GFDL - Geophysical Fluid Dynamics Laboratory

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Approaching storm iStockphoto.com/MvH

Welcome

The Geophysical Fluid Dynamics Laboratory (GFDL) is engaged in comprehensive long lead-time research fundamental to NOAA's mission. Scientists at GFDL develop and use mathematical models and computer simulations to improve our understanding and prediction of the behavior of the atmosphere, the oceans, and climate. GFDL scientists focus on model-building relevant for society, such as hurricane research, prediction, and seasonal forecasting, and understanding global and regional climate change.

Since 1955, GFDL has set the agenda for much of the world's research on the modeling of global climate change and has played a significant role in the World Meteorological Organization, the Intergovernmental Panel on Climate Change assessments, and the U.S. Global Change Research Program. GFDL's mission is to be a world leader in the development of earth system models, and the production of timely and reliable knowledge and assessments on natural climate variability and anthropogenic changes.

GFDL research encompasses the predictability and sensitivity of global and regional climate; the structure, variability, dynamics and interaction of the atmosphere and the ocean; and the ways that the atmosphere and oceans influence, and are influenced by various trace constituents. The scientific work of the Laboratory incorporates a variety of disciplines including meteorology, oceanography, hydrology, classical physics, fluid dynamics, chemistry, applied mathematics, and numerical analysis.

Research is also facilitated by the Atmospheric and Oceanic Sciences Program (AOS), which is a collaborative program at GFDL with Princeton University. Under this program, Princeton faculty, research scientists, and graduate students participate in theoretical studies, both analytical and numerical, and in observational experiments in the laboratory and in the field. The program is supported in part by NOAA funding. AOS scientists may also be involved in GFDL research through institutional or international agreements.

For an overview of GFDL's work, see our Fact Sheet.

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Research Highlights

  • April 15, 2013 Response to CO2 doubling of the Atlantic Hurricane Main Development Region in a High-Resolution Climate Model - The authors simulated the response of sea surface temperature (SST) in the Atlantic Hurricane Main Development Region (MDR) to a doubling of CO2, using a cutting-edge global high-resolution coupled model developed at GFDL (CM2.5). The model has been shown to produce a very faithful simulation of the observed seasonal cycle and year-to-year (or interannual) variability in the tropical Atlantic. The skillful representation of Atlantic interannual variability enables the exploration of the response of interannual variability to increasing CO2 – in addition to exploring changes in the average conditions in the Atlantic. Read more
  • March 29, 2013 Sensitivity of tropospheric oxidants to biomass burning emissions: implications for radiative forcing - Biomass burning is one of the largest sources of trace gases and aerosols in the atmosphere, and has profound influence on tropospheric oxidants and radiative forcing. Using a fully coupled chemistry-climate model (GFDL AM3), the authors found that co-emission of trace gases and aerosol from present-day biomass burning increases the global tropospheric ozone burden by 5.1%, and decreases global mean OH, a major sink for methane, by 6.3%. Read more
  • March 11, 2013 Ocean Warming effect on Surface Gravity Wave Climate Change for the end of the 21st Century - Future changes in wind-wave patterns have broad implications for ecosystems, as well as the design and operation of coastal, near-and-off-shore industries. Changes in response to global warming may further exacerbate the anticipated vulnerabilities of coastal regions to projected sea-level rise. Read more
  • March 4, 2013 Cloud tuning in a coupled climate model: impact on 20th century warming - Clouds remain one of the largest sources of uncertainty in predictions from climate models. Globally, clouds cool the Earth through the net effect of two opposing contributions: cooling from reflection of incoming solar radiation and warming from trapping of infrared radiation emitted by the Earth. By comparison, the cooling effect of clouds is estimated to be about six times larger than the warming effect resulting from the increase in anthropogenic greenhouse gases since 1750. This is why uncertainties in the representation of clouds can have considerable impact on the simulated climate. Read more

Read more GFDL Research Highlights


Events & Seminars

  • June 20, 2013: Flooding over the Central US (abstract)
    Gabriele Villarini (University of Iowa)
    Time: 2:00 pm - 3:00 pm
    Location: Smagorinsky Seminar Room
  • June 26, 2013: Role of Storms in the Atmospheric General Circulation (abstract)
    William Rossow (City University of New York)
    Time: 12:00 pm - 1:00 pm
    Location: Smagorinsky Seminar Room
  • June 27, 2013: A convective quasi-equilibrium view of observed monsoons (abstract)
    William Boos (Yale)
    Time: 2:00 pm - 3:15 pm
    Location: Smagorinsky Seminar Room
  • July 10, 2013: TBD (abstract)
    Jingqiu Mao (AOS)
    Time: 12:00 pm - 1:15 pm
    Location: Smagorinsky Seminar Room
  • July 11, 2013: TBA
    Tiffany Shaw (Columbia University)
    Time: 2:00 pm - 3:00 pm
    Location: Smagorinsky Seminar Room
  • July 17, 2013: Preindustrial to present-day changes in tropospheric hydroxyl radical and methane lifetime from the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP) (abstract)
    Vaishali Naik (GFDL)
    Time: 12:00 pm - 1:00 pm
    Location: Smagorinsky Seminar Room
  • July 18, 2013: TBA
    Vernon Morris (Howard U.)
    Time: 2:00 pm - 3:00 pm
    Location: Smagorinsky Seminar Room
  • July 31, 2013: TBA
    Michael Herzog (Cambridge University, UK)
    Time: 12:00 pm - 1:00 pm
    Location: Smagorinsky Seminar Room

More events & seminars...