Although everyone knows that seawater is salty, few know that even small variations in ocean surface salinity (i.e., concentration of dissolved salts) can reveal important information about changes in Earth's water cycle, ocean circulation and climate. Throughout Earth's history, the weathering of rocks has delivered minerals, including salt, into the ocean. Over decades to centuries, the amount of salt in ocean basins has remained relatively constant. On the other hand, processes that move water into, out of, and around the ocean are in constant motion. As a result, monitoring salinity allows scientists to better understand these processes and how they are changing. The impact of such changes could include altering ocean circulation patterns which move heat around the globe, drive Earth's climate, and affect our daily lives.
Some water cycle processes, including evaporation of ocean water and formation of sea ice, increase the ocean's salinity. These salinity-raising factors, however, are offset by processes that decrease salinity: input of fresh water from rivers, precipitation of rain and snow, and melting of ice. On land, water cycle processes are tied to vegetation patterns: deserts occur in regions where evaporation is high and rain forests occur in areas of high precipitation. Similarly, over the ocean, the regional differences between evaporation and precipitation are correlated with patterns of sea surface salinity. This can be seen by comparing historical maps of ocean surface salinity with data showing the imbalance between evaporation and precipitation. In general, ocean regions dominated by evaporation have higher salinities and areas with high precipitation have lower salinities.
Several recent studies have suggested that seawater is becoming fresher in high latitudes and tropical areas dominated by rain, while in sub-tropical high evaporation regions, waters are getting saltier. Since August 2011, NASA’s salinity instruments have delivered steady and reliable information about the vast ocean where about 86% of global evaporation and 78% of global precipitation occur. This continuous coverage has allowed scientists to monitor variations in the water cycle and determine if it is indeed accelerating in response to climate change.
Surface winds drive currents in the upper ocean. Deep below the surface, however, ocean circulation is primarily driven by changes in seawater density, which is determined by salinity and temperature. In some regions — such as the North Atlantic near Greenland — cooled high-salinity surface waters can become dense enough to sink to great depths. Perturbations to this process, for example from melting of polar ice and associated decrease in seawater salinity, could have significant impacts on Earth's climate. This is because the ocean holds and transports a tremendous amount of thermal energy: the heat stored in the top 3 meters (10 feet) of the ocean is equivalent to the amount held by the entire atmosphere, with an average thickness of about 100 kilometers (62 miles).
NASA's program to monitor salinity is crucial because the geographic coverage from in-water observing systems (e.g., ships, buoys) is not extensive enough to fully understand how changes in global salinity affect climate, and vice versa. Excess heat associated with the increase in global temperature during the last century is being absorbed and moved by the ocean. Surface ocean and atmospheric temperature changes may cause evaporation to intensify and, as a result, significantly alter sea surface salinity and ocean circulation patterns. Ocean change may seem like a "faraway" problem but, as the major driver of our planet's climate, it has the potential to impact humans everywhere.