盛東升 的英文怎麼說

中文拼音 [chéngdōngshēng]
盛東升 英文
sheng dongsheng
  • : 盛動詞1. (把東西放在器具里; 裝) fill; ladle 2. (容納) hold; contain
  • : Ⅰ動詞1 (由低往高移動) rise; hoist; go up; ascend 2 (等級提高) promote Ⅱ量詞1 (容量單位) lit...
  1. At first, analysis of extreme temperature ' s spatial distribution of variety trend shows that the minimum temperature in the north are going up while the maximal temperature in east china declining widely, which is a numerical characteristics of prevailing warmer - winter in recent years. so the change of minimum and maximal temperature are dissymmetrical

    首先從總體上,分析極端最高和極端最低溫度變化趨勢的空間分佈:北方地區極端最低溫度普遍上,且幅度較大,是近年來暖冬行的一個數值化特徵;極端最高溫度在部普遍下降,最低最高溫度變化具有不對稱性。
  2. Globigerina bulloides, which was regarded as the mark species for the sw monsoon prevailing in the arab sea, while in this area, it ' s more likely to be a mark species for the strong ne monsoon

    在阿拉伯海被認為是西南季風行的上流標志種globigerinabulloides在本區更可能是北季風增強、西南季風減弱的標志種。
  3. His representative works including : darwin central hotel ( australia ), hongkong sunbeam center, shanghai golf club, beijing shengshilong celebrity restaurant, hongkong nison center, hongkong pokwong center, hongkong hilder center, houses of hongkong redhill peninsula, shanghai dasheng asset club, guangzhou linguaphone, shenzhen noble center, shenzhen shen mao commerce center, shenzhen wanhao commercial plaza, shenzhen donghai shopping mall, vanke oriental zunyu club etc

    代表項目:澳洲達爾文中心酒店、香港日豐酒店、上海高爾夫球會、北京世隆名流食尚、香港日中心、香港寶光中心、香港富德中心、香港紅山半島獨立屋、上海大資產辦公會所、廣州靈格風、深圳諾德中心、深圳深茂商業中心、深圳萬豪商業廣場、深圳海購物步行街、萬科方尊峪會所等。
  4. It was dark, but at eleven o clock the moon rose in the midst of the ocean, whose every wave she silvered, and then, " ascending high, " played in floods of pale light on the rocky hills of this second pelion. the island was familiar to the crew of the young amelia, - it was one of her regular haunts. as to dant

    天很黑,但到了十一點鐘,月亮從海上了起來,把海面上染成了一片銀色,然後,又一步步上,把蒼白色的光瀉滿了這座堪稱皮隆此山為希臘北境內的高山,山中林木茂,景色秀麗,在希臘神話詩等文學記載中十分著名。
  5. But in flood years, the convergences in mid - and low - level of troposphere are strong. divergence departure in 200hpa is positive, so the pumping cause the updraft stronger. as we all know, the updraft is better to the rain

    澇年對流層中下層輻合偏強, zoohpa上,高原北側地區為正散度距平區,輻散較常年偏強,高空輻散抽吸作用使得該區行上氣流,有利於降水的形成。
  6. The east, where the sun rises, represents life ' s fertility with the end of winter and coming of spring

    太陽初方代表了冬去春來、萬物繁衍昌的景象。
  7. In 1999, the dipole existed in between the okhotsk high and the depression in the north of northeast china, thus the okhotsk high became active and maintained, the subh was located to an area quite further south than usual. the high persisted in the east region of nw china, the cold air flowed to the mid - lower reaches of the yangtze river along the high. in the east region of nw china, air steam under troposphere was strong sinking motion, and formatted the negative vorticity region, the vapour flux divergence was divgence. lt was apparently that the rain could n ' t occur in the eastern portin of nw china. in 2000 year, okhotsk high was very weak or did n ' t exist in, there was high in the east asia - japan, the subh is located to an area further north than usual. in the east region of nw china, the trough maintained, air stream under troposphere was strong ascending motion, the cycolonic circulation was prevailing, the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china

    4多梅雨1999年鄂霍茨克海阻塞高壓與我國北北部低壓形成偶極子,使得阻塞高壓穩定少動,西太副高位置偏南,西北地區部持續受高壓控制,冷空氣沿此高壓流經長江中下游地區上空;在西北地區部對流層中下層氣流下沉運動較強,呈反氣旋渦度,水汽通量散度輻散,不利於西北地區部降水。空梅雨2000年相反,鄂霍茨克海高壓減弱甚至不存在,亞-日本為高壓,西太副高位置偏西偏北,西北地區部處于西風槽中,對流層中下層氣流上運動增強,行低壓環流,水汽通量散度強烈輻合,有利於降水生成。
  8. When the spatial pattern is of the north - south asymmetry, in the warm north - cold south years, there is a anticyclone circulation existing over the warm pool at 850hpa, easterly at 15 n and westerly in the tropical region have been greatly strengthened, while the center of anticyclone circulation moves to the east asia at 200hpa, and the hadley circulation has been affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river, vice versa. there are different relations to east asia atmospheric circulation and summer rainfall in china

    當ssta為南北半球反對稱分佈時,與ssta北暖南冷分佈相對應, 850hpa暖池區上空為一反氣旋偏差環流, 15 n附近風氣流和赤道附近西風氣流增強,長江中下游地區行偏南風氣流; 200hpa反氣旋偏差環流中心移到亞大陸上空;副熱帶高壓強度、西伸脊點都明顯變強、西伸; hadley環流得到發展,長江中下游(華北)地區為上(下沉)氣流,降水明顯增多(減少) ,北冷南暖年則相反。
  9. Firstly, subtropical high center lay to the north than usual, and forms a blocking high in combination with land high in eastern asia. secondly, on account of the strong southwest current which occurred at the west side of the subtropical high and dynamic effect of the typhoon itself, the landing northward tropical cyclone ( 9711 ) landed in liaoning again. thirdly, a trough with some weak air from ural mountain and the northeast cold air entering into the tropical cyclone showed that the systems in different latitudes had some effects each other

    模擬結果表明:此次熱帶風暴造成遼寧全省大暴雨的天氣背景是:副熱帶高壓偏北並與大陸高壓疊加,構成了穩定的亞阻塞形勢; 9711臺風減弱的熱帶風暴,在其自身內力和副高西側的強偏南氣流引導下,持續北上並在遼寧營口至盤錦之間登陸;從烏拉爾山冷堆分裂南下出的弱冷空氣不斷南下,與熱帶風暴在遼寧產生了相互作用,增強了上運動,致使大暴雨出現。
  10. Results show that there are two main spatial patterns of the wp ssta : one is uniform in the whole area, the other is of the north - south asymmetry. when the spatial pattern is uniform in the whole area, in the warm years, there is a anticyclone circulation existing over the warm pool and westerly in the subtropical region and easterly in the tropical region have been greatly strengthened at 850hpa, while a anticyclone circulation over the india region at 200hpa, the walker circulation has been strengthened, the summer rainfall may be above normal in the upper and middle reaches of the yangtze river, vice versa

    當ssta為一致性分佈時,暖異常年, 850hpa暖池區上空為一反氣旋偏差環流,副熱帶地區西風和低緯度地區風得到加強,長江中上游地區行偏南風氣流; 200hpa南亞上空為一反氣旋偏差環流,長江中上游地區為北風; walker環流加強,副熱帶高壓偏強,經向垂直環流在25 35 n附近為上氣流,長江中上游地區降水偏多,是lanina事件的多發年,對應的soi指數偏高,冷異常年則相反。
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