雨反射 的英文怎麼說

中文拼音 [yǔfǎnshè]
雨反射 英文
rain return
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 反 : Ⅰ名詞1 （方向相背） reverse side 2 （造反） rebellion 3 （指反革命、反動派） counterrevolutionari...
  • 射 : Ⅰ動詞1 （用推力或彈力送出） shoot; fire 2 （液體受到壓力迅速擠出） discharge in a jet 3 （放出） ...
  1. In spring and autumn, the landscape also has a special charm ? created by the way the light is reflected off the steep, rain - wet mountainsides, the clear crystal water of the lakes and fjords, or the high peaks with their mantles of eternal snow

    在春秋兩季的時候，景色別有一番風情? ?被雨水打濕的陡峭山腹、湖泊和峽灣中如水晶般透徹的流水，或者是常年積雪的挺拔峰頂會使光線出現反射現象。
  2. In spring and autumn, the tomato flavour also has a special charm vc created by the way the light is reflected off the steep, rain - wet mountainsides, the clear crystal water of the lakes and fjords, or the high peaks with their mantles of tombstone

    在春秋兩季的時候，內地景色別有一番風情? ?被雨水打濕的陡峭山腹、湖泊和峽灣中如色戒與性般透徹的流水，或者是常年積雪的挺拔峰頂會使光線出現反射現象。
  3. The reflected microwave would give the radar a false impression of rain

    這從地面反射回來的回波會使雷達誤以為是降雨。
  4. The maximum of instantaneous global radiation is beyond 1000w / m2 and the ten - days average intensity is 338. 90w / m2 because of high atmospheric transparency over semi - arid rainfed agriculture region of loess plateau between june and august. global radiation, reflected global radiation and surface long wave radiation emerge the characteristic of daily variations on a typical clear day and cloudy day, whereas atmospheric long wave radiation has not this characteristic. meanwhile, net radiation, latent heat flux sensible heat flux and soil heat flux appear the same characteristic as the mean daily variations above spring wheat field and bare soil on a typical clear day and cloudy day

    黃土高原半乾旱雨養農業區夏秋季大氣透明度較高，晴天地面的總輻射值最大瞬時值均超過1000w m ~ 2 ， 6 8月總輻射旬平均強度為338 . 90w m ~ 2 ；典型晴天和陰天總輻射、反射輻射、地表長波輻射均表現出明顯的日變化特徵，而雨天沒有明顯的日循環規律；無論是晴天、陰天還是雨天，大氣長波輻射基本沒有明顯的日變化規律。
  5. Based on rain drop size distribution ( dsd ) data measured in qingdao, guangzhou and xinxiang, the radar reflectivity factor z for spherical rain drops, the radar reflectivity factor zh and differential reflectivity zdr for oblate ellipsoid rain drops have been calculated. the relation of reflectivity and rainfall rate for conventional meteorological radar and the relation of reflectivity, differential reflectivity and rainfall rate for multiparameter radar are regressed, the performance difference of two kinds of radar for measuring rainfall and difference for measuring rainfall in different regions are also discussed

    基於我國青島、廣州和新鄉地區雨滴尺寸分佈數據，計算了球形雨滴雷達反射因子，橢球形雨滴雷達水平極化反射因子和差分反射率，回歸給出了這些地區的常規氣象雷達反射因子與降雨率的經驗關系和多參數雷達水下極化雷達反射因子、差分反射率和降雨率關系，並對其測雨精度和地區差異進行了比較。
  6. Although the radiant of the leonids is close to the star adhafera zeta leonis, do not look directly at it. a distance between 40 to 60 degrees away from the radiant is optimal

    雖然獅子座流星雨輻射點在軒轅十一附近，流星不一定出現在輻射點附近的天區，反而出現在輻射點40至60度以外的機會更大
  7. Then, after computing xpd induced by rain, its forecast model at different propagation distance is found. this paper also discusses the relation of reflectivity of rain with rainfall rate, taking different polarization wave into account, and that of fog with visibility

