A 2.5-layer thermodynamic ocean model has been used to understand the processes associated with the formation of cold pool off southern tip of India. The mean model simulations from the 13 year integration for the period 1992-2004 renders a cold region off southern tip of India during the months of June to September which is recognized as mini cold pool (MCP). The inter-annual and intra-seasonal variability of the MCP for the 5 years from 2000 to 2004 is explored in detail in the present paper. The analysis of model SST shows intense and widespread MCP during the long breaks occurred in the months of July and August of the bad monsoon years 2002 and 2004. The intense cooling is in response to the wind induced upwelling and the resultant ent...
ABSTRACT: The Indian subcontinent divides the north Indian Ocean into two tropical basins, namely th...
The structure of the warm pool (region with temperature greater than 28°C) in the equatorial Indian ...
219-223As summer is the season of mixing and winter the season of stratification in the Arabian Sea ...
The observed evolution of a mini-cold pool (MCP) off the southern tip of India (STI) and its intrusi...
In Lakshadweep Sea, the distribution of observed sea surface temperature (SST) during summer monsoon...
The observed mini-cold pool (MCP) off the southern tip of India (STI) and its intrusion into the sou...
A pool of relatively cooler water, called here as the southern Bay of Bengal cold pool, exists aroun...
Around Sri Lanka and to the south of India sea surface temperatures (SST) are cooler compared to the...
Coastal upwelling regions are among world´s most productive areas, with high levels of primary produ...
During the summer monsoon season, strong coastal upwelling occurs along the southwest coast of India...
During winter, south of the Indo-Sri Lanka Channel (ISLC), the observed sea-surface temperature (SST...
An Ocean General Circulation Model of the Indian Ocean with high horizontal (0.25 degrees x 0.25 d...
The Indian subcontinent divides the north Indian Ocean into two tropical basins, namely the Arabian ...
Warm pools – regions with sea surface temperature (SST) in excess of 28°C – in the ocean occupy a sp...
A suite of Regional Climate Model (RegCM) experiments are performed over south Asia to examine the s...
ABSTRACT: The Indian subcontinent divides the north Indian Ocean into two tropical basins, namely th...
The structure of the warm pool (region with temperature greater than 28°C) in the equatorial Indian ...
219-223As summer is the season of mixing and winter the season of stratification in the Arabian Sea ...
The observed evolution of a mini-cold pool (MCP) off the southern tip of India (STI) and its intrusi...
In Lakshadweep Sea, the distribution of observed sea surface temperature (SST) during summer monsoon...
The observed mini-cold pool (MCP) off the southern tip of India (STI) and its intrusion into the sou...
A pool of relatively cooler water, called here as the southern Bay of Bengal cold pool, exists aroun...
Around Sri Lanka and to the south of India sea surface temperatures (SST) are cooler compared to the...
Coastal upwelling regions are among world´s most productive areas, with high levels of primary produ...
During the summer monsoon season, strong coastal upwelling occurs along the southwest coast of India...
During winter, south of the Indo-Sri Lanka Channel (ISLC), the observed sea-surface temperature (SST...
An Ocean General Circulation Model of the Indian Ocean with high horizontal (0.25 degrees x 0.25 d...
The Indian subcontinent divides the north Indian Ocean into two tropical basins, namely the Arabian ...
Warm pools – regions with sea surface temperature (SST) in excess of 28°C – in the ocean occupy a sp...
A suite of Regional Climate Model (RegCM) experiments are performed over south Asia to examine the s...
ABSTRACT: The Indian subcontinent divides the north Indian Ocean into two tropical basins, namely th...
The structure of the warm pool (region with temperature greater than 28°C) in the equatorial Indian ...
219-223As summer is the season of mixing and winter the season of stratification in the Arabian Sea ...