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

被引:12
作者
Subrahamanyam, D. Bala [1 ]
Anurose, T. J. [1 ]
Kumar, N. V. P. Kiran [1 ]
Mohan, Mannil [1 ]
Kunhikrishnan, P. K. [1 ]
John, Sherine Rachel [1 ]
Prijith, S. S. [1 ]
Dutt, C. B. S. [2 ]
机构
[1] Indian Space Res Org, Govt India, Dept Space, Space Phys Lab,Vikram Sarabhai Space Ctr, Thiruvananthapuram 695022, Kerala, India
[2] Indian Space Res Org, Govt India, Dept Space, Natl Remote Sensing Ctr, Hyderabad 560625, Andhra Pradesh, India
关键词
Marine Atmospheric Boundary Layer; Mixed layer height; Turbulent flow; Bulk Richardson number; Bay of Bengal ICARB; SEA INTERFACE FLUXES; CENTRAL ARABIAN SEA; INDIAN-OCEAN; HEIGHT; INDOEX; THUMBA; ICARB; MODEL;
D O I
10.1016/j.atmosres.2011.12.014
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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 (theta(v)) 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 (Ri(B)) 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 MW showed good correlation with the surface-layer sensible heat flux which is one of the driving mechanisms in mixing processes. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:178 / 185
页数:8
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