Author: AOML Communications

Researchers and Forecasters Team Up to Improve Forecasts in the New Hurricane and Ocean Testbed

After a year and a half of concerted effort between NOAA’s National Hurricane Center (NHC), Atlantic Oceanographic and Meteorological Laboratory (AOML), and other NOAA offices, including the Weather Program Office, the Hurricane and Ocean Testbed (HOT) has been successfully launched in the newly designed William M. Lapenta Laboratory, named in memory of the late director of the National Centers for Environmental Protection. This testbed establishes a physical and virtual collaboration space for researchers and forecasters.

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A satellite image showing the murky brown water of the Mississippi River plume mixing with the dark blue water of the Gulf two days after a rainstorm. Image Credit: NASA’s MODIS

River Runoff Creates a Buffer Zone for Ocean Acidification in the Gulf of America

A new study by scientists at NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML) and Northern Gulf Institute (NGI) has revealed the alkalinity of river runoff to be a crucial factor for slowing the pace of ocean acidification along the Gulf of America’s northern coast. This valuable, first-time finding may be indicative of ocean carbon chemistry patterns for other U.S. coastal areas significantly connected to rivers.

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Frontiers in Ocean Observing front cover image.

Frontiers in Ocean Observing

Kappel, E.S., S.K. Juniper, S. Seeyave, E. Smith, and M. Visbeck, eds. 2021. Frontiers in Ocean Observing: Documenting Ecosystems, Understanding Environmental Changes, Forecasting Hazards. A Supplement to Oceanography 34(4), 102 pp., https://doi.org/10.5670/oceanog.2021.supplement.02.

Articles in this inaugural Frontiers in Ocean Observing supplement to Oceanography describe new technologies and reveal some exciting results that advance our understanding of the world ocean and its resources and support its sustainable use and management. Topics covered align with the priorities of the UN Decade of Ocean Science for Sustainable Development (2021–2030). Five articles in this Supplement were co-authored by AOML scientists and science support personnel: Climate-Relevant Ocean Transport Measurements in the Atlantic and Arctic Oceans, Monitoring Boundary Currents Using Ocean Observing Infrastructure, An Integrated Observing Effort for Sargassum Monitoring and Warning in the Caribbean Sea, Tropical Atlantic, and Gulf of America, Uncrewed Ocean Gliders and Saildrones Support Hurricane Forecasting and Research, and The Technological, Scientific, and Sociological Revolution of Global Subsurface Ocean Observing.

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Environmental DNA Sampling Gets an Upgrade and Transitions to New Open-Source Technology

Scientists at NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML),the Cooperative Institute for Marine and Atmospheric Studies (CIMAS) at the University of Miami Rosenstiel School of Marine and Atmospheric Science, and the Northern Gulf Institute at Mississippi State University have engineered a new instrument that will provide valuable information about the biodiversity of aquatic ecosystems. A recently published paper in Hardware X describes the design and creation of a low-cost, open-source sub-surface automated environmental DNA (eDNA) sampler (SASe), for sampling eDNA in the water column. The SASe represents a milestone for AOML as one of the first pieces of technology to go through a rigorous transition process from the desks of scientists in the laboratory, through organizational approval channels, to the wider scientific community with full accessibility to the public.

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Infographic showing vertical wind shear in a hurricane. Image Credit: NOAA.

Research Explores Impact of Wind Shear Direction on Tropical Cyclone Intensity

The amount of wind shear, i.e., the change of the wind with height, is one of the most commonly used predictors of tropical cyclone intensity change, with large amounts of wind shear generally being unfavorable for intensification. Regardless of the direction of the wind shear, tropical cyclones in the North Atlantic basin usually have warm, moist air from the environment near the sea surface on their east side (solid red arrows in the images) and cool, dry air from the environment on their west side (solid blue arrows in images).

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First page of ' Revisiting the recharge and discharge processes for different flavors of El Nino' publication

Revisiting the Recharge and Discharge Processes for Different Flavors of El Niño

Chakravorty, S., Perez, R. C., Gnanaseelan, C., & Anderson, B. T. (2021). Revisiting the recharge and discharge processes for different flavors of El Niño. Journal of Geophysical Research: Oceans, 126(11), e2020JC017075.

Plain Language Summary: The El Niño-Southern Oscillation (ENSO) is the largest source of year-to-year climate variability. ENSO has a pronounced influence on regional and global circulation and precipitation patterns and thus has considerable worldwide socio-economical impacts. El Niño, the warm phase of ENSO, exhibits modulation in the longitudinal location of its maximum warming, creating what is referred to as ENSO diversity. For conventional El Niño events, maximum surface warming is located in the eastern equatorial Pacific, for which subsurface warming along the tropical Pacific has proven to serve as a predictor several months in advance. Previous studies disagree on whether this subsurface warming is similarly essential for El Niño events that have peak surface warming in the central Pacific. The authors developed an improved method for identifying these two types of El Niño in an ocean reanalysis product. Using this improved method, they found no clear evidence of a subsurface warming precursor for the central Pacific El Niño events along the equator. This lack of a tropical subsurface precursor limits our ability to predict these types of El Niño events.

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First page of 'Coral persistence despite extreme periodic pH fluctuations at a volcanically acidified Caribbean reef' publication.

Coral persistence despite extreme periodic pH fluctuations at a volcanically acidified Caribbean reef

Enochs, I. C., Formel, N., Manzello, D., Morris, J., Mayfield, A. B., Boyd, A., … & Hendee, J. (2020). Coral persistence despite extreme periodic pH fluctuations at a volcanically acidified Caribbean reef. Coral Reefs, 39(3), 523-528.

Abstract: Naturally acidified environments, such as those caused by volcanic CO2 venting, reveal how complex coral reef ecosystems may respond to future ocean acidification conditions. Few of these sites have been described worldwide, and only a single such site is known from the Caribbean. Herein, we have characterized an area of volcanic acidification at Mayreau Island, St. Vincent and the Grenadines. Despite localized CO2 enrichment and gas venting, the surrounding area has high hard and soft coral cover, as well as extensive carbonate frameworks. Twice daily extremes in acidification, in some cases leading to undersaturation of aragonite, are correlated with tidal fluctuations and are likely related to water flow. Corals persisting despite this periodic acidification can provide insights into mechanisms of resilience and the importance of natural pH variability on coral reefs.

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