溫度訂正 的英文怎麼說

中文拼音 [wēndùdìngzhēng]
溫度訂正 英文
temperature correction
  • 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
  • 訂 : 動詞1 （經過研究或商議后立下） conclude; draw up; agree on 2 （預先約定） subscribe to （a newspa...
  • 正 : 正名詞（正月） the first month of the lunar year; the first moon
  • 溫度 : [物理學] temperature
  • 訂正 : make corrections; correct; revise; emend; correction; reduction
  1. 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。
  2. Thermograph correction card

    溫度計訂正表
  3. During the course of the research, the criterions of the interpolation effect are mean error ( me ), mean absolute error ( mae ), root mean squared interpolation error ( rmse ) and the difference of mean square deviation between the measured and the estimated surface air temperature. the conclusions are as follows : ( 1 ) by contrasting the gaussian weighted model associated with the error modification with the gaussian weighted model, the error modification is proved to considerably ameliorate the precision of spatial interpolation ; ( 2 ) on the base of the gaussian weighted model, taking altitudinal effect into account can reflect the trend in which temperature changes according to the topographic altitude and may ameliorate the precision of spatial interpolation correspondingly and apparently, which indicates that topographical effect on the preciseness of spatial interpolation can not be disregarded in terms of the region with complicated topography ; ( 3 ) the map of daily surface air temperature distribution, using the modified gaussian weighted model a and b, can accurately reflect the temperature - changing - with - topographical - altitude trend. among them, the better is the model a, whose me is below 0. 03 ?

    在此過程中，採用平均誤差（ me ） ，平均絕對誤差（ mae ） ，插值平均誤差平方的平方根（ rootmeansquaredinterpolationerror ，簡稱rmsie ） ，插值前後測站要素值的均方差（ meansquaredeviation ，簡稱msd ）差值作為判定插值效果的標準，得出如下結論：通過高斯權重法與結合逐步訂正的高斯權重法的對比，說明結合逐步訂正方案的高斯權重法可大大提高地面日氣溫的插值精度；在高斯權重法中加入海拔影響項可以反映出溫度隨地形高度的變化趨勢，同時也能較大地提高地面日氣溫的空間插值精度，說明在地形復雜的區域，地形影響在插值精度中是不可忽略的；對于高斯權重法的兩種改進方案得到的地面日氣溫分布圖都能很好地反映出表面大氣氣溫隨地形高度的變化趨勢。
  4. Relation between virtual temperature correction and humidity, influence of humidity on accuracy firing data, and problem of using identical relative humidity to substituted real humidity distribution are analyzed

    分析了濕度與虛溫訂正值的關系、濕度對射擊諸元精度的影響和用統一溫度替代濕度空間實際分佈的問題。
  5. The correction methed mentioned above, employed in this paper can assimilate tbb data to numerical model directly, and it has phisical significance clearly other than regressive method also. 2 ) the experiments verify that correction method gives better results than conventional regressive method in intensively convective zone

    而且模擬試驗結果也表明，用t _ （ bb ）資料溫度訂正法和在較強對流雲區t _ （ bb ）資料相對濕度增強訂正方法可取得比傳統的統計反演方法更好的效果。
  6. In recent years, the u. s. has reached 22 market opening agreements with japan in areas such as autos and auto parts, telecommunications, investment, and intellectual property

    5 .訂定監測若發現未達某個臨界限制時應採取的糾正行動，比方若是未能達到最起碼的烹煮溫度，就需將食品再加工或廢棄。
  7. Single - layer model is convenient to apply but the unclear relationship between radiative and aerodynamic temperatures is still a bottleneck in this field. a new method was developed to derive reliable surface heat fluxes from radiative temperature viewed from arbitrary zenith angle. aerodynamic and radiative temperatures are connected through a so - called optimum component fraction ( ocf ) parameter - the fraction of vegetation in the field of view when the two temperatures are equivalent in oblique viewing

    該方法利用表面熱輻射方向性和顯熱通量都是源於土壤和植被溫度的貢獻這一共同點，發現在一定傾斜角度的觀測下，視場中植被與土壤的比例可以較好地反映植被和土壤與大氣進行湍流熱交換的貢獻率，所以稱該方法為最佳組分面積比法，用最佳組分面積比可以將任意角度下觀測到的輻射溫度訂正為空氣動力學溫度，經過地面和遙感數據驗證表明，用該方法計算的通量精度高於普通的單層模型。
  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. During the research also found that during the time " scale the temperature have the good relationship with astronomical radiation and global relationship as well as direct radiation. however, the correlation between the temperature with the global radiation and direct radiation ca n ' t find. and the temperature and the astronomical radiation is also very well

    研究發現，在時間尺度上，單站點訂正到海平面的氣溫與天文輻射、總輻射和直接輻射都有良好的相關性；在同一時段內的空間尺度上，多站點訂正到海平面的氣溫與天文輻射有較好的相關性。
  10. 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。
  11. Statistical regressive method are employed to retrieve temperature and humidity fields in low - level atmosphere, and then assimilated into mm5 by variational technique. secondly a method is applied to add cloud tbb data to numerical model, which corrects the temperature and amplify the humidity simultaneously

    其次，雲圖t _ （ bb ）資料的定量應用採用了t _ （ bb ）資料溫度訂正和t _ （ bb ）資料相對濕度增強訂正的方法，經訂正後的溫度和相對濕度直接應用於模式中。
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