The Impact of Saharan dust aerosols on tropical cyclones using wrf-chem: Model framework and satellite data constraint technique



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Figure 8. a) 532 nm attenuated backscatter measured by the CALIOP lidar along the transect occurring at approximately 0300 UTC on 5 September which is the central transect shown in Figure 2a. b) Our calculated mass concentrations along the CALIPSO transect in panel a).




Figure 9. Percentage difference in the mass concentration values calculated by our satellite data constraint technique along the CALIPSO transect on 5 September at 0300 UTC when changing the constant lidar ratio and imaginary index values to 35 sr and 0.0015. The original mass concentrations values when using a constant lidar ratio and imaginary index of 39 sr and 0.0022 were already presented in Figure 8a.




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