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    Improvement of Short-Term Climate Prediction with Indirect Soil Variables Assimilation in China

    Source: Journal of Climate:;2017:;volume 031:;issue 004::page 1399
    Author:
    Wang, Chenghai
    ,
    Cui, Zhiqiang
    DOI: 10.1175/JCLI-D-17-0210.1
    Publisher: American Meteorological Society
    Abstract: AbstractShort-term climate prediction based on a regional climate dynamical model heavily depends on atmospheric forcing and initial soil moisture state. In this study, the Weather Research and Forecasting (WRF) Model with different nudging schemes is used for approximate 2-yr simulations for investigating the importance of soil variables in seasonal temperature and precipitation simulations. The results show that the improvement of seasonal climate simulation (precipitation and air temperature) is more evident in the experiment of assimilating both soil and atmospheric variables than that in the experiments of assimilating atmospheric variables only. Further investigation of the impact of indirectly assimilating soil moisture on precipitation prediction with an indirect soil nudging (ISN) scheme shows that the precipitation reproducibility in summer is better than that in winter, and the effect of ISN is particularly prominent in the region where seasonal precipitation exceeds 200 mm. Moreover, statistical results also illustrate that initial soil moisture plays a crucial role in seasonal precipitation forecasts because of its slowly evolving nature, and its effect is more distinct in semiarid and semihumid regions than in arid and humid regions. The effects of indirectly assimilating soil moisture on precipitation can last two and three months in semiarid and semihumid areas, respectively.
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      Improvement of Short-Term Climate Prediction with Indirect Soil Variables Assimilation in China

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4262031
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    contributor authorWang, Chenghai
    contributor authorCui, Zhiqiang
    date accessioned2019-09-19T10:08:40Z
    date available2019-09-19T10:08:40Z
    date copyright11/21/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-17-0210.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262031
    description abstractAbstractShort-term climate prediction based on a regional climate dynamical model heavily depends on atmospheric forcing and initial soil moisture state. In this study, the Weather Research and Forecasting (WRF) Model with different nudging schemes is used for approximate 2-yr simulations for investigating the importance of soil variables in seasonal temperature and precipitation simulations. The results show that the improvement of seasonal climate simulation (precipitation and air temperature) is more evident in the experiment of assimilating both soil and atmospheric variables than that in the experiments of assimilating atmospheric variables only. Further investigation of the impact of indirectly assimilating soil moisture on precipitation prediction with an indirect soil nudging (ISN) scheme shows that the precipitation reproducibility in summer is better than that in winter, and the effect of ISN is particularly prominent in the region where seasonal precipitation exceeds 200 mm. Moreover, statistical results also illustrate that initial soil moisture plays a crucial role in seasonal precipitation forecasts because of its slowly evolving nature, and its effect is more distinct in semiarid and semihumid regions than in arid and humid regions. The effects of indirectly assimilating soil moisture on precipitation can last two and three months in semiarid and semihumid areas, respectively.
    publisherAmerican Meteorological Society
    titleImprovement of Short-Term Climate Prediction with Indirect Soil Variables Assimilation in China
    typeJournal Paper
    journal volume31
    journal issue4
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-17-0210.1
    journal fristpage1399
    journal lastpage1412
    treeJournal of Climate:;2017:;volume 031:;issue 004
    contenttypeFulltext
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