atmospheric water vapor 中文意思是什麼

atmospheric water vapor 解釋
大氣水蒸汽
  • atmospheric : adj. 1. 大氣（中）的。2. 大氣所致的。3. 空氣的。4. 氣壓的。5. 有…氣氛的。adj. -ical ,-ically adv. 在大氣影響下，氣壓上。
  • water : n 1 水；雨水；露；〈常作 pl 〉 礦泉，溫泉；藥水。2 〈常 pl 〉水體；水域；水道；海；湖；河；海域；...
  • vapor : n. 〈美國〉＝ vapour.
  1. Atmospheric precipitable water vapor is one of the most important parameter to li model

    在li模式中有一個重要的輸入參數是大氣可降水量。
  2. The modis atmospheric precipitable water vapor is precise enough as the input parameter to li - model

    這樣的精度對作為li模式的輸入參數來說精度已經足夠了。
  3. In order to verify the reliability of modis atmospheric precipitable water vapor, we used the ncep atmospheric water vapor data

    為了驗證modis大氣可降水量資料的可靠程度，本文利用ncep的大氣可降水量資料對其進行了檢驗。
  4. When the southwesterly ( northeasterly ) moisture flux over southern china and its vicinity increased, then more ( less ) water vapor was transported from the low latitudes to the atmosphere over southern china, which resulted in strong ( weak ) atmospheric moisture sinks over the above - regions in southern china

    華南中東部以及廣西北音隊湖南西部貴州東部地區水汽匯的強度異常與東亞上空水汽輸送異常導致上述地區垂直積分的水汽通量輻合的異常密切相關，當中國南方上空有西南（東北）風水汽通量距平，即西南風水汽輸送增強（減弱）時，則上述地區上空的水汽匯偏強（偏弱） 。
  5. Rust is the product of a slow combination of iron with atmospheric oxygen and water vapor.

    銹是鐵和空氣中的氧和水蒸汽緩慢結合的產物。
  6. The co, water vapor, ch4 and other minor gases have been measured in beijing since 1996 by lageo, institute of atmospheric physics, chinese academy of sciences, using an infrared grating spectrometer of moderate resolution. the observation site locates on the roof of the building of the institute of atmospheric physics located in the right north between the 3rd and 4th circles. the co and water vapor column contents have been measured during autumn since 1996, summers of 1997 and 1999, and through 2003, and ch4 column content for autumns of 1996, 1998, 2001 and 2002

    自1996年以來，中國科學院大氣物理研究所中層大氣與遙感研究部利用中解析度紅外光譜儀系統，在北京市區北三環和北四環中路之間的中國科學院大氣物理研究所主樓樓頂進行了co 、水汽和ch _ 4等大氣微量氣體柱總量的觀測，獲得每年秋季（ 10 、 11月） ， 1997 、 1999年夏季和2003年一整年的co和水汽的資料： 1996 、 1998 、 2001和2002年秋季ch _ 4的資料。
  7. The comparison showed that the difference between two data is less 0. 5cm in chinese main land area, and the same time we found that modis atmospheric precipitable water vapor is greater than the ncep data in the area of northwest and north of china and less it in the area of southeast of china. if we multiply modis atmospheric precipitable water vapor data with 0. 933983 and 1. 07686 respectively on above area the difference will below to 0. 2cm

    結果發現：在中國大陸地區， modis與ncep的大氣可降水量之差在絕大部分地區在0 . 5cm以內，但是在中國西北、華北地區普遍偏大一些，在東南地區則普遍偏小一些，如果給上述地區的modis大氣可降水量分別乘以0 . 933983和1 . 07686進行修正，則兩者之差在0 . 2cm以內。
  8. ( 2 ) model correction and comparison in the process of conversion from zenith day delay to gps water vapor and precision evaluation. saastamoinen ( sa ) model and hopfield ( h ) for dry delay and bevis model for atmospheric weighted temperature are adopted

    （ 2 ）模型訂正與比較在gps水汽反演過程中，一般干延遲和大氣加權平均溫度的計算是採用「普適性」模型，目前應用較多的有saastamoinen （ sa ）模型、 hopfield （ h ）模型和bevis模型。
  9. The hydrologic cycle, a major topic in this science, is the complete cycle of phenomena through which water passes ， beginning as atmospheric water vapor, passing into liquid and solid form as precipitation, thence along and into the ground surface, and finally again returning to the form of atmospheric water vapor by means of evaporation and transpiration

    水循環，自然科學中的主要課題，通過水的流動形成一個完整的圈的現象，大氣水轉化液體和固體的形式形成降水，然後，沿著地表或地下流動，最後通過蒸發和蒸騰作用又變成大氣水的形式存在。
  10. The hydrologic cycle ， a major topic in this science ， is the complete cycle of phenomena through which water passes ， beginning as atmospheric water vapor ， passing into liquid and solid form as precipitation ， thence along and into the ground surface ， and finally again returning to the form of atmospheric water vapor by means of evaporation and transpiration

    水循環在這門科學中是主要課題，它是一個完整的循環現象，首先，水在大氣中以水蒸氣存在，然後形成液態，通過降水這種形式流到地表，最後通過揮發或蒸發再次以水蒸氣的形式回到大氣中
  11. The paper have built the local correction models for dry delay and atmospheric weighted temperature and have made a comparison between two models for calculating actual water vapor on the basis of actual upper - air detecting data. ah results show that the conclusion is satisfied

    本研究利用實際探空資料建立了大氣干延遲和大氣加權平均溫度的局地訂正模型，並對實際水汽計算模型進行了比較，得到了滿意的結果。
  12. Knowledge of atmospheric water vapor are related to many aspects such as rainstorm forecast, preventing and managing of droughts and floods, protecting and improving of ecology and environment and so on

    摘要大氣中水分的生成、活動關聯降水預報、旱澇防治、保護和改善生態環境等方面。
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