japan stream 中文意思是什麼
japan stream
解釋
黑潮黑潮-
Dihao holiday hotel located in the timor - west restaurant called the largest - west restaurant to appear for the 360 - degree panoramic vision radius, the hong kong central gaze afar a thorn, on the downtown urban stream, is " sitting in japan ok 80, 000, dwarfs yaokan 1000 river.
位於帝濠度假酒店的旋轉西餐廳堪稱最大的旋轉西餐廳，以數十米為半徑的360度全景視野，環眺百年金港秀色，縱覽都市流金繁華，可謂「坐地日行八萬里，巡天遙看一千河」 。 -
The latter part of the programme is divided into japanese language and japanese studies streams. the japanese language stream includes business japanese, conversation, reading comprehension, writing and translation courses. the japanese studies stream includes courses on japanese cultural history, traditional cultural patterns and modern society, japanese popular culture, understanding japanese culture and society through movies, chinese - japanese - korean movies, japanese linguistics, anthropology of japan, japan and hong kong, sino - japanese relations, and japanese economy
後期課程分日語及日本研究兩大領域，前者包括商業日語、會話、讀解、作文、翻譯等科目，後者包括日本文化史、日本傳統文化與現代社會、日本流行文化、從電影分析日本文化與社會，中、日、韓電影的欣賞與比較、日本語言學、日本文化的人類學研究、日本與香港、中日關系及日本經濟等科目。 -
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東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，西北地區東部持續受高壓控制，冷空氣沿此高壓流經長江中下游地區上空；在西北地區東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，不利於西北地區東部降水。空梅雨2000年相反，鄂霍茨克海高壓減弱甚至不存在，東亞-日本為高壓，西太副高位置偏西偏北，西北地區東部處于西風槽中，對流層中下層氣流上升運動增強，盛行低壓環流，水汽通量散度強烈輻合，有利於降水生成。 -
In the 80 ’ s and early 90 ’ s ? japan ' s boom period ? this stream of western architects became a river
還是在80年代至90年代初的時候，正值日本經濟發展的黃金時期，大量的西方建築師如過江之鯽，從西方來到日本。
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