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meteorological satellite
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  气象卫星
     The Operation and Application of FY-1C/D Polar Orbiting Meteorological Satellite
     FY-1C/D极轨气象卫星的运行和应用
短句来源
     FY-1C/D Polar Orbiting Meteorological Satellite and Its Orbital Running
     FY-1C/D极轨气象卫星及其在轨运行
短句来源
     FY-2C Geostationary Meteorological Satellite and Its Development Prospect
     FY-2C业务静止气象卫星及发展展望
短句来源
     10-Band Scanning Radiometer of FY-1C/D Polar Orbiting Meteorological Satellite and Its Orbital Running
     FY-1C/D极轨气象卫星10通道扫描辐射计及其在轨运行
短句来源
     Summary on Computer Processing System (V3.2) of Meteorological Satellite Remote Sensing Data
     气象卫星遥感资料微机处理系统(V3.2)简介
短句来源
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  卫星气象
     This solution is based on theexisting network environment , the software and hardware platform , andthe Archive System construction of NSMC(National SatelliteMeteorological Center), and is implemented by the three Layer SystemStructure Web Browser ,Web Server and Web Database. It alsoimplemented and published the Internet/Intranet based catalogue retrievalvocational system of data from meteorological satellite.
     该方案基于国家卫星气象中心实际的网络环境、软硬件平台及气象卫星资料存档系统的建设,采用Web浏览器/Web服务器/Web数据库三层体系结构,实现并发布了基于Internet/Intranet的气象卫星资料编目检索业务系统。
短句来源
     In this project, the trajectories of MCS over the Qinghai-Xizang Plateau are automatically tracked using CMS ( Geostationary Meteorological Satellite) infrared black-body temperature (Tbb) and High Resolution Limited Area Analysis and Forecasting System (HLAFS) values provided by China National Satellite Meteorological Center from June to August 1998. Among these data, spatial resolution of Tbb is 0.5° lat (0.5°long, time resolution of Tbb is one hour).
     运用1998年夏季日本静止气象卫星(GMS)探测反演出的红外辐射亮温资料和国家卫星气象中心高分辨率有限区域分析预报系统产品中的数值格点预报资料(HLAFS)对青藏高原上的中尺度对流系统(MCS)进行了自动追踪。
短句来源
     A compression software for meteorological satellite cloud-chart realized with JPEG algorithm is proposed,which has been sucessfully used in the colud-chart data compression and transmitting system included in Jiangxi Anti-flood Computer Network.
     本文介绍了在计算机上以JPEG算法实现的红外卫星气象云图数据压缩软件,该软件已成功地应用于江西省防汛计算机网上的卫星气象云图的数据压缩和传输系统。
短句来源
     PROGRESS AND PROSPECT OF CHINA METEOROLOGICAL SATELLITE AND SATELLITE METEOROLOGY
     中国气象卫星和卫星气象研究的回顾和发展
短句来源
     Based on the structure of Meteorological satellite products distributed by national meteorology satellite center,by using data compress stock technology,we have discussed the stock compression and application of meteorological satellite data in the meteorological operation.
     根据国家卫星气象中心分发的气象卫星产品的格式规范,利用数据压缩存储技术,讨论了气象卫星资料在气象业务工作中的存储及应用.
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  “meteorological satellite”译为未确定词的双语例句
     Control Subsystem Design of FY-2C Meteorological Satellite
     FY-2C星控制分系统设计
短句来源
     Data Application of FY-2C Meteorological Satellite in Weather and Environment Monitoring Service
     FY-2C星在天气与环境监测服务中的应用
短句来源
     The retrievals from the AVHRR/HRPT data sea surface temperature computation software system using the NOAA-7 and NOAA-9 AVHRR data received at Beijing Meteorological Satellite Ground Station during the periods of 17, February and 7, September 1984, and 19-20, August, 14, September and 13-15, October, 1986, respectively, were compared with simultaneous measurements from ships and buoys.
     我们将AVHRR/HRPT资料海面温度计算软件系统,用1984年2月17日和9月7日北京地面站接收的NOAA-7 AVHRR资料,以及1986年8月19日、20日,9月14日和10月13、14、15日的NOAA-9 AVHRR资料的海面温度计算结果同相应时期的船泊或浮标测量的海面温度进行了比较。
短句来源
     The Geostationary Meteorological satellite (GMS-5) derived wind data from infrared and water vapor images and TIROS Operational Vertical Sounder (TOYS) temperature and humidity data enter the assimilation system after the quality control of MM5 model.
     地球同步卫星(Geostationary Meteorological Satellite(GMS-5))的红外和水汽轨迹风数据及来自NOAA极轨卫星的TOVS(TIROS Operational Vertical Sounder)温、湿数据作为观测资料,经过MM5模式的质量控制而最终进入该同化系统。
短句来源
     Flood Dynamic Monitoring of Nenjiang River in 1998 with NOAA Meteorological Satellite
     基于NOAA气象卫星的1998年嫩江洪水动态监测
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  meteorological satellite
Defense Meteorological Satellite Program are all examined for two contrasting monsoon years, namely 1987 (deficit rainfall) and 1988 (excess rainfall).
      
