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Cirrus feedback on interannual climate fluctuations

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2014GL062095· OSTI ID:1174296
 [1];  [2];  [1];  [2];  [3]
  1. Lawrence Livermore National Laboratory, Livermore, CA (United States). Program for Climate Model Diagnosis and Intercomparison
  2. Texas A&M Univ., College Station TX (United States). Department of Atmospheric Sciences
  3. Jet Propulsion Lab./Caltech, Pasadena, CA (United States)

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 (optical depth <3.6, cloud top pressure <440 hPa) increase in response to inter-annual surface warming. Thus, cirrus clouds are likely to act as a positive feedback on short-term climate fluctuations, by reducing the planet’s ability to radiate longwave radiation to space in response to planetary surface warming. Using cirrus cloud radiative kernels, the magnitude of cirrus feedback is estimated to be 0.20±0.21W/m2/°C, which is comparable to the surface albedo feedback. Most of the cirrus feedback comes from increasing cloud amount in the tropical tropopause layer (TTL) and subtropical upper troposphere.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC52-07NA27344
OSTI ID:
1174296
Report Number(s):
LLNL-JRNL--661816
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 24 Vol. 41; ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English

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