sinking of japan 中文意思是什麼

sinking of japan 解釋
日本沉沒
  • sinking : n. 1. 沉沒;沉下;低陷,塌下,凹下。2. 試掘;投資。3. 【建築】孔;凹處。4. (饑餓、勞苦等造成的)衰弱。
  • of : OF =Old French 古法語。
  • japan : n 日本,日本國〈亞洲〉。 the Japan Current 日本海流,黑潮。 the Sea of Japan 日本海。n 1 日本漆;...
  1. 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。
  2. Japan enjoyed tremendous growth under the bubble economy, but with the burst of the bubble at the beginning of the 1990s, sinking tax revenues caused by the protracted economic slump led to a critical state in metropolitan finances

    日本在泡沫經濟下得到了巨大的發展,但是隨著二十世紀九十年代初泡沫的破裂,長期的經濟萎靡產生稅收衰減,導致了都政府的財政危機。
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