日平均溫度 的英文怎麼說

中文拼音 [rìpíngjūnwēndù]
日平均溫度 英文
average diurnal temperature
  • 日 : Ⅰ名詞1 （太陽） sun 2 （白天） daytime; day 3 （一晝夜; 天） day 4 （泛指某一段時間） time 5 （日...
  • 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
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 度 : 度動詞[書面語] （推測; 估計） surmise; estimate
  • 日平均 : [氣象學] daily mean
  • 溫度 : [物理學] temperature
  1. The variations of sea ice in the arctic ocean are simulated by using a improved high resolution hibler dynamic - thermodynamic sea ice model during 1979 - 1998. the model is driven by surface atmospheric and oceanic forcing consists of geostrophic winds, surface air temperature, specific humidity, and longwave and shortwave radiative fluxes provided by international arctic buoy program ( iabp ). the simulated results show that arctic sea ice have noticeable seasonal and annual variability

    利用一個hibler海冰熱動力模式，在改進了其熱力部分和改變模擬范圍以及提高解析度的基礎上，以北極國際浮標計劃（ iabp ）提供的1979 - 1998年間逐日變化的日平均海平面氣溫場，濕度場，長短波輻射場，風場，洋流場，海洋熱流量場為強迫場，模擬了上述20年間北極海冰的時空演變。
  2. As a result, in the paper, considering the altitudinal effect ( topography factor ) and the influence on the temperature lapse rate by topography and latitude and longitude and moisture transfer, the study on the daily surface air mean, max and min temperature in the reaches of yangtze rive is attempted by five models, which include the gaussian weighted model, the gaussian weighted model associated with the error - modification, the gradient plus inverse distance squared model and the modified gaussian weighted model a and b that take topography - factor into account

    本文考慮海拔高度和溫度直減率受地形和經、緯度及水汽等因素的影響，通過利用高斯權重法、結合逐步訂正的高斯權重法、梯度距離權重反比法和加入地形影響項（地形因子）的兩種改進高斯權重法的方案a 、 b ，對長江流域的地面日平均、最高和最低氣溫場進行了空間化插值研究。
  3. Zhoushan has a northern subtropical monsoon marine climate with clear four seasons ; leading wind directions are southeast wind in summer, northwest wind in winter. with an annual average wind speed of 3. 3m s ; and an average temperature of 15. 6 - 16. 6, and the frost free period reaches 251 - 303 days perannum, annual average sunshine time 1941 - 2257 hours, and the annual preeipitation is 927 - 1620 mm

    舟山屬北亞熱帶南緣季風海洋型氣候，四季分明主導風向，夏季為東南風，冬季為西北風，年平均風速3 . 3米秒年平均氣溫15 . 6 . - 16 . 6 ，冬季最低溫為- 1 ，夏季最高溫度為37無霜期251 - 303天，年日照時數1941 - 2257小時年降雨
  4. Evaporation : two u. s. weather bureau class a pans are operated at king s park. the mean water temperature is taken to be the mean of the daily maximum and minimum surface water temperature

    蒸發：天文臺使用兩個美國氣象局甲級蒸發皿于京士柏氣象站量度蒸發量，以皿內每日量得的最高及最低水面溫度之平均數作為當日的平均水溫。
  5. Based on the u. s. navy generalized digital environmental model ( gdem ) climatological temperature and salinity data on a 0. 5 x 0. 5 grid, the three - dimensional current system in the kuroshio south of japan and kuroshio extension is determined and analyzed by using the p - vector method

    本文選用美國海軍gdem全球氣候月平均溫鹽資料，空間解析度為0 . 5 0 . 5 ，應用p矢量方法對日本以南黑潮和黑潮延續體三維流場進行了診斷計算和分析研究。
  6. Outdoor design mean daily temperature for summer air conditiouing

    以日平均溫度為基礎
  7. Outdoor design temperature for winter air conditioning

    以日平均溫度為基礎
  8. Abstract : by using the correlation analysis of cotton climatic output and temperature elements of different temperature types and different length periods of time in akesu cotton region, the results obtained indicate ( 1 ) using daily temperature elements of different length periods of time correlated with cotton climatic output is more useful, more reasonable and more easily in founding out optimum temperature elements with biological significance than using ten - days temperature elements ; ( 2 ) in three temperature elements of mean temperature, maximum temperature and minimum temperature, the effect of maximum temperature on cotton climatic output is the greatest, mean temperature is greater, and minimum temperature is the least ; ( 3 ) the low temperature in later spring and summer have some limiting effects on forming cotton climatic output in akesu cotton region

    文摘:通過對阿克蘇棉區棉花氣候產量與不同長度時段、不同類型溫度要素的相關分析，結果表明： （ 1 ）採用不同長度時段的日溫度要素與棉花氣候產量進行相關分析，比採用旬溫度要素的工作更細致，更合理，更易找出對棉花氣候產量影響較大的有生物學意義的較佳時段和溫度要素； （ 2 ）在平均溫度、最高溫度及最低溫度3個溫度要素中，以最高溫度對棉花氣候產量的影響最大，其次是平均溫度，最低溫度最小； （ 3 ）春末及夏季的低溫對阿克蘇棉區的棉花氣候產量形成具有一定的制約作用。
  9. Mean monthly minimum temperature

