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Inter-annual variability of sea surface temperature, wind speed and sea surface height anomaly over the tropical Indian Ocean
(NIO, Dona Paula, Goa (India), 2000)
Being land-locked at the north, the Indian Ocean and its surrounding atmosphere behave in such a way that the ocean-atmosphere interaction over this domain is different from that over the other oceans, exhibiting a peculiar ...
An interactive software package for validating satellite data
(Universidad de Concepcion, 2004)
Earth observation satellite launched in the last three decades have made vital contributions to the understanding of the planet. The earth system consisting of land, oceans and atmosphere is linked together by a number of ...
A cold pool south of Indo-Sri Lanka channel and its intrus on into the southeastern Arabian Sea during winter
(Elsevier, 2008)
During winter, south of the Indo-Sri Lanka Channel (ISLC), the observed sea-surface temperature (SST) distribution shows a distinct mini-cold pool (MCP) with relatively cooler waters (SST is less than 28 degrees C). All ...
A quality-control procedure for surface temperature and surface layer inversion in the XBT data archive from the Indian Ocean
(American Meteorological Society, 1999)
A quality control procedure has been developed and validated for Expendable Bathythermograph (XBT) data from Indian Ocean archieved at Indian Oceanographic Data Centre (IODC). Two possible sources of errors are considered ...
Validation of multi-channel scanning microwave radiometer onboard OCEANSAT - 1
(Allied, India, 2003)
IRS-P4 (OCEASAT-1) was the first operational oceanographic satellite that India has launched. An extensive validation campaign was unleashed immediately after its launch in May 1999. Various platforms (Ship, Moored buoy, ...
Surface layer temperature inversion in the Bay of Bengal
(NIO, Dona Paula, Goa (India), 2000)
Hydrographic and XBT data archived in the Indian Oceanographic Data Centre (IODC) are used to understand the process of temperature inversions occurring in the Bay of Bengal. The following aspects of the inversions are ...