Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon
Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling...
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| Autor*in: |
Vimal Kumar, K. G. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2007 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media B.V. 2007 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental monitoring and assessment - Springer Netherlands, 1981, 140(2007), 1-3 vom: 02. Aug., Seite 231-247 |
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| Übergeordnetes Werk: |
volume:140 ; year:2007 ; number:1-3 ; day:02 ; month:08 ; pages:231-247 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10661-007-9863-3 |
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OLC2073728375 |
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| 245 | 1 | 0 | |a Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon |
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| 520 | |a Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. | ||
| 650 | 4 | |a Upwelling | |
| 650 | 4 | |a Arabian Sea high salinity water | |
| 650 | 4 | |a Pole-ward undercurrent | |
| 650 | 4 | |a Arabian Sea | |
| 650 | 4 | |a Hydrography | |
| 700 | 1 | |a Dinesh Kumar, P. K. |4 aut | |
| 700 | 1 | |a Smitha, B. R. |4 aut | |
| 700 | 1 | |a Habeeb Rahman, H. |4 aut | |
| 700 | 1 | |a Josia, Jacob |4 aut | |
| 700 | 1 | |a Muraleedharan, K. R. |4 aut | |
| 700 | 1 | |a Sanjeevan, V. N. |4 aut | |
| 700 | 1 | |a Achuthankutty, C. T. |4 aut | |
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10.1007/s10661-007-9863-3 doi (DE-627)OLC2073728375 (DE-He213)s10661-007-9863-3-p DE-627 ger DE-627 rakwb eng 333.7 VZ Vimal Kumar, K. G. verfasserin aut Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2007 Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography Dinesh Kumar, P. K. aut Smitha, B. R. aut Habeeb Rahman, H. aut Josia, Jacob aut Muraleedharan, K. R. aut Sanjeevan, V. N. aut Achuthankutty, C. T. aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 140(2007), 1-3 vom: 02. Aug., Seite 231-247 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:140 year:2007 number:1-3 day:02 month:08 pages:231-247 https://doi.org/10.1007/s10661-007-9863-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 140 2007 1-3 02 08 231-247 |
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10.1007/s10661-007-9863-3 doi (DE-627)OLC2073728375 (DE-He213)s10661-007-9863-3-p DE-627 ger DE-627 rakwb eng 333.7 VZ Vimal Kumar, K. G. verfasserin aut Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2007 Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography Dinesh Kumar, P. K. aut Smitha, B. R. aut Habeeb Rahman, H. aut Josia, Jacob aut Muraleedharan, K. R. aut Sanjeevan, V. N. aut Achuthankutty, C. T. aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 140(2007), 1-3 vom: 02. Aug., Seite 231-247 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:140 year:2007 number:1-3 day:02 month:08 pages:231-247 https://doi.org/10.1007/s10661-007-9863-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 140 2007 1-3 02 08 231-247 |
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10.1007/s10661-007-9863-3 doi (DE-627)OLC2073728375 (DE-He213)s10661-007-9863-3-p DE-627 ger DE-627 rakwb eng 333.7 VZ Vimal Kumar, K. G. verfasserin aut Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2007 Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography Dinesh Kumar, P. K. aut Smitha, B. R. aut Habeeb Rahman, H. aut Josia, Jacob aut Muraleedharan, K. R. aut Sanjeevan, V. N. aut Achuthankutty, C. T. aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 140(2007), 1-3 vom: 02. Aug., Seite 231-247 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:140 year:2007 number:1-3 day:02 month:08 pages:231-247 https://doi.org/10.1007/s10661-007-9863-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 140 2007 1-3 02 08 231-247 |
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10.1007/s10661-007-9863-3 doi (DE-627)OLC2073728375 (DE-He213)s10661-007-9863-3-p DE-627 ger DE-627 rakwb eng 333.7 VZ Vimal Kumar, K. G. verfasserin aut Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2007 Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography Dinesh Kumar, P. K. aut Smitha, B. R. aut Habeeb Rahman, H. aut Josia, Jacob aut Muraleedharan, K. R. aut Sanjeevan, V. N. aut Achuthankutty, C. T. aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 140(2007), 1-3 vom: 02. Aug., Seite 231-247 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:140 year:2007 number:1-3 day:02 month:08 pages:231-247 https://doi.org/10.1007/s10661-007-9863-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 140 2007 1-3 02 08 231-247 |
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10.1007/s10661-007-9863-3 doi (DE-627)OLC2073728375 (DE-He213)s10661-007-9863-3-p DE-627 ger DE-627 rakwb eng 333.7 VZ Vimal Kumar, K. G. verfasserin aut Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2007 Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography Dinesh Kumar, P. K. aut Smitha, B. R. aut Habeeb Rahman, H. aut Josia, Jacob aut Muraleedharan, K. R. aut Sanjeevan, V. N. aut Achuthankutty, C. T. aut Enthalten in Environmental monitoring and assessment Springer Netherlands, 1981 140(2007), 1-3 vom: 02. Aug., Seite 231-247 (DE-627)130549649 (DE-600)782621-7 (DE-576)476125413 0167-6369 nnns volume:140 year:2007 number:1-3 day:02 month:08 pages:231-247 https://doi.org/10.1007/s10661-007-9863-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OLC-IBL GBV_ILN_22 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4219 AR 140 2007 1-3 02 08 231-247 |
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333.7 VZ Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon Upwelling Arabian Sea high salinity water Pole-ward undercurrent Arabian Sea Hydrography |
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Vimal Kumar, K. G. Dinesh Kumar, P. K. Smitha, B. R. Habeeb Rahman, H. Josia, Jacob Muraleedharan, K. R. Sanjeevan, V. N. Achuthankutty, C. T. |
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hydrographic characterization of southeast arabian sea during the wane of southwest monsoon and spring intermonsoon |
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Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon |
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Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. © Springer Science+Business Media B.V. 2007 |
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Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. © Springer Science+Business Media B.V. 2007 |
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Abstract Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September–October 2003 (later phase of Southwest monsoon, SWM) and March–April 2004 (Spring inter monsoon, SIM). During the later phase of the SWM, upwelling was in the withdrawal phase and the frontal structure was clearer in the northern sections (13 and 15°N lat) indicating strong upwelling in the area. The driving force of upwelling is identified as the combination of alongshore wind stress and remote forcing with a latitudinal variability. Although a more prominent upwelling was found in the north, a maximum surface Chlorophyll-a was found in the south (10°N). During the SIM, the area was characterized by oligotrophic water with relatively high Sea Surface Temperature (>29°C) and low salinity (33.8 to 35.4). During March, the surface hydrography was found to be controlled mainly by the intrusion of low-saline waters from the south, while during September by the high saline water from the north. The presence of various water masses [Arabian Sea High Salinity Water (ASHSW), Persian Gulf Water (PGW), Red Sea Water (RSW)] and their seasonal variations in the region is discussed and their decreasing influence towards the south is noted during both periods of observation. During the SWM, the dynamic topography showed the equator-ward flow of the West India Coastal Current (WICC) at the surface and a pole-ward coastal under current at sub-thermocline depth. During the SIM, surface circulation revealed the WICC flowing pole-ward north of 13°N, but equator-ward flow in the south, with a clockwise circulation around the Lakshadweep High. © Springer Science+Business Media B.V. 2007 |
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