Flight 3, Transit to Cabo Verde, 15 Aug 2006
August 27th, 2006Flight Team: Winstead, Anderson, Diskin (DLH), Podolske (Cobalt)
Instruments: All instruments worked well. However, software problems caused the data acquisition system to crash at frequent intervals, which kept us on our toes during the flight.
Observations: Satellite images recorded just prior to takeoff showed enhanced aerosol optical depths over the Atlantic just north of Sal, Cape Verde, indicating the presence of Saharan dust. The transit flight plan was thus modified to include a constant altitude flight leg within the layer to characterize its composition using in situ sensors. On the leg and an associated vertical sounding, we found that the dust layer resided between 5 and 15 kft and that it exhibited the highest particle loadings around 7.5 kft altitude. Scattering coefficients peaked near 200 Mm-1 in the layer, but exhibited substantial horizontal and vertical variability. Surprisingly, relative humidities measured by DLH were correlated with scattering and varied between 60 and 70% within the thickest part of the layer.