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Observations of Upper Ocean Temperature and Salinity Structure During the POLE Experiment
Upper Ocean Temperature Salinity Structure POLE Experiment
2009/2/13
Mid-ocean observations (35°N, 155°W) of temperature and salinity were made from R/P Flip during the period 28 January-14 February 1974 as part of the NORPAX POLE Experiment.
Autocorrelations for th...
Upper Ocean Temperature Structure, Inertial Currents, and Richardson Numbers Observed during Strong Meteorological Forcing
Upper Ocean Temperature Inertial Currents Meteorological Forcing
2009/1/16
Upper ocean currents and temperature in the northeastern Pacific were measured during a 14-day period in November 1980 as part of STREX. Velocities in the upper ocean are dominated by near-inertial fr...
Statistics of Internal Wave Overturning from Observations of Upper Ocean Temperature
Internal Wave Upper Ocean Temperature
2009/1/13
The seasonal thermocline in the Sargasso Sea near 30°45′N, 71°45′W was measured in July 1981 using a towed thermistor army with 0.5 m horizontal and vertical resolution. A 200-km long section of the s...
ENSO Signals in Global Upper-Ocean Temperature
Global Upper-Ocean Temperature sea surface temperature
2008/12/12
The time-space evolution of the El Niño-Southern Oscillation in sea surface temperature (SST) and heat storage of the upper 400 m (HS400) for the Pacific, Indian, and Atlantic Oceans is investi...
Evolution of Interdecadal Variability in Sea Level Pressure, Sea Surface Temperature, and Upper Ocean Temperature over the Pacific Ocean
Interdecadal Variability Sea Level Pressure Sea Surface Temperature Upper Ocean Temperature Pacific Ocean
2008/7/16
Interdecadal variability in sea level pressure (SLP) and sea surface temperature (SST) anomalies in the Pacific Ocean was “quasiperiodic” from 1900–91. The coherent variability of this phenomenon is i...
Inversion of Upper Ocean Temperature Time Series for Entrainment, Advection, and Diffusivity
Upper Ocean Temperature Time Series Entrainment Advection Diffusivity
2008/6/26
An inversion technique for estimating the terms of the oceanic near-surface heat transport is extended to include the vertical heat flux at the bottom of the surface mixed layer. The mixed-layer heat ...