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模式输出的英文

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"模式输出"怎么读用"模式输出"造句

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  • model output

例句与用法

  • Check of the temperature and relative humidity output from mesoscale numerical forecast model
    中尺度数值预报模式输出产品温度和相对湿度的检验
  • By using the psu / ncar mm5 model , we made a numerical simulation about the severe sand - dust storm that occured in the north china on 20march in 2002
    20 ”强沙尘暴天气过程进行了数值模拟,并利用模式输出的各物理量对沙尘暴进行诊断分析,得出了华北地区沙尘暴的形成、发展机制。
  • The retrieval atmospheric three - dimensional wind field are compared with the three - dimensional wind field output by mm5 numerical simulation to show the reliability of this retrieval method
    反演出的三维风场再与mm5数值模式输出的三维风场加以比较,验证此种反演方法的可靠性。
  • Use one of the databases whose schema language is supported by tranql , and then use the tranql schema generator within your build system to generate the schema output at build time
    使用某种数据库,其模式语言受tranql支持,然后使用构建系统内部的tranql模式生成器在构建时生成模式输出
  • Apart from technical exchanges , discussion was made on the enhancement of weather information exchanges including the provision of numerical model output , automatic weather station and radar data
    研讨会中,双方除作技术交流外,更讨论了如何增加天气资料的交换,包括提供数值模式输出、自动气象站和雷达等数据。
  • Apart from technical exchanges , discussion was made on the enhancement of weather information exchanges including the provision of numerical model output , automatic weather station and radar data
    研讨会中,双方除作技术交流外,更讨论了如何增加天气资料的交换,包括提供数值模式输出、自动气象站和雷达等数据。
  • The simulative cloud image , made from the mixing ratios of cloud liquid water , rain water , ice crystal , snow , graupel which were outputted by the mesoscale model mm5 , resemble the gms satellite infrared image very well and also show the cloud evolution of typhoon winnie from tropical cyclone to extratropical cyclone after landing
    利用高分辨率中尺度数值模式输出的大气中云水冰水雨水雪水成功地模拟出1997年登陆台风winnie的云系结构。模拟云图与气象卫星实际观测的台风云图非常相似。由于模拟云图可以给出大气中不同形态水物质的三维空间分布,弥补了卫星只能观测云顶表面的不足。
  • Because the system error is ineluctable for mode , it is necessary to correct the simulation fielde effectively . in this paper , based on the idea of combined eof correction , the interannual simulation of sea surface wind stress anomalies of the tropical pacific ocean by lap two - level atmosphereic model have been corrected , result of corrected erperiment shows that the corrected field is more similar to the observation field , especially on the distribution of the space . three prediction experiments also shew that correcting scheme of combined eof can improve the interannual prediction veracity of model
    在本文中,基于“联合自然正交展开误差订正”的思想,将中科院大气物理研究所两层大气环流模式输出的热带太平洋海表风应力异常的跨年度模拟场进行订正,订正试验的分析结果表明,订正后的热带太平洋海表风应力距平场与相应观测场年际变率分量的相似程度远远好于模式模拟的结果,尤其是在空间分布方面的改善非常显著;三组跨年度订正检验结果也表明,订正后的跨年度预测结果明显好于模式的预测结果。
  • Hunan limited - region numerical weather prediction system is based upon the fifth - generation psu / ncar meso - scale model ( version 3 . 4 ) , named mm5 which is a non - hydrostatic model . the initial and lateral boundary conditions of the system are generated from the output of the t213 model of the national meteorology center ( nmc ) and the routine observation data of surface and high levels
    湖南省有限区域数值天气预报系统是以psu / ncar的mm5v3 . 4 (第五代中尺度模式版本3 . 4 )非静力中尺度模式为基础,与国家气象中心t213模式输出场资料连接,并应用最临近常规高空、地面观测资料做初始场及参数修订,在银河机群服务器系统yh / cs16并行运算环境下运行的中尺度数值模式。
  • Based on the observation data such as coads and soda , the main climatological features of the tropical indian ocean and relationships of sea surface temperature ( sst ) , heat budget with ocean dynamics and thermodynamics processes are analyzed ; the seasonal and interannual variability of the tropical indian ocean are well simulated using a ocean general circulation model ; based on the thermal equation and model output data , the variation mechanism of sst and heat budget are investigated in the tropical indian ocean ; besides , the effect of seasonal variation of wind stress , ekman pumping and horizontal diffusivity on the ocean current and heat budget are studied , using both ideal model and complex model
    本文根据coads 、 soda等实际观测资料,较全面的分析了热带印度洋主要的气候特点,并研究了海表面温度( sst ) 、热收支与海洋动力、热力过程的联系;利用全球海洋环流模式较好地模拟出热带印度洋的季节和年际变化;基于热力学方程和海洋环流模式输出结果,探讨了热带印度洋sst和北印度洋热量收支的季节和年际变化机制,进一步揭示了海洋动力过程在北印度洋热平衡中的重要作用;在此基础上,利用理想化的数值试验与数值模拟结果相结合的方式,证实了风应力的季节变化和ekman抽吸,以及水平热量扩散系数对北印度洋海洋环流和热收支的影响。
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