月平均氣溫 的英文怎麼說

中文拼音 [yuèpíngjūnqìwēn]
月平均氣溫 英文
mean monthly air temperature
  • 月 : Ⅰ名詞1 （月球; 月亮） the moon 2 （計時的單位） month 3 （姓氏） a surname Ⅱ形容詞1 （每月的） mo...
  • 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
  • 氣 : Ⅰ名詞1 （氣體） gas 2 （空氣） air 3 （氣息） breath 4 （自然界冷熱陰晴等現象） weather 5 （氣味...
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 氣溫 : [氣象學] air temperature; atmospheric temperature
  1. The city had over 250 thousand inhabitants in 2000, of which the majority was uyghurs. because of its geographical condition, the foehn phenomenon occurs and raises average temperature to 32. 7 degrees in july

    由於吐魯番盆地四周的山嶺高聳，盆地內部受熱快而散熱慢，形成了那裡夏天高溫乾燥的氣候，在舉辦自行車賽的7月，平均氣溫高達32 . 7度。
  2. When the rainy season is over, the real summer comes. ogasawara islands, in particular, being 1000 km away from tokyo and belonging to a semitropical zone, are an area of the eternal summer throughout the year

    23區（東京?新木場?羽田?練馬?世田谷）月平均氣溫和降水量多摩地區（小河內?青梅?八王子?府中?小澤）月平均氣溫和降水量
  3. The models were validated with adopting local weather ( average temperature per month, average maximum temperature per month ; average minimum temperature per month ; sunlight times per month, and latitude ), varieties, and experiment data from different yielding levels in nanjing and jinan areas, the correlation coefficient, standard error of absolute deviation, and average absolute deviation between the observed and the stimulated were 0. 9761 and 0. 9620 with 0. 01 significant level, 0. 5891 and 0. 7094, and 0. 12 and 0. 43, respectively

    所建模型可以利用當地常年氣象資料（ 30年平均值，如月平均氣溫、月平均最高和最低氣溫以及月日照時數、緯度） ，確定不同地區、產量水平與品種最適葉面積指數動態，為小麥數字化栽培提供科學依據。
  4. Normal hottest 3 - month period normal three summer months

    累年逐月平均氣溫最高的三個月
  5. Normal coldest month

    累年逐月平均氣溫最低的月份
  6. Normal hottest month

    累年逐月平均氣溫最高的月份
  7. Annual hottest month

    每年逐月平均氣溫最高的月份
  8. Annual coldest month

    每年逐月平均氣溫最低的月份
  9. In this paper, a research of spatial distribution of solar radiation and temperature over mountainous area of qinling is presented. the research is based on monthly mean temperature and sunshine ratio data of 36 meteorological observe stations over qinling zone in 1971 - 2000, and xian solar radiation data in 1961 - 2000, and 1km 1km dem data over qinling zone

    本文用秦嶺地區36個氣象觀測站1971 - 2000年30年氣候整編資料的月平均氣溫、日照百分率資料， 1961 - 2000年西安日射資料，以及秦嶺地區1km 1kmdem數據，對秦嶺地區山地輻射和氣溫空間分佈進行研究。
  10. Kunming belongs to the low latitude plateau mountainous country monsoon climate, because of locating in the western region of yungui plateau, the degree of latitude is low, the elevation is high, there are the wumeng mountains to be as the natural screen in the north, separating the cold air to go down south, the whole area is subjected to influence that come from southwest and warm moisture of indian ocean s flow more, adding there are the plateau lakes to regulate degree of humidity, becoming the four seasons of " summer have no intense heat, winter have no strict and cold ", such as pleasant weather of the spring

    昆明屬低緯高原山地季風氣候，由於地處雲貴高原西部，緯度低，海拔高，北部有烏蒙山等群山作為天然屏障，阻隔南下的冷空氣，全區多受來自印度洋西南暖濕氣流的影響，加之有高原湖泊滇池陽宗海調節溫濕度，形成「夏無酷暑，冬無嚴寒」四季如春的宜人氣候。年平均氣溫為14 . 5 ，最熱月平均氣溫19 . 7 ，最冷月平均氣溫7 . 5 ，年平均日照時數為2400多小時。
  11. Based on the monthly mean surface air temperature ( sat ) and monthly precipitation of 160 meteorological stations over china from 1951 to 2006, the relationship between climate change and drying trend was analyzed in the last 56 years