    一個月逐日最低溫度的平均值
  10. Mean monthly maximun temperature

    一個月逐日最高溫度的平均值
  11. The net result is little change in the daily maximum temperature. overall, the annual mean temperature rises but at a slower rate than the annual mean minimum temperature

    綜合最高和最低氣溫的變化，日平均溫度有上升的趨勢，但速度較日最低氣溫慢。
  12. The rise in temperatures during daytime was reduced but this is more or less offset by the heat generated from air conditioning and other urban activities. the net result is little change in the daily maximum temperature. overall, the annual mean temperature rises but at a slower rate than the annual mean minimum temperature

    綜合最高和最低氣溫的變化，日平均溫度有上升的趨勢，但速度較日最低氣溫慢。楊繼興說：換句話說，日間酷熱的情?並未有惡化，但寒冷的夜晚卻少了。
  13. Mean annual maximun temperature humidity

    一個月逐日平均溫濕度的平均值
  14. The main results indicated that : significant differences exist in diurnal average transpiration rate and the range of diurnal transpiration rate ; the transpiration rate of sawtooth oak, amorpha, lalang grass varied with a regular double apex rhythm, but that of the rest varied with a regular single apex rhythm, stomatal conductance play a maximal important role in transpiration rate, temperature ( air temperature, the earth ' s surface temperature ) also influence the transpiration rate ; transpiration rate has prominent negative correlation with the relative air humidity, the biggest coefficient is 0. 866

    筆者對日照沿海防護林幾種主要木本植物和草本植物的蒸騰速率和環境因子的關系進行了研究，結果表明： 8種植物日平均蒸騰速率和蒸騰速率日變幅各異；麻櫟、紫穗槐和白茅的蒸騰速率日變換呈現出雙峰式的變化規律，其它5種植物蒸騰速率表現為單峰式的變化規律；氣孔導度影響著植物的蒸騰速率，溫度（氣溫、地面溫度）是影響植物蒸騰速率的主要因子；空氣相對濕度和蒸騰速率表現為顯著或極顯著負相關，相關系數高達0 . 866 。
  15. Mean dekad temperature humidity ten - days average temperature humidity

    一旬逐日平均溫濕度的平均值
  16. Because this area receives plenty of rain ， the day and night temperature difference reaches 6 10 degrees ， thus tonkan growing here are particular delicious and sweet. harvest time is january ~ april

    峨眉春冬季雨量豐沛，日夜溫差高達6 10度，很適合桶柑生長。這里的桶柑皮薄、汁多、無子，平均甜度12度以上，產期為1 4月。
  17. The thermal process model of imbed pipe floor heating room at intermittent operation was set up by analyzing the thermal storage of enclosure. then, a solution method was give for it basing on duhamel theorem. the calculation results shown a good indoor thermal environment can be hold when the system, which designed on out door temperature for heating basis, operates half day in night under outer door mean temperature in winter

    對典型房間的計算結果顯示:系統間歇運行時，供暖系統開啟和關閉后室內溫度呈指數規律變化;當系統按供暖室外計算溫度設計，實際運行日的室外平均溫度等於供暖期室外日平均溫度時，在室外逐時溫度較低的時段低溫熱水地板輻射供暖系統運行半天左右可滿足全天供暖室內計算溫度要求。
  18. The coldest months are january and february with mean daily air temperatures of between 4c and 7c, while july and august are the warmest 14c to 16c

    最冷的月份是一月和二月，這段時間的日平均氣溫在4到7之間；最熱的月份是七月和八月，這期間的平均溫度在14到16之間。
  19. As far as daily surface air mean temperature, rmsie is below 0. 5ctc. as for daily surfac e air max and min temperature, the rmsie are respectively lower than 0. 74 and 0. 58. ( 4 ) the model a takes into account the fact that temperature lapse rate changes according to such factors as topography, latitude, longitude and moisture transfer, etc. the effect of spatial interpolation that uses it is not noticeably ameliorated by contrast with using the model a. there remains a need for further study

    其中，改進方案a與其它方法相比，效果較好，其me均在0 . 03以下，對于地面日平均氣溫場， rmsie均在0 . 50以下，對于表面大氣日最高溫度場， rmsie均在0 . 74以下，對于地面日最低氣溫場， rmsie均在0 . 58以下；在方案a的基礎上，考慮溫度直減率隨經、緯度和地形以及水汽輸送等因素變化的分區插值方案，與方案a比較，插值效果沒有明顯改善，因此還需要進一步的研究。
  20. Using monthly and daily mean temperature data from 726 stations ' s across china mainland for period of 1951 to 2001, the author established the time series of mean temperature for the region, and analyzed the decadal variation and change trend in temperature and temperature - defined growing season over the past 51 years

    利用中國726個站點1951 - 2001年的逐月和逐日平均氣溫記錄，分析研究了中國1951 - 2001年氣溫和1961 - 2000年溫度生長期的變化及其趨勢。結果表明， 1951 - 2001年期間，中國氣溫上升明顯，增暖過程從80年代開始， 1987年以後，增暖趨勢有了進一步加快的趨勢。
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