Correlation between TOMS aerosol index and astronomical extinction

Author(s):  
El Arbi Siher ◽  
Sergio Ortolani ◽  
Marc S. Sarazin ◽  
Zouhair Benkhaldoun
2010 ◽  
Vol 4 (1) ◽  
pp. 101-113 ◽  
Author(s):  
J. Barkan ◽  
P. Alpert

The annual link between the solar insolation, the surface temperature, and the dust load in the atmosphere as estimated by the TOMS Aerosol Index was compared in five major sandy deserts around the globe. A high correlation was found between the insolation and the dust in all deserts, while the correlation of dust with temperature was lower. The peaks of the insolation and the dust occurred almost simultaneously on the same date in three out of the five deserts i.e. Sahara, S.W. North American, Atacama. In the other two deserts i.e., Australian, Taklimakan, the peak of the dust occurs earlier in the year. The temperature peaks occur on a later date in all the deserts. Our conclusion is, that in the deserts of the world the radiation is the major cause of the total dust loading.


2006 ◽  
Vol 40 (28) ◽  
pp. 5367-5378 ◽  
Author(s):  
M KOUKOULI ◽  
D BALIS ◽  
V AMIRIDIS ◽  
S KAZADZIS ◽  
A BAIS ◽  
...  

1999 ◽  
Vol 104 (D6) ◽  
pp. 6269-6279 ◽  
Author(s):  
N. C. Hsu ◽  
J. R. Herman ◽  
O. Torres ◽  
B. N. Holben ◽  
D. Tanre ◽  
...  

2007 ◽  
Vol 7 (5) ◽  
pp. 14351-14367 ◽  
Author(s):  
R.-M. Hu ◽  
R. S. Sokhi

Abstract. Oceanic phytoplankton can affect in-water and atmospheric radiation fields. In this study, we develop case 1 (without noncovarying particles) and case 2 (including noncovarying particles) waters model including Raman scattering in order to examine the chlorophyll impacts on the Total Ozone Mapping Spectrometer (TOMS) Aerosol Index and aerosol single scattering albedo. The waters model is coupled with a radiation transfer model (VLIDORT) for calculating TOMS Aerosol Index and retrieval of aerosol single scattering albedo. The retrieval is constrained by chlorophyll concentration from Sea-viewing Wide Field-of-view Sensor (SeaWiFS) and Moderate Resolution Imaging SpectroRadiometer (MODIS) data, aerosol optical depth from MODIS, and aerosol vertical profiles from a global chemical transport model (GEOS-CHEM). We find the retrieved aerosol single scattering albedo is strongly influenced by chlorophyll concentration, particularly in the regions of subtropical Atlantic Ocean and Indian Ocean. The maximum deviation between the aerosol single scattering albedo retrieved with and withouout considering chlorophyll can reach 10 percent. Thus, it is important to take account of the phytoplankton impacts on atmospheric remote sensing measurements.


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