weather layer 中文意思是什麼
weather layer
解釋
風化層-
2. dynamic meteorology : equations of motion ; geostrophic, ageostrophic and gradient winds ; thickness and thermal wind ; continuity equation ; stream function ; vorticity equation ; divergence equation ; omega equation ; rossby wave ; ekman layer ; numerical weather prediction
2 .動力氣象學：運動方程地轉風非地轉風及梯度風厚度及熱成風連續方程流函數渦度方程輻散方程奧米茄方程羅斯貝波埃克曼層數值天氣預報。 -
However, today ' s natural gut strings are coated with a protective layer to prevent water and weather damage
然而，當今的羊腸線被包裹了一層保護層去防止水或者天氣的破壞。 -
2 ) from the analysis of the aerodynamic parameters and turbulent flux transfer under different synoptic conditions we achieve the conclusion that on sands raising and sandstorm days turbulent momentum and sensible - heat fluxes are important exchange factors in the boundary layer, with turbulent exchange stronger in sandstorm weather than both on fine and sand raising days. prior to the occurrence of such an event, in particular, the super - adiabatic instability in the near - surface boundary will reinforce sandstorm weather condition. 3 ) atmospheric turbulent diffusion parameters z and y have apparent daily variation
沙塵天氣下以親地殼元素為主的氣溶膠元素濃度均高於背景大氣和浮塵天氣，而且沙塵天氣強度愈強，元素濃度的增加愈顯著；背景大氣、浮塵天氣條件下親地殼元素的濃度一般在10 ~ （ - 1 ） 10 ~ 0 g m ~ 3量級，揚沙、沙塵暴時一般達10 ~ 1 g m ~ 3量級，特強沙塵暴時高達10 ~ 2 g m ~ 3量級。 -
The abnormalities in the seasons and the weather, the rapid melting of the polar ice cap, the rising temperature of the oceans, the continuous expansion of the hole in the ozone layer, the acid rain given back to us by mother earth, sinking land masses and rising sea levels - what do all these reactions of the natural environment tell us that things turn for the worse when they reach the extreme seems not to be something which people take heed of
人類賴以生存的地球已是岌岌可危，生態環境在不斷的破壞下已產生了顯著的變化，四季氣溫異常北極冰巖急速溶化海水水溫高漲臭氧層的破洞繼續擴張大自然「還贈」給人們的酸雨陸地下陷海平面上升，這種種的自然界反應到底給了我們什麼啟示？物極必反的道理，似乎很難在人們心中起警惕的效應。 -
It is the important mechanism that middle - level dry and cold air current sunk, low - level warm and wet air current ascended. level direction energy sharp section is important to blaze middle scale hypo - circumfluence. severe convection weather was brought by layer - knot latent instability
上層乾冷、下層暖濕的位勢不穩定層結可以使對流層中低層出現明顯的逆溫層，有利於不穩定能量積累，此次天氣過程產生的對流不穩定能量大，形成的上升氣流深厚。 -
A similar haze layer on the ancient earth would have also cooled the climate, thus shifting the methanogen population back toward those slower - growing species that prefer cooler weather and thereby limiting further increases in methane production
類似的霾層同樣使古地球的氣候變冷，導致產甲烷菌的菌落演變回偏好較冷天氣而生長緩慢的菌種，因而進一步抑制甲烷產量的增加。 -
The squall line is a kind of instable and strong convective weather caused by the air with upper - layer dry and lower - layer wet in front of the upper - troposphere trough
分析指出，該颮線系統是由高空槽前型的上干下濕引起的不穩定強對流天氣。 -
You can support this by adding a good layer of new mulch over your garden as it dies off due to colder weather setting in ; and then just as the snow melts, add another layer of mulch in the spring
你可以在植物相繼死去的寒冷季節里為你的菜園加上一層優質的新覆蓋物，並當春暖雪化時加上另一層覆蓋物以支持這一目標。 -
Planetary boundary layer ( pbl ) parameterization is an essential part of numerical weather prediction model. there have been many pbl schemes applied in all kinds of models, such as mm5, wrf and so on
在中尺度模式、大氣環流模式、中長期天氣預報模式及模擬氣候變化的數值模式中，人們已經注意到邊界層所起的作用。 -
People in buffalo, new york got a fresh new layer of snow overnight. the weather forced these drivers to slow down. some accidents were reported
紐約州法布羅市的市民昨晚得到了一層新鋪的雪花。寒冷的天氣使這些司機只能慢速行駛。據報道發生了一些交通事故。 -
Ozone - layer depletion above the arctic is not as extensive as expected because of unusually warm weather
因為不正常的暖氣候，北極上空臭氧層消耗的范圍並不像我們預期的那麼大。 -
A severe rainstorm over liaoning occurring from august 19th to 21st in 1997 by a landing northward tropical cyclone ( 9711 ) was simulated by mm5 non - hydrostatic model. through comparing the simulate results with the real weather, the different layer synoptic - scale circulation, height field, temperature field and precipitation were successfully reappeared. the main synoptic background in the case was as follow
使用psu ncarmm5v3非靜力模式，對1997年登陸北上的11號臺風， 8月20日夜間在遼寧登陸前後，給遼寧帶來的大范圍大暴雨進行了數值模擬，並通過模擬的高、中、低空形勢場（高度場、溫度場） ，降雨量以及降雨強度與實況進行對比分析，是一次比較成功模擬，基本再現了遼寧大暴雨過程物理量場變化的全貌。 -
Cover layer and stiffener have similar properties, both possess high flexibility, good weather - ability, flame retardation, anti - ion - migration and heat resistance
覆蓋膜和補強版的黏膠設計，具有穩定的抗撕強度與耐噴錫性，並確保貼合時不塞孔、不包氣泡。 -
Based on five years regional water - salt monitoring data and related hydrological and weather information in the smaller scale experiment zone ( shahaoqu ), the regional water - soil ( salt ) environment regime including grounder water table depth, water quality, superficial layer ( 0 - 40cm ) and middle layer ( 40 - 70cm ) soil moisture and saline concentration are simulated, tested and predicted using bp model. at the same time, the rbf model is be used to calibrate the results of bp
以一個小尺度試驗區的多年區域水鹽監測資料及水文氣象資料為建模依據，對試區非凍期（作物生長期）的地下水位、地下水質、土壤水鹽（ o - 40cm ， 40 - 70cm ）的水-土（鹽）環境狀況進行了較為深入全面的模擬預測，並進行了rbf模型預測結果的對比。
分享友人