Web-resolution - August 27, 2011 - June 2, 2012QuickTime
High-definition - August 27, 2011 - June 2, 2012QuickTime
Salinity—the amount of dissolved salt in the water—is critical to so many aspects of the ocean, from circulation to climate to the global water cycle. For much of the past year, NASA and Argentina’s ComisiÃ³n Nacional de Actividades Espaciales (CONAE) have been making comprehensive observations of sea surface salinity from space. Launched on June 10, 2011, the Aquarius mission is slowly compiling a more complete picture of the salty sea and how it varies.
Click on the animation below the main image to see salinity patterns changing week by week over the past year. A few features stand out. As oceanographers have known for many years—but now can “see”—the Atlantic Ocean is saltier than the Pacific and Indian Oceans. Rivers such as the Amazon carry tremendous amounts of fresh runoff from land and spread plumes far into the sea. And in the tropics—particularly near the Pacific’s Inter-Tropical Convergence Zone—extra rainfall makes equatorial waters somewhat fresher.
Near most coastlines and inland seas in the map, waters appear much fresher or saltier than in open-ocean locations. Look, for instance, at the Red Sea and the Mediterranean for saltier waters; significantly fresher waters appear in the Black Sea, in the icy high latitudes, and around the many islands and peninsulas of Southeast Asia. Indeed, runoff from rivers and melting ice does make water fresher, and strong evaporation and other processes do make the Red and Mediterranean Seas saltier. But mostly those extreme salinity measurements around the coastlines are a distortion of the satellite signal.
Technically, Aquarius measures the emissivity or “brightness temperature” of the surface waters, notes Gary Lagerloef, Aquarius principal investigator, based at Earth and Space Research in Seattle. Land masses have a higher emissivity than the ocean, so any measurement close to land tends to be skewed by its brightness. Over time, the Aquarius research team should be able to calibrate the measurements and develop mathematical tools to better distinguish the salt signal. But for now, the measurements are so new that the team is still working on the big picture of ocean salinity.
Aquarius is the first NASA instrument specifically designed to study surface ocean salinity from space, and it does so at a rate of 300,000 measurements per month. It uses three passive microwave sensors, called radiometers, to record the thermal signal from the oceans' top 10 millimeters (about 0.4 inches).
“An overarching question in climate research is to understand how changes in the Earth’s water cycle—meaning rainfall and evaporation, river discharges and so forth—ocean circulation, and climate link together,” said Lagerloef. Most global precipitation and evaporation events take place over the ocean and are very difficult to measure. But rainfall freshens the ocean’s surface waters, and Aquarius can detect these changes in saltiness. “Salinity is the variable we can use to measure that coupling. It’s a critical factor, and it will eventually be used to improve climate forecasts.”
NASA images by Norman Kuring, Goddard Space Flight Center. Animation by Robert Simmon. Caption by Mike Carlowicz, Earth Observatory, with reporting from Maria-Jose Vinas, NASA Earth Science News Team.
One year after its launch, the Aquarius instrument is giving ocean sciences its first global view of sea surface salinity.
Examining temperatures from the depths of the ocean, JPL scientists have found that lower layers of the Western Pacific and Indian Oceans grew much warmer during a decade when surface temperatures cooled.
Submerged in the Atlantic Ocean off the coast of Spain and Portugal are giant, salty whirlpools of warm water. These deep-water whirlpools are part of the ocean’s circulatory system, and they help drive the ocean currents that moderate Earth’s climate. Warm water ordinarily sits at the ocean’s surface, but the warm water flowing out of the Mediterranean Sea is so salty (and therefore dense) that when it enters the Atlantic Ocean at the Strait of Gibraltar, it sinks to depths of more than 1,000 meters (one-half mile) along the continental shelf. This underwater river then separates into clockwise-flowing eddies that may continue to spin westward for more than two years, often coalescing with other eddies to form giant, salty whirlpools that may stretch for hundreds of miles. Because the eddies originate from the Mediterranean Sea, scientists call them “Meddies.”