surface heat flux造句
例句與造句
- for the northern i ndian ocean, the net surface heat flux and entrainment through the bottom of mixed layer have semiannual period, which is the major cause of semiannual variations in sst
就赤道以北印度洋而言，海面凈熱通量和混合層底的卷夾過程都有半年周期，這是sst呈現(xiàn)半年周期變化的主要原因。 - furthermore, how to get the surface heat flux of the billet by its surface temperature and initial temperature is a typical inverse heat conduction problem ( ihcp ) in the mathematical sense
在數(shù)學意義上，就是一個利用偏微分方程的初始條件和一個邊界條件來求得另一個邊界條件的問題，這又恰恰就是一個典型的逆熱傳導問題(ihcp)。 - the results show that the ssc can cause the topography flattening only in constant viscosity model; for the model with temperature-dependent viscosity, although the ssc enhances the surface heat flux, it has little effects on topography
數(shù)據(jù)結果顯示，在常粘性模型中，小尺度地幔對流可造成海底地形抬升；但對與溫度相關的粘性模型，小尺度對流對地形幾乎不產(chǎn)生影響。 - though we want to get the optimized values of the unknown controlling parameters in cc process through the surface temperature of the billet, the direct solution is difficult . of course, those unknown parameters have close relation with the surface heat flux of the billet
由于這些待辨識的工藝參數(shù)是與連鑄坯的表面熱流有著密切的關系，所以需要首先利用連鑄坯的表面溫度測量值來計算出連鑄坯的表面熱流，然后再辨識出未知的工藝參數(shù)。 - 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于土壤和植被溫度的貢獻這一共同點，發(fā)現(xiàn)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(jīng)過地面和遙感數(shù)據(jù)驗證表明，用該方法計算的通量精度高于普通的單層模型。 - It's difficult to find surface heat flux in a sentence. 用surface heat flux造句挺難的
- it is showed that the heat transport crossing the equator has the similar magnitude and the same period of one year, compared with that of 10 n in arabian sea . by contrast, the heat transport across 10 n in bay of bengal has a much smaller value with a prominent semiannual period; there are tight relationship between integrated zonal wind stress in one latitude of the indian ocean north of 7 n and the total heat transport across that latitude, as well as the total net surface heat flux north of that latitude . the maximum correlation coefficient is less than-0.5
結果表明越赤道和越10on阿拉伯海的熱輸送量大小具有可比性，且有相同的年循環(huán)特征，而10on孟加拉灣緯度的經(jīng)向熱輸送較小，且具有半年變化周期;儼s以北印度洋任一緯度上的緯向風應力異常與此緯度上的經(jīng)向熱輸送異常以及此緯度以北印度洋總的海面凈熱通量異常有很好的相關關系，相關系數(shù)最大可達一0.5以上。 - in boreal summer, the entrainment dominates the western part of bay of bengal and most part of arabian coast; net surface heat flux is always a dominant factor controlling the sst variation in bay of bengal throughout a year . difference physical processes control the temperature of the mixed layer in different regions
在夏季，整個阿拉伯沿岸和孟加拉灣西部混合層底的卷夾作用占優(yōu)勢；海面凈熱通量在孟加拉灣sst的變化中始終是主要的影響因子；對幾個典型區(qū)域的研究表明，不同的區(qū)域的混合層溫度有著非常不同的變化機制。 - a transfer model is established, which can be used to study the interaction between the land surface physical processes of inhomogeneous region and the structure of atmosphere boundary-layer over urban and rural terrains . the model has simulated surface heat flux, surface temperature, temperature profiles, height of mixture layer and so on . and the differences between urban area, suburban area and rural area have been compared . this model mainly depends on the parameters below : surface albedo, surface roughness coefficient, moisture available coefficient of soil, thermal capacity and thermal diffusion coefficient of errain, cloudage . the result shows that this model can simulate the structure and eigenvalues of atmosphere boundary layer and their changes in a day . parameters used in this model aim at beijing city, and the time is at the beginning of september . to other cities, or other time, the parameters should be adjusted accordingly . in addition, being adjusted, the model can also be used for other homogeneous and inhomogeneous terrains
模式主要依賴于以下參數(shù)和物理量：地面反照率下墊面粗糙度土壤的可含水量下墊面的熱容量和熱擴散系數(shù)云量等參數(shù)。結果表明，本模式能合理地模擬不同地表熱量平衡地表氣溫混合層高度湍流交換系數(shù)湍流動能位溫廓線等，以及它們的日變化。該模式所取參數(shù)主要針對北京市，時間為九月初，對于其他城市，參數(shù)應作相應的調(diào)整。