Sound Speed Structure of the Western South Atlantic Ocean


Book Description

The sound speed structure of the western South Atlantic Ocean is far more variable than that found in the North Atlantic or North Indian Oceans, largely due to hemispheric position and a wide variety of surface, near-surface, intermediate depth, and near-bottom water masses. In the South Atlantic, summer is defined as January-March and winter as July-September. The wide variety of temperature and salinity variability throughout the western South Atlantic leads to entirely differently shaped sound speed profiles and entirely different values of the depth of the deep sound channel axis and critical depth. These differences undoubtedly have significant effects on acoustic propagation. This report examines western South Atlantic sound speed variability along three cross-sections for both summer and winter, relates variability in sound speed structures to surface currents, the Antarctic Intermediate Water, Mediterrannean Intermediate Water, and Antarctic Bottom Water core flows west of the Mid-Atlantic Ridge, and defines the number of observations deeper than the depth of the deep sound channel axis during both summer and winter for the entire South Atlantic Ocean between the Equator and 45 S latitude. (Author).




Sound-speed Distribution in the Western Indian Ocean


Book Description

Initial results of a continuing study to analyze and summarize the acoustically significant characteristics of the vertical sound-speed structure in the Indian Ocean are presented for purposes of acoustic model inputs and future exercise planning in the region. Data displays cover the western Indian Ocean west of 75 degrees E and north of 20 degrees S. Hydrocast data with computed sound speeds at standard depths provide the basic information to define areas of the Indian Ocean that are reasonably homogeneous with regard to sound-speed properties and can be summarized by a single profile for each season. Seasonal data presentations of bottom conjugate depth (the shallow conjugate of the bottom sound speed) and depth excess (water depth below the deep conjugate of the near-surface sound-speed maximum) indicate the primarily bottom-limited situation in the western Indian Ocean and identify the restricted areas of the Somali Basin with convergence-zone propagation potential. The upper-layer characteristics of layer depth, in-layer gradient, and below-layer gradient are displayed seasonally in contour format based on sound-speed-converted BT and XBT temperature data. Emphasis is placed on the significant effects of the seasonal monsoons, and in particular the strong SW Monsoon, on the near-surface structure. Results based on the two data sources are presented separately and some comparisons are made.




The Upper and Deep Sound Channel in the Northeast Atlantic


Book Description

Analysis of extensive historical sound velocity profile data east of the Mid-Atlantic Ridge between 20 degrees N latitude and Iceland indicates that warm, saline Mediterranean Intermediate Water and the effects of annual heating and cooling are responsible for marked departures from the basic trilinear vertical sound velocity structure found in most open ocean areas. South of about 43 degrees N latitude, Mediterranean Intermediate Water between 1000 and 1300 meters causes the formation of a subsurface sound velocity maximum, thereby creating an upper sound channel and a depressed deep sound channel. North of about 50 degrees N latitude, winter cooling causes the formation of a subsurface sound velocity maximum and summer warming results in the formation of a somewhat shoaler upper sound channel. Temperature-salinity and sound velocity comparisons for 12 selected locations throughout the Northeast Atlantic Ocean are presented in the appendix. (Author).




The Sound Velocity Structure of the North Atlantic Ocean


Book Description

All available sound velocity data in the North Atlantic Ocean between 15 degrees and 65 degrees N. latitude and east of 65 degrees W. longitude (excluding the Labrador Sea) have been analyzed in terms of the seasonal areal extent and average axial depth of the upper sound channel, the annual areal extent and average depth of the subsurface sound velocity maximum, and the annual average depth of the deep sound channel axis. The vertical extent of these and other sound velocity structures are shown on nine north-south and nine east-west sound velocity cross-sections that extend to a maximum depth of 5000 meters. These cross sections include four winter/summer pairs along the same meridian and three winter/summer pairs along the same parallel. In addition, sound velocity/temperature-salinity comparisons for winter and summer are given for 50 locations throughout the North Atlantic Ocean. (Author).













Tables of the Velocity of Sound in Sea Water


Book Description

Tables of the Velocity of Sound in Sea Water contains tables of the velocity of sound in sea water computed on a "Strela-3" high-speed electronic computer and a T-5 tabulator at the Computational Center of the Academy of Sciences. Knowledge of the precise velocity of sound in sea water is of great importance when investigating sound propagations in the ocean and when solving practical problems involving the use of hydro-acoustic devices. This book demonstrates the computations made for the velocity of sound in sea water, which can be found in two ways: by direct measurement with the aid of suitable equipment, and by calculation from formula expressing the dependence of the velocity on the temperature and salinity of the water. This book will be of great value to researchers and students.