Uc. Mohanty et al., Numerical study of the role of land-air-sea interactions for the northeasterly monsoon circulations over Indian Ocean during INDOEX, CURRENT SCI, 80, 2001, pp. 60-68
One of the principal objectives of the Indian Ocean Experiment (INDOEX) was
to study the aerosol transport from the Indian subcontinent to the pristin
e oceanic environment. The underlying hypothesis for INDOEX is that, during
the northeasterly monsoon, the intruding aerosols and other anthropogenic
pollutants can entrain into the Inter Tropical Convergence Zone (ITCZ) and
the Equatorial Indian Ocean and finally into the clouds, The altered clouds
influence the radiative transfer processes at the regional and possibly gl
obal scale. The driving mechanism for the regional transport was the bounda
ry layer circulation. In this study, it was hypothesized that the circulati
on pattern, which affects the regional transport, was strongly influenced b
y the land-air-sea interactions. To test this, a zonally symmetric version
of a primitive equation numerical weather prediction model, called the Adva
nced Regional Prediction System (ARPS), was used. A number of numerical exp
eriments were performed for a 2-D domain ranging from 14 degreesN to 16 deg
reesS centered over 76 degreesE, In the experiments, the influence of land-
sea interaction (differential heating), topography (Western Chats), and the
thermal gradients (SST and land surface temperature) on the coastal circul
ations over Equatorial Indian Ocean were studied. Results indicated a stron
g land-air-sea interaction and feedback teleconnection between the local an
d large scale features. Interestingly, the model generated land influence t
o the order of 1000 km offshore in the simulation domain, consistent with d
ifferent observations. Results suggest that the oceanic environment in the
northeast monsoon over Arabian Sea and the Indian Ocean can display signifi
cant diurnal variability and heterogeneity due to topography and surface te
mperature gradients, and that the local features have interactive feedback
on the large scale circulations and transport.