Radiative Properties Of Saharan Mineral Dust Measured Using Neodymium: Yttrium-aluminium-garnet (532 Nm) Backscatter Lidar
Price
Free (open access)
Transaction
Volume
28
Pages
9
Published
1998
Size
638 kb
Paper DOI
10.2495/AIR980881
Copyright
WIT Press
Author(s)
J.P. Diaz, F.J. Exposito, I.R. Martin and R. Barrena
Abstract
Saharan mineral dust is studied with a neodymium: yttrium-aluminium-garnet (Nd-YAG) backscatter lidar system in Tenerife, Canary Islands (28.5°N, 16.3°W). Recent studies have shown the importance of this atmospheric component as a climate forcing agent. This radiative forcing has been quantified between -1 to -2 W/nf, values comparable in magnitude to the positive forcing attributed to greenhouse gases. The main sources of this kind of aerosols are the arid zones. The dust plumes from sources in North Africa are the most prominent and cover the largest ocean areas (400-700 Tg/year). Lidar techniques allow one to obtai
Keywords