Numerical study of the role of land-air-sea interactions for the northeasterly monsoon circulations over Indian Ocean during INDOEX

Citation
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
Citations number
15
Categorie Soggetti
Multidisciplinary,Multidisciplinary
Journal title
CURRENT SCIENCE
ISSN journal
00113891 → ACNP
Volume
80
Year of publication
2001
Supplement
S
Pages
60 - 68
Database
ISI
SICI code
0011-3891(20010410)80:<60:NSOTRO>2.0.ZU;2-7
Abstract
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.