BOMEX: period III upper ocean soundings
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BOMEX: period III upper ocean soundings

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Published by U.S. Dept. of Commerce, National Oceanic and Atmosphereic Administration, Environmental Research Laboratories; [for sale by the Supt. of Docs., U.S. Govt. Print. Off., Washington] in Rockville, Md .
Written in English



  • North Atlantic Ocean.


  • Oceanography -- North Atlantic Ocean

Book details:

Edition Notes

Bibliography: p. 352.

Statement[by] Victor E. Delnore [and] John McHugh.
ContributionsMcHugh, John, joint author., Environmental Research Laboratories (U.S.)
LC ClassificationsGC491 .D42
The Physical Object
Paginationiii, 352 p.
Number of Pages352
ID Numbers
Open LibraryOL5024726M
LC Control Number73603137

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  Numerical simulation of thermohaline convection in the upper ocean - Volume 96 Issue 4 - Victor E. Delnore J. BOMEX Period III Upper Ocean Soundings. Nat. Oceanic and Atmospheric Admin. Washington: U.S C. A. Numerical simulations of the natural variability in water temperature during BOMEX using alternative forms of the Cited by: 7. The regularity and completeness of temperature soundings for a day period during the Barbados Oceanographic and Meteorological Experiment (BOMEX) has permitted an analysis of the diurnal variation in temperature at all depths in the oceanic mixed layer at five fixed-ship by: Fig. 1. BOMEX fixed-ship array during Phases 1, 2 and 3. the fixed ship locations during the analysed period. The rawinsonde observations extend from the sea surface to mb above the surface with a vertical resolution of 10mb. The time interval between soundings is /2 hours with the exception of. Bathymetric Soundings. The sources of soundings used in SRTM30_PLUS (version ) are detailed in Becker et al.. They listed 10 of the largest compilation sources, which are (1) Marine Geophysical Trackline Data (GEODAS) archived at the IHO Data Center for Digital Bathymetry, (2) gridded swath multibeam bathymetry data cleaned and.

Deep seismiC sounding was proposed by G. A. Gamburtsev and developed under his guid­ ance during the period at the Institute of Physics of the Earth of the Academy of Sciences of the USSR. During that period also, the first geophysical results concerning the deep structure of the earth's crust in several regions in Tien-Shan, the. Felt, Hali. Soundings: The Story of the Remarkable Woman Who Mapped the Ocean Floor., Print. Awards: N/A. Quantitative Reading Level: Lexile: N/A, ATOS Book Level: , AR Interest Level: Upper Grades () Plot: I t is the story of Marie Tharp a woman geologist who mapped out the ocean floor. Before her theories were accepted, Marie had a hard time in the scientific community because. Select a region. North America ; South America ; South Pacific ; Antarctica ; Arctic ; Europe ; Africa ; Southeast Asia ; Mideast. a. vertical distance from the chart sounding datum to the ocean bottom, plus the height of tide b. vertical distance from the chart sounding datum to the ocean bottom c. average height of water over a specified period of time. d. average height of all low waters at a place A .

The time scale begins at UTC 1 Sep The small diamond symbols denote the time the profiler started rising. Strong vertical shear was observed between and 1 Sep, with concurrent upper-ocean cooling shown by the rise of isotherms to the surface and the propagation of momentum into the stratified upper ocean.   Temperature, relative humidity, and mixing ratio differences ( hPa to the surface) between the Jordan mean sounding and the mean sounding presented here ranged from only ° to °C, % to %, and to g kg −1, suggesting that the two soundings were quite highly correlated. GOES SAL-tracking satellite imagery was then.   An observational evidence in support of such a trend is given by SethuRaman (), who also shows dramatic changes in CON in response to a rapid shift in wind direction. Parameterization of Air-Sea Exchanges PARAMETERIZATION OF AIR-SEA EXCHANGES In addition to the transfer of momentum between the atmosphere and the ocean at their. Wind rose for the Guadeloupe upper-air station for the average and hPa level winds. Radius is the relative frequency of soundings in a 10° azimuthal increment over a 3-yr period (–07).