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Negative Oceanic Heat Flux as a Cause of Water-Mass Formation
Negative Oceanic Heat Flux Water-Mass Formation
2009/4/3
Regions of large (>60 kcal cm−2 year−1) net annual heat flux from the oceans to the atmosphere are found only on the western sides of Northern Hemisphere oceans and in the Norwegian Sea, a...
The problem of mass transport induced by monochromatic waves in a viscous fluid of infinite depth and infinite lateral extent is examined. The fluid viscosity is assumed constant and the effects of Co...
Winter Circulation in the Western Gulf of Maine：Part 1. Cooling and Water Mass Formation
Winter Circulation Western Gulf Water Mass Formation
2009/2/23
The mean circulation on the northeast continental shelf in the region of the Gulf of Mexico is discussed in terms of a simple box model, based on volume transports and mean salinities estimated from e...
On the Momentum, Vorticity and Mass Balance on the Oregon Shelf
Mass Balance Oregon Shelf Velocity measurements
2009/2/23
Velocity measurements from the continental shelf off Oregon taken during the Coastal Upwelling Experiment CUE-2 in the summer of 1973 are utilized to investigate momentum, vorticity and mass balance r...
On Lateral Water Mass Interaction—A Case Study, Bristol Bay, Alaska
Lateral Water Mass Interaction Bristol Bay Alaska
2009/2/13
Salinity-temperature-depth data obtained on several spring and summer cruises during 1976 and 1977 from outer Bristol Bay in the southeast Bering Sea indicate the existence of a zone, between two well...
Mixing and Water-Mass Formation in the Australian Subantarctic
Water-Mass Formation Australian Subantarctic
2009/2/10
A cruise south of eastern Australia confirmed the formation of a Subantarctic Mode Water type in late winter on the equatorward side of the Subantarctic Front. This water type, mixed with the winter s...
Water-Mass Distributions at Intermediate Layers off the Somali Coast during the Onset of the Southwest Monsoon, 1979
Water-Mass Distributions Intermediate Layers Somali Coast
2009/2/8
Hydrographic observations at intermediate depth in the Somali Basin have been made during and after the transition from the northeast monsoon to the southwest monsoon, 1979. The data are discussed in ...
Estimates of Mass, Momentum and Kinetic Energy Fluxes of the Gulf Stream
Kinetic Energy Fluxes Gulf Stream
2009/2/6
Mass, momentum and kinetic-energy fluxes in the Gulf Stream have been estimated from hydrographic data taken by Fuglister in the Gulf Stream ’60 project; the data cover the Stream as it flows eastward...
Development of Near-Surface Flow Pattern and Water Mass Distribution in the Somali Basin in Response to the Southwest Monsoon of 1979
Somali Current East African Coastal Current East African Coastal Current
2009/2/6
Near-surface observations of temperature, salinity and current are used to describe the seasonal reversal of the Somali Current during 1979, in response to the onset of the southwest monsoon winds. Du...
Mass, Heat, Salt and Nutrient Fluxes in the South Pacific Ocean
Mass Heat Salt Nutrient Fluxes South Pacific Ocean
2009/2/5
An inverse method has been applied to the Scorpio sections spanning the subtropical gyre of the South Pacific. In addition to constraints upon geostrophic fluxes of mass and salt, constraints were wri...
Water-Mass and Transport Variability at 110°W in the Equatorial Pacific
North Equatorial Countercurrent Northern Subsurface Countercurrent empirical orthogonal function
2009/1/22
An analysis of nine hydrographic sections collected in 1979–81 along 110°W in the equatorial Pacific Ocean is presented. Sections typically sampled the upper 500 m of the water column from 10°N to 3°S...
The Relative Roles of Diapycnal and Isopycnal Mixing on Subsurface Water Mass Conversion
Isopycnal Mixing Fluid motion Subsurface Water Mass Conversion
2009/1/21
Fluid motion in the sea is known to occur predominantly along quasi-horizontal neutral surfaces but the very small diapycnal (i.e., across isopycnal) velocities often make a significant contribution t...
Poleward heat transport by the own implies warm Water mass formation, i.e., the retention by the tropical and subtropical ocean of some of its net radiant heat gain. Under what condition net heat rete...
Mass, Heat and Freshwater Fluxes in the South Indian Ocean
Mass Heat Freshwater Fluxes South Indian Ocean
2009/1/13
Six hydrographic sections were used to examine the circulation and property fluxes in the South Indian Ocean from 10° to 32°S. The calculations were made by applying an inverse method to the data. In ...
Water Mass Structure during the POLYMODE Local Dynamics Experiment
local Dynamics Experiment Water Mass Structure
2009/1/10
The seven intensive hydrographic surveys of temperature, salinity and oxygen of the POLYMODE local Dynamics Experiment (LDE) (15 May–15 July 1978) were carded out in a 200 km-wide octagonal region cen...