moisture transport 中文意思是什麼

moisture transport 解釋
水分輸送
  • moisture : n. 濕氣,水分,潮濕；濕度；（空氣中的）水蒸氣；淚。
  • transport : vt 1 運輸，運送，輸送。2 【歷史】處流刑，流放。3 殺死。4 〈常用被動語態〉使心情極度激動，使欣喜若...
  1. Climatological characteristics, which can provide some drought or flood years with large - scale background, are investigated for large - scale water vapor transport over asian - australian monsoon region based on vertically integrated water vapor flux by pentad from 1980 to 1997. at the same time, the differences of moisture transport over the yangtze river basin between drought and flood and the moisture budgets over eastern china from april to september are examined. major results are as follows : i

    使用1980 ? 1997年垂直積分的整層水汽輸送通量資料，從氣候平均的角度分析了亞澳季風區大尺度水汽輸送演變和偏南風水汽輸送在東亞地區推進的氣候特徵，為研究異常年份旱澇事件的產生提供了相應的大尺度背景；同時還討論了長江流域旱澇年水汽輸送的差異以及4 - 9月我國東部各區域的水分收支情況。
  2. In drought ( flood ) years over the yangtze river basin, the southerly moisture transport with the summer monsoon can shift to northern ( southern ) than the normal, the southeasterly water vapor from south

    雨季建立之前和雨季結束之後，華北和東北地區西邊界的偏西風水汽輸入占絕對優勢;雨季中南邊界的偏南風水汽輸送對華北最為重要，東北地區雨季期間南邊界的水汽輸入和與來自西邊界的水汽輸入貢獻相當。
  3. The results showed that the combination of both capillary absorption and moisture diffusion fitted the experimental data very well, pore structures of cement - based materials had great effect on the kinetics of water transport in the materials

    結果表明：只有結合毛細吸收和擴散2種傳輸過程才能很好地表徵水泥基材料內部的水分傳輸過程，材料內部孔隙結構時水分傳輸的動力學過程有很大的影響。
  4. The air used to dry grain in ventilated stores provides both the energy needed to evaporate the moisture from the grain and the medium to transport this moisture out of the store

    在裝備有通風設備的糧庫里，用於使穀物保持乾燥的空氣不僅提供了穀物中水分蒸發所需要的能量，而且還是將這些水分排出糧庫的媒介。
  5. It was found that the " key regions " from which moisture transports influenced shandong summer rainfall lies in tropical india ocean, south china sea to tropical west pacific, china mainland to japan sea and the upstream area in westerly belt by analysis of svd method on water vapor transport

    夏旱年則相反。通過對旱澇年水汽輸送與山東夏季降水的相關分析，山東夏季降水和水汽輸送svd分析，發現：影響山東夏季降水的水汽輸送「關鍵區」主要位於熱帶印度洋、南海-西太平洋、中國大陸-日本海以及山東上游西風帶地區。
  6. Tensile strength and elongation, weight, elasticity, resistance to flammability and high heat levels, moisture - transport capabilities, durability, and weatherability are some examples of attributes that could be included in a technical textile performance specification

    拉伸強度、抗張伸展率、重量、彈性、耐燃性、耐高熱水平、水分輸送能力、耐久性和耐候性都包括在技術紡織的性能規范中。
  7. The change of transport pattern from winter to summer closely relates with the change of the direction of the cross equatorial moisture transports, especially nearl 05 e and 45 e. ii

    水汽輸送形勢的季節轉變跟南北半球間的越赤道輸送的轉向密切相關，尤其是在105 e 、 45 e附近。
  8. The northward march of the southerly moisture transport with the summer monsoon transport over the east asian ( 110 - 130 e ) shows the feature of staged jumps. each jump relates with the large - scale important weather incident in china

    （ 2 ）氣候平均狀態下，夏季偏南風水汽輸送在東亞地區（ 110 ? 130 e ）的向北推進有階段式跳躍的特點，每次跳躍均與影響我國的大型天氣事件相聯系。
  9. The 1st time coefficient shows the staged feature of the progression of the moisture transport over asian - australian monsoon region, which relates with the large - scale important weather incidents in asian - australian monsoon region. iv

    第一特徵向量對應的時間系數圖表現了亞澳季風區4 - 9月份的水汽輸送階段性的時間演變特徵，可反映夏季亞澳季風區的大型天氣事件的發生變化過程。
  10. Using the summer rainfall data from twenty - six observatories in shandong province from 1961 to 2001, the subtropical high index data from 1961 to 2002 and the monthly mean reanalysis data of wind, moisture, height and olr of ncep / ncar from 1958 to 1998, the characteristics of abnormal circulation in the northern hemisphere, the abnormal strength and location of subtropical high, the abnormal strength of monsoon and water vapor transport over the areas of east asian were studied

    利用山東26個代表站1961 2001年夏季降水、 1961 2001年副高特徵指數以及1958 1998年ncep ncar再分析月平均風場、高度場、比濕、 olr等資料，對山東夏季發生旱澇的北半球大氣環流、副熱帶高壓、東亞夏季風以及季風區水汽輸送等異常特徵進行了合成對比分析。對山東夏季旱澇形成的原因，從季風區水汽輸送和出現降水異常的物理機制等方面進行了較深入的研究。
  11. Both ion diffusion and transport of ions to the root surface by mass flow appear to be dependent on soil moisture content.