    在研究了雨、霧介電特性的基礎上，計算了雨的去極化解析度，得到了不同頻率、不同傳播距離的去極化解析度預報模型；計算了不同極化狀態的波的反射率隨降雨率的變化規律。
  8. According to different water phenomena, we use two different method to produce waves source : the first method is by specifying the boundary conditions and initialization conditions, this method simulate the dam breaking, reflection and diffraction of water waves ; the second method is by specifying disturbance model, this method simulate water droplets, waterfall, waves of ship ; in the first part of this thesis, we discuss the prevalent methods of the simulation of water scenes, in the second part of this thesis, we describe the numerical methods of solving the shallow water equations using the finite difference method and the finite volume method respectively, in the third part of this thesis, we simulate some realistically liquid phenomena such as rain droplets, the waves of ship, dam breaking etc

    產生水波首先要有波源，設置不同的波源便可以得到不同的水流情形，我們用兩種方法來產生波源：一種是通過設置邊界條件和初始條件產生，這種方法用於模擬潰壩波的反射、折射等現象；另一種是通過擾動控制產生，這種方法用於模擬雨滴、瀑布、船波等自然現象。本論文的第一部分我們討論了目前水動畫模擬常用的幾種方法；在第二部分討論了我們所使用的兩類數值方法：有限差分方法和有限體積方法；在第三部分我們模擬了雨滴、船波、潰壩波等一些水流現象。
  9. Reflectivity by local raingauge data, is incorporated into the model through a physical initialization process

    反射率所得出的每小時雨量資料，經物理初始化過程被納入模式內。
  10. That enables use to be made of what was previously just irritating noise ? the part of a radar beam that is reflected not from raindrops, but from fixed objects such as buildings

    這種方法使運用那些原先被認為只是由惱人的噪聲組成的東西成為可能? ?這一部分的雷達波不是從雨滴反射來得，而是來自諸如建築物那樣的固定物體。
  11. For the case of a doppler radar, the faster the raindrops move towards the radar, the higher will be the frequency i. e. pitch of the microwave reflected from raindrops fig. 1

    多普勒雷達利用同一原理：雨點移近雷達的速度越快，反射回來的微波頻率即聲調就越高圖1 。
  12. Weather radar may occasionally pick up reflected signals from sources other than rain, such as reflections from clouds, trees, buildings, birds, hills, sea waves and even distant land mass

    天氣雷達偶然會接收到並非來自降雨的反射信號，這包括來自雲樹木建築物雀鳥山海浪，甚至遙遠陸塊的反射。
  13. Here precipitation is shown in 6 levels of rainfall intensity or radar reflectivity on a 6 - degree elevation scan

    雨量是以6度仰角掃描所得的6層降雨強度雷達反射率來顯示。
  14. Here precipitation is shown in 6 levels of rainfall intensity ( or radar reflectivity ) on a 6 - degree elevation scan

    雨量是以6度仰角掃描所得的6層降雨強度（雷達反射率）來顯示。
  15. The biggest diurnal albedo is 0. 24 and the smallest 0. 11. moreover, the peak occurs on the day that radiation is very strong and the soil surface is dry and the valley appears on the day that rainfall is much more before this day and the soil water content of upper layer is high

    就反射率的日際變化而言，最大反射率為0 . 24 ，最小為0 . 11 ，相差一倍以上，其峰值均出現在輻射比較強，地表比較乾燥的日期，而谷底一般是在前期降雨較大，表層土壤濕潤時出現。
  16. The bottom image of reflectivity which provides estimation of the rain intensity depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado

    下圖為反射率表示估計的降雨強度圖像，顯示出該風暴出現了狀回波，這是卷風另一典型特徵。
  17. The bottom image of reflectivity ( which provides estimation of the rain intensity ) depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado

    下圖為反射率（表示估計的降雨強度）圖像，顯示出該風暴出現了?狀回波，這是龍卷風另一典型特徵。
  18. Occasionally, a microwave pulse reflected from a distant rain area may arrive at the radar after the radar has emitted the next pulse of microwave

    有些時候，當從遙遠的雨區反射回來的微波到達雷達時，雷達已經再次發出脈沖。
  19. In general, the more intense the reflected signals, the higher will be the rain intensity

    一般來說，反射回來的訊號越強，雨勢就越大。
  20. One reason is that radars used to track storms can detect water in the atmosphere only once it has condensed into clouds or raindrops, and thus reflects the beam

    一個原因是被用來追蹤雷暴的雷達只可以發現大氣中凝結成雲或雨滴的水，因為水能以這樣的形態反射波束。
分享友人
分享到 Line

分享到臉書