Analysis And Prediction Of The Depth Of The Thermocline And Near Surface Thermal Structure PDF Download

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ENVPREDRSCHFAC Technical Paper

ENVPREDRSCHFAC Technical Paper
Author: Environmental Prediction Research Facility (U.S.)
Publisher:
Total Pages: 40
Release: 1975
Genre: Climatology
ISBN:

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Classification and Analysis/Forecasting of Near-Surface Ocean Thermal Structure

Classification and Analysis/Forecasting of Near-Surface Ocean Thermal Structure
Author: Taivo Laevastu
Publisher:
Total Pages: 35
Release: 1975
Genre: Ocean temperature
ISBN:

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The near-surface ocean thermal structure (surface to ca 400 m) is classified into nine distinct types. The time and space distribution of these types is briefly discussed. A rational method for analysis/prediction of mixed layer depth (MLD) and near-surface thermal structure, which has produced satisfactorily verifiable results, is described and flow diagrams for it are given.


Effects of Weather Upon the Thermal Structure of the Ocean

Effects of Weather Upon the Thermal Structure of the Ocean
Author: United States. Hydrographic Office
Publisher:
Total Pages: 116
Release: 1952
Genre: Ocean temperature
ISBN:

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An investigation was made of the meteorological factors which a ffect the thermal structure of the ocean, and an attempt was made to develop techniques for predicting this structure. A prediction technique is proposed which is based on relationships giving the magnitude of the effects of radiation, evaporation and molecular conduction, convection, and turbulent mixing on the thermal structure. A sample prediction showed promise, but the data indicated that an accurate and operationally useful prediction method required a consideration of the internal waves which produce vertical motion. This factor was investigated for a 2-layer system and for a model in which the density was a continuous function of depth. The main considerations in the first model were seasonal and monthly variations, semidiurnal and diurnal tidal variations, short period variations, and random variations, Study of semidiurnal and diurnal tidal variations led to an empirical formula giving the amplitudes of oscillation in one area as a function of the thickness and density discontinuity of the 2-layer system. Where the data were adequate for a forecast, the formula predicted amplitudes with a fair degree of accuracy. Methods were also developed for predicting the internal oscillations of the continuous density model. A sample prediction showed good agreement at the greater depths; however, discrepancies occurred near the surface.