What's New Archive
On October 19, 2017, the OCS KEO mooring broke from its anchor and went adrift. Though it drifted in the North Pacific for two full months before being rescued, the buoy stayed in the Kuroshio Extension’s recirculation gyre, and had nearly made its way back to the original anchor location to meet the rescue ship.
The KEO station is located off the coast of Japan. NOAA has maintained a surface mooring there since 2004, and Japan Agency for Marine-Earth Science and Technology (JAMSTEC) has maintained a subsurface sediment trap at KEO since 2014. The KEO surface mooring carries a suite of instrumentation to monitor air-sea exchanges of heat, moisture, momentum (wind stress), and carbon dioxide; surface ocean acidification; and upper ocean temperature, salinity and currents. The combined data sets from both moorings enable computation of the physical and biological pumps of the carbon cycle in this key region of the North Pacific. As such, the site has become a focal point for international climate research.
Researchers are now looking with interest at the data set recorded during the time when the buoy was drifting. The path taken by the buoy is interesting in itself, as it outlines the anti-cyclonic flowing recirculation gyre south of the Kuroshio Extension. Because the mooring still carried subsurface instruments down to 425m, the drifting mooring observations can be used to study the air-sea interactions along the entire recirculation gyre.
The drifting buoy was rescued and redeployed by PMEL technicians aboard a JAMSTEC ship at the end of December 2017. Now that it has been redeployed, the KEO mooring will continue to provide high quality measurements for research. In January 2018, it will be at the center of an international science expedition studying upper ocean heat and carbon exchanges. The mission includes researchers from University of Tokyo, JAMSTEC, Monterey Bay Aquarium Research Institute, and North Carolina State University.
Thanks to the joint efforts of PMEL and JAMSTEC, the NOAA KEO mooring is back where it belongs, continuing to be a central part of the research in this region.
By: Jennifer Keene
Excited to be doing our first mission using Saildrones, the OCS project has launched the OCS Saildrone Mission Blog.
This is where we’ll be posting regular updates about the mission, so be sure the check in to get the latest on what’s happening. We’ll discuss where the drones are, where they’re going, what they’re doing, and what we’re studying.
When we find something interesting, we’ll write about it here first!
For background on the Saildrones, and the purpose of this mission, you can learn more on our Saildrone page. You can also watch a great news clip about the launch, that happened on September 1, 2017.
Be sure to bookmark the blog for regular news about the latest mission developments!
By: Jennifer Keene
Typhoon Sanvu, the first big storm of the 2017 North Pacific season, will be passing nearly directly over the OCS KEO mooring between September 1st and 2nd, 2017.
The current forecast from the Joint Typhoon Warning Center (JTWC) has the eye passing very near the buoy, which is likely to experience some of the strongest winds. Sanvu is expected to achieve peak wind gusts to around 110 knots as it passes KEO. Impressive wave heights approaching 16m (>50 ft!) could be present near the storm’s center.
Sanvu is occurring during record sea surface temperatures at the KEO site. This is the first time in the KEO records when sea surface temperature averages have consecutively exceeded 29.3°C for more than a week. These high temperatures, coupled with low shear and strong outflow, contribute to the growing intensity of the storm.
After passing the KEO mooring, the storm is expected to accelerate to the northeast. As Sanvu becomes embedded in a mid-latitude trough, increased shear will quickly erode the storm’s strength, and it is not expect to pose much threat to land.
The KEO mooring is often in the path of large storms, and scientists use the data to analyze and improve forecasting models. Higher than average sea surface temperatures, known to contribute to cyclone intensification, were also observed preceding Hurricane Harvey, which recently caused devastating damage in Texas. By learning more about these storms and how they behave, we hope to help prepare a more weather-ready nation.
By: Nathan Anderson and Jennifer Keene
Two PMEL technicians sailed out of Yokohama, Japan on July 13th on a six-day mission to service the PMEL Ocean Climate Stations KEO mooring.
Located just south of the Kuroshio Extension Current off the coast of Japan, the KEO mooring has been in place since 2004. Equipped with meteorological and oceanographic sensors, the mooring measures the exchange of heat and moisture between the ocean and atmosphere. These exchanges affect the development of storms over the north Pacific before they reach the United States. Scientists also use the KEO data to improve hurricane predictions.
Once a year, technicians visit the site to refresh the mooring. A full set of fresh equipment is deployed. Gear that was out for the previous year is recovered, and refurbished for the following year. This has allowed the mooring to survive in very harsh conditions, providing an important climate data set for nearly 15 years.
By: Jennifer Keene
Path of Tropical Storm Lionrock, as it passed the NOAA KEO mooring, and makes it way toward Japan. Storm track image from the Joint Typhoon Warning Center.
