Title of article :
Spatial and temporal variabilities in vertical structure of the Marine Atmospheric Boundary Layer over Bay of Bengal during Winter Phase of Integrated Campaign for Aerosols, gases and Radiation Budget
Author/Authors :
Subrahamanyam، نويسنده , , D. Bala and Anurose، نويسنده , , T.J. Prasanna Kumar، نويسنده , , N.V.P. Kiran and Mohan، نويسنده , , Mannil and Kunhikrishnan، نويسنده , , P.K. and John، نويسنده , , Sherine Rachel and Prijith، نويسنده , , S.S. and Dutt، نويسنده , , C.B.S.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2012
Pages :
8
From page :
178
To page :
185
Abstract :
Spatial and temporal variabilities in the vertical structure of Marine Atmospheric Boundary Layer (MABL) over the Bay of Bengal (BoB) are investigated through a ship-borne field experiment measurements pertaining to three different classes, namely: night, morning and afternoon conditions. High-resolution vertical profiles of meteorological parameters obtained through balloon-borne GPS Sondes during the Winter phase of Integrated Campaign for Aerosols, gases and Radiation Budget (W-ICARB) formed the primary database for the present investigation. The study advocates usage of wind shear profiles in association with virtual potential temperature (θv) and specific humidity (q) profiles for determination of the mixed layer heights (MLH). The mean values of turbulent flow thickness (TFT) obtained from the vertical profiles of Bulk Richardson Number (RiB) and MLH magnitudes for the entire cruise did not show any appreciable variations for three classes. During the entire cruise period, the MLH varied in a range from 450 m to 1500 m with a mean of about 900 m, whereas the TFT variations were confined between 125 m and 1475 m with a mean of about 581 m. The statistical means of TFT and MLH were similar for nighttime profiles, whereas they showed significant differences in the morning and afternoon conditions. Spatio-temporal variability in the MLH showed good correlation with the surface-layer sensible heat flux which is one of the driving mechanisms in mixing processes.
Keywords :
Turbulent flow , Bulk Richardson number , Marine Atmospheric Boundary Layer , Bay of Bengal ICARB , Mixed layer height
Journal title :
Atmospheric Research
Serial Year :
2012
Journal title :
Atmospheric Research
Record number :
2247443
Link To Document :
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