ERA5 reanalysis data: Difference between revisions
(Adding file name pattern for pl, sfc, and pv2-data.) |
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pv2/ Data on the PV2-surface following the format of ERA-interim. | pv2/ Data on the PV2-surface following the format of ERA-interim. | ||
sfc/ Single-level data following the format of ERA-interim. | sfc/ Single-level data following the format of ERA-interim. | ||
slope/ Isentropic slope data and its tendencies following the format of ERA-interim | |||
Data in the '''ml'''-folder are contained in subdirectories for each year and month: | Data in the '''ml'''-folder are contained in subdirectories for each year and month: | ||
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Until now, the years 1999-2018 have been retrieved, the period will successively be extended back to 1979, and forward in time. | Until now, the years 1999-2018 have been retrieved, the period will successively be extended back to 1979, and forward in time. | ||
Data in the '''pl_*''', '''sfc''' and ''' | Data in the '''pl_*''', '''sfc''', '''pv2''' and '''slope'''-folders is organised in one file per month, variable and level, for example: | ||
pl/ea.[ans|for].YYYYMM.PLEV.VAR | pl/ea.[ans|for].YYYYMM.PLEV.VAR | ||
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Please see [https://confluence.ecmwf.int//display/CKB/ERA5+data+documentation#ERA5datadocumentation-Parameterlistings ECMWF ERA5 data documentation] for parameter abbreviations. | Please see [https://confluence.ecmwf.int//display/CKB/ERA5+data+documentation#ERA5datadocumentation-Parameterlistings ECMWF ERA5 data documentation] for parameter abbreviations. | ||
The folder '''slope''' contains the following variables (see [https://doi.org/10.1002/qj.2605 Papritz and Spengler, 2015], for further details on meaning of variables): | |||
{| class="wikitable" | |||
!colspan="1"|Variable name | |||
!colspan="1"|Description | |||
!colspan="1"|Equation | |||
!colspan="1"|Units | |||
!colspan="1"|Notes | |||
|- | |||
|slope | |||
|Slope of isentropic surface | |||
| S = abs(grad<sub>θ</sub>z) | |||
|m m<sup>-1</sup> | |||
|Instantaneous | |||
|- | |||
|tilt | |||
|Tendency in slope due to tilting | |||
| grad<sub>θ</sub>z /S · grad<sub>θ</sub> w<sub>id</sub> | |||
|m m<sup>-1</sup> s<sup>-1</sup> | |||
|Instantaneous | |||
|- | |||
|diab | |||
|Tendency in slope due to diabatic heating | |||
| -dz/dθ grad<sub>θ</sub>z /S · grad<sub>θ</sub> (dθ/dt) | |||
|m m<sup>-1</sup> s<sup>-1</sup> | |||
|Accumulated over 6-hour period centred on instantaneous time step | |||
|- | |||
|iadv | |||
|Tendency in slope due to isentropic advection | |||
| '''u''' · grad<sub>θ</sub>S | |||
|m m<sup>-1</sup> s<sup>-1</sup> | |||
|Instantaneous | |||
|- | |||
|w_ci | |||
|Cross isentropic vertical velocity | |||
| w - w<sub>iu<sub> | |||
|m s<sup>-1</sup> | |||
|Instantaneous | |||
|- | |||
|mask_slope | |||
|Combination of masks from slope, diab and tilt | |||
| - | |||
|0-1 | |||
|Instantaneous | |||
|} | |||
'''Conditions of use:''' When using the ERA5 data from this archive please make sure to reference "[https://cds.climate.copernicus.eu/cdsapp#!/home Copernicus Climate Change Service (C3S) (2017): ERA5: Fifth generation of ECMWF atmospheric reanalyses of the global climate. Copernicus Climate Change Service Climate Data Store (CDS)], date of citation" and acknowledge "ECMWF for providing ERA-5 data“. Also, please acknowledge "Michael Sprenger (ETH Zurich)“ for the support in providing the data. | '''Conditions of use:''' When using the ERA5 data from this archive please make sure to reference "[https://cds.climate.copernicus.eu/cdsapp#!/home Copernicus Climate Change Service (C3S) (2017): ERA5: Fifth generation of ECMWF atmospheric reanalyses of the global climate. Copernicus Climate Change Service Climate Data Store (CDS)], date of citation" and acknowledge "ECMWF for providing ERA-5 data“. Also, please acknowledge "Michael Sprenger (ETH Zurich)“ for the support in providing the data. |
Revision as of 14:26, 20 March 2023
Documentation of the ERA5 archive at GFI
GFI is building up an archive of ERA5 reanalysis data on the local linux system cyclone.hpc.uib.no. ERA5 supersedes the ERA-Interim reanalysis data, which ended in August 2019. More information about the ERA5 reanalysis data set is available at ECMWF's ERA5 websites.
