積雲參數化 的英文怎麼說

中文拼音 [yúnshēnshǔhuà]
積雲參數化 英文
cumulus parameterization
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : Ⅰ動詞[書面語] (說) say Ⅱ名詞1. (雲彩) cloud 2. (雲南) short for yunnan province3. (姓氏) a surname
  • : 參構詞成分。
  • : 數副詞(屢次) frequently; repeatedly
  1. ( 5 ) parameterization of infrared satellite cloud imagery and its application in rainfall predication obvious correlation exist between the probability of rain and parameterization estimate such as average brightness temperature ( tb ), brightness temperature variance ( f ), equivalent cloudage ( cn ), brightness temperature area index ( al - the first a5 - the fifth grade, a6 - the sixth grade )

    ( 5 )衛星及在降雨預測中的應用紅外衛星估計值,與局地降雨過程的發生、發展具有較為密切的關系。相關較密切的有平均亮溫、亮溫方差、等效量、亮溫面( 1級、 5級、 6級) 。
  2. The neogene is a key stage of terrestrial environmental evolution in yunnan. three stratigraphic sections including luhe ( late miocene ), yangyi and longling ( late pliocene ) were selected to reconstruct vertical landscape of paleovegetation in these areas, based on palynological data. according to principle of the coexistence approach, seven quantitative paleoclimatic parameters of each deposit area were obtained by using meteorological data ( 1951 - 1980 ) of the distribution area of extant taxa found each palynoflora in china

    晚第三紀是南地區環境演變過程中的關鍵地質歷史時段,本論文以晚第三紀晚中新世(呂合) 、晚上新世(羊邑和龍陵)地層中的孢粉為研究對象,結合同層位大石植物證據,照現代植被,恢復了南三個石出產地區的古植被垂直分佈景觀,並定性地描述了古氣候;同時運用共存分析方法( theco - existenceapproach )定量地重建了三個地區的古氣候值;初步推測了沉地可能的古海拔。
  3. The horizontal scalelength of model variables ( u. v. t, p and q ) is closely related to the average time of nmc technique and convective parameteric scheme of mm5 which affect the 12h and 24h outputs of mm5 integration

    、 、 、 t 、 p和q )對應的誤差水平尺度與nmc方法中預報誤差的平均時間長度和模式提供1zh和24h預報所選用的積雲參數化方案有直接的關系。
  4. Mm5 has a ability of simulating zwd on the whole with a bias larger than zhd ' s, which manipulates the bias of ztd simulation. the increase of mm5 resolution can improve the ability of simulating and depicting zhd, zwd and pw distribution. kf, bm and grell parametric schemes have a close ability of simulating pw at the beginning of 10 - 11h integration of mm5 model, and then the prediction bias of pw increases obviously after 20 - 21h integration

    在mm5模式24h分的前10 11h ,選用kf 、 bm和grell三種積雲參數化方案模式對可降水量的預報偏差基本接近,對可降水量具有較好的預報能力,其後三種積雲參數化方案對可降水量的預報偏差差異增大,模式分至20 21h后對可降水量的預報能力明顯減小。
  5. The results also show that the precipitation forecast of the system is very sensitive to cumulus parameterization scheme, planet boundary layer ( pbl ) scheme and radiation scheme. for smaller meshes, the grell cumulus parameterization scheme is better than the other three cumulus parameterization schemes that are also tested in the experiments

    值模擬試驗結果還顯示,模擬降水預報對積雲參數化方案、邊界層方案、輻射方案等比較敏感;在網格比較小時, grell積雲參數化方案優于本文試驗的另外三種積雲參數化方案。
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