What's New Archive
An article just published in Oceanography by PMEL’s Dr. Robert Embley and collaborators at Japan's JAMSTEC, Oregon State University (CIMRS), Washington University, and the University of Texas, Dallas describes the site of a 2010 submarine eruption of a 200 meter deep seamount in the Mariana arc that was powerful enough to produce an atmospheric plume. Comparisons of pre- (2002) and post- (2013) eruption bathymetric surveys reveal a new 400m diameter crater. This new map targeted dives with a JAMSTEC remotely operated vehicle in 2013. This new information will help evaluate the hazard potential of submarine eruptions.
For more information please visit the PMEL Earth-Ocean Interactions website.
Led by Dr. Jeremy Mathis, PMEL teamed up with the University of Alaska and the Alaska Ocean Observing System this summer and early fall to use new unmanned tools to study how melting glaciers in Alaska’s Prince William Sound may be intensifying ocean acidification in the sound and on the Gulf of Alaska continental shelf. PMEL engineers outfitted two Carbon Wave Gliders and one underwater Slocum glider with sensors to help better understand the unique processes of glacial melt water and how they change the chemistry of the water column in Prince William Sound.
Researchers at PMEL and JISAO are monitoring an area of warm surface water that has been occupying the Northeast Pacific near Ocean Climate Station Papa buoy. This mass of water, nicknamed “The Blob”, was about 3 degrees Celsius warmer than normal in February and is maintaining its abnormal heat into the summer. The warm water has implications for the marine ecosystem and could affect the weather in the Pacific Northwest. Past summers with especially warm water off the coast have tended to be warmer and more humid than usual.
To check out the latest conditions with The Blob, visit the Ocean Climate Station Papa buoy page.
PMEL’s Dr. Trish Quinn led a group of PMEL and JISAO scientists on a recent cruise in the North Atlantic Ocean to assess how ocean biogeochemistry impacts sea spray particles. Quantifying the size and composition of sea spray particles is critical for parameterizing cloud condensation nuclei in climate models. The particles are generated using the PMEL developed Sea Sweep device that is deployed over the side of the ship to collect samples.
The study, which ended on June 5, is part of the Western Atlantic Climate Study II (WACS II) and was conducted using the Woods Hole Oceanographic Institute’s R/V Knorr. For more information please visit PMEL’s Atmospheric Chemistry website.
PMEL and Alaska Fisheries Science Center’s EcoFOCI program just deployed the M2 mooring in the southeastern Bering Sea for the 20th consecutive year. The mooring has been providing year-round measurements of temperature, salinity, nitrite, chlorophyll, and currents in this highly productive area since 1994. These measurements are used in annual report cards and stock assessments provided to the North Pacific Fishery Management Council. Long-term time-series at this site are a critical tool for adapting to climate change and guiding sustainable management of living resources in the Bering Sea.
Visit the EcoFOCI website for more information on their work in the Bering Sea, Gulf of Alaska, and Arctic waters.
PMEL carbon scientists Drs. Nina Bednarsek and Richard Feely were part of a NOAA-led team to find the first evidence that acidity of continental shelf waters off the West Coast dissolving the shells of pteropods. Their research, published April 30 in the Proceedings of the Royal Society B, estimates that the percentage of pteropods in this region with dissolving shells due to ocean acidification has doubled since the pre-industrial era and is on track to triple by 2050 when coastal waters become 70 more corrosive due to human-caused ocean acidification.
NOAA Arctic Program Leads, including PMEL scientist and Arctic expert Dr. James Overland, collaborated on the development and recent publication of NOAA's Arctic Action Plan. The plan provides a roadmap to making shared progress in monitoring, understanding, and protecting the vulnerable Arctic region. PMEL is actively involved in Arctic climate dynamics research, conducting observations and evaluating models of Arctic sea ice to document and predict climate change impacts on Arctic marine ecosystems.
The Bering Sea Project, a 6-year multidisciplinary program encompassing the work of more than 100 collaborating scientists, has led to major new understanding of the role of sea ice and changing climate in one of the world’s most commercially viable fisheries. The timing of spring sea ice retreat influences large zooplankton yields, an important prey species, and impacts pollock recruitment in the Bering Sea Fisheries.
Immediately following a magnitude 8.2 earthquake off the coast of Chile on April 1, scientists at PMEL began modeling the event using real-time data from DART® moorings that measured the tsunami 30 minutes after the earthquake struck. They accurately predicted wave arrival times and heights for US coastal communities like Hilo, Hawaii, where a tide gauge recorded a 50 cm tsunami wave.
Please visit the Chile tsunami event page for more information, including tide gauge comparisons with model data for other communities.
Research published recently in Global Biogeochemical Cycles describes how observations in the tropical Pacific now show human activity is contributing to increasing CO2 levels where, previously, natural variability has dominated ocean CO2 patterns. Lead author, PMEL/JISAO scientist Adrienne Sutton, along with PMEL’s Dr. Richard Feely also conclude that the rates of CO2 and acidity in seawater are just as rapid in the tropical Pacific as in polar regions, which are considered one of the harbingers of ocean acidification.
To read more please visit the NOAA Research news page.