Physical Oceanography

123456789
Across
  1. 2. the number of heat units needed to raise the temperature of a body by one degree.
  2. 6. a layer in an ocean or other body of water in which water density increases rapidly with depth.
  3. 7. the degree or intensity of heat present in a substance or object, especially as expressed according to a comparative scale and shown by a thermometer or perceived by touch.
  4. 8. the concentrations of salts in water or soils
  5. 9. seawater density to between 1.02 and 1.03 g/cm3. The density of seawater can be increased by reducing its temperature, increasing its salinity , or increasing the pressure.
Down
  1. 1. vertical zone in the oceanic water column in which salinity changes rapidly with depth
  2. 3. property of a material that expresses the degree of slowness with which its temperature reaches that of the environment
  3. 4. the transition layer between warmer mixed water at the ocean's surface and cooler deep water below
  4. 5. the quality of being hot; high temperature.