气象专业英语3汇编

1、 New words: Warning 警报 GMT （Greenwich Mean Time) 格林威治时间 Upper-air 高空的 Sounding 探测 WWW(world weather watch) 世界天气监视网 Code 电码 GTS（global telecommunication system) 全球电传通信系统 Strip 长带 belt band NOAA(National Oceanic and Atmospheric Administration) 诺阿卫星（美国国家海洋大气管理 局） GOES (geostationary operational environ

2、ment satellite) 地 球静止业务环境卫星 Multi-channel 多通道的 Assemble 组装，汇编 集合 Short-range 短期的 Long-range 长期的 nowcasting 现时预报，临近预报 Extrapolation 外推 interpolation 内插 Divergence 辐散 barotropic正压的 Prognosis 预测 smooth 平滑 filter 滤波 Geopotential 位势的 Prediction 预报 spectral 谱的 integrate 积分 Nest 嵌套 predictor 预报因子 MSL (mean

3、 sea level)平均海平面 MOS (model output statistic) 模式输出统计预报 Thunderstorm 雷暴 hurricane 飓风 Typhoon 台风 Subgrid 次网格 Substructure n. 次级结构次级结构 sub+ 亚；次级；下级亚；次级；下级 （构词法）（构词法） Subtropic 副热带，亚热带副热带，亚热带 Unpredictable 不可预报的不可预报的 predictable 可预报的可预报的 Predictability 可预报性可预报性 Frame-work 框架框架 Topographic 地形的地形的 orograp

4、hic Gust 阵风阵风 tornado （陆）龙卷（陆）龙卷 Freezing 冻结的冻结的 Doppler(radar)多谱勒雷达多谱勒雷达 Index(indices)指数指数 shear 切变切变 Downburst 下击暴流下击暴流 Serve as 充当，作为 P1National Meteorological Services perform a variety of activities in order to provide weather forecasts. The principal ones are data collection, the preparation

5、of basic analyses and prognostic charts of short-and long-term forecasts for the public as well as special services for aviation, shipping , agricultural and other commercial and industrial users, and the issuance of severe weather warnings. 1. Data sources P2: The data required for forecasting and

6、other services are provided by worldwide standard synoptic reports at 00, 06, 12, and 18 GMT, similar observations made hourly, particularly in support of national aviation requirements, upper- air soundings (at 00 and 12 GMT), satellite data and other specialized networks such as radar stations for

7、 severe weather . Under the World Weather Watch (WWW) program, synoptic reports are made at some 4,000 land stations and by 7,000 ships. There are about 700 stations making upper-air soundings (temperature, pressure, humidity, and, wind). These data are transmitted in code via teletype and radio lin

8、ks in regional or national centers and into the high-speed Global Telecommunications System (GTS) connecting World Weather Centres in Melbourne, Moscow and Washington and eleven Regional Meteorological Centres for redistribution. Some 157 states and territories cooperate in this activity under the a

9、egis of the World Meteorological Organization (WMO). P3:Meteorological information has been collected operationally by satellites of the United States and USSR since 1965 and, more recently, by the European Space Agency, India and Japan. There are two general categories of weather satellite: polar o

10、rbiters providing global coverage twice per 24 hours in orbital strips over the poles (such as the Unites States NOAA and TIROS series, and the USSRs Meteor) and geosynchronous satellites(such as the Geostationary Operational Environmental Satellites (GOES) and Metosat ) , giving repetitive(30-minut

11、e) coverage of almost one third of the earths surface in low middle latitudes. Information on the atmosphere is collected as digital data or direct readout visible and infrared images of cloud cover and sea-surface temperature, but also includes global temperature and moisture profiles which receive

12、 radiation emitted from particular levels in the atmosphere. Additionally, satellites have a data collection system (DCS) that relays data on numerous environmental variations from ground platforms or ocean buoys to processing centres; GOES can also transmit processed satellite images in facsimile a

13、nd the NOAA polar orbiters have an automatic picture transmission (APT) system that is utilized at 900 stations worldwide. 2. Forecasting P4:Modern forecasting did not become possible until weather information could be rapidly collected, assembled and processed. The first development came in the mid

14、dle of the last century with the invention of telegraphy, which permitted immediate analysis of weather data by the drawing of synoptic charts. These were first displayed in Britain at the Great Exhibition of 1851. Sequences of weather change were correlated with barometric pressure patterns both in

15、 space and time by such workers as Fitzroy and Abereroleby, but it was not until later that theoretival models of weather system were devisednotably the Bjerknes depression model. P5:Forecasts are usually referred to as short-range, medium (or extended) range and long-range. The first two can for pr

16、esent purposes be considered together. Short-range forecasting P6: Forecasting procedures developed up to the 1950s were based on synoptic principles but, since the 1960s, practices have been revolutionized by numerical forecasting models and the adoption of “nowcasting ” techniques. P7: During the

