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Observational evidence for westward propagation of temperature inversions in the southeastern Arabian Sea
(American Geophysical Union, 2004)
A warm pool forms in the southeastern Arabian Sea (SEAS) prior to the onset of the summer monsoon over India in early June; the core
of this warm pool is in the Lakshadweep Sea (LS). XBT and surface salinity data collected ...
Remote forcing annihilates barrier layer in southeastern Arabian Sea
(American Geophysical Union, 2004)
Time-series measurements of temperature and salinity profiles were made every two hours at 74 deg 30'E, 9 deg 13'N in the southeastern Arabian Sea (SEAS) during 22 March to 7 April and 23 May to 7 June 2003 as part of ...
On the diurnal ranges of sea surface temperature (SST) in the north Indian Ocean
(Indian Academy of Sciences, 2009)
This paper describes the variability in the diurnal range of SST in the north Indian Ocean using in situ measurements and tests the suitability of simple regression models in estimating the diurnal range. SST measurements ...
Modeling the barrier-layer formation in the South-Eastern Arabian Sea
(American Meteorological Society, 2007)
The effect of salinity on the formation of the barrier layer (BL) in the South-Eastern Arabian Sea (SEAS) is investigated using an ocean general circulation model. In accordance with previous studies, the runoff distribution ...
Intraseasonal response of the northern Indian Ocean coastal waveguide to the Madden-Julian Oscillation
(American Geophysical Union, 2009)
A new observational record of upper-ocean currents at 15 degrees N on the western coast of India is dominated by intraseasonal (55-110 day) variations of alongshore currents, whereas sea level at the same location has a ...
Minima of interannual sea-level variability in the Indian Ocean
(Elsevier, 2010)
Wavelet analysis of altimeter sea level in the Indian Ocean shows regions of high variability (maxima) and low variability (minima) at all time scales. At interannual time scales, i.e., at periods of 17 months or more, ...
Comment on "The Great Sumatra-Andaman Earthquake of 26 December 2004"
(American Association for the Advancement of Science, 2005)
Lay et al. (Special Section, 20 May 2005, p.1127) estimated a 600-km length for the tsunami source region. Adding tide-gauge data from Paradip, the northernmost of the Indian east-coast stations and therefore the most ...