cloudy surface 中文意思是什麼

cloudy surface 解釋
霧面
  • cloudy : adj. 1. 陰天的,陰雲密布的。2. 雲(狀)的。3. 朦朧的。4. 愁容滿面的。5. 受人懷疑[蔑視]的。6. (水晶等)帶雲霧紋的;(酒等)混濁的。n. 多雲天。
  • surface : n 1 表面;地面;水面;廣場,空地。2 外觀,外表,皮毛。3 【幾】面;切口;【航空】翼面。adj 表面的...
  1. According to the data of infrared nephogram of satellite, provides the concept of demct ( digital elevation model of cloudy top ), studies the technology of modeling of the surface of demct. 3. the arithmetic of triangulated network of 3d - visulazation of cloud

    2 .根據雲圖三維表現原理,從二維紅外衛星雲圖得出雲頂表面高度值,獲取雲的三維信息,類比地形數字高程模型,提出了雲頂數字高程模型( demct )的概念。
  2. The maximum of instantaneous global radiation is beyond 1000w / m2 and the ten - days average intensity is 338. 90w / m2 because of high atmospheric transparency over semi - arid rainfed agriculture region of loess plateau between june and august. global radiation, reflected global radiation and surface long wave radiation emerge the characteristic of daily variations on a typical clear day and cloudy day, whereas atmospheric long wave radiation has not this characteristic. meanwhile, net radiation, latent heat flux sensible heat flux and soil heat flux appear the same characteristic as the mean daily variations above spring wheat field and bare soil on a typical clear day and cloudy day

    黃土高原半乾旱雨養農業區夏秋季大氣透明度較高,晴天地面的總輻射值最大瞬時值均超過1000w m ~ 2 , 6 8月總輻射旬平均強度為338 . 90w m ~ 2 ;典型晴天和陰天總輻射、反射輻射、地表長波輻射均表現出明顯的日變化特徵,而雨天沒有明顯的日循環規律;無論是晴天、陰天還是雨天,大氣長波輻射基本沒有明顯的日變化規律。
  3. It is found in this paper that : 1. the radiation computing solution developed by zhou suoquan et al. shows good performance on the fluxes simulation of the total surface radiation and net surface radiation, which can reflect the annual and daily radiation change very well, and radiation differences between clear day and cloudy day as well

    結果表明: 1 )該輻射計算方案對于漠河總輻射通量和凈輻射通量有較好的模擬性能,能夠較好地模擬出輻射通量的年變化和日變化的特點,對于晴天和雲雨天氣輻射通量的差別也能較好地模擬出來。
  4. The daily variation of surface o3 is different under different weather condition, the variation of surface o3 in spring, autumn and summer is almost same when it is clear. in spring and autumn, under the condition of clear sky, its value is higher than that in cloudy or rainy / snowy day, while its variation is not obvious in winter and summer ; in rainy and snowy season, the variation of surface o3 in spring, autumn and winter is insignificant, bnt in summer, it is significantly different from other seasons, daily difference is the highest among all seasons, it has some important relationship with rain / snow, moreover, the function of rain and snow to the varation of surface o3 is different

    ( 2 )不同天氣條件下,春、夏、秋、冬四個季節地面o _ 3濃度變化不盡相同,晴天和多雲天,春、夏、秋季的地面o _ 3變化趨勢基本一致,其中,春秋季,晴天o _ 3值高於多雲天和降雨天,而冬季和夏季則不明顯;各季節降雨、雪天o _ 3濃度的變化情況來看,地面o _ 3在春、秋、冬三個季節變化不大,而夏季與其它季節明顯不同,變化幅度很大,日較差在四個季節中為最大,這與降雨、降雪關系很大,並且可能存在雨、雪的差異。
  5. The character of surface radiation and energy expended over soil temperature variation is that the temperature variation at surface, 5cm depth and 10cm depth are approximately sine curve on clear and cloudy day while this way the temperature variation at 20cm depth shows small extent anti - phase variation and the temperature under 50cm is no diurnal. in contrast, the temperature at 5m, 10cm and 20cm shows linear decrease and the soil - surface temperature is concaved on rainy day

    地表輻射和能量耗散反映在土壤溫度變化上的特徵是晴天和陰天地表、 5cm 、 10cm的溫度變化表現為準正玄曲線, 20cm深處的溫度變化呈現出幅度很小的反位向變化, 50cm以下地溫已不存在日變化特徵;雨天5cm 、 10cm和20cm的溫度呈線性遞減,地表溫度表現出由降雨引起的凹陷現象。
  6. In this paper, the solar and land - atmosphere radiation rates are calculated by modtran3 model and satellite observation as well as surface data, solar direct irradiance infrared irradiance solar heating rate and infrared cooling rate were calculated from 43 samples of sunshine day and 5 samples of cloudy day 3 samples of rainy day of different latitudes in 12 stations. the paper analyzed solar heating rate and infrared cooling rate in sunshine day, the factors such as zenith angle, water vapor and latitude were found out correlating with solar heating rate and infrared cooling rate. solar heating rate and infrared cooling rate change on the same day and at the same station

    在對晴空大氣的計算中,本文對太陽的直接輻射與地氣系統的紅外輻射狀況進行了分析,並討論在不同的大氣狀況下太陽加熱率和紅外冷卻率的情況,找出與太陽加熱率和紅外冷卻率變化相關較大的因子?太陽天頂角和水汽條件、緯度;本文還進一步分析了不同緯度樣本的太陽加熱率與紅外冷卻率日變化及有雲、有雨情況下太陽加熱率和紅外冷卻率的變化情況:另外,文中通過改變二氧化碳在大氣中含量的方法,討論了它對太陽加熱率與紅外冷卻率的影響。
  7. The results of radiation simulating, summer better than winter and clear day better than cloudy day, can be used in bats directly, which give a good solution for lacking of land surface radiation observation

    模擬結果夏季好於冬季,晴天好於陰雨天氣,可以在bats模式中應用,以解決沒有輻射觀測資料的問題。
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