Summer cooling of the Arabian Sea during contrasting monsoons
نویسندگان
چکیده
منابع مشابه
Moored observations of upper-ocean response to the monsoons in the Arabian Sea during 1994–1995
The role of surface forcing in the semiannual evolution of the upper-ocean temperature, salinity, and velocity fields in the Arabian Sea is examined. To do so, variability in the upper ocean in the central Arabian Sea was observed from an array of moorings deployed from October 1994 to October 1995. The Northeast (NE) Monsoon was characterized by moderate winds, clear skies, and dry air; sea-su...
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For more informat ion, c o n t a c t E t i enne Ruellan, CNRS, G e o s c i e n c e s Azur, 2 5 0 Rue A. Ein stein, S o p h i a Antipolis , 0 6 5 6 0 V a l b o n n e , F r a n c e (e-mai l r ue l l an@fa i l l e . un i ce . f r ) . The five elements of the moored array were set in a 50-km 2 pattern centered at 15°30'N, 61°30'E. The central mooring was the most heavily instrumented. Two meteoro...
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[1] Positive Indian Ocean Dipole (IOD) events generally tend to be accompanied by intensified summer monsoon flows and above normal precipitation over the subcontinent; although strong monsoons have not always coincided with positive IOD events. Numerical simulation experiments and supplementary data diagnostics are performed to understand the IOD sub-surface dynamics in relation to the monsoon...
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[1] We describe the dynamics of the formation of an elevated land plume over the Arabian Sea and northern Indian Ocean observed during the 1999 Indian Ocean Experiment (INDOEX). The presence of the elevated plume above the marine boundary layer for a depth of about 2000 m could be inferred from the thermodynamic profiles of the lower troposphere obtained from research vessels in 1997, 1998, and...
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ژورنال
عنوان ژورنال: Geophysical Research Letters
سال: 2004
ISSN: 0094-8276
DOI: 10.1029/2004gl019961