In spring preceding the record minimum summer ice cover detailed microstructure measurements were made from drifting pack ice in the Arctic Ocean, 110 km from the North Pole. Profiles of hydrography, shear, and temper...In spring preceding the record minimum summer ice cover detailed microstructure measurements were made from drifting pack ice in the Arctic Ocean, 110 km from the North Pole. Profiles of hydrography, shear, and temperature microstructure collected in the upper water column covering the core of the Atlantic Water are analyzed to determine the diapycnal eddy diffusivity, the eddy diffusivity for heat, and the turbulent flux of heat. Turbulence in the bulk of the cold halocline layer was not strong enough to generate significant buoyancy flux and mixing. Resulting turbulent heat flux across the upper cold halocline was not significantly different than zero. The results show that the low levels of eddy diffusivity in the upper cold halocline lead to small vertical turbulent transport of heat, thereby allowing the maintenance of the cold halocline in the central Arctic.展开更多
CTD data on standard levels collected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity. The thermocline...CTD data on standard levels collected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity. The thermocline undergoes remarkable seasonal variation in the South China Sea (SCS), and especially in the region of the north shelf where the thermocline disappears in December. The thermocline is stronger and thicker in July than in December. There is no obvious seasonal variation in the halocline. Due to the upper Ekman transport caused by monsoon over the SCS, the thermocline slopes upward in July and downward in December from east to west in the northern SCS. The characteristics of the thermocline and halocline are influenced by local eddies in the SCS. The Zhujiang diluted flow influences significantly the SCS shelf’s halocline.展开更多
This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the clim...This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the climatological mean conditions and four extreme events, the analysis indicates that wind-induced Ekman transport plays an important role in the extension of the CRDW. The strong northeastward Ekman transport induced by southeasterly wind in 1996, 2003, 2004, and 2006 pushes the core of the CRDW to the sea adjacent to Cheju-do. A comparison of the wind variation before observation among these four extreme events indicates that the expansion pattern of the CRDW is primarily changed by synoptic variation with timescales of days to weeks, such as during a typhoon. The weak eastward extension of the CRDW in 2004, accompanied with a relatively strong southerly wind, implies that the oceanographic state (e.g., the depth of halocline) may strongly affect the impact of wind on the extension of the CRDW.展开更多
基金funded by the Research Council of Norway, through NORKLIMA Young Investigator grant
文摘In spring preceding the record minimum summer ice cover detailed microstructure measurements were made from drifting pack ice in the Arctic Ocean, 110 km from the North Pole. Profiles of hydrography, shear, and temperature microstructure collected in the upper water column covering the core of the Atlantic Water are analyzed to determine the diapycnal eddy diffusivity, the eddy diffusivity for heat, and the turbulent flux of heat. Turbulence in the bulk of the cold halocline layer was not strong enough to generate significant buoyancy flux and mixing. Resulting turbulent heat flux across the upper cold halocline was not significantly different than zero. The results show that the low levels of eddy diffusivity in the upper cold halocline lead to small vertical turbulent transport of heat, thereby allowing the maintenance of the cold halocline in the central Arctic.
文摘CTD data on standard levels collected during July and December in 1998 and the cubic spline interpolating method were used to study the characteristics of the transition layer temperature and salinity. The thermocline undergoes remarkable seasonal variation in the South China Sea (SCS), and especially in the region of the north shelf where the thermocline disappears in December. The thermocline is stronger and thicker in July than in December. There is no obvious seasonal variation in the halocline. Due to the upper Ekman transport caused by monsoon over the SCS, the thermocline slopes upward in July and downward in December from east to west in the northern SCS. The characteristics of the thermocline and halocline are influenced by local eddies in the SCS. The Zhujiang diluted flow influences significantly the SCS shelf’s halocline.
基金supported by the National Natural Science Foundation of China (40906014 and 40976015)the Marine Science Foundation of State Oceanic Administration of China for the Youth (2010218)
文摘This paper presents an analysis of the impact of wind on the transport of the Changjiang River Diluted Water (CRDW) in August by using the salinity data collected on two zonal sections near Cheju-do. Based on the climatological mean conditions and four extreme events, the analysis indicates that wind-induced Ekman transport plays an important role in the extension of the CRDW. The strong northeastward Ekman transport induced by southeasterly wind in 1996, 2003, 2004, and 2006 pushes the core of the CRDW to the sea adjacent to Cheju-do. A comparison of the wind variation before observation among these four extreme events indicates that the expansion pattern of the CRDW is primarily changed by synoptic variation with timescales of days to weeks, such as during a typhoon. The weak eastward extension of the CRDW in 2004, accompanied with a relatively strong southerly wind, implies that the oceanographic state (e.g., the depth of halocline) may strongly affect the impact of wind on the extension of the CRDW.
