Impact of satellite-derived shortwave attenuation depth and its spatial variability on the upper ocean dynamics has been studied using a numerical ocean model over the Bay of Bengal. We conducted two simulations, differing in the spatial distribution of shortwave attenuation depth for
the period 2014–2015. The control run use a constant attenuation depth of 23 m (the default case for Type-I water) while the experimental run (ER) use spatially varying attenuation depths derived from daily climatology of the diffuse attenuation coefficient ([Inline formula]).
Simulated parameters like sea surface temperature (SST) and mixed-layer depth (MLD) are sensitive to [Inline formula] that limits the penetration of downwelling shortwave radiation into the ocean. It has been found that [Inline formula] alters the upper ocean thermodynamics significantly.
Validation has been performed using satellite, moored-buoy and profile data, for the year 2015. During spring, the errors in SST in the ER are reduced up to 35% at buoy location. The impact of improving shortwave attenuation depth is found to be maximum in the upper ocean (50–150 m).
Error in simulated temperature at 100 m depth is reduced by 15% in the ER. MLD, barrier layer thickness, and the depth of 26 °C isotherm also show significant improvements in the ER.
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Bay of Bengal;
diffuse attenuation coefficient;
shortwave attenuation depth
Document Type: Research Article
OSD/AOSG/EPSA, Space Applications Centre (ISRO), Ahmedabad, India;
Department of Meteorology and Oceanography, Andhra University, Visakhapatnam, India;
Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
November 2, 2019
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