FN Archimer Export Format
PT J
TI Hydrology and circulation in the Strait of Hormuz and the Gulf of Oman - Results from the GOGP99 experiment: 2. Gulf of Oman - art. no. C12038
BT 
AF POUS, Stephane
   CARTON, Xavier
   LAZURE, Pascal
AS 1:;2:;3:;
FF 1:PDG-DEL-AO;2:;3:PDG-DOP-DCB-DYNECO-PHYSED;
C1 IFREMER BREST, Lab Phys Oceans, Direct Environm & Amenagement Littoral Applicat O, F-29280 Plouzane, France.
   IFREMER, CNRS, UBO, Lab Phys Oceans, Brest, France.
C2 IFREMER, FRANCE
   IFREMER, FRANCE
SI BREST
   UBO
SE PDG-DEL-AO
   PDG-DOP-DCB-OPS-LPO
   PDG-DOP-DCB-DYNECO-PHYSED
IN WOS Ifremer jusqu'en 2018
IF 2.839
TC 36
UR https://archimer.ifremer.fr/doc/2004/publication-390.pdf
LA English
DT Article
DE ;Persian Gulf Water outflow;Regional circulation;Gulf of Oman
AB Hydrological, ADCP, and drifting buoy data obtained during the GOGP99 Experiment in October and early November 1999 are analyzed to describe the Persian Gulf Water (PGW) core and the regional circulation in the Gulf of Oman. The warm and salty PGW core flows out of the Strait of Hormuz heading southeastward unto (25degrees20'N, 57degreesE), approximately. From there, it cascades down the continental slope, veers southwestward, and joins the Omani coast near (24degrees50'N, 56degrees50'E) to form a slope current. This PGW current has then thermohaline maxima on isopycnal sigma(0) = 26.5, near 220 m depth. Its thermohaline characteristics decrease along its progression to Ra's al Hadd ( and then offshore into the Arabian Sea) but maintain a sharp contrast with surrounding waters. Outflow variability at the Strait of Hormuz can be related to downstream fluctuations of the thermohaline maxima in the PGW core at gulf scale and over a 2- to 3-week period. Moreover, several mechanisms (baroclinic instability, flow intermittency, cape effects) are examined to explain the widening of this PGW core upstream and downstream of Ra's al Hamra. In the eastern part of the Gulf of Oman, the regional circulation is a cyclonic gyre. The circulation in the western part of the Gulf is more complex, with the outflow of PGW and southeastward currents in the upper 250 m near the Omani coast, and a recirculation of upwelled waters near Ra's Jagin (on the Iranian coast). The large cyclonic gyre occupies at least the upper 300 m of the water column and undergoes little variation over a month. The PGW outflow in the northern Arabian Sea is southward and located 50-100 km from the coast. It borders a shallower northward current located offshore.
PY 2004
PD DEC
SO Journal of Geophysical Research Oceans
SN 0148-0227
PU American Geophysical Union
VL 109
IS C12
UT 000226134700002
DI 10.1029/2003JC002146
ID 390
ER

EF