Scientists use salinity to trace changes in the US Northeast Coastal Ocean
Woods Hole Oceanographic InstitutionPeer-Reviewed Publication
The near-bottom water on the U.S. Northeast continental shelf provides a critical cold-water habitat for the rich regional marine ecosystem. This “cold pool” preserves winter temperatures, even when waters elsewhere become too warm or salty during the summer.
• The U.S. Northeast coastal ocean has experienced accelerated warming in recent years, compared to the global average. Now, scientists using salt as a tracer are investigating how much the influx of salty offshore water onto the continental shelf contributes to the observed “erosion” of the seasonal cold pool.
• This paper provides the first evidence for a seasonal salinification of the cold pool on the US Northeast continental shelf, as consistently observed in the multi-year mooring record of the [Ocean Observatories Initiative] Coastal Pioneer Array.
- Journal
- Journal of Geophysical Research Oceans
- Funder
- NASA Ocean Salinity Science Team, National Science Foundation’s (NSF) Ocean Science Division, George E. Thibault Early Career Scientist Fund, Scripps Chair for Excellence in Oceanography.