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      Hydrological Consequences of Solar Geoengineering

      1 , 2 , 1 , 1 , 1
      Annual Review of Earth and Planetary Sciences
      Annual Reviews

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          Abstract

          As atmospheric carbon dioxide concentrations rise and climate change becomes more destructive, geoengineering has become a subject of serious consideration. By reflecting a fraction of incoming sunlight, solar geoengineering could cool the planet quickly, but with uncertain effects on regional climatology, particularly hydrological patterns. Here, we review recent work on projected hydrologic outcomes of solar geoengineering, in the context of a robust literature on hydrological responses to climate change. While most approaches to solar geoengineering are expected to weaken the global hydrologic cycle, regional effects will vary based on implementation method and strategy. The literature on the hydrologic outcomes and impacts of geoengineering demonstrates that its implications for human welfare will depend on assumptions about underlying social conditions and objectives of intervention as well as the social lens through which projected effects are interpreted. We conclude with suggestions to reduce decision-relevant uncertainties in this novel field of Earth science inquiry. ▪ The expected hydrological effects of reducing insolation are among the most uncertain and consequential impacts of solar geoengineering (SG). ▪ Theoretical frameworks from broader climate science can help explain SG's effects on global precipitation, relative humidity, and other aspects of hydroclimate. ▪ The state of the knowledge on hydrological impacts of SG is unevenly concentrated among regions. ▪ Projected hydrological impacts from SG are scenario dependent and difficult to characterize as either harmful or beneficial.

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          Most cited references129

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          Robust Responses of the Hydrological Cycle to Global Warming

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            Global Warming Pattern Formation: Sea Surface Temperature and Rainfall*

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              Migrations and dynamics of the intertropical convergence zone.

              Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clouds centred on average around six degrees north of the Equator. The mean position of the ITCZ north of the Equator arises primarily because the Atlantic Ocean transports energy northward across the Equator, rendering the Northern Hemisphere warmer than the Southern Hemisphere. On seasonal and longer timescales, the ITCZ migrates, typically towards a warming hemisphere but with exceptions, such as during El Niño events. An emerging framework links the ITCZ to the atmospheric energy balance and may account for ITCZ variations on timescales from years to geological epochs.
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                Author and article information

                Journal
                Annual Review of Earth and Planetary Sciences
                Annu. Rev. Earth Planet. Sci.
                Annual Reviews
                0084-6597
                1545-4495
                May 31 2023
                May 31 2023
                : 51
                : 1
                : 447-470
                Affiliations
                [1 ]Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA;
                [2 ]School of Global Policy and Strategy, University of California, San Diego, La Jolla, California, USA
                Article
                10.1146/annurev-earth-031920-083456
                aedaf29a-32ef-4f16-8c6a-a1eba9dfadfc
                © 2023

                http://creativecommons.org/licenses/by/4.0/

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