N: 90 S: -90 E: 180 W: -180
Description
This dataset contains monthly-averaged ocean and sea-ice surface stress interpolated to a regular 0.5-degree grid from the ECCO Version 4 revision 4 (V4r4) ocean and sea-ice state estimate. Estimating the Circulation and Climate of the Ocean (ECCO) ocean and sea-ice state estimates are dynamically and kinematically-consistent reconstructions of the three-dimensional, time-evolving ocean, sea-ice, and surface atmospheric states. ECCO V4r4 is a free-running solution of the 1-degree global configuration of the MIT general circulation model (MITgcm) that has been fit to observations in a least-squares sense. Observational data constraints used in V4r4 include sea surface height (SSH) from satellite altimeters [ERS-1/2, TOPEX/Poseidon, GFO, ENVISAT, Jason-1,2,3, CryoSat-2, and SARAL/AltiKa]; sea surface temperature (SST) from satellite radiometers [AVHRR], sea surface salinity (SSS) from the Aquarius satellite radiometer/scatterometer, ocean bottom pressure (OBP) from the GRACE satellite gravimeter; sea ice concentration from satellite radiometers [SSM/I and SSMIS], and in-situ ocean temperature and salinity measured with conductivity-temperature-depth (CTD) sensors and expendable bathythermographs (XBTs) from several programs [e.g., WOCE, GO-SHIP, Argo, and others] and platforms [e.g.,research vessels, gliders, moorings, ice-tethered profilers, and instrumented pinnipeds]. V4r4 covers the period 1992-01-01T12:00:00 to 2018-01-01T00:00:00.
Product Summary
Citation
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Variables
The table below lists the variables contained within a single granule for this dataset. Variables often contain observed or derived geophysical measurements collected from a variety of sources, including remote sensing instruments on satellite and airborne platforms, field campaigns, in situ measurements, and model outputs. The terms variable, parameter, scientific data set, layer, and band have been used across NASA’s Earth science disciplines; however, variable is the designated nomenclature in NASA’s Common Metadata Repository (CMR). Variable metadata attributes such as Name, Description, Units, Data Type, Fill Value, Valid Range, and Scale Factor allow users to efficiently process and analyze the data. The full range of attributes may not be applicable to all variables. Additional information on variable attributes is typically available in the data, user guide, and/or other product documentation.
For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor | Offset |
|---|---|---|---|---|---|---|---|
| EXFtaue | Zonal (east-west) component of wind stress. Note: EXFtaue is the zonal wind stress applied to the ocean and sea-ice. When sea-ice is present, the total zonal stress applied to the ocean surface is NOT EXFtaue, but a combination of the wind stress in the open water fraction (EXFtaue) and a stress from sea-ice in the ice-covered fraction (see oceTAUE). EXFtaue is calculated by interpolating the model's x and y components of wind stress (EXFtaux and EXFtauy) to tracer cell centers and then finding the zonal component of the interpolated vectors. It is NOT recommended to use EXFtaue and EXFtaun for momentum budget calculations because interpolating EXFtaux and EXFtauy from the model grid to the lat-lon grid introduces errors. For momentum fluxes to the ocean surface see oceTAUx and oceTAUy. | N m-2 | float | 9.96921E+36 | -75.45976 to 66.26148 | 1 | N/A |
| EXFtaun | Meridional (north-south) component of wind stress. Note: EXFtaun is the stress applied to the ocean and sea-ice. When sea-ice is present, the total meridional stress applied to the ocean surface is NOT EXFtaun, but a combination of the wind stress in the open water fraction (EXFtaun) and a stress from sea-ice in the ice-covered fraction (see oceTAUN). EXFtaun is calculated by interpolating the model's x and y components of wind stress (EXFtaux and EXFtauy) to tracer cell centers and then determining the meridional component of the interpolated vectors. It is NOT recommended to use EXFtaue and EXFtaun for momentum budget calculations because interpolating EXFtaux and EXFtauy from the model grid to the lat-lon grid introduces errors. For momentum fluxes to the ocean surface see oceTAUx and oceTAUy. | N m-2 | float | 9.96921E+36 | -82.73749 to 154.34361 | 1 | N/A |
| latitude | uniform grid spacing from -89.75 to 89.75 by 0.5 | degrees_north | float | N/A | N/A | 1 | N/A |
| latitude_bnds | latitude bounds grid cells | N/A | float | N/A | N/A | 1 | N/A |
| longitude | uniform grid spacing from -179.75 to 179.75 by 0.5 | degrees_east | float | N/A | N/A | 1 | N/A |
| longitude_bnds | longitude bounds grid cells | N/A | float | N/A | N/A | 1 | N/A |
| oceTAUE | Zonal (east-west) component of ocean surface stress due to wind and sea-ice. Note: oceTAUE is calculated by interpolating the model's x and y components of ocean surface stress (oceTAUX and oceTAUY) to tracer cell centers and then finding the zonal component of the interpolated vectors. | N m-2 | float | 9.96921E+36 | -75.89108 to 58.705616 | 1 | N/A |
| oceTAUN | Meridional (north-south) component of ocean surface stress due to wind and sea-ice. Note: oceTAUN is calculated by interpolating the model's x and y components of ocean surface stress (oceTAUX and oceTAUY) to tracer cell centers and then finding the meridional component of the interpolated vectors. | N m-2 | float | 9.96921E+36 | -78.09064 to 75.20025 | 1 | N/A |
| time | center time of averaging period | hours since 1992-01-01T12:00:00 | int | N/A | N/A | 1 | N/A |
| time_bnds | Start and end times of averaging period. | N/A | int | N/A | N/A | 1 | N/A |