海岸淺水帶 的英文怎麼說

中文拼音 [hǎiànjiānshuǐdài]
海岸淺水帶 英文
offshore coastal strip
  • : Ⅰ名詞(水邊的陸地) bank; shore; coast Ⅱ形容詞[書面語] (態度嚴峻或高傲) lofty
  • : 形容詞1 (從上到下或從外到里的距離小) shallow 2 (淺顯) simple; easy 3 (淺薄) superficial 4 ...
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • 海岸 : seaboard; seabeach; seashore; seacoast; coast; shore
  1. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃中部泥質區和東中陸架的兩個鉆孔巖芯的古生物、 ams ~ ( 14 ) c測年、地層剖面等,參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古團、沉積速率、古深、沉積物源、平面平均上升率,討論目前中國東部平面上升的狀況、溫室效應及保護。
  2. If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific

    當熱東太平洋的溫為暖異常,它將激發澳大利亞的東部沿的大氣產生反氣旋性風應力異常,在這種風場的作用,下方向四周輻散,導致熱西南太平洋的溫躍層變,產生負的溫度異常。
  3. Occur mostly in shallow, sheltered soft - bottom marine coastlines and estuaries of the world

    草主要在世界各地的而軟底之遮蔽及河口地出現。
  4. Wave off into shallow waters, seabed by the friction effect change steep wave front, trough ice, water points trajectory showed reciprocating flow, but also to the shore into the flow speed usually return rate greater than offshore, the net result of sediment at the bottom to the shore handling, and was the shock waves on the shore with the water current - riviera online accumulation

    波浪傳入近區,受到底的摩擦作用,波鋒變陡、波谷變緩,質點運動軌跡呈現往復流動,而且向進流速度通常大於離迴流速度,導致底部泥沙凈向搬運,並被激浪的上沖濱線上堆積。
分享友人