潤濕氣候 的英文怎麼說

中文拼音 [rùnshīhòu]
潤濕氣候 英文
humid climate
  • : 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 ...
  • : 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
  • : 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. The sahara is known to have had a humid climate during the last glacial stage of the pleistocene epoch.

    據了解,撒哈拉沙漠在更新世最後一個冰川期間的。
  2. 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;全新世中期溫暖,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,向乾冷方向轉化,但變化幅度遠小於末次冰期。
  3. On the influence of global change of cenozoic climate and uplift of himalayas, the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in pliocene

    受新生代全球變冷和喜馬拉雅運動的影響,該盆地一方面受印度洋季風的影響增強,干季節交替明顯;另一方面受地形地貌影響,沿襲了溫暖條件。
  4. 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指數根據溫、土壤度及前期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,,土壤度增墑較明顯; 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雖乾旱,但沒有1990 』 s中後期顯著。
  5. Yueyang is a wettish area of confienental subtropical monsoon with mild climate, plenty of rainfall and four distinct seasons. annually, the average temperature is about 17, the average precipitation is 1387. 93. mm, the average sunlight time is 1680 hours, and the frost - free period lasts 270 days

    岳陽市屬亞熱帶季風區、溫和、雨量充沛、四季分明,年平均溫17左右,多年平均降雨量1387 . 93毫米,年平均日照1680小時,無霜期270天。
  6. In the south west county cork and county kerry, there are areas rich in plants that thrive in the mild and humid climate of the region

    在愛爾蘭西南部(科克郡和凱里郡)的一些地方,溫和而,很多植物在這里生長茂盛。
  7. West of the mountains, the climate is damp from pacific winds.

    山的西面,因太平洋的風而變得
  8. 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季風區,溫暖,熱量充足,雨量豐沛,空度大,日照少,霜期短,風力小。
  9. 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,生長于亞熱帶溫涼的山地環境中,當時當地的誨拔高度在1800 3000米之間。
  10. 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,為早期的千燥中新世早期的溫暖中新世中晚期的寒冷陰上新世的乾燥,而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油的形成提供了有利條件。
  11. 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,為早期的千燥中新世早期的溫暖中新世中晚期的寒冷陰上新世的乾燥,而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油的形成提供了有利條件。
  12. The comparison of stomatal parameters in leaf cuticles between two fossil angiosperms from the pliocene in west yunnan and their nearest living equivalent species indicates a little higher atmospheric co2 level at that time than the present, while carbon isotopic composition of fossil cuticles demonstrates much higher carbon isotopic discrimination and slight lower water use efficiency, showing a warmer and wetter climate than today

    摘要對滇西騰沖新近紀兩種被子植物葉片及其現存對應種的孔參數和碳同位素組成的綜合分析表明:當時的大co2濃度略高於現在水平;化石種的碳同位素分餾值高於現存對應種,但水分利用效率低於現存對應種;這證明當時的條件比當前更為溫暖
  13. The dalian area have the latest type and structure of landform that consist of mountain, hills, mesa, marine corrosion land. in the aspect of area distribution, the east is warm and moist continental monsoon climate, but the west is the warm and submoist continental monsoon climate

    大連地區具有山地? ?丘陵? ?臺地? ?海蝕階地組成的現代地貌類型及其結構;在地域分佈上,東部為暖溫性大陸性季風,西部則為暖溫性亞大陸性季風
  14. Drought and flood are two of the major disasters that human being have to face. the losses due to them may be more than 50 % of the total disaster losses in jiangsu province. many valuable researches on meteorological and agricultural drought and flood have been done in world

    江蘇省地處北亞熱帶、東臨海洋,雨量充沛,,但降雨量年際間變化大,年內分佈不均勻,造成不同年份干狀況差異較大,常有非旱即澇的現象,給主要作物生產帶來非常不利的影響。
  15. They represent a humid and warm climate condition

    昆蟲群落反映的是一種溫暖條件。
  16. In worm and dank southeast hubei, aquosity is a big problem that the traditional dwellings have to be faced with

    摘要溫暖的鄂東南山區,潮是當地傳統民居面臨的一大問題。
  17. The correlativity between theoretical value and the actual value of soil moisture content in 93. 3 percent of observational stations is distinct. all this shows that calculational methods of zndx is more reason for studing the flood or drought of northwest chine. ( 2 ) index _ z and index _ k ca n ' t objectively remark extent of drought and flood event. both ca n ' t distinguish the difference of some years which have the same precipitation and have different temperature, awc

    西北地區10個代表站三種指數值的對比表明, z指數與k指數僅反映西北地區同期的降水,而zndx指數不僅反映了同期降水狀況,且與同期溫及前期度有關。 ( 2 )通過z 、 k與zndx指數對西北地區旱澇等級的對比研究表明, z指數與k指數對西北地區旱澇等級的確定不具有客觀性。
  18. ( 2 ) the analysis by characteristic section planes can draw that the ancient climate in deposit period of the characteristic section plane one sediments ( about seventeen thousand years before present ) is warm - dry and has relative humid and dry evolution rule, from fifteen to thirty years as its evolution period, that the ancient climate in deposit period of the characteristic section plane two sediments ( about fourteen thousand years before present ) is humid and has relative alternate very humid and humid evolution rule, from two to fourteen years as its evolution rule

    ( 2 )通過對兩個典型剖面的綜合分析得出,典型剖面沉積物沉積時期(距今約17kab . p . )的古特徵總體上為暖干,並具有以15 30年為演化周期,相對的-乾燥-的演變規律。典型剖面沉積物沉積時期(距今約14kab . p . )的古總體特徵為,並具有以2 14年為演變周期,相對的很-交替的演化規律。
  19. They liked the cold wet weather there and their number increased year by year

    糜鹿喜歡那裡涼爽,因此它們的數量逐年增長。
  20. In calcutta ' s hot and humid climate , it was easy for them to get sick

    在加爾各答炎熱中,他們很容易得病。
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