Geophysical Fluid Dynamics Laboratory

Last updated
US-GeophysicalFluidDynamicsLaboratory-Logo.svg

The Geophysical Fluid Dynamics Laboratory (GFDL) is a laboratory in the National Oceanic and Atmospheric Administration (NOAA) Office of Oceanic and Atmospheric Research (OAR). The current director is Venkatachalam Ramaswamy. It is one of seven Research Laboratories within NOAA's OAR. [1]

Contents

GFDL is engaged in comprehensive long-lead-time research to expand our scientific understanding of the physical and chemical processes that govern the behavior of the atmosphere and the oceans as complex fluid systems. [2] These systems can be modeled mathematically and their phenomenology can be studied by computer simulation methods.

GFDL's accomplishments include the development of the first climate models to study global warming, [3] [4] the first comprehensive ocean prediction codes, and the first dynamical models with significant skill in hurricane track and intensity predictions. Much current research within the laboratory is focused around the development of Earth System Models for assessment of natural and human-induced climate change. [5]

Accomplishments

Scientific divisions

The GFDL has a diverse community of about 300 researchers, collaborators and staff, with many from Britain, India, China, Japan, France, and other countries around the world. The laboratory is currently organized into several scientific divisions (listed alphabetically below). There is also a large group of scientific programmers known as the Modeling Systems Division, as well as a large computer support group. [7]

Atmospheric Physics

Current head: Venkatachalam Ramaswamy

This divisions goal is to employ numerical models and observations of the Earth System to characterize and quantify atmospheric physical processes, particularly those involving greenhouse gases, aerosols, water vapor, and clouds, and their roles in atmospheric general circulation, weather and climate.

Biogeochemistry, Atmospheric Chemistry, and Ecosystems

Current head: John P. Dunne

This divisions goal is to develop and use the GFDL’s earth system models to create a more comprehensive understanding of the interactions between physical, chemical, and ecological drivers and feedbacks on the earth system.

Ocean and Cryosphere

Current head: Rong Zhang [8]

This divisions goal is to conduct leading research to understand ocean and cryosphere changes and variability; their interactions with weather, climate, sea level, and ecosystems; and advance prediction and projection of future changes. To support this goal, we are developing state-of-the-science numerical models for the ocean, sea ice, land ice, and fully coupled models.

Seasonal-to-Decadal Variability and Predictability

Current head: Thomas L. Delworth [9]

This divisions goal is to improve our understanding of climate variability, predictability and change on time scales ranging from seasonal to multidecadal. This includes internal variability of the coupled climate system, and the response to changing radiative forcing. We are actively working to develop a next-generation experimental seasonal-to-decadal prediction system.

Weather and Climate Dynamics

Current head: Thomas Knutson

This divisions goal is to develop innovative physical and dynamical components for the next generation of earth system models, with special emphasis on high resolution (1–25 km) atmospheric model development. We aim to explore the frontiers of weather and climate modeling and analysis, and to improve the predictions of high-impact events such as hurricanes, floods, severe storms, and droughts, from weather to seasonal and interannual (2 year) time-scales.

Facilities

The GFDL is located at Princeton University's Forrestal Campus in Princeton, NJ. [10] [11]

Since March 2011, the GFDL no longer possesses an on-site supercomputer. They instead utilize a massively parallel Cray supercomputer with over 140,000 processor cores which is currently located at Oak Ridge National Laboratory in Oak Ridge, Tennessee. This contrasts from their previous systems architecture, which consisted of eight Silicon Graphics Altix computers, each housing 1024 processor cores. [12] Hardware updates occur on average, every 18 months.

The GFDL has been using high-performance computing systems to perform numerical modeling since the 1950s.

Alumni[12]

See also

Related Research Articles

<span class="mw-page-title-main">Climate model</span> Quantitative methods used to simulate climate

Numerical climate models are mathematical models that can simulate the interactions of important drivers of climate. These drivers are the atmosphere, oceans, land surface and ice. Scientists use climate models to study the dynamics of the climate system and to make projections of future climate and of climate change. Climate models can also be qualitative models and contain narratives, largely descriptive, of possible futures.