    摘要利用1951 - 2006年中國區域160個站的月降水及月平均氣溫資料，對中國區域近56a氣候要素的變化及其與乾旱化聯系的事實進行了分析。
  12. Using monthly temperature and rainfall data of 160 stations in china and global sea surface temperature and heat content data, diagnostic analysis is performed by means of harmonic analysis, correlation analysis, svd and corresponding statistical significance test methods

    利用全球海溫、熱含量、中國160站月平均氣溫和降水資料，通過周期分析、相關分析和奇異值分解（ svd ）以及相應的統計學顯著性檢驗方法，分析比較了全球海洋熱狀況與氣候異常的相關聯系。
  13. In the study of the mechanism of precipitation anomalies, the discovery is then chiefly to study the effect of ssta on precipitation and temperature in pre - floods period in south of china, concluding that there is a high con - elation between season precipitation in south of china and ssta ssta distribution

    本文利用國家氣候中心整編的1951 - 2000年中國160個站的月平均降水和月平均氣溫資料，重點分析了華南前汛期降水和氣溫異常的時空變化特徵及其與海溫異常的關系。
  14. The climate characteristics of water resources in north china are analyzed by eof method and gaoqiao equation using monthly precipitation and monthly mean air temperature data of 27 stations in north china from 1951 - 1995

    利用華北地區27個臺站1951 - 1995年月平均氣溫及月降水總量資料，用eof分析方法及高橋浩一郎公式計算並分析了華北地區水資源的氣候特徵。
  15. The article made the research based on the months " average temperature data range from 1971 to 2000 and the radiation data collected by the radiation station of whole country, as well as the 1 : 250000 dem data

    本文用重慶地區34個氣象觀測站1971 - 2000年30年月平均氣溫資料，全國部份日射站資料，以及重慶地區1 ： 25萬dem數據，對重慶地區山地輻射和氣溫空間分佈進行研究。
  16. The warmer weather continued into february. due to the abundance of sunshine, the mean temperature of 17. 7 degrees was 1. 8 degrees above normal and ranked the tenth highest for february

    在陽光充沛下，月平均氣溫為17 . 7度，較正常高1 . 8度，是有記錄以來第十個最溫暖的二月。
  17. The causation and solution of regional difference of prediction model are analyzed and monthly historical average air temperature is introduced into model as regional correction coefficient

    分析了預估模型地區差異的產生原因和解決途徑，並引入歷年月平均氣溫作為地區修正系數。
  18. Using mountainous climate theory and gis technology, a series of radiation spatial distribution models has been set up, and the spatial distribution over qinling zone has been calculated

    根據山地氣候學原理，利用gis技術，建立秦嶺地區輻射空間分佈模型，計算秦嶺山地天文輻射空間分佈。分析氣溫空間分佈的影響因子，建立秦嶺山地月平均氣溫空間分佈模型，計算秦嶺山地月平均氣溫空間分佈。
  19. The annual mean temperature of 23. 5 degrees was 0. 5 degree higher than normal. with the northeast monsoon weaker than normal over china, the monthly mean temperatures of october 2006 26. 4 degrees equaled the record of october set in 1983, while that of november 2006 23. 3 degrees broke the record of november 23. 2 degrees set in 1998

    由於影響中國的東北季候風較正常弱，二零零六年十月的月平均氣溫26 . 4度平了1983年所創的十月最高紀錄，而二零零六年十一月的月平均氣溫23 . 3度則破了十一月的最高紀錄1998年所創的23 . 2度。
  20. A spherical functions analysis scheme is expounded to analysis the monthly mean temperature field by using the results of the spherical functions assay of the height field. we using it principally study the spectral structure of the spherical function of the ncep / ncar monthly mean temperature field and its anomaly field

    本文給出了一個利用高度場球函數分析結果進行半球月平均氣溫場球函數分析的方案，主要用它分析了ncep / ncar月平均氣溫場氣候及其異常場集的球函數譜結構。
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