I have been comparing the ERA5 single level datasets and EAC4 multilevel data and I am confused.
If I use the EAC4 data to compute the total column concentrations for ozone, for example, I get a different value than I receive from the ERA5 single level dataset.
To be more precise, I use the mass ratio data from EAC4 and the surface pressure value for my location. Then I compute the pressure profile using the PSAB method with the 60 level specification. Using this pressure profile I compute the total column concentration of ozone.
I do notice, that my way of computing the total column concentration becomes consistent with the single level data from ERA5, if I assume 1013 hPa surface pressure and ignore the actual value.
So, finally, to come back to my question:
What is the relationship between the ERA5 single level data (total column ozone) and EAC4 multi level data? Which of these two values is computed from the other? Am I right in suspecting, that the default L60 level definitions, with 1013 hPa surface pressure, are used to compute the ERA5 single level value from the EAC4 multi level data?
Ah, I just had another thought: Is it possible, that the single level data is computed using the Mean sea level pressure, instead of the surface pressure?
Hi,
the two datasets are produced independently. Here a table with some info:
|
EAC4 |
|
ERA5 |
Exp ID |
exp=eac4, class=mc |
Period covered |
1940 - present |
Period covered |
2003 - present (though only 2003 - Dec 2022) |
Production Period |
Jan 2016 – end 2017, then continued in near real-time |
Production Period |
Jan 2017 – Dec 2018, then continued in near real-time |
Model version |
IFS Cycle 41r2 |
Assimilation system |
IFS Cycle 42r1 4D-Var |
Assimilation system |
IFS Cycle 41r2 4D-Var |
Spatial resolution |
80 km globally (T255), 60 levels to 0.1 hPa |
Spatial resolution |
31 km globally, 62km for the Ensemble of Data Assimilations (EDA), 137 levels to 0.01 hPa |
Output frequency (temporal resolution) |
3-hourly analysis fields,3-hourly forecast fields from 0 UTC up to 48 hours,1-hourly surface forecast fields from 0 UTZ up to 48 hours |
Output frequency (temporal resolution) |
Hourly analysis fields, 3-hourly for the Ensemble of Data Assimilations (EDA), Hourly forecast fields, 3-hourly for the Ensemble of Data Assimilations (EDA), up to 18 hours, with reduced frequency up to 10 days (not in initial release) |
Anthropogenic missions |
MACCity (trend: ACCMIP + RCP8.5) & CO emission upgrade Stein et al. (2014) |
Uncertainty estimates |
From a 10-member Ensemble of Data Assimilations (EDA) at 63 km resolution |
Biomass burning emissions |
GFAS v 1.2 |
Model input |
Appropriate for climate (e.g. CMIP5 greenhouse gases, volcanic eruptions, SST and sea-ice cover) |
Biogenic emissions |
Monthly mean VOC emissions calculated by the MEGAN model using MERRA reanalysed meteorology (Sindelarova et al., 2014) for the whole period. |
Input observations |
In addition, various newly reprocessed datasets and recent instruments that could not be ingested in ERA-Interim |
Chemistry modules |
IFS CB05 (Flemming et al. 2015, with updates as given in CAMS: Reanalysis data documentation) & Cariolle ozone parametrisation in stratosphere |
Variational bias scheme |
Also ozone, aircraft and surface pressure data |
Aerosol modules |
See CAMS: Reanalysis data documentation |
Satellite data |
RTTOV-11, all-sky for various components |
Input meteorological observations |
As in ERA5 (2003-2016?), OPS for later years |
New parameters |
ERA5 contains over 240 parameters on surface and single level alone, plus parameters on other level types. For specific parameters please compare the technical documentation linked below. |
Input atmospheric composition observations |
See CAMS reanalysis data documentation |
Parameters removed |
A few parameters present in ERA-Interim are not available in ERA5. For availability of specific parameters please see the technical documentation linked below. |
Aerosol used in radiation scheme |
Interactive active aerosols, i.e. aerosol fields from eac4 used in radiation scheme |
Handling of accumulated parameters |
Accumulated from previous post-processing |
Ozone used in radiation scheme |
Interactive ozone, i.e. ozone field from eac4 used in radiation scheme |
Product main page |
Climate reanalysis | Copernicus |
Parameters |
Full chemistry output archived as type=an every 3 hours (see parameter lists on CAMS: Reanalysis data documentation) |
Technical documentation |
ERA5 data documentation |
Stratospheric chemistry |
No, but Cariolle ozone parametrisation in stratosphere and stratospheric O3 available. |
Additional innovations |
Long-term evolution of CO2 in RTTOV, cell-pressure correction SSU, improved bias correction for radiosondes, EDA perturbations for sea-ice cover |
Product main page |
CAMS: Reanalysis data documentation |
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Technical documentation |
CAMS: Reanalysis data documentation |
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