2014
DOI: 10.1117/12.2074670
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Specific features of spatial distribution of atmospheric aerosol optical depth along northern sea route

Abstract: We discuss the aerosol optical depth (AOD) measurements with the sun photometers onboard "Akademik Fedorov" and "Professor Khlyustin" research vessels in Arctic and Far East seas along the Northern Sea Route. Coastal observations in Barentsburg, Tiksi, and Vladivostok are employed to analyze the ship-based measurements. It is shown that AOD in Arctic differs little, with the average AOD values being much less than in the background midlatitude regions. In the spatial distributions of AOD and water vapor in Far… Show more

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Cited by 1 publication
(2 citation statements)
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“…Analysis of (MODIS) satellite measure ments of the AOD [18,33,38] showed that the aerosol turbidity in most of Siberia (northward of Trans Sibe rian Railway) and Ural largely shows a decrease in the northern direction and only minor variations with lon gitude. The average gradient of the latitudinal decrease in AOD (0.55 μm) for the central months of summer and fall is 0.002-0.003 per degree of latitude.…”
Section: Spatial Aod Distributionmentioning
confidence: 99%
See 1 more Smart Citation
“…Analysis of (MODIS) satellite measure ments of the AOD [18,33,38] showed that the aerosol turbidity in most of Siberia (northward of Trans Sibe rian Railway) and Ural largely shows a decrease in the northern direction and only minor variations with lon gitude. The average gradient of the latitudinal decrease in AOD (0.55 μm) for the central months of summer and fall is 0.002-0.003 per degree of latitude.…”
Section: Spatial Aod Distributionmentioning
confidence: 99%
“…Tri modal structure with maxima in January, in summer, and fall; μ = 0.14; max/min ≈ 0.18/0.09 μ is the annual average under usual ("smoke free") conditions, max/min is the amplitude of annual behavior, and Δ S is the smoke addition. In addition to this latitudinal dependence, the sat ellite data can be used to perform the spatial clustering of AOD according to three "signs" [18,38]: 1) with respect to the average level of aerosol turbidity; 2) with respect to the character of the annual AOD behavior; and 3) with respect to interrelation between variations in monthly AOD values in separate regions.…”
Section: Spatial Aod Distributionmentioning
confidence: 99%