As residents in Japan prepare for Tropical Storm Lionrock today, scientists at NOAA and the University of Washington’s Joint Institute for the Study of the Atmosphere and Ocean (JISAO) study the behavior of the storm. Lionrock is expected to make landfall across northern Japan, affecting many highly populated areas, including Fukushima and other areas impacted by the 2011 tsunami.
With funding awarded for research after Super Storm Sandy caused massive damage to the east coast of the US, NOAA and JISAO scientists aim to improve storm track models to better predict where storms will go, and how powerful they might become. To achieve this, they are using data from the NOAA Kuroshio Extension Observatory (KEO), along with model simulations performed at NOAA’s Environmental Modeling Center.
KEO is a moored buoy, located off the coast of Japan, where it is frequently in the path of storms and tropical cyclones. When Lionrock passed over KEO on Monday, wind gusts were recorded at over 81mph, and storm-induced currents approached 3 knots, some of the highest ever recorded at the site. These data, along with other measurements of the ocean state, both before and after the passage of the storm, will be valuable tools in assessing, and ultimately improving, storm prediction models.
By: Jennifer Keene
Two valuable partnerships have allowed successful servicing of the NOAA Ocean Station Papa mooring this year.
The June 2016 deployment of the NOAA Papa mooring in the Gulf of Alaska was accomplished aboard the CCGS John P. Tully, in partnership with Canada’s Institute of Ocean Sciences, Department of Fisheries and Oceans Line P Program. These long time project partners have been providing ship time and assistance servicing the NOAA Papa mooring since it was first deployed in 2007. This year, for the first time in nine years, conditions prevented the recovery of the NOAA mooring that had been deployed in 2015.
That mooring was instead recovered aboard the NOAA Ship Ronald H. Brown, which was working in the same area for Ocean Observing Initiative (OOI) operations, just weeks after the Tully cruise. Though the work schedule was shortened due to unforeseen issues, the ship was still able to accomplish all of their planned work, as well as the recovery of the NOAA Papa mooring.
Thanks to the captain and crew of the NOAA Ship Ronald H. Brown, members of the WHOI mooring group, and Oregon State University OOI technicians, who made the recovery operations a success. Grateful thanks also go to the chief scientist of the cruise, Dr. Ed Dever, who coordinated with NOAA and the NSF cruise sponsor to make this recovery possible. Continued thanks to the Line P Program for their ongoing support of NOAA mooring operations.
By: Jennifer Keene
Members of the PMEL Ocean Climate Stations Project (OCS) and the PMEL Carbon Program recently published two companion papers describing ocean processes in the North Pacific that play a role in the Earth’s climate system.
OCS Principal Investigator Dr. Meghan Cronin and her co-authors examined the exchanges of heat and salt affecting the mixed water layer of the upper ocean, since exchanges of heat and freshwater between the ocean and the atmosphere can have an effect on weather and climate. Using data from the OCS KEO and Papa moorings, satellites, Argo floats, and a glider, the authors calculated and closed the heat budget for the mixed layer at both KEO and Station Papa, and also closed the salt budget at Papa. The good agreement between the diffusive coefficients from the heat and salt budgets suggested that this coefficient could be used to help close the mixed layer budgets of other ocean properties.
Building on these results, PMEL Carbon Program scientist Dr. Andrea Fassbender and her co-authors used this coefficient to close the carbon budget at Station Papa. The authors analyzed seven years of carbon observations from the OCS Papa mooring, along with data from research vessels, satellites, and a glider. From this, they were able to study seasonal carbon exchanges, and evaluate the amount of carbon going into the deep sea. This study provided new insights about the carbon cycle and climate responses in this region.
The PMEL OCS and Carbon groups have worked together for over a decade, deploying moorings and instrumentation in the North Pacific. Both the partnership and the mooring measurements have advanced understanding of the roles of ocean processes in the Earth’s climate system.
By: Jennifer Keene
Read the papers:
Cronin, M. F., N. A. Pelland, S. R. Emerson, and W. R. Crawford (2015), Estimating diffusivity from the mixed layer heat and salt balances in the North Pacific, J. Geophys. Res. Oceans, 120, 7346-7362, doi:10.1002/2015JC011010
Fassbender, A.J., C. L. Sabine, and M. F. Cronin (2016), Net community production and calcification from seven years of NOAA Station Papa Mooring measurements, Global Biogeochem. Cycles, doi:10.1002/2015GB005205
EOS Research Spotlight: https://eos.org/research-spotlights/moored-ocean-buoy-tracks-marine-carbon-cycle-variations
Personnel from NOAA's Pacific Marine Environmental Lab participated in a research cruise aboard the Canadian Coast Guard Ship JOHN P. TULLY, and recorded some great videos of mooring operations. Watch the two short videos at the end of this article, to see the deployment of one climate mooring, and the recovery of the buoy that had been in the water for a year. Get a first hand look at a day in the life of a NOAA buoy technician!
