Publications

Zhang, ZB; Meyer, K; Yu, HB; Platnick, S; Colarco, P; Liu, ZY; Oreopoulos, L (2016). Shortwave direct radiative effects of above-cloud aerosols over global oceans derived from 8 years of CALIOP and MODIS observations. ATMOSPHERIC CHEMISTRY AND PHYSICS, 16(5), 2877-2900.

Abstract
In this paper, we studied the frequency of occurrence and shortwave direct radiative effects (DREs) of above-cloud aerosols (ACAs) over global oceans using 8 years (2007-2014) of collocated CALIOP and MODIS observations. Similar to previous work, we found high ACA occurrence in four regions: southeastern (SE) Atlantic region, where ACAs are mostly light-absorbing aerosols, i.e., smoke and polluted dust according to CALIOP classification, originating from biomass burning over the African Savanna; tropical northeastern (TNE) Atlantic and the Arabian Sea, where ACAs are predominantly windblown dust from the Sahara and Arabian deserts, respectively; and the northwestern (NW) Pacific, where ACAs are mostly transported smoke and polluted dusts from Asian. From radiative transfer simulations based on CALIOP-MODIS observations and a set of the preselected aerosol optical models, we found the DREs of ACAs at the top of atmosphere (TOA) to be positive (i.e., warming) in the SE Atlantic and NW Pacific regions, but negative (i.e., cooling) in the TNE Atlantic Ocean and the Arabian Sea. The cancellation of positive and negative regional DREs results in a global ocean annual mean diurnally averaged cloudy-sky DRE of 0.015aEuro-WaEuro-m(-2) (range of -0.03 to 0.06aEuro-WaEuro-m(-2)) at TOA. The DREs at surface and within the atmosphere are -0.15aEuro-WaEuro-m(-2) (range of -0.09 to -0.21aEuro-WaEuro-m(-2)), and 0.17aEuro-WaEuro-m(-2) (range of 0.11 to 0.24aEuro-WaEuro-m(-2)), respectively. The regional and seasonal mean DREs are much stronger. For example, in the SE Atlantic region, the JJA (July-August) seasonal mean cloudy-sky DRE is about 0.7aEuro-WaEuro-m(-2) (range of 0.2 to 1.2aEuro-WaEuro-m(-2)) at TOA. All our DRE computations are publicly available(1). The uncertainty in our DRE computations is mainly caused by the uncertainties in the aerosol optical properties, in particular aerosol absorption, the uncertainties in the CALIOP operational aerosol optical thickness retrieval, and the ignorance of cloud and potential aerosol diurnal cycle. In situ and remotely sensed measurements of ACA from future field campaigns and satellite missions and improved lidar retrieval algorithm, in particular vertical feature masking, would help reduce the uncertainty.

DOI:
10.5194/acp-16-2877-2016

ISSN:
1680-7316