14. Figure 5B-4 shows temperature and salinity values representative of waters at those same depths throughout much of the Mediterranean. This water flows over the Gibraltar sill (which rises to a depth of about 290 m) and into the Atlantic, where it mixes with some cooler and less saline water then sinks to within a few hundred meters of 1000 m depth. This is the origin of the a. North Atlantic Central Surface Water b. Mediterranean Intermediate Water c. North Atlantic Deep Water
14. Figure 5B-4 shows temperature and salinity values representative of waters at those same depths throughout much of the Mediterranean. This water flows over the Gibraltar sill (which rises to a depth of about 290 m) and into the Atlantic, where it mixes with some cooler and less saline water then sinks to within a few hundred meters of 1000 m depth. This is the origin of the a. North Atlantic Central Surface Water b. Mediterranean Intermediate Water c. North Atlantic Deep Water
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Water mass is a volume of seawater with temperature, salinity and therefore density. There are numerous water masses in the ocean, mainly in the Atlantic. There are three three types of water masses-upper waters(0-500m), intermediate waters(500m-1500m) and deep waters(1500m-bottom).
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