Title: |
ESPC-D-V02: Global 1/12° Analysis (Aug-10-2024 to Present with 8-day forecast) output on the GLBy0.08 grid
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Resolution: |
ESPC-D-V02 daily 1/25° (GLBz0.04) deterministic run decimated to the GLBy0.08 1/12° grid
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Institution: |
Fleet Numerical Meteorology and Oceanography Center (FNMOC) |
Date/Data Range: |
2024-Aug-10 to Present with 8-day forecast [no known missing data] |
Experiment Sequence: |
expt_03.1
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Generating Model: |
ESPC-D V02: HYCOM 2.2.99, CICE 5.1.2, expt_03.1
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Input Data Source: |
FNMOC NAVGEM, Satellite SSH, SST, SMMI, in situ observations
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2d Variables 1-hourly: |
1-hourly temporal frequency:
- ice
- sic = sea_ice_area_fraction
- sih = sea_ice_thickness
- siu = eastward_sea_ice_velocity
- siv = northward_sea_ice_velocity
- sss = sea_water_salinity
- sst = sea_water_temperature
- ssu = eastward_sea_water_velocity
- ssv = northward_sea_water_velocity
- surtx = surface_downward_eastward_stress
- surty = surface_downward_northward_stress
- ssh
- surf_el = Water Surface Elevation
- Sssh
- steric_ssh = steric SSH
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3z Variables 3-hourly: |
3-hourly temporal frequency:
- s3z
- salinity = Salinity
- t3z
- water_temp = Water Temperature
- u3z
- water_u = Eastward Water Velocity
- v3z
- water_v = Northward Water Velocity
with Vertical Levels ( depth ) : 0.0 2.0 4.0 6.0 8.0 10.0 12.0 15.0 20.0 25.0 30.0 35.0 40.0 45.0 50.0 60.0 70.0 80.0 90.0 100.0 125.0 150.0 200.0 250.0 300.0 350.0 400.0 500.0 600.0 700.0 800.0 900.0 1000.0 1250.0 1500.0 2000.0 2500.0 3000.0 4000.0 5000.0 m
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Unaggregated Data: |
archive: data in the "archive" folder aims to be a consistent time series for each day. It contains a copy of the "best" t0000 to t0023 forecast files (note: t0024 to t0047 files from the previous forecast can be substituted when a run is missing).
forecasts: data in the "forecasts" folder contains the full forecasts for each model run. note: only the last 8 full model runs are available here. A scrubber deletes all forecasts older than 8 days.
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Data Format(s): |
NetCDF
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Detailed Dataset Info/Description Coming Soon...
Differences between ESPC-D-V01 and ESPC-D-V02
- Overview
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ESPC-D-V01 is the "high-resolution deterministic system" described in Barton et al. (2021).
The coupled components have been slightly upgraded for V02:
- NAVGEM
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Still T681, but increased from 60 to 143 levels with a high altitude option
(model top around 114 km). Updated tropospheric physics.
- HYCOM
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Eight tidal constituents (V01 only used 5).
- CICE
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Using version 6.1.4.
- WW3
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One-way coupling to WW3 at 1/8° resolution (new component in V02, no feedback to the ocean).
TIDES in ESPC-D-V02
HYCOM 41-layer 1/25 degree global (86S to 90N), sunk ice shelf, 8 tides + atmospheric pressure, 49-hour tidal drag filter, Jayne St.Laurent scalar drag, drgscl = 0.3, observed SAL, with ASEnKF correction (Ngodock et al, 2016).
See Tidal Analysis of ESPC-D-V02
References
- The Navy's Earth System Prediction Capability: A New Global Coupled Atmosphere-Ocean-Sea Ice Prediction System Designed for Daily to Subseasonal Forecasting
- Barton, N., Metzger, E. J., Reynolds, C. A., Ruston, B., Rowley, C., Smedstad, O. M., et al. (2021). The Navy's Earth System Prediction Capability: A new global coupled atmosphere-ocean-sea ice prediction system designed for daily to subseasonal forecasting. Earth and Space Science, 8, e2020EA001199. doi.org/10.1029/2020EA001199
- On improving the accuracy of the M2 barotropic tides embedded in a high-relolution global ocean circulation model
- Hans E. Ngodock, Innocent Souopgui, Alan J. Wallcraft, James G. Richman, Jay F. Shriver, Brian K. Arbic,
On improving the accuracy of the M2 barotropic tides embedded in a high-resolution global ocean circulation model,
Ocean Modelling, Volume 97, 2016, Pages 16-26, ISSN 1463-5003, doi.org/10.1016/j.ocemod.2015.10.011
- A Primer on Global Internal Tide and Internal Gravity Wave Continuum Modeling in HYCOM and MITgcm
- Arbic, Brian K., Matthew H. Alford, Joseph K. Ansong, Maarten C. Buijsman, Robert B. Ciotti, J. Thomas Farrar, Robert W. Hallberg, et al. “A Primer On Global Internal Tide And Internal Gravity Wave Continuum Modeling In Hycom And Mitgcm”. New Frontiers In Operational Oceanography, August 1, 2018. doi.org/10.17125/gov2018.ch13
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