Seawater Flashcards

1
Q

three fundamental properties of water that are of most interest to marine geochemists are:

A

salinity
temperature
pressure

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2
Q

used to characcterize water masses

A

salinity and temperature

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3
Q

moves water and chemical components around the oceans

A

thermohaline circulation

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4
Q

this circulation also moves heat around the oceans, and indeed the planet, and is also therefore a fundamental component of the climate system

A

thermohaline circulation

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5
Q

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

A

salinity

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6
Q

In theory, the simplest direct method for the measurement of salinity is:

A

evaporate the water and weigh the salt residue

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7
Q

Salinity in surface ocean waters usually ranges between

A

32-37 (ppt)

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8
Q

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

A

False

evaporation exceeds precipitation

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9
Q

Salinity of mediterranean sea

A

37-39 (ppt)

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9
Q
A
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10
Q

Salinity of Red Sea

A

40-41 (ppt)

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11
Q

True or False: Coastal waters run-off can result in an increase in surface salinities

A

False;

increase in surface salinities

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12
Q

regions in the water column over which rapid salinity changes take place are termed as

A

haloclines

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13
Q

True or False: Both horizontal and vertical temperature variations are found in the ocean

A

True

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14
Q

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

A

surface region

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15
Q

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.

A

∼28°C & ∼-1.9°C

16
Q

with in most cases the warm surface layer being separated from the main
body of the colder deep ocean by the thermocline.

A

vertical temperature stratification

17
Q

three main temperature zones in the vertical ocean

A

surface ocean
thermocline
deep ocean

18
Q

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

A

surface ocean

19
Q

In the surface ocea, heat is mized down to a depth of

20
Q

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

A

False

latitude

22
Q

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

A

thermocline

23
Q

depth of thermocline

A

surface water to 1000m

24
extends to the bottom of the water column
deep ocean
25
waters here are cold, most being at <5C, and although the temperature falls towards the bottom (to 1C), the rate of decrease is very much slower than that found in thermocline
Deep ocean
26
True or False: rate of decrease in temperature in deep ocean is very much slower than that found in thermocline
True
27
function of temperature, salinity, and pressure
density
28
The density of seawater exceeds that of pure water owing to the presence of _
dissolved salts
29
densities of seawater lie in the range of
1024-1028 kgm-3
30
most dramatic change in density with depth is found in the _
upper water layer
31
zone of rapidly increasing density
pynocline
32
acts as a barrier to the mixing of low-density surface ocean and the high denisty deep ocean
pynocline
33
formed in response to the combined rapid vertical changes in the salinity (halocline) and temperature (thermocline)
pynocline