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Interannual to Interdecadal Salinity Variations Observed Near Hawaii:Local and Remote Forcing by Surface Freshwater Fluxes
Interdecadal Salinity Variations Observed Near Hawaii Local and Remote Forcing Surface Freshwater Fluxes
2015/7/20
Ray Schmitt's introduction to this issue underlines the importance of including the oceanic component of the hydrological cycle in considerations of Earth's climate. Spatial and temporal salinity vari...
Recent Arctic Climate Change and Its Remote Forcing of Northwest Atlantic Shelf Ecosystems
Climate Change Northwest Atlantic Shelf Ecosystems
2015/7/15
During recent decades, historically unprecedented changes have
been observed in the Arctic as climate warming has increased precipitation, river
discharge, and glacial as well as sea ice melting. ...
The Seasonal Upwelling in the Gulf of Guinea Due to Remote Forcing
Seasonal Upwelling Remote Forcing Gulf of Guinea
2009/2/23
A linear model on an equatorial β plane is integrated over a 120-day period in a basin that approximates the tropical Atlantic Ocean. An increase in the westward wind stress of 0.025 N m−2 in th...
Evidence of Remote Forcing in the Equatorial Atlantic Ocean
sea-surface temperature Equatorial Atlantic Ocean
2009/2/7
An analysis of sea-surface temperature (SST) and surface winds in selected areas of the tropical Atlantic indicates that the nonseasonal variability of SST in the eastern equatorial Atlantic (Gulf of ...
Subtidal Response of Scotian Shelf Circulation to Local and Remote Forcing. Part II：Barotropic Model
Scotian Shelf Circulation Barotropic Model
2008/12/22
A linear, barotropic numerical model that features realistic bathymetry of the Scotian Shelf provides solutions forced by steady and periodic wind stress that are generally incoherent on spatial scale...
Subtidal Response of Scotian Shelf Circulation to Local and Remote Forcing. Part I：Observations
Canadian Atlantic Storms Program shelf subsurface pressure Scotian Shelf Circulation
2008/12/22
Data collected during the Canadian Atlantic Storms Program (CASP) suggest that two primary current regimes exist on the Scotian Shelf during winter. Moorings inside the 100-m isobath feature currents ...