4.7 Article

Cirrus feedback on interannual climate fluctuations

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 24, Pages 9166-9173

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL062095

Keywords

cirrus; cloud feedback; climate change and variability

Funding

  1. NASA [NNX10AM27G, NNX13AK25G]
  2. NASA Earth and Space Science Fellowship [NNX12AN57H]
  3. Regional and Global Climate Modeling Program of the Office of Science at the U.S. Department of Energy (DOE)
  4. DOE by Lawrence Livermore National Laboratory [DE-AC52-07NA27344]
  5. NASA [69783, NNX13AK25G, 471657, NNX10AM27G, 129964, NNX12AN57H] Funding Source: Federal RePORTER

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Cirrus clouds are not only important in determining the current climate but also play an important role in climate change and variability. Analysis of satellite observations shows that the amount and altitude of cirrus clouds (cloud optical depth<3.6, cloud top pressure<440hPa) increase in response to interannual surface warming. Using cirrus cloud radiative kernels, the magnitude of the interannual cirrus feedback is estimated to be 0.200.21W/m(2)/degrees C, which represents an important component of the cloud feedback. Thus, cirrus clouds are likely to act as a positive feedback on interannual climate fluctuations, by reducing the Earth's ability to radiate longwave radiation to space in response to planetary surface warming. Most of the cirrus feedback comes from increasing cloud amount in the tropical tropopause layer (TTL) and subtropical upper troposphere.

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