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    Evaluating Tropical Precipitation Relations in CMIP6 Models with ARM Data

    Source: Journal of Climate:;2022:;volume( 035 ):;issue: 019::page 2743
    Author:
    Todd Emmenegger
    ,
    Yi-Hung Kuo
    ,
    Shaocheng Xie
    ,
    Chengzhu Zhang
    ,
    Cheng Tao
    ,
    J. David Neelin
    DOI: 10.1175/JCLI-D-21-0386.1
    Publisher: American Meteorological Society
    Abstract: 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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      Evaluating Tropical Precipitation Relations in CMIP6 Models with ARM Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4289913
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    contributor authorTodd Emmenegger
    contributor authorYi-Hung Kuo
    contributor authorShaocheng Xie
    contributor authorChengzhu Zhang
    contributor authorCheng Tao
    contributor authorJ. David Neelin
    date accessioned2023-04-12T18:34:52Z
    date available2023-04-12T18:34:52Z
    date copyright2022/09/14
    date issued2022
    identifier otherJCLI-D-21-0386.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289913
    description abstractA 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.
    publisherAmerican Meteorological Society
    titleEvaluating Tropical Precipitation Relations in CMIP6 Models with ARM Data
    typeJournal Paper
    journal volume35
    journal issue19
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-21-0386.1
    journal fristpage2743
    journal lastpage2760
    page2743–2760
    treeJournal of Climate:;2022:;volume( 035 ):;issue: 019
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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