<span class="mw-page-title-main">General circulation model</span> Type of climate model

A general circulation model (GCM) is a type of climate model. It employs a mathematical model of the general circulation of a planetary atmosphere or ocean. It uses the Navier–Stokes equations on a rotating sphere with thermodynamic terms for various energy sources. These equations are the basis for computer programs used to simulate the Earth's atmosphere or oceans. Atmospheric and oceanic GCMs are key components along with sea ice and land-surface components.

The Carl-Gustaf Rossby Research Medal is the highest award for atmospheric science of the American Meteorological Society. It is presented to individual scientists, who receive a medal. Named in honor of meteorology and oceanography pioneer Carl-Gustaf Rossby, who was also its second (1953) recipient.

<span class="mw-page-title-main">Jule Gregory Charney</span> US meteorologist

Jule Gregory Charney was an American meteorologist who played an important role in developing numerical weather prediction and increasing understanding of the general circulation of the atmosphere by devising a series of increasingly sophisticated mathematical models of the atmosphere. His work was the driving force behind many national and international weather initiatives and programs.

<span class="mw-page-title-main">Numerical weather prediction</span> Weather prediction using mathematical models of the atmosphere and oceans

Numerical weather prediction (NWP) uses mathematical models of the atmosphere and oceans to predict the weather based on current weather conditions. Though first attempted in the 1920s, it was not until the advent of computer simulation in the 1950s that numerical weather predictions produced realistic results. A number of global and regional forecast models are run in different countries worldwide, using current weather observations relayed from radiosondes, weather satellites and other observing systems as inputs.

<span class="mw-page-title-main">Office of Oceanic and Atmospheric Research</span> NOAA environmental products and services

Oceanic and Atmospheric Research (OAR) is a division of the National Oceanic and Atmospheric Administration (NOAA). OAR is also referred to as NOAA Research.

The Modular Ocean Model (MOM) is a three-dimensional ocean circulation model designed primarily for studying the ocean climate system. The model is developed and supported primarily by researchers at the National Oceanic and Atmospheric Administration's Geophysical Fluid Dynamics Laboratory (NOAA/GFDL) in Princeton, NJ, USA.

<span class="mw-page-title-main">Joseph Smagorinsky</span> American meteorologist

Joseph Smagorinsky was an American meteorologist and the first director of the National Oceanic and Atmospheric Administration (NOAA)'s Geophysical Fluid Dynamics Laboratory (GFDL).

<span class="mw-page-title-main">Atmospheric model</span> Mathematical model of atmospheric motions

In atmospheric science, an atmospheric model is a mathematical model constructed around the full set of primitive, dynamical equations which govern atmospheric motions. It can supplement these equations with parameterizations for turbulent diffusion, radiation, moist processes, heat exchange, soil, vegetation, surface water, the kinematic effects of terrain, and convection. Most atmospheric models are numerical, i.e. they discretize equations of motion. They can predict microscale phenomena such as tornadoes and boundary layer eddies, sub-microscale turbulent flow over buildings, as well as synoptic and global flows. The horizontal domain of a model is either global, covering the entire Earth, or regional (limited-area), covering only part of the Earth. Atmospheric models also differ in how they compute vertical fluid motions; some types of models are thermotropic, barotropic, hydrostatic, and non-hydrostatic. These model types are differentiated by their assumptions about the atmosphere, which must balance computational speed with the model's fidelity to the atmosphere it is simulating.

<span class="mw-page-title-main">Syukuro Manabe</span> Japanese–American meteorologist and climatologist

Syukuro "Suki" Manabe is a Japanese–American physicist, meteorologist, and climatologist, who pioneered the use of computers to simulate global climate change and natural climate variations. He was awarded the 2021 Nobel Prize in Physics jointly with Klaus Hasselmann and Giorgio Parisi, for his contributions to the physical modeling of Earth's climate, quantifying its variability, and predictions of climate change.

Geophysical Fluid Dynamics Laboratory Coupled Model is a coupled atmosphere–ocean general circulation model (AOGCM) developed at the NOAA Geophysical Fluid Dynamics Laboratory in the United States. It is one of the leading climate models used in the Fourth Assessment Report of the IPCC, along with models developed at the Max Planck Institute for Climate Research, the Hadley Centre and the National Center for Atmospheric Research.

