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2 - Global Climate Change and the Rivers

from Part II - Challenge

Published online by Cambridge University Press:  16 September 2021

By
Gerald R. North
Edited by
Jurgen Schmandt  and
Aysegül Kibaroglu
Edited in association with
Regina Buono  and
Sephra Thomas
Jurgen Schmandt
Affiliation:
Houston Advanced Research Center
Aysegül Kibaroglu
Affiliation:
MEF University, Istanbul
Regina Buono
Affiliation:
University of Texas, Austin
Sephra Thomas
Affiliation:
University of Texas, Austin
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Summary

Currently available climate models predict the planet will be warmer at the end of this century by about 3C plus/minus 1.50C, while certain regions (the polar regions and the interiors of larger landmasses) will warm slightly more and ocean surfaces will warm at a slower pace. Climate modeling also tells us that the midlatitude storm belts will recede gradually toward their respective poles, causing the Hadley Cells to widen and expanding the arid subtropical zones. Warming in the cloud-free subtropics will lead to more warming and hence more evaporation of soil water. This chapter presents a thorough and accessible discussion of climate modeling to estimate future conditions in the Earth-hydrological system. It analyzes patterns of rainfall, potential evapotranspiration, actual evaporation, and runoff, among other factors, as well as the feedback mechanisms in the climate system that will impact water availability and use in the SERIDAS basins.

Keywords

climate changeclimate modelsHadley Cellssea levelcirculation modelsprecipitationevaporation
Type
Chapter
Information
Sustainability of Engineered Rivers In Arid Lands
Challenge and Response
 , pp. 13 - 30
Publisher: Cambridge University Press
Print publication year: 2021

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References

Adams, B. (2018). Understanding the Impact of Internal Variability on Our Estimates of the Transient Climate Response. Master’s Thesis Report. College Station: Texas A&M University.Google Scholar
Etheridge, D. M. et al. (1996). Natural and Anthropogenic Changes in Atmospheric CO2 over the Last 1000 Years from Air in Antarctica Ice and Firn. Journal of Geophysical Research, 101(D2), pp. 4115–4128.Google Scholar
Feng, S. and Fu, Q. (2013). Expansion of Global Drylands under a Warming Climate. Atmospheric Chemistry and Physics, 13(9), pp. 10081–10094. https://doi.org/10.5194/acp-13-10081-2013CrossRefGoogle Scholar
Hartmann, D. L. (2014). Global Physical Climatology, 2nd ed., San Diego, CA: Academic Press.Google Scholar
IPCC (2013). AR5 Climate Change 2013: The Physical Science Basis. Cambridge and New York: Intergovernmental Panel on Climate Change.Google Scholar
Johanson, C. M. and Fu, Q. (2009). Hadley Cell Widening: Model Simulations versus Observations. Climate, 22, pp. 2713–2725.Google Scholar
National Research Council (2006). Surface Temperature Reconstructions for the Last 2,000 Years. Washington, DC: National Academies Press. https://doi.org/10.17226/11676Google Scholar
Seidel, D. J. and Randel, W. J. (2007). Recent Widening of the Tropical Belt: Evidence from Tropopause Observations. Journal of Geophysical Research, 112, D20113. https://doi.org/10.1029/2007JD008861CrossRefGoogle Scholar
Seidel, D. J., Fu, Q., Randel, W. J., and Reichler, T. J. (2007). Widening of the Tropical Belt in a Changing Climate. Nature Geoscience, 1, 21–24.Google Scholar
USGCRP (2017). Climate Science Special Report: Fourth National Climate Assessment. Volume I. Washington, DC: U.S. Global Change Research Program, p. 470. https://doi.org/10.7930/J0J964J6Google Scholar

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