4.7 Article

Evaluating Tropical Precipitation Relations in CMIP6 Models with ARM Data

Journal

JOURNAL OF CLIMATE
Volume 35, Issue 19, Pages 2743-2760

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-21-0386.1

Keywords

Atmosphere; Convection; Convective clouds; Precipitation; Climate models; Clouds

Funding

  1. U.S. Department of Energy [AGS-1936810]
  2. National Science Foundation [DE-AC52-07NA27344]
  3. U.S. Department of Energy's Atmospheric Radiation Measurement (ARM) program
  4. U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research
  5. DOE ARM program under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory
  6. U.S. Department of Energy by Lawrence Livermore National Laboratory
  7. [DE-SC0011074]

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A set of diagnostics is used to assess the behavior of the Coupled Model Intercomparison Project (CMIP6) models with respect to precipitation. The models show significant errors in the relationship between precipitation and column water vapor (CWV). Models also exhibit biases in column relative humidity (CRH) statistics, with compensating biases often occurring.
A set of diagnostics based on simple, statistical relationships between precipitation and the thermodynamic environment in observations is implemented to assess phase 6 of the Coupled Model Intercomparison Project (CMIP6) model behavior with respect to precipitation. Observational data from the Atmospheric Radiation Measurement (ARM) permanent field observational sites are augmented with satellite observations of precipitation and temperature as an observational baseline. A robust relationship across observational datasets between column water vapor (CWV) and precipitation, in which conditionally averaged precipitation exhibits a sharp pickup at some critical CWV value, provides a useful convective onset diagnostic for climate model comparison. While a few models reproduce an appropriate precipitation pickup, most models begin their pickup at too low CWV and the increase in precipitation with increasing CWV is too weak. Convective transition statistics compiled in column relative humidity (CRH) partially compensate for model temperature biases-although imperfectly since the temperature dependence is more complex than that of column saturation. Significant errors remain in individual models and weak pickups are generally not improved. The conditional-average precipitation as a function of CRH can be decomposed into the product of the probability of raining and mean precipitation during raining times (conditional intensity). The pickup behavior is primarily dependent on the probability of raining near the transition and on the conditional intensity at higher CRH. Most models roughly capture the CRH dependence of these two factors. However, compensating biases often occur: model conditional intensity that is too low at a given CRH is compensated in part by excessive probability of precipitation.

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