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    Variational Assimilation of Cloud Liquid/Ice Water Path and Its Impact on NWP

    Source: Journal of Applied Meteorology and Climatology:;2015:;volume( 054 ):;issue: 008::page 1809
    Author:
    Chen, Yaodeng
    ,
    Wang, Hongli
    ,
    Min, Jinzhong
    ,
    Huang, Xiang-Yu
    ,
    Minnis, Patrick
    ,
    Zhang, Ruizhi
    ,
    Haggerty, Julie
    ,
    Palikonda, Rabindra
    DOI: 10.1175/JAMC-D-14-0243.1
    Publisher: American Meteorological Society
    Abstract: nalysis of the cloud components in numerical weather prediction models using advanced data assimilation techniques has been a prime topic in recent years. In this research, the variational data assimilation (DA) system for the Weather Research and Forecasting (WRF) Model (WRFDA) is further developed to assimilate satellite cloud products that will produce the cloud liquid water and ice water analysis. Observation operators for the cloud liquid water path and cloud ice water path are developed and incorporated into the WRFDA system. The updated system is tested by assimilating cloud liquid water path and cloud ice water path observations from Global Geostationary Gridded Cloud Products at NASA. To assess the impact of cloud liquid/ice water path data assimilation on short-term regional numerical weather prediction (NWP), 3-hourly cycling data assimilation and forecast experiments with and without the use of the cloud liquid/ice water paths are conducted. It is shown that assimilating cloud liquid/ice water paths increases the accuracy of temperature, humidity, and wind analyses at model levels between 300 and 150 hPa after 5 cycles (15 h). It is also shown that assimilating cloud liquid/ice water paths significantly reduces forecast errors in temperature and wind at model levels between 300 and 150 hPa. The precipitation forecast skills are improved as well. One reason that leads to the improved analysis and forecast is that the 3-hourly rapid update cycle carries over the impact of cloud information from the previous cycles spun up by the WRF Model.
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      Variational Assimilation of Cloud Liquid/Ice Water Path and Its Impact on NWP

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217441
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    • Journal of Applied Meteorology and Climatology

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    contributor authorChen, Yaodeng
    contributor authorWang, Hongli
    contributor authorMin, Jinzhong
    contributor authorHuang, Xiang-Yu
    contributor authorMinnis, Patrick
    contributor authorZhang, Ruizhi
    contributor authorHaggerty, Julie
    contributor authorPalikonda, Rabindra
    date accessioned2017-06-09T16:50:37Z
    date available2017-06-09T16:50:37Z
    date copyright2015/08/01
    date issued2015
    identifier issn1558-8424
    identifier otherams-75138.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217441
    description abstractnalysis of the cloud components in numerical weather prediction models using advanced data assimilation techniques has been a prime topic in recent years. In this research, the variational data assimilation (DA) system for the Weather Research and Forecasting (WRF) Model (WRFDA) is further developed to assimilate satellite cloud products that will produce the cloud liquid water and ice water analysis. Observation operators for the cloud liquid water path and cloud ice water path are developed and incorporated into the WRFDA system. The updated system is tested by assimilating cloud liquid water path and cloud ice water path observations from Global Geostationary Gridded Cloud Products at NASA. To assess the impact of cloud liquid/ice water path data assimilation on short-term regional numerical weather prediction (NWP), 3-hourly cycling data assimilation and forecast experiments with and without the use of the cloud liquid/ice water paths are conducted. It is shown that assimilating cloud liquid/ice water paths increases the accuracy of temperature, humidity, and wind analyses at model levels between 300 and 150 hPa after 5 cycles (15 h). It is also shown that assimilating cloud liquid/ice water paths significantly reduces forecast errors in temperature and wind at model levels between 300 and 150 hPa. The precipitation forecast skills are improved as well. One reason that leads to the improved analysis and forecast is that the 3-hourly rapid update cycle carries over the impact of cloud information from the previous cycles spun up by the WRF Model.
    publisherAmerican Meteorological Society
    titleVariational Assimilation of Cloud Liquid/Ice Water Path and Its Impact on NWP
    typeJournal Paper
    journal volume54
    journal issue8
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-14-0243.1
    journal fristpage1809
    journal lastpage1825
    treeJournal of Applied Meteorology and Climatology:;2015:;volume( 054 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian