southeasterly adj.向[在、自]東南的。 southeasterly...
adj. 向[在、自]東南的。 southeasterly gale 東南烈風。 adv. 向[在、自]東南。 n. 東南大風。 “southeastern“ 中文翻譯: adj. 1.向[在、自]東南的。 2.東南部的;〔S-〕美國東南部的。 “southeaster“ 中文翻譯: n. 東南大風。 “southeastern asiatic squirrel“ 中文翻譯: 紅頰長吻松鼠“southeast wind“ 中文翻譯: 東南風“southeastern cancer study group“ 中文翻譯: 東南亞癌癥研究小組“southeast university gymnasium“ 中文翻譯: 東南大學體育館/“southeastern conference“ 中文翻譯: 東南聯盟“southeast university“ 中文翻譯: 東南大學“southeastern culture“ 中文翻譯: 東南文化“southeast trades“ 中文翻譯: 東南信風
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The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows , so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening , one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea . furthermore , with the effect of terrain , the southern shaanxi province became the center of this extremely heavy rain process 中尺度結構分析表明,本次暴雨具有明顯的中尺度特征,是由三支氣流共同作用的結果,分析發現( 1 )地面東南風和地形在這次大暴雨過程起主要作用; ( 2 )東路冷空氣主要是通過中低層侵入陜南地區的,并與地面冷式錮囚鋒的形成密不可分; ( 3 )夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因,一個是由于地形山谷風的作用,另一個是降水的潛熱釋放激發了上升運動: ( 4 )位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; ( 5 )本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部,為暴雨的發生提供了必要熱力條件。 |
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Temporarily between 0800 utc and 1200 utc surface wind direction 170 degree south - southeasterly winds ; wind speed 25 knots gusting to 40 knots ; visibility 1000 m in thunderstorm with moderate rain ; scattered cloud at 1000 feet including cumulonimbus cloud and broken cloud at 2000 feet 在0800 utc至1200 utc之間,地面風向間中為170度東南偏南風,風速25海里小時,陣風達40海里小時能見度在雷暴及和緩雨勢中為1000米1000尺有零散云層,包括積雨云, 2000尺有疏松云層 |
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Temporarily between 0800 utc and 1200 utc surface wind direction 170 degree ( south - southeasterly winds ) ; wind speed 25 knots gusting to 40 knots ; visibility 1000 m in thunderstorm with moderate rain ; scattered cloud at 1000 feet including cumulonimbus cloud and broken cloud at 2000 feet 在0800utc至1200utc之間,地面風向間中為170度(東南偏南風) ,風速25海里小時,陣風達40海里小時;能見度在雷暴及和緩雨勢中為1000米; 1000尺有零散云層,包括積雨云, 2000尺有疏松云層 |
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The doppler radial winds from the terminal doppler weather radar ( tdwr ) 0 . 6 - degree elevation scan over the hkia and its western approach were generally away from the radar ( positive radial velocity - - warm colours ) , consistent with the low - level east - southeasterly flow ( figure 12 ) 機場多普勒天氣雷達對香港國際機場及西面著陸區的0 . 6度仰角掃描顯示,多普勒徑向風大致離開雷達(正徑向風速暖色) ,與低空東南偏東氣流吻合(圖12 ) 。 |
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The southerly water vapor can progress to 50 n near north - east in china - , the southeasterly water vapor from south side of the west pacific subtropical high and north side of the monsoon trough can march westward to 100 e near south - east part of gansu in summer 東亞夏季偏南風水汽輸送所能到達的北界為50 n附近的東北北部。西太平洋副高南側、亞洲季風槽北側的東南風水汽輸送在夏季可向西擴展到甘肅東南部地區( 100 e附近) 。 |
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The doppler radial winds from the terminal doppler weather radar tdwr 0 . 6 - degree elevation scan over the hkia and its western approach were generally away from the radar positive radial velocity - warm colours , consistent with the low - level east - southeasterly flow figure 12 機場多普勒天氣雷達對香港國際機場及西面著陸區的0 . 6度仰角掃描顯示,多普勒徑向風大致離開雷達正徑向風速暖色,與低空東南偏東氣流吻合圖12 。 |
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In drought ( flood ) years over the yangtze river basin , the southerly moisture transport with the summer monsoon can shift to northern ( southern ) than the normal , the southeasterly water vapor from south 雨季建立之前和雨季結束之后,華北和東北地區西邊界的偏西風水汽輸入占絕對優勢;雨季中南邊界的偏南風水汽輸送對華北最為重要,東北地區雨季期間南邊界的水汽輸入和與來自西邊界的水汽輸入貢獻相當。 |
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From 1200 utc surface wind direction 150 degree ( south - southeasterly winds ) ; wind speed 15 knots ; visibility 10 km or above ; nil significant weather ; broken cloud at 2000 feet and broken cloud at 10000 feet 由1200utc開始,地面風向為150度(東南偏南風) ,風速15海里小時;能見度10公里或以上;并無顯著天氣狀況; 2000尺有疏松云層, 10000尺亦有疏松云層 |
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From 1200 utc surface wind direction 150 degree south - southeasterly winds ; wind speed 15 knots ; visibility 10 km or above ; nil significant weather ; broken cloud at 2000 feet and broken cloud at 10000 feet 由1200utc開始,地面風向為150度東南偏南風,風速15海里小時能見度10公里或以上并無顯著天氣狀況2000尺有疏松云層, 10000尺亦有疏松云層 |
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York swept across the southwestern part of lantau island in the afternoon and winds over the hkia turned southeasterly 下午約克掠過了大嶼山的西南部,香港國際機場轉吹東南風。 |
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Surface wind direction 130 degree ( east - southeasterly winds ) ; wind speed 18 knots 地面風向為130度(東南偏東風) 、風速18海里小時 |
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Surface wind direction 130 degree east - southeasterly winds ; wind speed 18 knots 地面風向為130度東南偏東風風速18海里小時 |