A Plan for a Research Program on Aerosol Radiative Forcing by National Research Council, Division on Earth and Life PDF

By National Research Council, Division on Earth and Life Studies, Environment and Resources Commission on Geosciences, Panel on Aerosol Radiative Forcing and Climate Change

ISBN-10: 030905429X

ISBN-13: 9780309054294

Panel on Aerosol Radiative Forcing and weather switch, surroundings and assets fee on Geosciences, department in the world and lifestyles stories, nationwide examine Council

This booklet recommends the initiation of an "integrated" study software to review the function of aerosols within the envisioned international weather swap. present knowing recommend that, even now, aerosols, basically from anthropogenic resources, will be decreasing the speed of warming because of greenhouse gasoline emissions. as well as particular study ideas, this ebook forcefully argues for 2 varieties of study software integration: integration of the person laboratory, box, and theoretical examine actions and an built-in administration constitution that comprises all the involved federal firms.

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Extra resources for A Plan for a Research Program on Aerosol Radiative Forcing and Climate Change

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1994) found, in both continental and maritime clouds, systematically smaller effective drop radius in Northern Hemisphere midlatitudes. It was suggested that because of the effect of the inherent variability of liquid water path on cloud albedo, cloud drop radius is a more sensitive indicator of anthropogenic influence than is cloud albedo. Boucher (1995) constrained a global climate model with the satellite retrievals of Han et al. and determined the climate forcing that can be inferred from the observed distribution of cloud droplet radii.

Within two to three months, perturbed stratospheric optical depths were observed to at least 70°N, along with an enhancement in the Southern Hemisphere. Directly observed narrow and broadband total solar irradiance effects (IPCC, 1995a) indicate that reductions in surface solar flux ranged from <5 to 20 W m-2 in the diurnal mean, depending on prevailing aerosol optical depth. Satellite observations indicate a global mean decrease of about 5 W m-2 in the absorbed solar radiation in the period immediately following the eruption (IPCC, 1995a).

For example, the current, enhanced level of CO2 represents an accumulation of many decades of emission, whereas the current anthropogenic aerosol derives from emissions during only the previous few days. EVIDENCE FOR RADIATIVE FORCING BY ANTHROPOGENIC AEROSOLS The first question the panel addressed was: is anthropogenic aerosol forcing of climate a sufficiently important element of the overall climate system, such that its uncertainty is limiting our ability to quantitatively assess the effect of anthropogenic emissions on climate change?

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A Plan for a Research Program on Aerosol Radiative Forcing and Climate Change by National Research Council, Division on Earth and Life Studies, Environment and Resources Commission on Geosciences, Panel on Aerosol Radiative Forcing and Climate Change


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