Seawater Flashcards
three fundamental properties of water that are of most interest to marine geochemists are:
salinity
temperature
pressure
used to characcterize water masses
salinity and temperature
moves water and chemical components around the oceans
thermohaline circulation
this circulation also moves heat around the oceans, and indeed the planet, and is also therefore a fundamental component of the climate system
thermohaline circulation
measure of the degree to which the water in the oceans is salty, and is a weight of total solids dissolved in a quantity of seawater
salinity
In theory, the simplest direct method for the measurement of salinity is:
evaporate the water and weigh the salt residue
Salinity in surface ocean waters usually ranges between
32-37 (ppt)
True or False: Higher values of salinity are found in some semi-enclosed, mid-latitude seas and coastal water where evaporation does not exceed precipitation and runoff
False
evaporation exceeds precipitation
Salinity of mediterranean sea
37-39 (ppt)
Salinity of Red Sea
40-41 (ppt)
True or False: Coastal waters run-off can result in an increase in surface salinities
False;
increase in surface salinities
regions in the water column over which rapid salinity changes take place are termed as
haloclines
True or False: Both horizontal and vertical temperature variations are found in the ocean
True
The main horizontal variations occur in the __ with temperatures ranging from 28 C in the equatorial zones to as low as -1.9C, freezing point of seawater, in the polar seas
surface region
The main horizontal
variations occur in the surface region, with temperatures ranging from _ in the equatorial zones to as
low as _, the freezing point of seawater, in the polar seas.
∼28°C & ∼-1.9°C
with in most cases the warm surface layer being separated from the main
body of the colder deep ocean by the thermocline.
vertical temperature stratification
three main temperature zones in the vertical ocean
surface ocean
thermocline
deep ocean
waters are heated by solar energy and the heat is mixed down to a depth of around 100-200 m, with the temperatures reflecting those of the latitude at which the water is found
surface ocean
In the surface ocea, heat is mized down to a depth of
100-200 m
True or False: In the surface ocean, the waters are heated by solar energy and the heat is mized down to a depth of around 100-200m, witht the temperatures reflecting those of the longitude at which the water is found
False
latitude
Below the surface, or mixed, layer, the temperatures decrease rapidly with depth through a zone that extends from the base of the surface layer down to as deep as 1000m in some places
thermocline
depth of thermocline
surface water to 1000m