Although anyone knows the seawater is salty, couple of know the even little variations in s surface salinity (i.e., concentration of liquified salts) deserve to have dramatic impacts on the water cycle and ocean circulation. Transparent Earth"s history, particular processes have actually served to make the s salty. The weathering the rocks it is intended minerals, including salt, into the ocean. Evaporation of ocean water and also formation of sea ice both increase the salinity the the ocean. However these "salinity raising" components are continually counterbalanced by procedures that diminish salinity such together the continuous input of fresh water from rivers, precipitation of rain and snow, and also melting of ice.

You are watching: Which is not a process that decreases the salinity of seawater

The Aquarius instrument aboard Argentina"s SAC-D satellite is designed to measure global sea surface ar salinity. This movie shows salinity patterns as measure up by Aquarius indigenous December 2011 with December 2012. Red colors represent locations of high salinity, if blue shades represent locations of short salinity. It is important to know salinity, the amount of dissolved salts in water, since it will certainly lead united state to much better understanding the the water cycle and can command to boosted climate models. High concentrations (over 37 practical salinity units) space usually in the center of the ocean containers away from the mouths the rivers, which input fresh water. High concentration are also in sub-tropical regions because of high prices of evaporation (clear skies, tiny rain, and also prevailing winds) and in landlocked seas in arid regions. At high latitudes, salinity is low. This deserve to be meeting to reduced evaporation rates and also the melting of ice that dilutes seawater. To sum up, salinity is low wherein precipitation is greater than evaporation, greatly in seaside or equatorial regions. Credit:


Salinity & The Water Cycle

Understanding why the sea is salty begins with knowing just how water cycles among the ocean"s physical states: liquid, vapor, and ice. As a liquid, water dissolves rocks and also sediments and also reacts v emissions from volcanoes and also hydrothermal vents. This creates a complicated solution that mineral salt in our ocean basins. Conversely, in other states such together vapor and also ice, water and also salt space incompatible: water vapor and also ice are basically salt free.

Since 86% of worldwide evaporation and also 78% of global precipitation occur over the ocean, s surface salinity is the key variable for understanding exactly how fresh water input and also output affects s dynamics. By tracking ocean surface salinity us can straight monitor variations in the water cycle: floor runoff, sea ice freezing and also melting, and also evaporation and precipitation over the oceans.

Salinity, ocean Circulation & Climate

Surface winds journey currents in the upper ocean. Deep listed below the surface, however, s circulation is generally driven by alters in seawater density, which is determined by salinity and temperature. In some areas such as the north Atlantic near Greenland, cooled high-salinity surface ar waters can come to be dense sufficient to sink to good depths. The "Global Conveyor Belt" visualization (below) reflects a simplified design of how this kind of circulation would work-related as one interconnected system.The ocean stores an ext heat in the uppermost three (3) meters than the entire atmosphere. For this reason density-controlled circulation is key to transporting heat in the ocean and maintaining Earth"s climate. Overabundance heat associated with the boost in worldwide temperature during the critical century is being took in and relocated by the ocean. In addition, studies imply that seawater is coming to be fresher in high latitudes and tropical locations dominated through rain, if in sub-tropical high evaporation regions, waters are acquiring saltier. Such changes in the water cycle can significantly influence not only ocean circulation but likewise the climate in which us live.

"The an international Conveyer Belt" represents in a simple way how currents relocate beneath the wind-driven upper ocean. This movie begins by concentrating on the north Atlantic eastern of Greenland, wherein cold surface ar waters get saltier because of evaporation and/or sea ice cream formation. In this region, surface ar waters deserve to becomes dense enough come sink come the s depths. This pumping of surface water right into the deep ocean forces the deep water to move horizontally till it have the right to find locations where it deserve to rise earlier to the surface. This an extremely large, slow existing -- approximated to it is in on the stimulate of 1000 years to complete a full circuit -- is referred to as the thermohaline circulation due to the fact that it is brought about by temperature (thermo) and salinity (haline) variations. Credit:


Measuring Salinity

Throughout many of history, global understanding of ocean surface salinity was an overwhelming because sampling through ships, buoys, drifters, and moorings was very limited. In between 300 and also 600 AD, awareness of transforms in salinity, temperature, and also smell assisted Polynesians explore the southern Pacific Ocean. In the 1870s, researchers aboard H.M.S. Challenger systematically measured salinity, temperature, and water thickness in the world"s oceans. Over the years, approaches for measure such s water properties have readjusted drastically in an approach and accuracy.

