cloudy rainy 中文意思是什麼

cloudy rainy 解釋
天陰的下雨的
  • 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。
  • rainy : adj （rainier; iest） 下雨的，常下雨的，多雨的，含雨的；像要下雨的。 a rainy day 雨天；蕭條[遭難...
  1. It ' s sunny ( snowy / rainy / cloudy / windy ) and warm ( cold / hot cool )

    「天氣是晴朗的（有雪的/下雨的/多雲的/刮風的）和暖和的（冷的/熱的/涼爽的） 。 」
  2. B : it ' s sunny ( snowy / rainy / cloudy / windy ) and warm ( cold / hot cool )

    「天氣是晴朗的（有雪的/下雨的/多雲的/刮風的）和暖和的（冷的/熱的/涼爽的） 。 」
  3. Sunny. / windy / rainy / snowy / cloudy

    晴朗的/有風的/下雨的/下雪的/多雲的。
  4. Today is cloudy and rainy, but not very cold

    今天是陰有雨的天氣，但是不怎麼冷。
  5. B : sunny and mild today, cloudy and rainy tomorrow

    今天晴朗溫和，明天多雲有雨。
  6. But when it is continuosly cloudy and the raising temperature effect is lost in sequential low temperature and rainy days, it seriously harms the cotton growth

    但如果遇到連續陰雨天氣，沙漠增溫效應喪失，氣溫驟降，往往導致棉花冷害。
  7. Cloudy and rainy weather associated with the remnant of aere continued to affect the south china coast for the rest of the month

    與艾利的殘餘相關的陰雨天氣在本月餘下時間持續影響華南沿岸。
  8. Soil heat flux from atmosphere to soil is about 5 % of net radiation on a clear and cloudy day and soil discharge energy to atmosphere on a rainy day above the same field. in brief, average latent heat, sensible heat and soil heat flux is 40 %. 50 % and 10 % of net radiation respectively

    在春小麥下墊面，晴天能量主要消耗于農田蒸散，而在陰天顯熱交換大於農田蒸散耗熱；在晴天和陰天大氣向土壤的能量傳輸均維持在凈輻射的5左右，雨天時，土壤熱通量為負值。
  9. 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。
  10. When sky was cloudy and rainy, the infrared cooling rate was different form that on sunshine day. further more, the effect of thickness of co2 was discussed in this paper. compared with the model output and the observation, the model result is reasonable

    將個別站點大氣輻射情況與實測值進行了分析研究，並將本文的計算結果與前人的結論比較，發現利用衛星資料來計算當時大氣輻射狀況是基本可信的。
  11. 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。
  12. 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。
  13. On the other hand, as there was very little cloudy weather, and seldom or never any fogs in those parts, there was the less occasion for a compass, seeing the stars were always to be seen by night, and the shore by day, except in the rainy seasons, and then no body car d to stir abroad, either by land or sea

    只是羅盤這個東西，我卻始終無法使他理解它的作用，好在這一帶很少有雲霧天氣，白天總能看到海岸，晚上總能看到星星，所以也不大用得著羅盤。當然雨季情況就不同了，可是雨季一般誰都不出門，不要說出海航行了，就是在島上走走也很少。
  14. 10 light 12hours day, even under cloudy rainy day for 5 days above

    8光照12小時每天，陰雨天持續5天
  15. June was dominated by cloudy and rainy weather

    六月受多雲及有雨天氣影響。
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