NRL HYCOM 1/25 deg model output, Gulf of Mexico The HYCOM consortium is a multi-institutional effort sponsored by the National Ocean Partnership Program (NOPP), as part of the U. S. Global Ocean Data Assimilation Experiment (GODAE), to develop and evaluate a data-assimilative hybrid isopycnal-sigma-pressure (generalized) coordinate ocean model (called HYbrid Coordinate Ocean Model or HYCOM).

The Ocean Data Inventory database is an inventory of all of the oceanographic time series data held by the Ocean Science Division at the Bedford Institute of Oceanography. The data archive includes about 5800 current meter and acoustic doppler time series, 4500 coastal temperature time series from thermographs, as well as a small number (200) of tide gauges. Many of the current meters also have temperature and salinity sensors. The area for which there are data is roughly defined as the North Atlantic and Arctic from 30° - 82° N, although there are some minor amounts of data from other parts of the world. The time period is from 1960 to present. The database is updated on a regular basis.

The Summary

Arctic sea surface salinity retrieved from SMOS, spatial resolution 0.25 deg (EASE grid 2.0), temporal resolution 9-day maps generated daily. The product contains the following data: i) sea surface salinity (p.s.u), ii) sea surface salinity uncertainty (p.s.u), and iii) sea surface salinity anomaly (p.s.u): difference between sea surface salinity provided by SSS field and the annual sea surface salinity provided by WOA 2018 A5B7. Product version 3.1. The product will be freely distributed at the BEC webpage http://bec.icm.csic.es and at the project webpage https://arcticsalinity.argans.co.uk.

The Ocean Data Inventory database is an inventory of all of the oceanographic time series data held by the Ocean Science Division at the Bedford Institute of Oceanography. The data archive includes about 5800 current meter and acoustic doppler time series, 4500 coastal temperature time series from thermographs, as well as a small number (200) of tide gauges. Many of the current meters also have temperature and salinity sensors. The area for which there are data is roughly defined as the North Atlantic and Arctic from 30° - 82° N, although there are some minor amounts of data from other parts of the world. The time period is from 1960 to present. The database is updated on a regular basis.

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.

This is monthly ocean 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.

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.

This is monthly ocean 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.

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.