2016
DOI: 10.1134/s0001433816010035
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Long-term changes in the aerosol optical thickness in moscow and correction under strong atmospheric turbidity

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Cited by 7 publications
(3 citation statements)
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“…These inhomogeneities, in the general case, do not have a regular spatial distribution and, apparently, depend on the transfer of smoke aerosol arising as a result of forest fires. In [21], the authors analyzed parameters of forest fires in the Baikal region using VEGA PRO remote sensing data for 2002-2017. One of the results from this analysis is shown as a dotted line in Figure 4 as the count of forest fires per year.…”
Section: Discussionmentioning
confidence: 99%
“…These inhomogeneities, in the general case, do not have a regular spatial distribution and, apparently, depend on the transfer of smoke aerosol arising as a result of forest fires. In [21], the authors analyzed parameters of forest fires in the Baikal region using VEGA PRO remote sensing data for 2002-2017. One of the results from this analysis is shown as a dotted line in Figure 4 as the count of forest fires per year.…”
Section: Discussionmentioning
confidence: 99%
“…1. Corrected aerosol optical depth at 500 nm (AOD500), by the method of Chubarova (2005) and by the method of Gorbarenko and Rublev (2013) for three different solar elevations, h, vs uncorrected AOD500*. The lowest curve, 1-to-1 line, is given for comparison.…”
Section: Model M2cmentioning
confidence: 99%
“…Recently Gorbarenko and Rublev (2013) reported about using a solar elevation-dependent correction of AOD500*. Assuming continental aerosols with a fixed Ångström exponent, α 1, = they derived a correction algorithm:…”
Section: Model M2cmentioning
confidence: 99%