17、first half of the century, short-range forecasts were based on synoptic principles, empirical rules and extrapolation of pressure changes. P8:Since 1955 routine forecasts have been based on numerical models. These predict the evolution of physical processes in the atmosphere by determinations of the

18、 conservation of mass, energy and momentum. The basic principle is that the rise or fall of surface pressure is related to mass convergence or divergence, respectively, in the overlying air column. P9:Forecast practices in the major national centres are basically similar. The forecasts are essential

19、ly derived from twice-daily (00 and 12 GMT) prognoses of atmospheric circulation. Since most techniques are now largely automated, the analyses of synoptic fields are based on the previous 12-hour forecast maps as a first guess. Three different interpolation methods are used to obtain smoothed, grid

20、ed data on temperature, moisture, wind and geopotential height for the surface at standard pressure levels (850,700,500,400,300,250,200 and 100 mb) over the globe. The NMC currently has two basic prediction models: a special model with (6 or) 12 layers (from the boundary layer into the upper stratos

21、phere), which is integrated for up to 10 days, and a regionally applicable nested grid model with finer horizontal resolution. It should be noted that typically the computer time required increases several-fold when the grid spacing is halved. The essential forecast products are MSL pressure, temper

22、ature and wind velocity for standard pressure levels, 1000-500mb thickness, vertical motion and moisture content in the lower troposphere, and precipitation amounts. P10:Actual weather conditions are now commonly predicted using the Model Output Statistics(MOS) technique developed by the US National

23、 Weather Service. Rather than relating weather variable to the predicted pressure/height patterns and taking account of frontal models, for example, a series of regression equations are developed for specific locations between the variable of interest and up to 10 predictors calculated by the numeri

24、cal models. Weather elements so predicted for numerous locations include daily maximum/minimum temperature, 12-hour probability of precipitation occurrence and precipitation amount, probability of frozen precipitation , thunderstorm occurrence, cloud cover and surface winds. These forecasts are dist

25、ributed as facsimile maps and tables to weather offices for local use. P11:Errors in numerical forecast arise from several sources. One of the most serious is the limited accuracy of the initial analyses due to data deficiencies. The average over the oceans is sparse and only a quarter of the possib

26、le ship reports may be received within 12 hours; even over the land more than one-third of the synoptic reports may be delayed beyond 6 hours. However, satellites-derived information and aircraft reports can help fill some gaps for the upper air. Another limitation is imposed by the horizontal and v

27、ertical resolution of the models and the need to parameterize subgrid processes such as cumulus convection. The small-scale nature of the turbulent motion of the atmosphere means that some weather phenomena are basically unpredictable, for example, the specific locations of shower cells in an unstab

28、le air mass. Greater precision that the “showers and bright periods” or “scattered showers” of the forecast language is impossible with present techniques. The procedure for preparing a forecasting is becoming much less subjective, although in complex weather situations the skill of the experienced

29、forecaster still makes the technique almost as much as art as a science. Detailed regional or local predictions can only be made within the framework of the general forecast situation for the country and demand thorough knowledge of possible topographic or other local effects by the forecaster. Nowc

30、asting P12: Severe weather is typically short-lived(2 hr ) and, due to its mesoscale character(100km), it affects local/regional areas necessitating site- specific forecasts. Include in this category are thunderstorms, gust fronts, tornadoes, high winds especially along coasts, over lakes and mounta

31、ins, heavy snow and freezing precipitation. The development of radar networks, now instruments and high-speed communication links has provided a means of issuing warnings of such phenomena. Several countries have recently developed integrated satellite and radar systems to provide information on the

32、 horizontal and vertical extend of thunderstorms, for example. Such data are supplemented by networks of automatic weather stations (including buoys) that measure wind, temperature and humidity. In addition, for detailed boundary layer and lower troposphere data, there is now an array of vertical so

33、undersacoustic sounders (measuring wind speed and direction from echoes created by thermal eddies), specialized (Doppler) radar measuring winds in clear air by returns either from insects(3.5 cm wavelength radar) or from variations in the airs refractive index(10 cm wavelength radar). Nowcasting tec

34、hniques use highly automated computers and image analysis systems to integrate data from a variety of sources rapidly. Interpretation of the data displays requires skilled personnel and/or extensive software to provide appropriate information. The prompt forecasting of wind shear and down-burst haza

35、rds at airports is one example of the importance of nowcasting procedures. P13: Overall, the greatest benefits from improved forecasting can be expected in aviation, construction and the electric power industry for forecast less than 6 hours ahead, in transpiration, construction and manufacturing for 12-24 hour forecasts and in agriculture for 2-5 day forecasts. In terms of economic losses, the last category could benefit the most from more reliable and preci