rain intensity 中文意思是什麼

rain intensity 解釋
降雨率
  • rain : n 1 雨,下雨;〈pl 〉陣雨。2 雨天;〈the rains〉(熱帶地方的)雨季;〈the rains〉大西洋北緯4 10度...
  • intensity : n. 1. (思想、感情的)強烈,激烈。2. 強度。3. 【攝影】(底片的)明暗度。
  1. Analyzing the physics structure of vorticity, divergence, vertical velocity, frontogenesis " function, apparent heat source and apparent moist sink etc. indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity

    主要分析了這次過程中的多種物理量,包括渦度、散度、垂直速度、鋒生函數、視熱源、視水汽匯等,對這一暴雨過程有了比較系統的認識。結果表明:在江淮流域存在著有利於發生暴雨的物理量場配置,渦度、散度、垂直速度等物理量,與暴雨的落區都很吻合的;低空急流的產生不僅有利於水汽的輸送,而且高低空急流的耦合造成了有利於強上升運動的配置;鋒生強度隨著降水系統的發展變化,並影響降水強度。
  2. The rain from thick stratiform clouds usually lasts longer than showers although the intensity is lighter

    由深厚層狀雲產生的降水,通常比驟雨持續的時間長,但雨勢較小。
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  4. This is often known as frontal rain, which is typically wide in extent and uniform in intensity

    鋒面雨的一般特徵是下雨范圍廣闊和雨勢平均。
  5. There was a highly significant correlation between the highest rain intensity in 30 minutes ( abbreviated as i30 ) and rv, and no significant correlation between rainfall capacity and 130. the soil conservation effects were better than the water conservation effects. the order of importance for water and soil conservation effects in different treatments was eragrostis curvula, kummerowia atriata, ixeris denticulata, with the most significantly positive correlation between each runoff and soil loss

    與裸坡相比,嚴重侵蝕地上植物籬笆的保土效果比保水效果更明顯,其中畫眉草( eragrostiscurvula )水土保持能力最強,雞眼草( kummerowiaatriata )次之,苦蕒菜( ixerisdenticulata )只具有保土作用;同時每次降雨產生徑流量與侵蝕量之間為極顯著相關關系。
  6. Parameter estimation in torrential rain intensity formula with its application

    暴雨強度公式參數估計及其應用
  7. Rain intensity has more effect on the loss of soil, slowly available k, and rapidly available k than slope gradient

    雨強比坡度對土壤、緩效鉀和速效鉀的流失影響更大。
  8. ( 5 ) the concentration of dissolved k and amount of dissolved k, rapidly available k, and slowly available k lost in the runoff increase obviously with the increase of rain intensity

    ( 5 )雨強(沖刷強度)增大,溶解態鉀濃度,溶解態鉀、緩效鉀和速效鉀流失量明顯增加。
  9. Rain intensity has little effect on er of rapidly available k and slowly available k, and leads some decrease of er of rapidly available k. er of rapidly available k increases with the decrease of slope gradient

    雨強對速效鉀、緩效鉀的富集率影響不大,速效鉀的富集率有一定的減少;隨著坡度的減小,速效鉀富集率有增大的趨勢。
  10. On the basis of analyzing factor ( soil particle composition, soil bulk density, water stable aggregate content, antecedent soil moisture, slope gradient, rain intensity, accumulation depth and soil crust, soil and water conservation tillage measures ) affecting soil infiltration rates, several relation models was obtained ; analyzed in detail different soil and water conservation tillage measures intensifying infiltration rates, while there have the same rainfall condition, the increasing infiltration rates of contour tillage and artificial digging and artificial hoeing in gully areas of loess plateau are 67 % and 41 % and 29 % ; the increasing infiltration rates in hilly areas of loess plateau is 45 % and 22 % and 14 %

    在相同的降雨條件下,黃土高原溝壑區等高耕作與直線坡相比,可提高入滲67 ,人工掏挖可提高入滲41 ,人工鋤耕可提高入滲29 ;黃土丘陵溝壑區等高耕作可提高入滲45 ,人工掏挖可提高入滲22 ,人工鋤耕可提高入滲14 。並根據黃土高原超滲產流的概念和水量平衡方程,建立了不同水土保持耕作措施強化入滲速率模型。
  11. Rainfall and vertical profile of hydrometers are retrieved for land and ocean using tmi 1b11 data. the comparison of retrievals of gprof v6. 1 and v6. 2 with ground - based radar and gauge data on land and pr data on ocean show that the gprof - v6 algorithm can retrieve rain intensity much well and indicate vertical distribution of hydrometers mainly. as far as retrieved precipitation area, it is better for convective precipitation type than stratified precipitation type

    將陸地的反演結果與地基雷達資料和地面雨量計資料進行比較,海洋的反演結果結合trmmpr的降水產品進行比較,結果表明: gprof - v6演算法反演的降水產品可以較好地反映降水強度並反映降水的主要垂直結構;在落區方面,對流降水反映較好,層雲降水則較差;雲-輻射數據集的擴充與改進可提高反演精度。
  12. The results shows that the motion track of the vortex is well coincident with the rainfall variation at the center of rain masses as well as the evolutions of rain intensity and the vortex intensity

    該低渦的移動路徑與雨團的活動近於一致,雨強和低渦的強度變化也近於一致。
  13. The observatory ' s weather radar system at tate ' s cairn detects rain within about 500 km of hong kong and gives estimates of rain intensity and movement

    天文臺設于大老山的天氣雷達,能監察香港約500公里范圍內的降雨區,和估計雨勢及雨區的移動。
  14. 2. on the basis of analyzing experimental data for slope land of loess plateau in different slope gradient and rain intensity and soil and water conservation tillage measures, using curve - fitting techniques, a soil infiltration rates model was woke out, the accuracy of the model is tested by a series of experiment data, the result of these indicate that the soil infiltration rates model is accurate and has good stability for slope land of loess plateau. 3. using soil infiltration rates and runoff time and wetting frontal surface depth of soil infiltration reflect effect of factor affecting soil infiltration rates

    ( 3 )採用土壤穩定入滲速率、坡面開始產流時間、土壤濕潤鋒面下滲深度三個指標來反映坡耕地土壤入滲影響(土壤性質、土壤初始含水率、地面坡度、降雨強度、積水深度、水土保持耕作措施等)因素效用大小,建立了各因素與三個指標的關系模型,詳細分析了不同水土保持耕作措施強化土壤入滲的影響,其中等高耕作作用最為顯著,其次是人工掏挖和人工鋤耕。
  15. In this thesis, with eight events of artificial water - washing test on five different slope gradients, factors affecting soil potassium loss by erosion, such as slope gradient, rain intensity, vegetation coverage, and amount of rainfall are discussed

    本文通過在5個不同坡度徑流小區進行的8次人工模擬沖刷試驗,探討了坡度、放水沖刷強度、植被和降雨量等因素對土壤鉀素徑流流失的影響。
  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. The rain intensity is represented by different colours as shown in the inset

    雨勢強度以不同顏色顯示,請參看小圖。
  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. The hong kong observatory announces the availability of radar pictures with rain intensity information in its website today ( august 9 )

    香港天文臺今日(八月九日)宣布在網上發放雷達圖像。雷達圖像提供了雨勢強弱的資料。
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