迎風流 的英文怎麼說

中文拼音 [yíngfēngliú]
迎風流 英文
windward set
  • 迎 : 動詞1. （迎接） go to meet; greet; welcome; receive 2. （對著;沖著） move towards; meet face to face
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 流 : Ⅰ動1 （液體移動; 流動） flow 2 （移動不定） drift; move; wander 3 （流傳; 傳播） spread 4 （向壞...
  • 風流 : 1 （有功績並有文採的） distinguished and admirable 2 （有才學但不拘禮法的） talented and romantic...
  1. Besides, the upward motion on the aweather slope of main mountains of zhoushan archipelago can induce more precipitation and orographic highs

    另外，氣流爬越島嶼的主要山脈時的上升運動，會導致迎風坡的降水增多，並誘生中小尺度的地形高壓。
  2. Its area of application is very broad, including daily commodities such as toothbrush shaft, comb shaft, clean brush shaft, knife shaft, scissors shaft, and electrical appliances such as torch handle, hair dryer handle, iron handle and electric toothbrush. the manufacturers have been exploring the way to add a tpe layer to make their products more diversified

    由於受到廣大消費者的歡迎，雙物料的應用在近幾年間已形成一大潮流，應用范圍極之廣泛，由牙刷手柄梳柄清潔刷柄刀具手柄剪刀柄等等日用品以至手電筒柄風筒手柄電熨斗手柄電動牙刷等家庭小電器，生產商無不想盡辦法加上一層tpe ，令產品更多元化。
  3. That was his most perfect idea of heaven s happiness : mine was rocking in a rustling green tree, with a west wind blowing, and bright white clouds flitting rapidly above ; and not only larks, but throstles, and blackbirds, and linnets, and cuckoos pouring out music on every side, and the moors seen at a distance, broken into cool dusky dells ; but close by great swells of long grass undulating in waves to the breeze ; and woods and sounding water, and the whole world awake and wild with joy

    那就是他所謂的天堂之樂的最完美的想法。而我想坐在一棵簌簌作響的綠樹上搖蕩，西風吹動，晴朗的白雲在頭頂上一掠而過不止有百靈鳥，還有畫眉雀山鳥紅雀和杜鵑在各處婉轉啼鳴，遙望曠野裂成許多冷幽幽的峽溪但近處有茂盛的長長的青草迎著微風形成波浪的起伏還有森林和潺潺的流水，而整個世界都已蘇醒過來，沉浸在瘋狂的歡樂之中。
  4. Adaptive upwind fem for nonlinear convection - diffusion equations

    非線性對流擴散方程迎風有限元的自適應方法
  5. The erosive and sedimentary behaviour of the shifting sand mimics an ever - changing terrain of windswept hills and of avalanches tumbling down steep slopes

    流沙的侵蝕及沉積作用生動地模擬了由迎風山丘及山崩所不斷塑造的地貌。
  6. Tour the zion national park where you can feast your eyes on all kinds of sentinel rocks, and other spectacular sights created by mother nature. proceed to bryce canyon national park where a variety of rock shapes and textures can be found. at an elevation of 8000 feet you will experience a wonderful view of the forest of rocks left standing after millions of years of erosion

    清晨即起，迎著清新的晨風，游覽秀麗的錫安公園，雄偉的赤壁潺潺的溪流傲立的蒼松冰河的遺跡，使您如置身於世外桃源，隨后轉往紅石峽谷，奇形怪狀的巖石陳列路旁，有的像秦俑有的像女王頭穿梭拱石門，抵達八千英尺高的布萊斯峽谷。
  7. The need to nurture this commercial potential actually is one of the answers to combatting the notion of global tv domination, of reversing the cultural and commercial tide because satellite tv is synonymous with the export of american culture, or cultural stylistics / colonisation

    必須培養這種商業潛力，這實際是答案之一，用以迎戰全球性電視控制觀念、阻擋文化和商業逆流；因為衛星電視就是美國文化出口、或者美國文化風格/殖民化的同義詞。
  8. Numerical simulation of square cavity flow by second - order up - wind finite volume method

    二階迎風有限體積法方腔流數值模擬
  9. T. george - zion national park - bryce canyon nat l park - salt lake city tour the zion national park where you can feast your eyes on all kinds of sentinel rocks, and other spectacular sights created by mother nature

    清晨即起，迎著清新的晨風，游覽秀麗的錫安公園，雄偉的赤壁潺潺的溪流傲立的蒼松冰河的遺跡，使您如置身於世外桃源
  10. The colourful and fascinating street decorations, the broad pavements and the palm trees along the roads will certainly attract your attention and make you forget anything about home

    這里七彩繽紛璀璨迷人的景緻，以及廣闊舒展的行人道和迎風搖曳的棕櫚樹，必能令您耳目一新，流連忘返。
  11. The discretization process is deduced in detail, and the final iteration formula is given. in the discretization equations, higher order upwind differencing scheme is introduced into the calculation of the convection flux, whereas as for diffusion term, a central differencing scheme is taken into account

    文中就具體離散過程進行了推導，給出了最終的迭代公式，其中，對微分方程的離散採用顯式格式、對流項採用高階迎風差分格式、擴散項應用中心差分格式。
  12. Upwind local differential quadrature method for solving coupled viscous flow and heat transfer equations

    求解粘性流體和熱遷移聯立方程的迎風局部微分求積法
  13. Abstract : approximate methods for calculating aerodynamic heating rates on space shuttles are discussed. various methods are given for predicting the heating rate at axisymmetric stagnation points, general three dimensional stagnationpoints and the leading edge stagnation point of wings. numerous laminar and turbulent heating techniques for flat plates and cones are analyzed and compared. a brief review of some methods is presented to predict heating rate for winward centerline and lateral direction off the symmetry plane. the results show that the methods are simpler and can guarantee enought precision for predicting aerodynamic heating environment of space shuttles