    離子擴散和通過質體流動把離子運送到根表面，看來似乎都取決于土壤的含水量。
  12. In this paper, we aim at establish heat and mass coupled transfer model in the building wall, the emphasis of this study lies in creating a coupled and non - linear diferential equation system for the heat air and moisture transfer in the wall, which can be described by means of continuum mechanics and irreversible thermodynamics, the most dominant factor is moisture conten 9la gas pressure pc and temperature t, for the description of heatair and moisture transport, the general mass balance equation can be expressed by the temporal change of moisture conten 9 l, gas pressure pc and temperature t that means, in order to create a closed solvable equation system, the other additional dependencies have to be found, which the other variable depending on the variables of the solution : moisture conten 6 l gas pressure pc and temperature to the model is verified by the numerical simulation software which has been developed about building wall.,

    根據節能設計要求，本文用熱力學的方法，並根據多孔介質中多相流體流動描述方面的最新研究成果? ?體積平均方程，建立了墻體熱、濕和空氣耦合熱質傳遞模型，並推導出熱、濕和空氣耦合傳遞等效擴散方程；找到建築墻體熱、濕及空氣耦合作用下熱質傳遞過程的主要影響因素濕容量_ l 、氣壓p _ c和溫度t 。開發了單體材料墻體熱質傳遞數值模擬軟體，用實測數據對軟體進行調試並對模擬計算結果進行了驗證。模擬出了單材料墻體在熱、濕和空氣耦合作用下建築墻體內的溫度和濕度分佈規律。
  13. The most obvious feature of the first leading term of eof applied to the climatic vertically integrated water vapor flux over asian - australian monsoon region shows a planetary - scale southwesterly moisture transport, starting from south hemisphere, passing over asian monsoon region and flowing into north pacific, which indicates the interaction between the northern and southern hemisphere as well as between mid and low latitudes in the northern hemisphere

    （ 3 ）亞澳季風區氣候平均狀態下4 - 9月份的水汽通量的eof矢量展開的第一特徵向量最顯著的特徵是存在一條行星尺度的強西南風水汽輸送帶，它源於南半球低緯地區，經過亞洲季風區，進入北太平洋地區，集中反映了南北半球和中低緯各支水汽輸送氣流的相互作用。
  14. In winter ( january ), there are four nearly latitudinal moisture transport belts ( channel ) over asian - australian monsoon region. they are closely related with the easterlies and westerlies over southern hemisphere and northern hemisphere. in boreal winter, asian monsoon region is moisture source ; the cross equatorial moisture transport channels transport the moisture to australian monsoon and south indian ocean from asian monsoon region

    主要結論如下： （ 1 ）冬季（ 1月）的水汽輸送形勢與南北半球東、西風帶緊密聯系，主要有四條近似緯向分佈的垂直積分的強水汽輸送帶，越赤道輸送將水汽從亞洲季風區輸送到南半球澳大利亞季風區和南印度洋季風區，亞洲季風區為水汽源區。
  15. In july, although the moisture transport from tropical indian ocean reaches its annual maximum to shandong, its contribution to summer rainfall over shandong during july and august is undistinguished. on the other hand, the contribution from sub - tropical west pacific is evident

    7月雖然來自熱帶印度洋季風區的水汽輸送通量達到最大值，但7 8月它們對山東夏季降水異常的貢獻並不顯著，相反來自南海-西太平洋、中國大陸-日本海的水汽輸送以及西風帶天氣系統對山東夏季降水異常的貢獻較顯著。
  16. Orsm includes physical processes such as radiative transfer, phase changes of water substance, re - distribution of energy due to cumulus convection, transport of momentum, energy and moisture by turbulence, and exchanges between the atmosphere and the surface layer

    ： orsm中的物理過程包括輻射交換水分的相變積雲對流所帶動的能量重新分佈湍流所引發的動量能量和水汽輸送大氣與地面層之間的各種交換等等。
  17. Storage and transport : lt should be stored in a dry, ventiiative and ciean warehouse ; kept away from moisture and hot, futhermore, it shouid be stored separateiy from poisonous substantes

    貯存與運輸:應貯在乾燥，通風清潔的庫房中，防止受潮、受熱，應與有毒物品隔離堆放。
  18. It has been found that ( 1 ) the first rainfall is mainly caused by the cold air from west ; ( 2 ) the convection systems over the qinghai - xizang plateau have direct impact on the rainfall ； ( 3 ) the moisture transport from the indochina peninsula through the south - western china provides a necessary condition for the first rainfall

    其特點：以西路冷空氣影響為主；與高原的對流系統有直接聯系；從中南半島向東北，經我國西南的低層暖濕空氣輸送帶是春季強降水的必要條件。
  19. In drought or flood years over the yangtze river basin, the features of the establishment, progression and decrease of moisture transport is significantly different, meanwhile the differences of the moisture transport by the monsoon circulation between mid and low latitudes in the northern hemisphere, and by the subtropical high are obvious, so are their convergence, especially over south china sea, the tropical west pacific, the yangtze river basin, north china and north - east in china

    （ 4 ）長江流域旱澇年亞澳季風區夏季風水汽輸送的建立、推進、減弱的階段性特徵顯著不同，對應的中低緯季風環流、副高環流等季風系統水汽輸送、匯合也有顯著差別，尤其是在南海、熱帶西太平洋、長江流域、華北和東北等地區。
  20. In the droughts or floods over the yangtze river basin, between june and the second dekad in july, the moisture transport from the southern boundary, originating from south china sea and south china, is the most important influence factor, but between the last dekad in july and august, the one flowing out from northern boundary is the most important influence factor

    長江流域旱澇年， 6 - 7月中旬來源於南海、華南地區的南邊界水汽輸入是主要影響因子， 7月下旬一8月北邊界的水汽輸出是主要影響因子。長江流域旱（澇）年夏季風水汽輸送的北界偏北（南） ，副高南側的東南風水汽輸送偏北（南） 。
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