CarbonTracker CT-NRT.v2018-1

CarbonTracker Near-Real Time (CT-NRT) is an extension of the formal CarbonTracker CO2 analysis system, designed to bridge the gap between annual updates of the formal CarbonTracker product. It extends model results past the end of the current CarbonTracker release up until the most recent date we can simulate. Usually this is limited by the availability of ERA-interim meteorology to drive the TM5 transport model. CT-NRT uses real-time meteorology, different flux priors, and assimilates only a small fraction of the CO2 observations assimilated by the formal CarbonTracker product. These are provisional, near-real time CO2 observations from the small set of sites able to provide them.

CT-NRT was created under funding from NASA, for use in the OCO-2 project.


CT-NRT.v2018-1 is the current release. It provides results from 2016-Dec-24 to 2018-Apr-29. CT-NRT.v2018-1 starts from a CT2017 initial condition on 2016-Dec-24 using the p1dm suite member. For dates before 1 January 2017, we recomment use of the standard CarbonTracker release (CT2017).

CT-NRT.v2018-1 results can be downloaded from ftp://aftp.cmdl.noaa.gov/products/carbontracker/co2/CT-NRT.v2018-1/.

CT-NRT.v2018-1 differs from our standard CarbonTracker product in the following ways:

  • Assimilation of provisional CO2 observations. In collaboration with measurement scientists from NOAA Global Monitoring Division and Environment Canada's Greenhouse Gas Measurement Program. (i.e., fewer obs and less quality control). CT-NRT.v2018-1 uses observational data from two ObsPacks: Prior to 2017-Jan-01, data are extracted primarily from the GLOBALVIEWplus_v3.1_2017-10-18 ObsPack. After 2017-Jan-01, data come from the_NRT_v4.2_2018-04-06 ObsPack. Decisions about which observations to assimilate, and with which level of model-data mismatch follow the CT2017 methodology.
  • Use of a different prior flux model. Our standard land biosphere flux prior is not available in near-real time, so we had to develop an alternative first-guess flux estimate. For this, we take the climatology of optimized land, wildfire, and ocean fluxes from the latest standard CarbonTracker release (for this release, that is CT2017). Since the majority of flux variability comes from the land biosphere, a land flux anomaly model also has been developed. This is a simple regression of CT2017 land flux anomalies as a function of anomalies of precipitation, shortwave radiation, and temperature. The statistical flux anomaly model was developed for each CarbonTracker ecoregion, and provides daily estimates of NEE anomaly. The radiation and temperature data for this model come from the ERA-interim meteorology used by TM5; the precipitation anomaly comes from the Global Precipitation Climatology Project. Although this flux prior does not reliably reproduce interannual variability, it is arguably a more statistically optimal prior than that for our standard release since it already represents the long-term mean CO2 sinks that we know exist. Since the priors for our standard release do not represent these sinks, the standard CarbonTracker requires that CO2 observations correct these biased priors.
  • High-temporal resolution FF emissions CT-NRT.v2018-1 does not yet apply the TIMES scaling factors to fossil fuel emissions, and therefore does not have diurnal and day-of-week variability in those emissions.


Previous releases of CT-NRT are available from ftp://aftp.cmdl.noaa.gov/products/carbontracker/co2/.