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Title: Quantifying the Importance of Rapid Adjustments for Global Precipitation Changes

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2018GL079474· OSTI ID:1480137
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  1. CICERO Center for International Climate Research Oslo Norway
  2. Rosenstiel School of Marine and Atmospheric ScienceUniversity of Miami Miami FL USA
  3. School of Earth and EnvironmentUniversity of Leeds Leeds UK
  4. Met Office Hadley Centre Exeter UK
  5. Institut Pierre‐Simon LaplaceCNRS/Sorbonne Université Paris France
  6. NASA Goddard Institute for Space Studies New York NY USA, Center for Climate Systems ResearchColumbia University New York NY USA
  7. Max‐Planck‐Institut für Meteorologie Hamburg Germany
  8. Department of PhysicsImperial College London London UK, Grantham Institute‐Climate Change and the EnvironmentImperial College London London UK
  9. Norwegian Meteorological Institute Oslo Norway
  10. NCAR/UCAR Boulder CO USA
  11. Nicholas School of the EnvironmentDuke University Durham NC USA
  12. Atmospheric, Oceanic &, Planetary Physics, Department of PhysicsUniversity of Oxford Oxford UK
  13. Research Institute for Applied MechanicsKyushu University Fukuoka Japan
  14. Department of PhysicsImperial College London London UK

Different climate drivers influence precipitation in different ways. Here we use radiative kernels to understand the influence of rapid adjustment processes on precipitation in climate models. Rapid adjustments are generally triggered by the initial heating or cooling of the atmosphere from an external climate driver. For precipitation changes, rapid adjustments due to changes in temperature, water vapor, and clouds are most important. In this study we have investigated five climate drivers (CO2, CH4, solar irradiance, black carbon, and sulfate aerosols). The fast precipitation responses to a doubling of CO2 and a 10-fold increase in black carbon are found to be similar, despite very different instantaneous changes in the radiative cooling, individual rapid adjustments, and sensible heating. The model diversity in rapid adjustments is smaller for the experiment involving an increase in the solar irradiance compared to the other climate driver perturbations, and this is also seen in the precipitation changes.

Research Organization:
Univ. of Colorado, Boulder, CO (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER); Research Council of Norway; National Aeronautics and Space Administration (NASA); Natural Environment Research Council (NERC); GENCI (Grand Equipement National de Calcul Intensif); European Research Council (ERC); Alexander von Humboldt Foundation; National Institute for Environmental Studies; Environmental Restoration and Conservation Agency of Japan; Japan Society for the Promotion of Science (JSPS)
Grant/Contract Number:
SC0012549; NAPEX (229778); 17-EARTH17R-015; NE/N006038/1; 724602; NE/K500872/1; JP15H01728
OSTI ID:
1480137
Alternate ID(s):
OSTI ID: 1480139; OSTI ID: 1611846
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Vol. 45 Journal Issue: 20; ISSN 0094-8276
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 23 works
Citation information provided by
Web of Science

References (16)

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Understanding Rapid Adjustments to Diverse Forcing Agents journal November 2018
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Two opposing effects of absorbing aerosols on global-mean precipitation: EFFECTS OF ABSORBING AEROSOLS ON PRECIPITATION journal July 2010
Radiative forcing due to changes in ozone and methane caused by the transport sector journal January 2011

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