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Description

This dataset provides instantaneous model ocean bottom pressure anomaly and sea surface height anomaly from the SASSIE ECCO Version 1 Release 1 (V1R1) ocean and sea-ice state estimate. ECCO (Estimating the Circulation and Climate of the Ocean) is a 4D ocean circulation model combining observations with a general circulation model (GCM) to estimate the complete time-evolving state of the global ocean. In this project, it was run over the Arctic polar region in support of the Salinity and Stratification at the Sea Ice Edge (SASSIE) field experiment - a NASA experiment focused on salinity anomalies in the upper ocean generated by melting sea ice. The SASSIE ECCO simulation was produced by downscaling the global ECCO state estimate from 1/3 to 1/12 degree grid cells, where the global solution provided initial and boundary conditions and atmospheric forcing. Model 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. The output fields for this dataset cover the period 2014-01-15T12:00:00 to 2021-02-07T12:00:00 and are consolidated onto a single curvilinear grid face focusing on the Arctic domain, using the 5 faces of the lat-lon-cap 1080 (llc1080) native grid from the original simulation. Monthly files are available in netCDF-4.
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This dataset is one of 22 produced by SASSIE ECCO - the full list can be found in the user guide. To cite all 22 datasets with a single DOI, please cite the user guide (citation details and DOI can be found within the user guide).

Version Description

Version 1, Release 1

Product Summary

Platforms
MITgcm
Location
ARCTIC
Coordinate System
GEODETIC
Granule Spatial Representation
GEODETIC
Temporal Extent
2014-01-15 to 2021-02-08
Temporal Resolution
1 Month
Data Partner
Physical Oceanography Distributed Active Archive Center, Jet Propulsion Laboratory, NASA (NASA/JPL/PODAAC)
Concept ID
C3878212857-POCLOUD
Data State
COMPLETE
Number of Files/Granules
85
Processing Level
4
Science Keywords
Ocean Bottom Pressure ,
Sea Level Anomaly

Citation

Citation is critically important for dataset documentation and discovery. This dataset is openly shared, without restriction, in accordance with the EOSDIS Data Use and Citation Guidance.

Copy Citation

Marie Zahn, M. W. (2026). SASSIE ECCO Ocean Bottom Pressure and Sea Surface Height - Snapshot llc1080 Grid (Version 1 Release 1) [Data set]. NASA Physical Oceanography Distributed Active Archive Center. https://doi.org/10.5067/SEL1S-OBP11 Date Accessed: 2026-01-29

Documents

Variables

Variables are a set of physical properties whose values determine the characteristics or behavior of something. For example, temperature and pressure are variables of the atmosphere. Parameters and variables can be used interchangeably. Variable level attributes provide individual information for each variable.

The Name in this table is the variable name. Fill value indicates missing or undefined data points in a variable. Valid range is the range of values the variable can store. Scale factor is used to increase or decrease the size of an object and can be used to correct for distortion. For questions on a specific variable, please use the Earthdata Forum.

Name Description Units Data Type Fill Value Valid Range Scale Factor
ETAN Model sea level anomaly WITHOUT corrections for global mean density (steric) changes, inverted barometer effect, or volume displacement due to submerged sea-ice and snow. . Note: ETAN should NOT be used for comparisons with altimetry data products because ETAN is NOT corrected for (a) global mean steric sea level changes related to density changes in the Boussinesq volume-conserving model (Greatbatch correction, see sterGloH) nor (b) sea level displacement due to submerged sea-ice and snow (see sIceLoad). The model has no atmospheric pressure forcing so there is no need to make an inverted barometer correction. m float 9.96921E+36 -7.7701148986816 to 0.79702681303024 1
i In the Arakawa C-grid system, tracer (e.g., THETA) and &#039;v&#039; variables (e.g., VVEL) have the same x coordinate on the model grid. N/A int N/A N/A 1
j In the Arakawa C-grid system, tracer (e.g., THETA) and &#039;u&#039; variables (e.g., UVEL) have the same y coordinate on the model grid. N/A int N/A N/A 1
PHIBOT PHIBOT = p_b / rhoConst - g H(t), where p_b = hydrostatic ocean bottom pressure, rhoConst = reference density (1027.5 kg m-3), g is acceleration due to gravity (9.81 m s-2), and H(t) is model depth at time t. Units: p:[kg m-1 s-2], rhoConst:[kg m-3], g:[m s-2], H(t):[m]. Note: PHIBOT is NOT corrected for global mean steric sea level changes related to density changes in the Boussinesq volume-conserving model (Greatbatch correction), and therefore should NOT be used for comparisons with ocean bottom pressure data. m2 s-2 float 9.96921E+36 -77.272216796875 to 1067.9703369141 1
time time of instantaneous snapshot hours since 1992-01-01T12:00:00 int N/A N/A 1
XC nonuniform grid spacing degrees_east float N/A -179.9994354248 to 179.99996948242 1
XC_bnds Bounds array follows CF conventions. XC_bnds[i,j,0] = &#039;southwest&#039; corner (j-1, i-1), XC_bnds[i,j,1] = &#039;southeast&#039; corner (j-1, i+1), XC_bnds[i,j,2] = &#039;northeast&#039; corner (j+1, i+1), XC_bnds[i,j,3] = &#039;northwest&#039; corner (j+1, i-1). Note: &#039;southwest&#039;, &#039;southeast&#039;, northwest&#039;, and &#039;northeast&#039; do not correspond to geographic orientation but are used for convenience to describe the computational grid. See MITgcm documentation for details. N/A float N/A N/A 1
YC nonuniform grid spacing degrees_north float N/A 48.678619384766 to 89.978286743164 1
YC_bnds Bounds array follows CF conventions. YC_bnds[i,j,0] = &#039;southwest&#039; corner (j-1, i-1), YC_bnds[i,j,1] = &#039;southeast&#039; corner (j-1, i+1), YC_bnds[i,j,2] = &#039;northeast&#039; corner (j+1, i+1), YC_bnds[i,j,3] = &#039;northwest&#039; corner (j+1, i-1). Note: &#039;southwest&#039;, &#039;southeast&#039;, northwest&#039;, and &#039;northeast&#039; do not correspond to geographic orientation but are used for convenience to describe the computational grid. See MITgcm documentation for details. N/A float N/A N/A 1
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