The first integration utilized sea ice albedos of the Arctic Basin for the spring and summer of 1977 derived from defence Meteorological Satellite Imagery (DMSP).
      
These data were received by using common heritage instrumentation installed on four PROGNOZ satellites, INTERBALL-1, PHOBOS, and the geosynchronous meteorological satellite ELECTRO.
      
The SSM/I microwave Brightness Temperatures (TB's) in the frequency domains of 85 and 19 GHz gathered from the Defense Meteorological Satellite Program (DMSP)-F8 satellite form the basis of this research.
      
Sea ice concentration and ice velocity datasets derived from images of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSM/I) are employed to reveal this mechanism.
      
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In this paper, using Geostationary Meteorological Satellite (GMS) cloud pictures and conventional meteorological data, an analysis of the process of the development of three typhoons in the ITCZ in July 1978 has been conducted. It is found that during the development of typhoon the ITCZ was consisted of two separate convergence zone in the East and West. They were closely connected with the large-scale circulation in the Northern and Southern Hemisphere. During the development of typhoons the tropical...

In this paper, using Geostationary Meteorological Satellite (GMS) cloud pictures and conventional meteorological data, an analysis of the process of the development of three typhoons in the ITCZ in July 1978 has been conducted. It is found that during the development of typhoon the ITCZ was consisted of two separate convergence zone in the East and West. They were closely connected with the large-scale circulation in the Northern and Southern Hemisphere. During the development of typhoons the tropical upper tropospheric trough (TUTT) over ocean areas was situated further north and west, and it directed from east to west. There were many active cloud clusters (cold vortices) in the trough. The initial perturbation of each typhoon was at the south side of TUTT. It is also found that during the development of typhoon, distribution of the low level inflow and of the upper level outflow were not symmetric.

本文利用地球静止卫星云图配合常规资料对1978年7月一次强热带辐合带上三个扰动发展成台风的过程进行了分析。结果表明,多台风发生时强赤道辐合带往往并不是完整的一条,而是由东西二段辐合带合并而成,它们与南北半球的大型环流有着密切的关系。在三个扰动发展时,对流层上层大洋中部槽的位置偏北、偏西,槽呈东—西走向,在槽中多冷涡活动。台风的初始扰动位于洋中槽南侧。我们还根据每隔三小时一张地球静止卫星云图分析。发现扰动云系发展成台风云系时,低空流入和高空流出分布是不对称的。

In this paper, using Geostationary Meteorological Satellite (GMS) imagery and conventional meteorological data, the spiral cloud band of the Typhoon is analysed. The discussion is mainly focused on the process of its formation and dissipation, and its movement and structure.

本文利用地球静止卫星云图配合其它资料分析台风螺旋云带,着重讨论台风螺旋云带的形成和消失过程,及螺旋云带的运动和结构等。

By use of the daytime visible cloud picture from TIROS-N meteorological satellite, statistics on the cloudiness distribution of high light clouds over the Qing Zang plateau month by month from May to August of 1979 has been made. It is found that there exists a good relationship between precipitation R and appearing frequency of high light clouds P over the Qing Zang plateau region to the west of 95E. This relation is expressed as R = APa. The linear correlation coefficients are 0.82 for May and greater...

By use of the daytime visible cloud picture from TIROS-N meteorological satellite, statistics on the cloudiness distribution of high light clouds over the Qing Zang plateau month by month from May to August of 1979 has been made. It is found that there exists a good relationship between precipitation R and appearing frequency of high light clouds P over the Qing Zang plateau region to the west of 95E. This relation is expressed as R = APa. The linear correlation coefficients are 0.82 for May and greater than 0.98 for June,July, and August. In addition,by making use of the measuring precipitation data from meteorological and hydrographical stations and also by coordinating with the calculated precipitation from the high light clouds observed from the satellite on 2×2 grid, the month by month summer precipitation distribution chart over the plateau is then obtained.From it we also find that in early summer, there is a high precipitation axial line and on its north and south sides there are less precipitation zones.

利用TIROS-N气象卫星白天可见光云图,统计了1979年5—8月青藏高原上空逐月高亮度云的云量分布。发现95°E以西高原地区的降水量R和高亮度云出现的频率P之间存在着良好的关系,即R=AP~α。线性化相关系数5月份为0.82,6、7和8月份均在0.98以上。利用气象站和水文站的实测降水资料,再配合2°×2°网格上由卫星高亮度云推算出来的降α水量,得到了高原地区夏季的和逐月的降水量分布图。发现初夏在34°—35°N有一条高降水轴线,其南北两侧则是少雨区。

 
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