Sea surface salinity (SSS) has been linked to changes in the
global water cycle and has been pointed to as an indicator variable that
can help us understand and even predict what will happen to the global
movement of water on a warming planet. Recent studies have shown that SSS
has changed over the 20th and 21st centuries. Those changes can be
attributed to human-induced climate forcing and are inconsistent with
natural forcing alone. Roughly, relatively fresh areas of the ocean have
gotten fresher and salty areas saltier, indicating an intensification of
evaporation and precipitation over the ocean.
Until about 2005, SSS was poorly observed throughout most of the world's
oceans. More recently, with the advent of Argo floats and salinity remote
sensing, we are now able to better observe the short-term, seasonal and
interannual variability of SSS and its relation to surface forcing and
internal ocean processes. While the original idea behind SSS remote
sensing was to use salinity as an "oceanic rain gauge", it has become
apparent over the past few years that internal ocean dynamics are just as
important as surface fluxes in regulating SSS. This makes understanding SSS
and its connection to internal processes in the ocean not only an
interesting scientific question, but a vitally important social goal to
help predict future changes in the global water cycle.
Dr. Frederick Bingham is a physical oceanographer and professor in the Department of Physics & Physical Oceanography at the University of North Carolina Wilmington. His current research interests are focused on the study of sea surface salinity and its relationship to the global water cycle on both a global and a regional scale. In the past, he has researched such diverse topics as the formation of subtropical mode water in the North Pacific, the Hawaiian Ridge Current, water mass distributions in the western equatorial Pacific and hurricane impacts on the North Carolina continental shelf. He also has interests in data management and real-time ocean data quality control.
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