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6. Salinity and Precipitation

 

 

The Briny Deep
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1. Objectives
2.  Salt in Seawater?
3. Ions of Salt
4. Source of the Salt?
5. Salinity Variability
6. Salinity & Precipitation
7. Salinity & Precipit II
8. Salinity Summary
9. Calculating Salinity
10. Ocean Temperature
11. Solar Radiation
12. Properties
13. Light Penetration
14. Temperature
15. Thermocline
16. Density
17. Layering

The map below shows the global distribution of the difference between the annual amount of precipitation (P) and evaporation (E),

or

P - E

This balance is influenced by the temperature and amount of water vapor in the atmosphere in a particular region.

Used with Permission of Matthias Tomczak ©Copyright 1997

The color scale of P-E, located at the bottom of the map, is given in centimeters per year (cm/yr) with reddish colors indicating more precipitation than evaporation , whereas blue to green colors indicate more evaporation than precipitation.

Notice the subtle difference in color between the dark purple (>250 cm/year), dark blue (-100 to -150 cm/year) and black (more negative than -150 cm/year).

By examining the P-E values in the map above at which latitude ranges  would you expect to find:

  1. the high salinity waters in the surface of the ocean?

  2. the low salinity sea water along the ocean surface?

©Copyright 1999
March 13, 1999

Send to Don Reed

Department of Geology
San Jose State University

#4 What influences the annual amount of precipitation and evaporation?

a) Temperature.
b) Water Vapor in the Atmosphere.
c) Salinity in the ocean.
d) All of the above.
e) a and b