) , phenology , agronomy , ecology , geography , photosynthesis , biology , medicine , botany , pathology , geology , meteorology
Global climate change is expected to alter seasonal patterns and rates of evapotranspiration in dry regions. Although climate change will involve elevated CO 2 and increased temperatures, independently, these factors may have different impacts on actual evapotranspiration (AET) due to their opposing effects on transpiration. We used canopy gas exchange chambers to quantify AET in a semiarid grassland experimentally altered by elevated CO 2 and warming over 3 years with contrasting ambient precipitation. Seasonal and interannual variations in AET due to background climate variability were larger than the effects of climate manipulation treatments. However, in a year with average precipitation, cumulative growing season AET was suppressed by warming by 23%. Across years, warming increased AET early in the growing season and suppressed it later in the growing season. By contrast, elevated CO 2 suppressed AET early in the growing season and enhanced it later, but only in years with average or above‐average precipitation. Vegetation greenness (a proxy for photosynthetically active leaf area) was consistently the strongest predictor of AET, whereas soil moisture and vapor pressure deficit were secondary drivers. Our research demonstrates that effects of increased atmospheric CO 2 and temperature on AET will be mediated by plant phenological development and seasonal climatic conditions.