Clouds in the Perturbed Climate System: Their Relationship by Jost Heintzenberg, Robert J. Charlson

By Jost Heintzenberg, Robert J. Charlson

Specialists think of the numerous roles that clouds play within the the altering climate--one of the least understood and such a lot difficult facets of atmospheric technology.

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Extra resources for Clouds in the Perturbed Climate System: Their Relationship to Energy Balance, Atmospheric Dynamics, and Precipitation (Strüngmann Forum Reports)

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R. Norris and A. Slingo Randall, D. , R. A. Wood, S. Bony et al. 2007. Climate models and their evaluation. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. S. Solomon, D. Qin, M. , pp. 591–662. New York: Cambridge Univ. Press. Rossow, W. , and R. A. Schiffer. 1999. Advances in understanding clouds from ISCCP. Bull. Amer. Meteor. Soc. 80:2261– 2287. Slingo, A. 1990. Sensitivity of the Earth’s radiation budget to changes in low clouds.

R. 2008. Calibration assessment of ISCCP geostationary infrared observations using HIRS. J. Atmos. Ocean. Technol. 25:183–195. , L. A. Remer, Y. J. Kaufman, Y. Rudich, and J. V. Martins. 2007. On the twilight zone between clouds and aerosols. Geophys. Res. Lett. 34:L08805. Loeb, N. , B. A. Wielicki, W. Su et al. 2007. Multi-instrument comparison of top-ofatmosphere reÀected solar radiation. J. Climate 20:575–591. , W. B. Rossow, T. Inoue, and C. J. Stubenrauch. 2002. Did the eruption of Mt. Pinatubo volcano affect cirrus properties?

B. A. Wielicki, R. B. Lee et al. 2006. Re-examination of the observed decadal variability of the earth radiation budget using altitude-corrected ERBE/ERBS nonscanner WFOV data. J. Climate 19:4028–4040. , D. L. Jackson, W. P. Menzel, and J. J. Bates. 2005. Trends in global cloud cover in two decades of HIRS observations. J. Climate 18:3021–3031. , W. B. Rossow, A. A. Lacis, V. Oinas, and M. I. Mishchenko. 2004. Calculation of radiative Àuxes from the surface to top of atmosphere based on ISCCP and other global data sets: Re¿nements of the radiative transfer model and the input data.

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