How much salt is there?
Probably more than you think. Some scientists estimate that the oceans contain as much as 50 quadrillion tons (50 million billion tons) of dissolved solids. If the
salt in the sea could be removed and spread evenly over Earth's land surface it would form a layer more than 500 feet thick (152.4 meters), about the height of a 40-story building.
Seawater is 220 times saltier than fresh lake water. Unrefined sea salt contains 98.0% sodium chloride and up to 2.0% other minerals (salts). Together there are over 100 minerals, composed
of 80 chemical elements, in sea salt. The composition of a single crystal of ocean salt is so complicated that no laboratory in the world can produce it from its basic 80 chemical elements.
(From "Why is the Ocean Salty" by Herbert Swenson, US Geological Survey)
Where does the salt come from?
The answer may surprise you.
How much salt is there relative to water?
Yes, there is a lot of salt in the ocean, but there is a lot more water. In ocean waters of average salt content (35 psu), the
weight of water is over 28.5 times greater than the weight of salt it contains. Oceanographers use the measure of salinity
to describe the relative amount of salt to water.
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Is salinity uniform throughout the ocean?
No. Although the amount of salt in the ocean is relatively constant on time scales of years to decades, sea surface salinity (SSS)
varies because freshwater input & ouput – part of the global hydrologic or water cycle – varies from place-to-place. The large scale
pattern of evaporation and precipitation is established by earth's atmospheric convection cells. In the simplest case – for example, if earth
were covered by oceans and not spinning (shown at right) – the atmosphere would move heat between the hot tropics and cold poles in a very simple way. Hot air would rise along
the equator, creating a band of low atmospheric pressure. Cold air would sink at the poles, creating regions of high atmospheric pressure.
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The presence of continents and earth's rotation complicates the idealized "two cell" system. A fairly realistic model of earth's atmospheric circulation
consists of six cells: three on each side of the equator (shown at left). This pattern has atmospheric pressure highs at the poles, 30°N and 30°S. It also
has atmospheric lows along the equator, 60°N and 60°S. Away from the poles, cloudiness and precipitation (P) dominate bands of low pressure: these latitudes
host the world's rainforests. Dryness and evaporation (E) dominate bands of high pressure: these latitudes are home to deserts.
In terms of SSS, lower salinity generally occurs where precipitation is greater than evaporation (P>E). Higher SSS generally occurs where evaporation is greater than precipitation (E>P).
Compare this "six cell" model with the map of global average SSS (below). How well do SSS patterns mirror bands of high and low atmospheric pressure? In places where they
do not match, what other types of freshwater inputs & outputs might be occurring?
To learn more about monthly SSS variations in our "saltiest" ocean, the North Atlantic, visit the "Salinity
Data and Tools" section.
To learn more about how salinity influences ocean circulation – and earth's climate zones – visit the "Ocean Circulation & Climate" section.
Aquarius is NASA's first mission to measure ocean salinity. Our first installment of educational materials –
"Salinity Patterns & the Water Cycle" – meet physical science content standards of the
National Science Education Standards. To learn more about the importance of ocean salinity, we offer several
classroom activities and supplemental ocean-atmosphere data investigation tools.
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