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    Sea level pressure based on the FNMOC 360x180 (1-degree) analyzed fields. ERD was established at the U.S. Navy Fleet Numerical Meteorology and Oceanography Center (FNMOC) to take advantage of the Navy's global oceanographic and meteorological databases. FNMOC produces operational forecasts of the state of the atmosphere and the ocean several times daily and maintains archives of several important parameters, such as sea level pressure and temperature. ERD derives a number of well-known environmental data and index products which are routinely distributed to researchers at many state and federal laboratories, as well as to academic and international researchers.

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    Global monthly derived winds and transports can be obtained for any point on the ocean (Northern Hemisphere: 1967 - present, Southern Hemisphere: 1981 - present). ERD was established at the U.S. Navy Fleet Numerical Meteorology and Oceanography Center (FNMOC) to take advantage of the Navy's global oceanographic and meteorological databases. FNMOC produces operational forecasts of the state of the atmosphere and the ocean several times daily and maintains archives of several important parameters, such as sea level pressure and temperature. ERD derives a number of well-known environmental data and index products which are routinely distributed to researchers at many state and federal laboratories, as well as to academic and international researchers.

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    Global monthly derived winds and Ekman transports can be obtained for any point on the ocean (Northern Hemisphere: 1967 - present, Southern Hemisphere: 1981 - present). ERD was established at the U.S. Navy Fleet Numerical Meteorology and Oceanography Center (FNMOC) to take advantage of the Navy's global oceanographic and meteorological databases. FNMOC produces operational forecasts of the state of the atmosphere and the ocean several times daily and maintains archives of several important parameters, such as sea level pressure and temperature. ERD derives a number of well-known environmental data and index products which are routinely distributed to researchers at many state and federal laboratories, as well as to academic and international researchers.

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    This dataset has the long term mean (monthly climatology) of the 2-degree, Global, Enhanced, simple gridded monthly summary product (1971 - 2000) from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS), the most extensive collection of surface marine data.

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    This dataset has the long term mean (monthly climatology) of the 2-degree, Global, Enhanced, simple gridded monthly summary product (1950 - 1979) from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS), the most extensive collection of surface marine data.

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    The NCEP/NCAR Reanalysis 1 project is using a state-of-the-art analysis/forecast system to perform data assimilation using past data from 1948 to the present. Data is from NMC initialized reanalysis (4x/day). See the PROBLEMS LIST at http://www.esrl.noaa.gov/psd/data/reanalysis/problems.shtml

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    This is monthly ocean forcing data, 1860-2000, run #5, from the NOAA Geophysical Fluid Dynamics Laboratory's (GFDL) CM2.1 climate model, specifically: GFDL CM2.1, 20C3M (run5) climate of the 20th Century experiment (20C3M) output for IPCC AR4 and US CCSP. In 2004, a new family of GFDL climate models (the CM2.x family) was first used to conduct climate research. The GFDL CM2.x models have become the workhorse model for GFDL's climate research. They are being applied to topics focusing on decadal-to-centennial (deccen) time scale issues (including multi-century control experiments and climate change projections), as well as to seasonal-to-interannual (si) problems, such as El Niño research and experimental forecasts.

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    This is monthly atmospheric forcing data, 1860-2000, run #5, from the NOAA Geophysical Fluid Dynamics Laboratory's (GFDL) CM2.1 climate model, specifically: GFDL CM2.1, 20C3M (run5) climate of the 20th Century experiment (20C3M) output for IPCC AR4 and US CCSP. In 2004, a new family of GFDL climate models (the CM2.x family) was first used to conduct climate research. The GFDL CM2.x models have become the workhorse model for GFDL's climate research. They are being applied to topics focusing on decadal-to-centennial (deccen) time scale issues (including multi-century control experiments and climate change projections), as well as to seasonal-to-interannual (si) problems, such as El Niño research and experimental forecasts.

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    This is monthly atmospheric model data, 2001-2100, run #3, from the NOAA Geophysical Fluid Dynamics Laboratory's (GFDL) CM2.1 climate model, specifically: GFDL CM2.1, SresA1B (run3) 720 ppm stabilization experiment (SRES A1B) output for IPCC AR4 and US CCSP. In 2004, a new family of GFDL climate models (the CM2.x family) was first used to conduct climate research. The GFDL CM2.x models have become the workhorse model for GFDL's climate research. They are being applied to topics focusing on decadal-to-centennial (deccen) time scale issues (including multi-century control experiments and climate change projections), as well as to seasonal-to-interannual (si) problems, such as El Niño research and experimental forecasts.

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    This is monthly ocean forcing data, 1860-2000, run #5, from the NOAA Geophysical Fluid Dynamics Laboratory's (GFDL) CM2.1 climate model, specifically: GFDL CM2.1, 20C3M (run5) climate of the 20th Century experiment (20C3M) output for IPCC AR4 and US CCSP. In 2004, a new family of GFDL climate models (the CM2.x family) was first used to conduct climate research. The GFDL CM2.x models have become the workhorse model for GFDL's climate research. They are being applied to topics focusing on decadal-to-centennial (deccen) time scale issues (including multi-century control experiments and climate change projections), as well as to seasonal-to-interannual (si) problems, such as El Niño research and experimental forecasts.