surface ice 中文意思是什麼
surface ice
解釋
表冰-
There are three main ways that charon ' s surface supply of crystalline ice could have been replenished
喀戎表面晶體冰的補給有三種主要的方式。 -
Because the road line is in mountainous region and heavy hilly area and its surface relief undulates greatly, more slope wash and dilurial layer distribution, there are more harm, for example, island shaped perennially frozen soil, drift ice and so on, which effect the stability of the road foundation
由於沿線地處山嶺重丘地區，地勢起伏較大，坡積物及洪積層分佈較多。故島狀多年凍土、涎流冰等病害較多，影響路基的穩定。 -
The firmament was a layer of frozen water ( ice ) above the earth ' s surface
冰天是地表上空的一個凍水層（冰） 。 -
As it vaporizes, tiny gas jets spin and tumble the ice shards across the surface of the water
乾冰氣化時產生的小噴流帶動乾冰碎片在水面不斷旋轉翻滾，互相碰撞，產生一團團有多個分支的白霧旋渦。 -
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。 -
The resulting brightness temperature ( tb ), hydrometeor structure, and surface rainfall rate relations show that the ice hydrometeor, espatially the ice at the top of the precipitating cloud, decreases the brightness temperature significantly at 85
結果表明，在85 . 5ghz ，冰相水汽凝結體尤其是處于降水雲頂部的冰晶粒子由於散射輻射而使得亮溫顯著降低。亮溫與冰相粒子的含量之間有很強的相關性。 -
The brightness temperature is highly related to the density of ice hydrometeor. since the convective cloud system is tilted, and the viewing angle is oblique, the area displacement between ice hydrometeor and the surface rainfall rate makes the relation between tb and surface rainfall rate is relatively small
但亮溫和地面降水強度之間的相關性較弱，這是由於該對流系統為傾斜的，冰相粒子和地面降水強度之間存在著位置上的不一致，並且觀測角為傾斜的。 -
Dark patches of ancient terrain are broken up by swaths of brighter, younger material, and the entire icy surface is peppered by more recent impact craters that have splashed fresh, bright ice across the surface
黑色古老地形的碎片被更明亮、更新物質分割開，整個冰封的表面不斷的被更新的隕石砸出的新鮮、明亮的冰更新著。 -
Evidence that the above - imaged plates really are dust - covered water - ice includes a similarity in appearance to ice blocks off earth ' s antarctica, nearby surface fractures from which underground water could have flowed, and the shallow depth of the craters indicating that something is filling them in
支持如上面影像的扁盤的確是被沙塵所掩的水冰的證據有：它有著與地球南極的冰塊相似的特徵、附近地表凹凸不平的部分曾經有被地下水淹沒的痕跡、影像中淺底的隕石坑也許表示有某種東西填滿了坑洞。 -
Venus and mars, our neighouring planets, are just located at the inner and outer rims of the habitable zone respectively. as a result, venus is hot like hell for reason of the runaway greenhouse effect whereas the surface of mars is so cold that water can only exit in the form of ice
在太陽系內，鄰近地球的金星和火星分別處于可居住區域的內外邊沿，故此金星因溫室效應失控而變成地獄般的火熱世界，而火星表面則冰冷得只容許冰粒存在。 -
Using data obtained by the omega spectrometer on board european space agency ' s mars express, the team found the existence of ice clouds which sometimes become so dense that they throw quite dark shadows on the dusty surface of the planet
根據歐洲航天局「火星快車」探測器上裝備的omega光譜儀獲取的數據，該科學家小組發現，由於火星上空的乾冰雲有時很密集，所以會在覆蓋著很多塵埃的火星表面投下陰影。 -
Sellars incorporated various empirical relations between ice cover and surface temperature.
塞拉斯處理了冰量和地表溫度的各種經驗關系。 -
Sea ice covers the arctic sea, occupying 7 % of the surface of the world ' s oceans
海冰覆蓋著北冰洋，它占據了世界大洋表面積的7 % 。 -
It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area. positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area. wind convergence existed at the height of 700hpa, and divergence existed above and below the height of 700hpa
通過對降水雲系的綜合研究，建立了河南省春季層狀雲降水概念模型：暖區降水主要通過雲水碰並形成，冷區降水機制以冰粒子融化等冷雲過程為主;暖區700一50ohpa通常有上升氣流，冷區上升氣流分佈在近地面附近: 700沖a存在風場的輻合，其上下則主要是輻散區;水汽主要集中在7o0hpa高度上，暖區水汽來自南、東南方向，冷區水汽以西南輸送為主;暖區位勢不穩定分佈在o 。 -
As it vaporizes, tiny gas jets spin and tumble the ice shards across the surface of the water. during their brief lifetimes, the dry ice shards collide and spin a multi - armed vortex of white mist
乾冰氣化時產生的小噴流帶動乾冰碎片在水面不斷旋轉翻滾，互相碰撞，產生一團團有多個分支的白霧旋渦。 -
Time - space distribution of water content in the snow on arctic sea ice surface in summer
北極夏季海冰表面積雪層內水分含量的時空分佈 -
The resulting gusts scour the ice surface, depositing snow on the other side instead of letting it build up against the station itself
這樣，被轉移的強風沖刷著冰面，對面的積雪就不會堆積起來抵住科考站。 -
Furthermore, this energy source is supplemented by increased absorption of sunlight by ice sheets darkened by black - carbon aerosols, and the positive feedback process as meltwater darkens the ice surface
此外，冰原被黑碳氣溶膠染黑而增加陽光吸收量，以及融化的冰原由於顏色變深而造成溫度上升的正回饋，都增大了地球能量的不平衡。 -
Net radiation absorbed by ice surface only account for 6 of that absorbed by the sea surface and it is consumed mainly by the processes of sensible heat exchange and ice melting, deficit part of the heat is compensated from the latent heat released when water vapor is frozen on ice surface and heat stored in ice
冰面吸收的凈輻射僅為海面的6左右，主要消耗于感熱輸送和冰面融化過程，不足部分由水汽在冰面上凝結釋放的潛熱和冰中的熱通量來補充。 -
Upon existent theoretical and experimental results and based on a great of laboratory investigations carried out in chongqing university, for the first time this paper studies systematically the insulators dc discharge performance and flashover mechanism of iced insulators in the complex atmospheric environment, which will contribute to the understanding of flashover phenomena observed on ice surface at low air pressure and provide the test and theoretical reference for hv and ehv transmission lines design and safety service
為此，在國內外現有工作的基礎上，通過大量的試驗研究，本文主要研究了復雜環境中絕緣子的直流閃絡特性及閃絡機理。其結果有助於進一步了解低氣壓下覆冰絕緣子的閃絡現象，並可為輸電線路的設計和安全運行提供理論依據。
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