長期平均流量 的英文怎麼說

中文拼音 [zhǎngqīpíngjūnliúliáng]
長期平均流量 英文
long period average flow
  • 長 : 長Ⅰ形容詞1 （年紀較大） older; elder; senior 2 （排行最大） eldest; oldest Ⅱ名詞（領導人） chief;...
  • 期 : 期名詞[書面語]1. （一周年） a full year; anniversary 2. （一整月） a full month
  • 平 : Ⅰ形容詞1 （沒有高低凹凸 不頃斜） flat; level; even; smooth 2 （高度相同; 不相上下） on the same l...
  • 均 : Ⅰ形容詞（均勻） equal; even Ⅱ副詞（都; 全） without exception; all
  • 流 : Ⅰ動1 （液體移動; 流動） flow 2 （移動不定） drift; move; wander 3 （流傳; 傳播） spread 4 （向壞...
  • 量 : 量動1. （度量） measure 2. （估量） estimate; size up
  • 長期 : over a long period of time; long-term; long range; secular
  • 流量 : rate of flow; flow; runoff; discharge; throughput; （flow） rate; quantity （of flow）; flux
  1. On the basis of sediment concentration field, the annual back silting intensity on the approach channel of 70000 dwt at lianyungang harbor was also simulated, and the calculated results was coincident with actual data

    鑒于進港航道回淤量是當地海域潮流、波浪、泥沙長期共同作用的結果，建議採用年平均含沙量場進行回淤計算，並在此基礎上模擬了連雲港7萬噸級進港航道的年回淤強度，計算結果與實測資料吻合較好。
  2. All these results confirm the important of wind in meridional circulation and heat transport. based on mom2 model, a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow. the effects of horizontal diffusivity, seasonal variations of

    我們還通過全球海洋環流模式，進一步證實了風應力的季節變化在北印度洋熱收支、 sst以及海洋環流變化中的作用:即包含風應力的季節變化將使長期平均的sst降低，海面凈熱通量增加。
  3. When making estimate of the cash flow after the year of the budget or forecast, the growth rates adopted shall not, unless the enterprise can prove that it is reasonable to adopt higher growth rates, exceed the long - term average growth rate of the products, or the market, or the industrial field which the enterprise belongs to, or the country or region where the enterprise is located, or the long - term average growth rate of the market where the asset is situated

    在對預算或者預測期之後年份的現金流量進行預計時，所使用的增長率除了企業能夠證明更高的增長率是合理的之外，不應當超過企業經營的產品、市場、所處的行業或者所在國家或者地區的長期平均增長率，或者該資產所處市場的長期平均增長率。
  4. The key area of the first eigenvector of eof for summer precipitation decadal change in china allots in south and north of changjiang river which vary contrary ; the second one ' s allots in middle valley of changjiang river and jianghuai valley ; the third one ' s allots almost in total china. ( 3 ) tropic and north pacific summer ssta ' s decadal change has good correlation with china summer precipitation ' s decadal change

    中國年平均與汛期平均降水eof分析的前三個特徵向量基本一致，第一特徵向量表現為長江南北反向的形態，第二特徵向量表現為中部為正，其餘為負的分佈形態，第三特徵向量表現為長江中游、江淮流域為正，其南北兩側為負的分佈形態。
  5. 2 ) the analyse of the structure of mei - yu low and the elationship between the low and rainfall three lows moved along the mei - yu front towards the northeast during mei - yu period in 1999, which produced three intensive rainfall periods along the yangtze river : ill the station of huangshan, the most heavy rainfall center, totally had 850mm rain during 11 days. the reason for the heavy rainfall was the sustaining moisture supply from the south, and the deep moist layer and the high relative humidity in the south - east quadrant

    2 ）梅雨鋒低渦的結構及其與降水關系分析1999年在梅雨鋒上有三個梅雨鋒低渦相繼在其上產生，冰箱東北方向移動，分別對應著長江中下游的三次強降水過程：最大降水中心黃山11天累計降水量達到850mm ，為梅雨期間平均降水量的150以上。低渦之所以產生這么大的降水和降水強度是因為低渦在移動過程中不斷有水汽輸入和補充，在其東南象限對流層中低層維持了深厚的濕層和很高的相對濕度。
分享友人
分享到 Line

分享到臉書