潤濕中溫氣候 的英文怎麼說

中文拼音 [rùnshīzhōngwēnqìhòu]
潤濕中溫氣候 英文
humid mesothermal climate
  • 潤 : Ⅰ形容詞（細膩光滑; 滋潤） moist; smooth; sleek Ⅱ動詞1 （加油或水 使不幹枯） moisten; lubricate 2 ...
  • 濕 : Ⅰ形容詞（沾了水的或顯出含水分多的） wet; damp; humid Ⅱ名詞（姓氏） a surname
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 氣 : Ⅰ名詞1 （氣體） gas 2 （空氣） air 3 （氣息） breath 4 （自然界冷熱陰晴等現象） weather 5 （氣味...
  • 潤濕 : madefaction; [物理學] wetting潤濕劑 wetting agent; wetting-out agent; syndets
  • 氣候 : 1. （氣象情況） climate; weather 2. （局勢） climate; situation 3. （結果; 成就） successful development
  1. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面分析來看，本區在全新世早期氣候回返，相對較寒冷乾燥，東亞冬季風影響較明顯，此時為沙層堆積向砂質土壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；全新世晚期至今，氣候向乾冷方向轉化，但變化幅度遠小於末次冰期。
  2. The modified zndx in comparison with others is well indicative of the severity and extent of flood / drought event and of more objective classification of them, which is therefore quite applicable to a extended area. ( 3 ) the main anomaly structures of grades of drought / food in summer over northwest china present pluvial pattern and dry pattern in all the areas, and spatial changes are opposite pattern from the noth to the south and the west to the east. the first four rotated loading vector fields represent four principal precipitation anomaly areas : the weishui river basin, east of the qinghai - xizang plateau

    但修訂過的zndx指數根據氣溫、土壤濕度及前期氣候濕潤度等因子能夠客觀的反映出西北地區的旱澇特徵。 （ 3 ）西北地區季與年區域旱澇等級表明：西北地區的乾旱雨澇有顯著的階段性和年際變化特徵。 1980 』 s到1990 』 s中期，氣候較濕潤，土壤濕度增墑較明顯； 1990 』 s中期以後是40年乾旱最異常的時段； 1960 』 s旱澇交替發生，旱澇趨勢接近常年； 1970 』 s氣候雖乾旱，但沒有1990 』 s中後期顯著。
  3. The location of quangan city is at subtropics moist monsoon climatic region with plenty heat, plenty rain

    廣安市地處中亞熱帶濕潤季風氣候區，氣候溫暖，熱量充足，雨量豐沛，空氣濕度大，日照少，霜期短，風力小。
  4. The existence of two taxa of taxodiceae reflects a warm - humid local environment under subtropical climate during late miocene. there are 4 taxa, pinus armandii, ericaceoxylon longlingense, ericaceoxylon hymenanthesoides and

    他們反映的古植被為針闊混交林，生長于亞熱帶溫涼濕潤的山地氣候環境中，當時當地的誨拔高度在1800 3000米之間。
  5. Comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period, expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch, warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment

    通過對雲南景谷盆地及隴川盆地新生代生物群特徵的對比，探討了新生代兩大盆地環境演變：早中新世到上新世為湖盆發展期湖盆擴大萎縮期，氣候為早期的千燥中新世早期的溫暖濕潤中新世中晚期的寒冷陰濕上新世的乾燥，而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油氣的形成提供了有利條件。
  6. Abstract : comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period, expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch, warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment

    文摘:通過對雲南景谷盆地及隴川盆地新生代生物群特徵的對比，探討了新生代兩大盆地環境演變：早中新世到上新世為湖盆發展期湖盆擴大萎縮期，氣候為早期的千燥中新世早期的溫暖濕潤中新世中晚期的寒冷陰濕上新世的乾燥，而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油氣的形成提供了有利條件。
  7. Climate : this zone mostly belongs to the subtropical monsoon climate, where four seasons are distinguishable, mild climate, winter is not too cold, summer is not too hot, rain fall is abundant

    氣候：大多屬于中亞熱帶季風濕潤氣候，四季分明，氣候溫和，冬無嚴寒，夏無酷暑，雨量充沛。
  8. No charm was wanting, no defect was perceptible ; the young girl had regular and delicate lineaments ; eyes shaped and coloured as we see them in lovely pictures, large, and dark, and full ; the long and shadowy eyelash which encircles a fine eye with so soft a fascination ; the pencilled brow which gives such clearness ; the white smooth forehead, which adds such repose to the livelier beauties of tint and ray ; the cheek oval, fresh, and smooth ; the lips, fresh too, ruddy, healthy, sweetly formed ; the even and gleaming teeth without flaw ; the small dimpled chin ; the ornament of rich, plenteous tresses - all advantages, in short, which, combined, realise the ideal of beauty, were fully hers

    英格蘭溫和的氣候所能塑造的最可愛的面容，英格蘭濕潤的風和霧蒙蒙的天空所能催生，所能庇護的最純正的玫瑰色和百合色這種描繪，在眼前這個例子中證明是恰到好處的。不缺一絲嫵媚，不見任何缺陷。這位年輕姑娘面部勻稱嬌嫩，眼睛的形狀和顏色就跟我們在可愛的圖畫上看到的無異，又大又黑又圓，眼睫毛又長又濃，以一種柔和的魅力圍著一對美麗的眼睛。
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