The ERA5 data files are available in a CF-compatible netCDF format on cyclone.hpc.uib.no and other computers that mount the UiB linux system at
/Data/gfi/share/era5
At GFI, we share the data format with the Atmospheric Dynamics group at IAC, ETH Zürich, Switzerland; the LSDP group at Karlsruhe Institute of Technology, Germany; and the Dynamical Meteorology Group, Weizmann Institute of Science, Rehovot, Israel. The data are organised as follows
ml/ 3-hourly data on a regular 0.5 deg lat-lon grid, with model-level and pressure level files (see below) pl/ pressure level data following the format of ERA-interim. pl_tendencies/ diabatic temperature tendencies on pressure levels, following the format of ERA-interim. pv2/ Data on the PV2-surface following the format of ERA-interim. sfc/ Single-level data following the format of ERA-interim. slope/ Isentropic slope data and its tendencies following the format of ERA-interim
Data in the ml-folder are contained in subdirectories for each year and month:
ml/yyyy/mm/[B|H|P|Z]yyyymmdd_hh
where yyyy is the year, mm the two-digit month, dd the two-digit day, and hh the two-digit hours, and Bxxx, Hxxx, Pxxx, Zxxx are different file types, as described in the table below.
Until now, the years 1999-2018 have been retrieved, the period will successively be extended back to 1979, and forward in time.
Data in the pl_*, sfc, pv2 and slope-folders is organised in one file per month, variable and level, for example:
pl/ea.[ans|for].YYYYMM.PLEV.VAR
This data is completely available for 1979-2020.
The data files contain the following variables:
ERA5 data files | |||||
---|---|---|---|---|---|
File name | Pyyyymmdd_hh | Zyyyymmdd_hh | Hyyyymmdd_hh | Byyyymmdd_hh | |
Leveltype | Model level | Surface | Pressure | Pressure | Surface |
Variables | T, Q, U, V, OMEGA, LWC, IWC, RWC, SWC | LSP, CP, SF, SSHF, SLHF, BLH, TCC, U10M, V10M, MSL, PS, SSTK | Z, T, Q, U, V | Z | PS, MSL, TCC, U10M, V10M, SSTK, CI, D2M, T2M, TCW, TCWV, VIWVD, E, MN2T, MX2T, SI, TTR, TTRC, WG10, LSP, CP, SF, SSHF, SLHF, BLH |
Levels | 40-137 | - | 900, 850, 800, 700, 600, 500, 400, 300, 250, 200, 100 hPa | 1000, 975, 950, 925, 900, 875, 850, 825, 800, 775, 750, 700, 650, 600, 550, 500, 450, 400, 350, 300, 250, 225, 200, 175, 150, 125, 100, 70, 50, 30, 20, 10, 70, 5, 3, 2, 1 hPa | - |
Times available | 00, 03, 06, 09, 12, 15, 18, 21 UTC |
Note that the variables LSP, CP, SF, SSHF, SLHF, and BLH are derived as prognostic variables from the short-range forecast. Data valid at 00, 03, 06, 09 UTC are 06, 09, 12, 15 h forecast of the 18 UTC forecast of the previous day. Accordingly, data valid at 12, 15, 18, 21 UTC are 06, 09, 12, 15 h forecast of the 06 UTC forecast. The prognostic variables are accumulated over the previous 1 h.
Please see ECMWF ERA5 data documentation for parameter abbreviations.
The folder slope contains the following variables (see Papritz and Spengler, 2015, for further details on meaning of variables):
Variable name | Description | Equation | Units | Notes |
---|---|---|---|---|
slope | Slope of isentropic surface | S = abs(gradθz) | m m-1 | Instantaneous |
tilt | Tendency in slope due to tilting | gradθz /S · gradθ wid | m m-1 s-1 | Instantaneous |
diab | Tendency in slope due to diabatic heating | -dz/dθ gradθz /S · gradθ (dθ/dt) | m m-1 s-1 | Accumulated over 6-hour period centred on instantaneous time step |
iadv | Tendency in slope due to isentropic advection | u · gradθS | m m-1 s-1 | Instantaneous |
w_ci | Cross isentropic vertical velocity | w - wiu | m s-1 | Instantaneous |
mask_slope | Combination of masks from slope, diab and tilt | - | 0-1 | Instantaneous |
Conditions of use: When using the ERA5 data from this archive please make sure to reference "Copernicus Climate Change Service (C3S) (2017): ERA5: Fifth generation of ECMWF atmospheric reanalyses of the global climate. Copernicus Climate Change Service Climate Data Store (CDS), date of citation" and acknowledge "ECMWF for providing ERA-5 data“. Also, please acknowledge "Michael Sprenger (ETH Zurich)“ for the support in providing the data.