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noresm:norstorearchive [2014-06-24 14:07:16]
alok.gupta@uni.no [Metadata example]
noresm:norstorearchive [2014-10-28 12:12:49]
alok.gupta@uni.no [Metadata recommendations]
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 ==== BibliographicCitation ==== ==== BibliographicCitation ====
  
-For NorESM1-M output: http://www.geosci-model-dev.net/6/687/2013/gmd-6-687-2013.html +Specify "http://cmip-pcmdi.llnl.gov/cmip5/terms.html" as value.
- +
-For NorESM1-ME output: http://www.geosci-model-dev.net/6/301/2013/gmd-6-301-2013.html+
  
 ==== Coverage ==== ==== Coverage ====
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 Mapping between CMIP5 experiment acronyms and NorESM1-M cases: Mapping between CMIP5 experiment acronyms and NorESM1-M cases:
 <file> <file>
- piControl      r1 NAER1850CNOC_f19_g16_06  + piControl      r1 NAER1850CNOC_f19_g16_06  (3.1) 
- 1pctCO2        r1 N1850RMAERCN_f19_g16_01 + 1pctCO2        r1 N1850RMAERCN_f19_g16_01  
  abrupt4xCO2    r1 N18504XAERCN_f19_g16_01   abrupt4xCO2    r1 N18504XAERCN_f19_g16_01 
  amip           r1 NFAMIP2005AERAMIPO_f19_f19_01 (1979-2005), NFAMIP2008AERAMIPO_f19_f19_01 (2006-2008)  amip           r1 NFAMIP2005AERAMIPO_f19_f19_01 (1979-2005), NFAMIP2008AERAMIPO_f19_f19_01 (2006-2008)
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 | **Conforms to** | Climate and Forecast (CF) metadata conventions |  | **Conforms to** | Climate and Forecast (CF) metadata conventions | 
 | **Provenance** | gzip compression of restart files and conversion of history output to compressed NetCDF-4 format | **Ingo:** specify time stamp of last compressed restart file |    | **Provenance** | gzip compression of restart files and conversion of history output to compressed NetCDF-4 format | **Ingo:** specify time stamp of last compressed restart file |   
-| **Coverage** | Box: southlimit=-90, northlimit=90, westlimit=-180, eastlimit=180, units=signed decimal degrees; Period: start=2006-01-01, end=2012-12-31, scheme=W3C-DTF | **Ingo:** use of DCMI standard makes it easy for external servers to interpret the coverage information | +| **Coverage** | Box: Southlimit=-90, Northlimit=90, Westlimit=-180, Eastlimit=180, Uplimit=20000, Downlimit=-9000, Units=signed decimal degrees, Zunits=m; Period: start=2006-01-01, end=2012-12-31, scheme=W3C-DTF | **Ingo:** use of DCMI standard makes it easy for external servers to interpret the coverage information | 
  
  
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 Technical details: Technical details:
-Model source: https://svn.met.no/viewvc/noresm/noresm/branches/noresm-ver1_cmip5-r112/ 
-Model revision number: 112 
 Production machine: Cray XT3 in Bergen (hexagon) Production machine: Cray XT3 in Bergen (hexagon)
-Model typeFully coupled +Model sourcehttps://svn.met.no/viewvc/noresm/noresm/branches/noresm-ver1_cmip5-r112 
-InitialisationStart from CMIP5 historical simulation r2 (N20TRAERCN_f19_g16_02) at 2006-01-01 +Model revision number112 
-Resolutionf19_g16=1.9×2.5 degree atmosphere/land. Dipolar ocean/ice grid, ~1 degree  +Model components: atmosphere=CAM4; ocean=MICOM; land=CLM; sea ice=CICE 
-Output frequency: Monthly + daily + 6h 3h as requested by CMIP5 +Horizontal resolution: atmosphere/land=1.9x2.5 degreeocean/sea ice=~1 degree   
-Changing forcing agents: prescribed GHG concentrations; aerosol emissions (SO4, POM and BCsee Kirkevåg et al. 2013)+Output frequency: monthly + daily + 6-hourly 3-hourly as requested by CMIP5 
 +Experiment type: fully coupled 
 +Initialisation: branched from CMIP5 historical simulation r2 (N20TRAERCN_f19_g16_02) at 2006-01-01 
 +Changing forcing agents: prescribed GHG concentration changes; aerosol emissions for SO4, POM and BC (see Kirkevåg et al. 2013)
 Tuning parameters changed relative to the host model CAM4: rhminl=0.90 (0.91 in CAM4) reduced RH threshold for formation of low stratiform clouds; critrp=5.0 mm/day (0.5 mm/day in CAM4) maximum precipitation rate for suppression of autoconversion of cloud water; r3lc=14 um (10 um in CAM4) critical mean droplet volume radius for onset of autoconversion Tuning parameters changed relative to the host model CAM4: rhminl=0.90 (0.91 in CAM4) reduced RH threshold for formation of low stratiform clouds; critrp=5.0 mm/day (0.5 mm/day in CAM4) maximum precipitation rate for suppression of autoconversion of cloud water; r3lc=14 um (10 um in CAM4) critical mean droplet volume radius for onset of autoconversion
 Other comments: - Other comments: -
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 http://search.es-doc.org (model system, boundary conditions, experiments, etc) http://search.es-doc.org (model system, boundary conditions, experiments, etc)
 http://noresg.norstore.no (Norwegian ESGF portal with post-processed CMIP5 data) http://noresg.norstore.no (Norwegian ESGF portal with post-processed CMIP5 data)
-http://www.cristin.no/as/WebObjects/cristin.woa/wo/18.Profil.29.25.2.3.3.7 (link to national publication database) 
 http://www.geosci-model-dev.net/special_issue20.html (NorESM special issue) http://www.geosci-model-dev.net/special_issue20.html (NorESM special issue)
 +http://www.cristin.no/as/WebObjects/cristin.woa/wo/18.Profil.29.25.2.3.3.7 (link to national publication database)
 </code> </code>
  • noresm/norstorearchive.txt
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