The effect of aerosol on surface cloud radiative forcing in the Arctic

• Main Authors: Hu, R.-M., Blanchet, J.-P., Girard, E.
• Other Authors: Thales Alenia Space Toulouse (TAS), THALES France, Département des sciences de la terre et de l'atmosphère Montréal (SCTA), Université du Québec à Montréal = University of Québec in Montréal (UQAM)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2005
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; Arctic; albedo; black carbon; Climate change
• Online Access: https://hal.science/hal-00301797; https://hal.science/hal-00301797/document; https://hal.science/hal-00301797/file/acpd-5-9039-2005.pdf

International audience Cloud radiative forcing is a very important concept to understand what kind of role the clouds play in climate change with thermal effect or albedo effect. In spite of that much progress has been achieved, the clouds are still poorly described in the climate models. Due to the complex aerosol-cloud-radiation interactions, high surface albedo of snow and ice cover, and without solar radiation in long period of the year, the Arctic strong warming caused by increasing greenhouse gases (as most GCMs suggested) has not been verified by the observations. In this study, we were dedicated to quantify the aerosol effect on the Arctic cloud radiative forcing by Northern Aerosol Regional Climate Model (NARCM). Major aerosol species such as Arctic haze sulphate, black carbon, sea salt, organics and dust have been included during our simulations. By inter-comparisons with the Atmospheric Radiation Measurement (ARM) data, we find surface cloud radiative forcing (SCRF) is ?22 W/m 2 for shortwave and 36 W/m 2 for longwave. Total cloud forcing is 14 W/m 2 with minimum of ?35 W/m 2 in early July. If aerosols are taken into account, the SCRF has been increased during winter while negative SCRF has been enhanced during summer. Our estimate of aerosol forcing is about ?6 W/m 2 in the Arctic.