EGU2020-10401
https://doi.org/10.5194/egusphere-egu2020-10401
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Rising Temperatures Increase Importance of Oceanic Evaporation as a Source for Continental Precipitation

Kirsten Findell1, Patrick Keys2, Ruud van der Ent3,4, Benjamin Lintner5, Alexis Berg6, and John Krasting7
Kirsten Findell et al.
  • 1Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States of America (kirsten.findell@noaa.gov)
  • 2School of Global Environmental Sustainability, Colorado State University, Fort Collins, Colorado (pkeys@rams.colostate.edu)
  • 3Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, Netherlands (R.J.vanderEnt@tudelft.nl)
  • 4Department of Physical Geography, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
  • 5Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, New Jersey (lintner@envsci.rutgers.edu)
  • 6Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts (alexis_berg@fas.harvard.edu)
  • 7Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States of America (john.krasting@noaa.gov)

Understanding vulnerabilities of continental precipitation to changing climatic conditions is of critical importance to society at large. Terrestrial precipitation is fed by moisture originating as evaporation from oceans and from recycling of water evaporated from continental sources. In this study, continental precipitation and evaporation recycling processes in the Earth system model GFDL-ESM2G are shown to be consistent with estimates from two different reanalysis products. The GFDL-ESM2G simulations of historical and future climate also show that values of continental moisture recycling ratios were systematically higher in the past and will be lower in the future.

Global mean recycling ratios decrease 2%–3% with each degree of temperature increase, indicating the increased importance of oceanic evaporation for continental precipitation. Theoretical arguments for recycling changes stem from increasing atmospheric temperatures and evaporative demand that drive increases in evaporation over oceans that are more rapid than those over land as a result of terrestrial soil moisture limitations. Simulated recycling changes are demonstrated to be consistent with these theoretical arguments. A simple prototype describing this theory effectively captures the zonal mean behavior of GFDL-ESM2G.

Key sources of terrestrial evaporation, notably the interior of the Amazon basin and parts of the Ganges-Brahmaputra and Indus River basins, may experience reductions in moisture recycling. This has implications for key sink regions of terrestrial recycled precipitation, especially in rain-fed agricultural regions where crop yields will become increasingly soil moisture limited, such as the La Plata River basin, the corn producing regions of North America, southern Africa and the Sahel.

The results presented here have been published last year in Journal of Climate dx.doi.org/10.1175/JCLI-D-19-0145.1

 

How to cite: Findell, K., Keys, P., van der Ent, R., Lintner, B., Berg, A., and Krasting, J.: Rising Temperatures Increase Importance of Oceanic Evaporation as a Source for Continental Precipitation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10401, https://doi.org/10.5194/egusphere-egu2020-10401, 2020

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