    文摘:介紹了國內外預測航天飛機氣動加熱的工程計算方法.給出了軸對稱、非軸對稱和機翼前緣等各種外形駐點熱流密度的計算，分析和比較了平板、錐體的層流和湍流熱流密度計算的各種方法，概述了航天飛機迎風面中心線和離開中心線橫向熱流密度的計算.計算結果表明，本文方法用在航天飛機氣動熱環境初步設計中比較簡單並且有足夠精度
  14. The distribution of lrgr summer mean rainfall was determined by the obstructing effect and two stronger ascending airflow that come from bengal bay and south sea and converge around corresponding windward slopes ; the general circulation distribution in meridional section is equal, which showed the passing - effect of lrgr

    縱向嶺谷區多年平均夏季降水空間分佈主要由縱向嶺谷的「阻隔」效應，以及夏季從孟加拉灣來的氣流和從南海來的氣流在相應迎風坡面輻合，形成兩支較強的上升氣流所致；而縱向剖面大氣環流的變化則較為均勻，顯示了縱向嶺谷的「通道」效應。
  15. Applications of higher - order upwind scheme for viscous flow of projectiles

    高精度迎風格式的射彈粘性繞流場數值模擬
  16. In addition, the paper uses first - order upwind scheme and second - order upwind scheme and quick scheme to compute convection. through comparison and analysis, the paper chooses second - order upwind scheme as discrete scheme of convection

    此外，對流項的離散格式分別採用一階迎風格式、二階迎風格式及quick格式進行計算，通過對比分析確定二階迎風格式作為對流項離散格式。
  17. The model of fpsa ( inter - phase slip algorithm ) provided in phofvmcs, the software used in computational fluid dynamics, which solves the navier - stokes equations of each phase with the interphase interactions between two phase of water and air, including the interphase drag forces, interphase lift forces, interphase pressure and virtual mass forces, is employed with the difference scheme of upwind and the orthonormal grid

    計算採用由phoenics （計算流體力學軟體）的ipsa （相間滑移演算法）模型，應用upwind （迎風）格式和直角坐標網格。 ipsa模型對每一相求解n - s方程，並考慮水-氣體兩相間的相間互互作用，包括相間阻力、相間升力、相間壓力和虛質量力。
  18. In this paper a numerical method for equations of transport and biodegradation in the fractured media is discussed. because the equations consist of terms related to advection, diffusion, biochemical as well as the term of exchange betwen the fracture and the porous media, it is very difficult to find their solution. in order to find more efficient method for solving these equations, several numerical methods for the equations without biochemical terms are discussed first. the numerical results show that the cubic spline method can be used to solve advection flow dominated problem which often occurred in the fractured media. then, the equation with both advection - diffusion term and biochemical term are discussed. the splitting - operator is used to decouple the advection and diffusion terms with biochemical term in the equations. the way to determine the smaller time step for solving fast biochemical terms is introduced through comparing the order of characteristic time of biochemical term with that advection ( diffusion ) term. numerical simulation results show that good agreement between analytical solution and experiment result is attained

    本文討論了含裂隙介質地下水污染物輸運與生物降解非線性方程組數值求解方法.方程含有對流項、擴散項、生長、死亡、吸附、解吸、趨化和孔隙與裂隙介質界面間的交換項的非線性偶合，使演算法十分困難.本文討論了無生化過程時的幾種求解方法，數值結果表明：用三次迎風插值法對常見的對流項占優勢，且場變量有較大梯度的問題較適用.在討論有生化反應過程時，利用對流項與生化反應項的特徵時間量級估算，給出了求生化過程作用子步的時間步長估算辦法.用上述方法所得到的模擬結果與解析解、無化學反應和有化學反應的實測值對比，吻合很好
  19. The numerical simulation is an effective method. the main task of this dissertation is to establish a hydrodynamic and pollutant transport model, and to simulate the tide field and concentration field of hakata bay : ( 1 ) dispersing the long - wave equation on interlaced grid by adi method, a two - dimension hydrodynamic model is established to simulate the tidal flow in hakata bay under the effects of m _ 2, s _ 2, o _ 1, k _ 1 tide

    本文的主要工作是建立一個深度平均的二維水動力及污染物擴散輸移的數值模型，並對一實際海灣的潮流場及濃度場進行數值模擬： （ 1 ）用深度平均淺水波動方程為控制方程，採用迎風adi有限差分方法（交替方向隱式法）在矩形交錯網格上離散潮波方程，建立了一個二維潮流數值模型。
  20. The fourth - order explicit upwind - biased compact difference schemes are used in the spatial discretization of the nonlinear convection terms. these difference schemes can be used in all computational region including the boundary neighborhood, and can overcome the difficulty not adapting simultaneously in the boundary neighborhood for general three - dimensional fourth - order central difference schemes, and improve computational stability a nd resolution. the compact difference equations with high accuracy and resolution for solving the incompressible n - s equations and perturbation equations are composed of these compact difference schemes, and provides an effective numerical method for the investigations of the turbulent spots and coherent structures

    文中發展了四階時間分裂法用於navier - stokes方程及其擾動方程的時間離散；對分裂得出的關于壓力的poisson方程和關于速度的helmholtz方程，建立三維耦合四階緊致迎風差分格式；這些格式適用於包括鄰近邊界點在內的計算區域，克服了三維各自用四階中心差分格式離散不適用於邊界鄰域的困難，並提高了穩定性和解析度，用這些格式分別組成了數值求解navier - stokes方程及其擾動方程的高精度、高解析度的緊致差分方程組，為湍斑及湍流相干結構的研究提供了有效的數值方法。
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