Lahouari Bounoua Ping Zhang Robert E. Wolfe Thomas G. Huntington Marc L. Imhoff Kurt Thome Genevieve L. Noyce Ryan J. Kramer 2015 <p><span>Most models evaluated by the Intergovernmental Panel for Climate change estimate projected increases in temperature and precipitation with rising atmospheric CO</span>_{<span>2</span>}<span>&nbsp;levels. Researchers have suggested that increases in CO</span>_{<span>2</span>}<span>&nbsp;and associated increases in temperature and precipitation may stimulate vegetation growth and increase evapotranspiration (ET), which acts as a cooling mechanism, and on a global scale, may slow the climate-warming trend. This hypothesis has been modeled under increased CO</span><span>₂&nbsp;</span><span>conditions with models of different vegetation-climate dynamics. The significance of this vegetation negative feedback, however, has varied between models. Here we conduct a century-scale observational analysis of the Eastern US water balance to determine historical evapotranspiration trends and whether vegetation greening has affected these trends. We show that precipitation has increased significantly over the twentieth century while runoff has not. We also show that ET has increased and vegetation growth is partially responsible.</span></p> application/pdf 10.3390/hydrology2020093 en European Geophysical Society Evapotranspiration trends over the eastern United States during the 20th century article