Authors: Heidi Van Buskirk Date: 5/31/19 Each year Miami Today publishes The Best of Miami edition to highlight people and organizations from multiple fields that make a difference in the community. The special edition articles focus on the best in each respective field from arts and culture to health and medicine to international business and role […]
Scientists from NOAA and the Monterey Bay Research Institute (MBARI) are teaming up on June 3-4, 2019 to conduct a complex mission which will integrate acoustic measurements and autonomous sample collection for analysis of environmental DNA (eDNA). Through these efforts NOAA scientists hope to develop faster and cheaper ecosystem assessment methods, ensure sustainable fisheries and broaden our understanding of life in the oceans.
Evans, C., K.M. Wood, S.D. Aberson, H.M. Archambault, S.M. Milrad, L.F. Bosart, K.L. Corbosiero, C.A. Davis, J.R. Dias Pinto, J. Doyle, C. Fogarty, T.J. Galarneau, C.M. Grams, K.S. Griffin, J. Gyakum, R.E. Hart, N. Kitabatake, H.S. Lentink, R. McTaggart-Cowan, W. Perrie, J.F. Quinting, C.A. Reynolds, M. Riemer, E.A. Ritchie, Y. Sun, and F. Zhang, 2017: The Extratropical Transition of Tropical Cyclones. Part I: Cyclone Evolution and Direct Impacts. Mon. Wea. Rev., 145, 4317–4344, https://doi.org/10.1175/MWR-D-17-0027.1
Abstract: Extratropical transition (ET) is the process by which a tropical cyclone, upon encountering a baroclinic environment and reduced sea surface temperature at higher latitudes, transforms into an extratropical cyclone. This process is influenced by, and influences, phenomena from the tropics to the midlatitudes and from the meso- to the planetary scales to extents that vary between individual events. Motivated in part by recent high-impact and/or extensively observed events such as North Atlantic Hurricane Sandy in 2012 and western North Pacific Typhoon Sinlaku in 2008, this review details advances in understanding and predicting ET since the publication of an earlier review in 2003. Methods for diagnosing ET…
NOAA and partners have launched a new buoy in Fagatele Bay within NOAA’s National Marine Sanctuary of American Samoa to measure the amount of carbon dioxide in the waters around a vibrant tropical coral reef ecosystem. “This new monitoring effort in a remote area of the Pacific Ocean will not only advance our understanding of changing ocean chemistry in this valuable and vibrant coral ecosystem but will also help us communicate these changes to diverse stakeholders in the Pacific Islands and across the United States,” said Derek Manzello, coral ecologist with NOAA’s Atlantic Oceanographic and Meteorological Laboratory.
Researchers with AOML’s Ocean Chemistry and Ecosystems Division have entered into a collaborative agreement with Reef Check Foundation to deploy an AOML-designed temperature sensor at coral reef sites around the world. Measuring only six inches in height, the inexpensive, highly-accurate sensors will greatly enhance efforts to more precisely monitor small-scale temperature fluctuations that occur at reefs over time and at various depths.
The global mean sea level rise caused by ocean warming and glacier melting over landforms such as Greenland is one of the most alarming aspects of a shifting global climate. However, the dynamics of the ocean and atmosphere further influence sea level changes region by region and over time. For example, along the U.S. East Coast, a pronounced acceleration of sea level rise in 2010-2015 was observed south of Cape Hatteras, while a deceleration occurred up North. These patterns provide background conditions, on top of which shorter-period (and often stronger) weather-driven sea level fluctuations compound what coastal communities directly experience day by day. Therefore, to develop or improve regional sea level predictions, it’s important to identify these patterns and explore how they change over time.
Gruber, N., Clement, D., Carter, B. R., Feely, R. A., van Heuven, S., Hoppema, M., … & Monaco, C. L. (2019). The oceanic sink for anthropogenic CO2 from 1994 to 2007. Science, 363(6432), 1193-1199.
Abstract:
We quantify the oceanic sink for anthropogenic carbon dioxide (CO2) over the period 1994 to 2007 by using observations from the global repeat hydrography program and contrasting them to observations from the 1990s. Using a linear regression–based method, we find a global increase in the anthropogenic CO2 inventory of 34 ± 4 petagrams of carbon (Pg C) between 1994 and 2007. This is equivalent to an average uptake rate of 2.6 ± 0.3 Pg C year−1 and represents 31 ± 4% of the global anthropogenic CO2 emissions over this period. Although this global ocean sink estimate is consistent with the expectation of the ocean uptake having increased in proportion to the rise in atmospheric CO2, substantial regional differences in storage rate are found, likely owing to climate variability–driven changes in ocean circulation.
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The new research published by NOAA and international partners in Science finds as carbon dioxide emissions have increased in the atmosphere, the ocean has absorbed a greater volume of emissions. Though the volume of carbon dioxide going into the ocean is increasing, the percentage of emissions — about 31 percent — absorbed by it has remained relatively stable when compared to the first survey of carbon in the global ocean published in 2004.
Hoffman, R. N., & Atlas, R. (2016). Future observing system simulation experiments. Bulletin of the American Meteorological Society, 97(9), 1601-1616.
Abstract: An additional set of challenges will arise when future DA systems strongly couple the different Earth system components. As operational forecast and data assimilation (DA) systems evolve, observing system simulation experiment (OSSE) systems must evolve in parallel. Expected development of operational systems—especially the use of data that are currently not used or are just beginning to be used, such as all-sky and surface-affected microwave radiances—will greatly challenge our ability to construct realistic OSSE systems.In response, future OSSE systems will require coupled models to simulate nature and coupled observation simulators. The requirements for future evolving OSSE systems and potential solutions to satisfy these requirements are discussed. It is anticipated that in the future the OSSE technique will be applied to…
The National Oceanic and Atmospheric Administration’s Oceanic and Atmospheric Research Dr. Daniel L. Albritton Outstanding Science Communicator Award recognizes outstanding achievement in communicating the meaning and value of NOAA-related science and research to non-scientific audiences. The award is named in honor of Dr. Daniel L. Albritton, a retired OAR scientist, who proved to be one of the most effective communicators of NOAA research and related science.
