Datasets
nextGEMS cycle2 coupled global 1-year simulation without parameterized deep convection. Grids: tco2559 for atmosphere and NG5 for ocean. Model versions: IFS 47r3.3 + upgrades and FESOM2.1. Starting date: 20/01/2020.
Examples
retrieve, class=rd, date=20200120, stream=LWDA, expver=hqys, type=fc, levtype=sfc, param=2t, anoffset=9, time=0, step=24, target='output.grib'Retrieve 2m temperature after 24 hours
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nextGEMS cycle2 coupled global 1-year simulation without parameterized deep convection. Grids: tco1279 for atmosphere and orca025 for ocean. Model versions: IFS 47r3.3 + upgrades and NEMO3.4. Starting date: 20/01/2020.
Examples
retrieve, class=rd, date=20200120, stream=LWDA, expver=hr2n, type=fc, levtype=sfc, param=2t, anoffset=9, time=0, step=24, target='output.grib'Retrieve 2m temperature after 24 hours
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nextGEMS cycle2 coupled global 2-year simulation with parameterized deep convection. Grids: tco1279 for atmosphere and orca025 for ocean. Model versions: IFS 47r3.3 + upgrades and NEMO3.4. Starting date: 20/01/2020.
Examples
retrieve, class=rd, date=20200120, stream=LWDA, expver=hrn6, type=fc, levtype=sfc, param=2t, anoffset=9, time=0, step=24, target='output.grib'Retrieve 2m temperature after 24 hours
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2003 to 2005. Spinup-time is two months (Nov-Dec 2002) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2006 to 2008. Spinup-time is two months (Nov-Dec 2005) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2009 to 2011. Spinup-time is two months (Nov-Dec 2008) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2012 to 2014. Spinup-time is two months (Nov-Dec 2011) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2015 to 2017. Spinup-time is two months (Nov-Dec 2014) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO CY49R1 free-running simulation of atmospheric composition (chemistry, aerosol), with meteorology re-initialized from ERA5 every day at 00UTC, with three-hourly output for the years 2018 to 2020. Spinup-time is two months (Nov-Dec 2017) and grid is reduced linear gaussian, TL255 (~80km horizontal resolution). Instantaneous aerosol MMR fields are stored on 16 pressure levels.
Examples
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IFS-COMPO Reference experiment for fire emission sensitivity evaluation. This experiment uses a CY50R1 esuite model configuration, but with updates to the isoprene degradation chemistry, along with a basic implementation of C2H2 chemistry, as planned for CY51R1. Otherwise, this experiment is run as a series of 24h forecasts excluding assimilation of atmospheric composition on T511 horizontal resolution. Default GFAS fire emissions are employed here.
Examples
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IFS-COMPO Reference experiment for fire emission sensitivity evaluation. This experiment uses a CY50R1 esuite model configuration, but with updates to the isoprene degradation chemistry, along with a basic implementation of C2H2 chemistry, as planned for CY51R1. Otherwise, this experiment is run as a series of 24h forecasts excluding assimilation of atmospheric composition on T511 horizontal resolution. This experiment uses daily fire emissions from the FINN database.
Examples
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