Radiative forcing and temperature response to changes in urban albedos and associated CO2 offsets

The two main forcings that can counteract to some extent the positive forcings from greenhouse gases from pre-industrial times to present day are the aerosol and related aerosol-cloud forcings, and the radiative response to changes in surface albedo. Here, we quantify the change in radiative forcing...

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Veröffentlicht in:	Environmental research letters 2010-01, Vol.5 (1), p.014005
Hauptverfasser:	Menon, Surabi, Akbari, Hashem, Mahanama, Sarith, Sednev, Igor, Levinson, Ronnen
Format:	Artikel
Sprache:	eng
Schlagworte:	AEROSOLS ALBEDO Atmospheric circulation Carbon dioxide CLIMATES EVALUATION General circulation models Global climate GREENHOUSE GASES Land area Land surface temperature Long wave radiation Offsets PAVEMENTS Radiation RADIATIONS Radiative forcing ROOFS Short wave radiation Temperature Tropical environment Tropical environments TROPICAL REGIONS URBAN AREAS
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