On this trip, the ship sailed out of Sidney, B.C. on June 7, 2015, and returned to port on June 22nd. As part of the science mission, the crew performed water sampling and net tows to study ocean physics, chemistry, and zooplankton. Ten NOAA drifter floats, used to study ocean currents, were also deployed. While the ship was still offshore, an important algal bloom was detected along the coast of North America. Ship's personnel were able to collect additional water samples in coastal waters, to verify the extent of the bloom in Canadian waters.
The ship spent several days at a site in the Gulf of Alaska, called Ocean Station Papa. Beginning in December 1949, Ocean Station Papa (50°N, 145°W) was occupied by a Weather Ship operated through the U.S. Coast Guard by the U.S. Weather Bureau. The site was taken over by a Canadian Weather Ship in December 1950, and several years later oceanographic measurements began to be routinely made. Though no longer under continuous observations by Weather Ships, the Canadian Institute of Ocean Sciences has been making trips to the site three to six times per year since 1981.
In 2007, the OCS program deployed their first surface mooring at Ocean Station Papa, which now uses satellite technologies to transmit weather and climate data to shore. This mooring took on the role of those old Weather Ships, and the climate record from Ocean Station Papa is one of the oldest on record. Watch videos showing how these moorings are deployed and recovered.
By: Jennifer Keene
The tropical cyclone Fengshen, named for the god of wind in Mandarin Chinese, passed over the NOAA mooring at the Kuroshio Extension Observatory (KEO) on September 8-9, 2014 GMT. The KEO mooring is located off the coast of Japan, where tropical cyclones and typhoons pass regularly during the autumn storm season. KEO has been specially adapted to be a "storm mooring," built to withstand extreme conditions, and also send data back to shore once per hour to allow scientists to monitor events in near real-time.
The buoy functioned exactly as planned throughout the storm, and a complete data record was captured. Barometric pressure dropped to a low of 971.5 hPa during the storm, and wind gusts reached 37 m/s (83 mph). The sea surface temperature dipped drastically from around 28°C to almost 25°C in just a few hours due to enhanced mixing of surface waters with cooler waters below.
With access to typhoon data in near real-time, scientists are able to verify and improve the accuracy of forecasts and storm prediction models. Researchers from NOAA's Pacific Marine Environmental Lab (PMEL), who deployed the KEO mooring, are working with partners at the NOAA's Environmental Modeling Center (EMC) to do just that. Model improvements can also be applied to hurricane forecasts for storms that might impact the east coast of the U.S.
The PMEL KEO mooring is part of a global network of time series reference stations. It carries a suite of sensors to monitor the ocean-atmosphere exchanges of heat, moisture, momentum and CO2, ocean acidification, and the upper ocean physical state. Deep ocean temperature and salinity are also measured by an instrument just above the sea floor.
By: Jennifer Keene
NASA Sees Tropical Storm Fengshen Looking More Like a Frontal System NASA web page
What Happens Underwater During a Hurricane? University of Miami, Rosensteil School of Marine & Atmospheric Science web page
Researchers at NOAA's Pacific Marine Environmental Laboratory (PMEL) and the University of Washington Joint Institute for the Study of Atmosphere and Oceans (JISAO) are watching with great interest as an area of warm surface water persists in the North Pacific.
During the fall and early winter of 2013 – 2014, residents of the Pacific Northwest enjoyed more dry weather than normal, with fewer and weaker storms. The weaker than usual winds resulted in reduced heat transfer between the air and ocean, less mixing of cold water from below, and reduced transport of warm water toward the equator. This left a large mass of warm water in the Northeast Pacific, nicknamed "The Blob." At its core, the water mass was ~3°C above normal temperatures in February 2014, and it is still prominent going into the summer months.
The PMEL Ocean Climate Stations (OCS) project Station Papa buoy ismoored in the heart of the blob, making continuous measurements of the atmosphere and ocean at this site since 2007. The Office of the Washington State Climatologist and other OCS scientists will use data from the mooring to evaluate the ocean processes related to the causes and effects of this warmer than usual water mass. PMEL researchers are also onboard a Canadian research vessel that will be servicing the mooring and taking measurements along "Line P" June 8 – 24, 2014.
According to climate models, the region of warm surface water may continue to be well above normal temperatures through late summer 2014. This could affect regional weather, as well as marine ecosystems. The weather could be warmer and more humid than normal, and more thunderstorms may develop. In the marine ecosystem, the warmer water provides more favorable habitat for tuna near the coast, but may adversely affect juvenile salmon through reduced supply of nourishing food sources.
By: Jennifer Keene