<span class="mw-page-title-main">Thomas Knutson</span>

Thomas R. Knutson is a climate modeller at the US Geophysical Fluid Dynamics Laboratory, a division of the National Oceanic and Atmospheric Administration (NOAA). His research covers hurricane activity, the link between climate change and hurricane incidence and intensity, and climate change detection and attribution.

Kirk Bryan Jr. is an American oceanographer who is considered to be the founder of numerical ocean modeling. He is the son of Kirk Bryan, Sr.. Starting in the 1960s at the Geophysical Fluid Dynamics Laboratory, then located in Washington, D.C., Bryan worked with a series of colleagues to develop numerical schemes for solving the equations of motion describing flow on a sphere. His work on these schemes led to the so-called "Bryan-Cox code" with which many early simulations were made, and which led to the Modular Ocean Model currently used by many numerical oceanographers and climate scientists.

A chemical transport model (CTM) is a type of computer numerical model which typically simulates atmospheric chemistry and may give air pollution forecasting.

<span class="mw-page-title-main">Isaac Held</span> American meteorologist (1948-)

Isaac Meyer Held is an American meteorologist. He is a retired senior research scientist at the Geophysical Fluid Dynamics Laboratory. Held was elected to the United States National Academy of Sciences in 2003.

The NOAA National Operational Model Archive and Distribution System (NOMADS) is a Web-services based project providing both real-time and retrospective format independent access to climate and weather model data.

Shian-Jiann Lin is a Taiwanese-American atmospheric scientist and meteorologist. He is currently the head of the Weather and Climate Dynamics Division at the Geophysical Fluid Dynamics Laboratory, the lead developer of the GFDL Finite-Volume Cubed-Sphere Dynamical Core (FV3). and a lead developer or key contributor to several weather and climate models developed using FV3.

<span class="mw-page-title-main">S. George Philander</span> South African scientist

Samuel George Harker Philander is a climate scientist, known for his work on atmospheric circulation and oceanic currents, particularly El Niño. He is the Knox Taylor Professor emeritus of Geosciences at Princeton University.

<span class="mw-page-title-main">Thomas L. Delworth</span> American oceanic climate scientist

Thomas L. Delworth is an atmospheric and oceanic climate scientist and Senior Scientist at the Geophysical Fluid Dynamics Laboratory (GFDL), part of NOAA. He also serves on the faculty of Oceanic Science at Princeton University.

<span class="mw-page-title-main">Ronald J. Stouffer</span> American climate scientist

Ronald J. Stouffer is a meteorologist and adjunct professor at the University of Arizona, formerly Senior Research Climatologist and head of the Climate and Ecosystems Group at the Geophysical Fluid Dynamics Laboratory (GFDL), part of NOAA. He has also served on the faculty of Princeton University.

References

  1. "Labs & Programs". NOAA Research. Retrieved 23 June 2023.
  2. Alvich, Jason. "About GFDL". www.gfdl.noaa.gov. Retrieved 23 June 2023.
  3. Manabe, Syukuro; Bryan, Kirk (1969). "Climate calculations with a combined ocean-atmosphere model" (PDF). Journal of the Atmospheric Sciences. 26 (4): 786–789. Retrieved 23 June 2023.
  4. Cooney, Catherine M. (2012). "Downscaling Climate Models: Sharpening the Focus on Local-Level Changes". Environmental Health Perspectives. 120 (1): A22–A28. ISSN   0091-6765. JSTOR   41352962.
  5. Alvich, Jason. "Most Recent Publications". www.gfdl.noaa.gov. Retrieved 23 June 2023.
  6. 1 2 3 4 5 "NOAA Magazine Article on GFDL". Archived from the original on 2012-04-15.
  7. "Geophysical Fluid Dynamics Laboratory". 6 October 2015.
  8. "Rong Zhang Homepage". Geophysical Fluid Dynamics Laboratory. NOAA.
  9. "Tom Delworth Homepage". Geophysical Fluid Dynamics Laboratory. NOAA.
  10. Alvich, Jason. "Visiting GFDL". www.gfdl.noaa.gov. Retrieved 23 June 2023.
  11. "Directions". Atmospheric & Oceanic Sciences. Princeton. Retrieved 23 June 2023.
  12. "Geophysical Fluid Dynamics Laboratory?NAAA Activities FY-80 Plans FY-81 Review of Twenty-Five years of Research. 1955-1980". September 1980.