Author: AOML Communications

Gliders lined up and ready for deployment. Photo Credit: NOAA.

Gliders Patrol Ocean Waters with a Goal of Improved Prediction of Hurricane Intensity

Scientists at NOAA’s Atlantic Oceanographic and Meteorological Laboratory are in the Caribbean to launch two underwater gliders from a vessel off Puerto Rico to collect temperature and other weather data to improve hurricane forecasting.One of the gliders will collect observations in the Caribbean Sea, and another in the North Atlantic Ocean. They are positioned to operate over the next six months (June-November) collecting data in areas where hurricanes are common and areas where there is a lack of environmental data.

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Diatoms as seen through a microscope.

NOAA Participates in International Ocean Sampling for Microbes

NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML) participated in Ocean Sampling Day on June 21, the first global simultaneous sampling for microbes in ocean, coastal and Great Lakes waters. Over time, sampling will support international and NOAA missions to provide a snapshot of the diversity of microbes, their functions, and their potential economic benefits. Among other economic applications, microbes have been used for novel medicines, as biofuels, and to consume spilled oil. Organized and led by the European Union’s MicroB3 organization, NOAA coordinated twelve sampling sites for Ocean Sampling Day 2014 within U.S. coastal waters.

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New Tools Bring Ecosystem Benefits to the Forefront of Decision Making

The Marine and Estuarine Goal Setting for South Florida (MARES) project, led by NOAA’s Cooperative Institute for Marine and Atmospheric Studies at the University of Miami, continues to increase awareness of and appreciation for the value of coastal marine ecosystems, and their impacts upon human society. From 2009 through 2013, NOAA’s National Centers for Coastal Ocean Science funded MARES with the goal of creating a consensus-based process for managing South Florida’s coastal marine environments. MARES is unique in that it was among the first major efforts to include human benefits in a systematic framework to enable integrated ecosystem based management. The MARES approach embodies NOAA’s effort to serve as the Nation’s environmental intelligence agency by providing actionable information from science-based models to support environmentally-sensitive decisions made every day by individuals, communities, and governments.

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Coral ecologist Ian Enochs dives in the carbon dioxide bubbles of Maug's coral reefs (credit: Stephani Gordon/Open Boat Films/NOAA)

Volcanic Island of Maug Provides Natural Lab for Ocean Acidification

Maug is a unique natural laboratory that allows us to study how ocean acidification affects coral reef ecosystems. We know of no other area like this in U.S. waters. Increasing carbon dioxide in seawater is a global issue because it makes it harder for animals like corals to build skeletons.

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(left) Location of the three repeat XBT transects (AX25, AX22, and IX28) in the Southern Ocean. (right) Altimetry-derived magnitude of surface geostrophic currents for November 10, 2010, showing the multi-front signature of the ACC, from which the SAF and APF are highlighted. Overlaid is the location of AX25 (gray line), and the location of these fronts for November 10, 2010 (shaded markers). Image Credit: NOAA AOML.

Wind forced variability of the Antarctic Circumpolar Current south of Africa between 1993 and 2010

Researchers from PhOD and from the University of Cape Town used temperature data from the AX25 repeat XBT transect (from South Africa to Antarctica) in combination with other hydrographic and satellite observations to report a mechanism by which local winds alter the structure of the Antarctic Circumpolar Current flow south of Africa.

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Composites of SST and surface wind anomalies for 21 canonical and 12 Modoki El Niño events running from the event peak in DJF to the following JJA. SST and wind vectors shown are significant at the 10% level based on a Student's one sample t test. Boxes in Figures 1a (1b) outline Niño-3 (El Niño Modoki) regions.Image Credit: NOAA AOML.

Impact of canonical and Modoki El Niño on tropical Atlantic SST

Results from research performed by Dillon Amaya, an undergraduate Hollings Scholar from Texas A&M University, were published recently in Journal of Geophysical Research. Dillon’s work was carried out in the Physical Oceanography Division of AOML during the summer of 2013 and focused on understanding the impacts of different types of El Niño events (“canonical” and “Modoki”) on sea surface temperatures in the tropical Atlantic. The main result from the research is that Modoki El Niño;s fail to produce significant warming in the tropical North Atlantic, in contrast to the well known warming following canonical events.

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In-situ surface current velocity from ADCP (red vectors) and CTD station markers are shown for the July 2010 survey. Marker colors indicate the station θ-S profile classification as either GCW, LCW, EFCW, Coastal Shelf Water (green), or mixed-interleaved (black). Stations lacking waters denser than σθ = 24.0 kg m-3 are shown as small black dots. Prototype profile locations are indicated by an "x" and an enlarged marker. Letters identify selected sections along the cruise track. Image Credit: NOAA AOML.

Oceanographic conditions in the Gulf of Mexico in July 2010, during the Deepwater Horizon oil spill

Results from collaborative research conducted by AOML and NOAA’s Southeast Fisheries Science Center (SEFSC) in response to the 2010 Deepwater Horizon oil spill, were recently published in Continental Shelf Research (December, 2013). PhOD oceanographers R. Smith, E. Johns, G. Goni, J. Trinanes, and R. Lumpkin, in collaboration with other researchers at AOML (M. Wood, C. Kelble, and S. Cummings) and SEFSC (J. Lamkin and S. Privoznik) report on the surface and subsurface connectivity across the eastern Gulf of Mexico (GOM) during July 2010.

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Distribution of long-term mean observed (a)-(b) and simulated (c)-(d) meridional velocity along 23°W and 10°W. Gray dots in (a)-(b) indicate statistically significant values. Contour interval is 2.5 cm s-1. Figure reproduced from Perez et al., (2013). Image Credit: NOAA AOML.

Mean Meridional Currents in the Central and Eastern Equatorial Atlantic

In an article recently published in Climate Dynamics (Perez et al., 2013) , scientists in PhOD (R. Perez, R. Lumpkin, C. Schmid) described for the first time the mean vertical and cross-equatorial structure of the upper-ocean meridional currents in the Atlantic cold tongue region, using in situ observations including drifters, Argo, shipboard/lowered ADCP, and moored ADCP. This study involves collaborations with scientists from the University of Miami, Scripps Institution of Oceanography, and several international institutions and makes use of data from several major tropical Atlantic field programs including NOAA’s PIRATA Northeast Extension.

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AOML Tests New Deep Water Data Pod System  “ABIISS” 

The AOML technology test of a system to autonomously retrieve data from subsurface moored instruments has had a major success. The Adaptable Bottom Instrument Information Shuttle System (ABIISS) is in the midst of its first 4000+ meter test, and on November 6th, 2015 the first data pod surfaced and successfully transmitted its daily data record from the ocean bottom pressure-equipped inverted echo […]

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NASA's Global Hawk headed away from NASA's Wallops Flight Facility, Wallops Island, Va. on Sept. 19, 2012 and headed to investigate Tropical Storm Nadine near the Azores Islands in the Eastern Atlantic Ocean. Global Hawks are part of the Hurricane and Severe Storm Sentinel (HS3) mission. Credit: NASA Wallops

Hurricane Researchers Achieve Important Milestones Despite Quiet 2013 Season

The 2013 Atlantic hurricane season, which officially ended on November 30th, will be noted in the record books as having been a relatively quiet year with the fewest hurricanes since 1982. In fact, it will be ranked as the sixth least-active Atlantic hurricane season since 1950. Despite this, the 2013 season was quite an active […]

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