*"s Aquarius instrument has been orbiting earth since June 2011, measuring alters in salinity, or salt concentration, in the surface of the oceans. In autumn 2011, the Aquarius team released this very first global map of s saltiness, a composite of the an initial two and also a fifty percent weeks of data since the instrument came to be operational on respectable 25, 2011. Click on image to see complete size version. Credit:

Launched June 10, 2011, plank the Argentine spacecraft Aquarius/Satélite de Aplicaciones Científicas (SAC)-D, Aquarius is’s first satellite tool specifically developed to study the salt content of ocean surface waters. Salinity variations, among the main motorists of ocean circulation, are closely connected with the cycling of freshwater about the earth and administer scientists with an important information on how the transforming global climate is altering worldwide rainfall patterns.

The salinity sensor detects the microwave emissivity the the top 1 to 2 centimeters (about one inch) of s water – a physical building that varies depending on temperature and also saltiness. The instrument collects data in 386 kilometer-wide (240-mile) swaths in an orbit designed to obtain a complete survey of worldwide salinity the ice-free oceans every 7 days.

This computer animation is an artist explicate of the Aquarius/SAC-D satellite in orbit approximately the earth, collecting data provided to derive salinity measurements. The satellite flies 657 kilometers (408 miles) over Earth in a sun-synchronous polar orbit the repeats every seven days. Keep in mind that this animation was developed prior to the June 2011 start of the satellite and thus shows simulated salinity data. Click on image or link over to check out video. Credit:


What deserve to salinity tell us?

Data indigenous Aquarius has actually unveiled a civilization of varying salinity patterns. The Arabian Sea, nestled up against the dry center East, shows up much saltier than the surrounding Bay the Bengal, which gets showered by intense monsoon rains and also receives freshwater discharges indigenous the Ganges and also other large rivers. One more mighty river, the Amazon, release a large freshwater plume the heads east toward Africa or bends up phibìc to the Caribbean, depending upon the prevailing seasonal currents. Pools of freshwater carried by ocean currents native the central Pacific Ocean’s areas of heavy rainfall heap up beside Panama’s coast, while the Mediterranean Sea sticks the end in the Aquarius maps together a an extremely salty sea.

One of the functions that stand out most clearly is a big patch of highly saline water across the north Atlantic. This area, the saltiest all over in the open up ocean, is analogous to deserts on land, where tiny rainfall and a most evaporation occur. A expedition, the Salinity procedures in the top Ocean regional Study (SPURS), travel to the north Atlantic’s saltiest point out to analyze the causes behind this high salt concentration and also to validate Aquarius measurements.

First full year the validated ocean surface salinityAnimation mirrors the first full year the validated ocean surface salinity native"s Aquarius instrument, averaged from December 2011 v December 2012. Red colour represent areas of high salinity, while blue shades represent locations of short salinity. Aquarius has noted a global view that salinity variability needed for climate studies. Credit:

Future Goals

In future years, one of the key goals is to fine-tune the readings and also retrieve data closer come the coasts and also the poles. Land and ice emit very bright microwave emissions the swamp the signal read by the satellite. At the poles, yes sir the included complication the cold polar waters require very big changes in their salt concentration come modify their microwave signal.

Another element that affect salinity readings is extreme rainfall. Heavy rain can impact salinity readings by attenuating the microwave signal Aquarius reads turn off the ocean surface as it travels with the soaked atmosphere. Rainfall can likewise create roughness and shallow pools of new water ~ above the ocean surface. In the future, the Aquarius team wants to use another instrument plank Aquarius/SAC-D, the Argentine-built Microwave Radiometer, to gauge the existence of intense rain concurrently to salinity readings, so that scientists deserve to flag data built up during hefty rainfall.

See more: If The Number 0.7777 Repeats Forever Therefore It Is Irrational

An ultimate goal is combine the Aquarius dimensions to those of its european counterpart, the soil Moisture and also Ocean Salinity satellite (SMOS) come produce more accurate and finer maps of ocean salinity. In addition, the Aquarius team, in cooperation with researchers at the U.S. Department of Agriculture, is about to relax its an initial global floor moisture dataset, i beg your pardon will enhance SMOS’ soil moisture measurements.

For an ext information about"s Aquarius mission, visit: