間冰期 的英文怎麼說

中文拼音 [jiānbīng]
間冰期 英文
interglacial epoch
  • : 間Ⅰ名詞1 (中間) between; among 2 (一定的空間或時間里) with a definite time or space 3 (一間...
  • : 期名詞[書面語]1. (一周年) a full year; anniversary 2. (一整月) a full month
  1. This succession was based primarily on a series of deposits and events not directly related to glacial and interglacial periods, rather than on the more usual modern method of studying biological remains found in interglacial beds themselves interstratified within glacial deposits

    這一順序主要是根據與間冰期沒什麼直接關系的一套沉積物或現象而排出的,現代更為通用的方法則是研究發現于間冰期河床的生物化石。
  2. These ice ages are also called glaciations and the periods of relative warmth between them are called interglacials.

    這些也叫,在各的相對溫暖時就叫間冰期
  3. Abrupt changes in earth ' s climate system since last interglacial

    末次間冰期以來地球氣候系統的突變
  4. We do not know whether we live in a postglacial period or an interglacial period

    我們不知道自己是生活在後還是生活于間冰期
  5. Ice age when someone summed up the reason as the earth history to once had and interglacial stage

    有人把原因歸結為地球歷史上曾經有過的間冰期
  6. The same thing happened 11, 000 years ago, just as the current interglacial period began

    1萬1000年前,也就是目前的間冰期剛開始的時候,也發生同樣的狀況。
  7. There is no conclusive evidence about the relative length, complexity, and temperatures of the various glacial and interglacial periods

    還無法確證不同間冰期的相對長度、復雜性及溫度。
  8. In interglacial periods, such as at the present time, the global sea level rose to its present level and higher, and marine sediments were deposited

    幾次間冰期內(目前也正值間冰期) ,全球海平面升至目前或更高水平,並沉積了海洋沉澱物。
  9. Correlation of environmental and climatic change between qaidam basin gamma ray logging curve and guliya ice core 18o record since the last interglacial cycle

    柴達木盆地自然伽瑪曲線與古里雅芯記錄的末次間冰期以來氣候環境變化過程的對比
  10. During the current interglacial interval, co2 concentrations reached the expected peak around 10, 500 years ago and, just as anticipated, began a similar decline

    目前的間冰期,二氧化碳濃度在10500年前達預的高峰,然後也如預的開始下降。
  11. With the uplift of qinghai - xizang plateau and the to - and - fro of the quarternary glaciation and interglaciation, the muscid fauna was distinctly diversified in habitat and vertical zone

    青藏高原的橫空崛起以及第四紀間冰期的循環往復,導致該地區生境千差萬別,使蠅科區系不僅有地域分異,且垂直差異顯著。
  12. Current research projects deals with the influence of climate change and land use, the extent of the last interglacial and other glacier studies, basin analysis, vegetation changes etc

    當今的研究計劃處理氣候變化和土地使用的影響、最後的間冰期和其他河研究的范圍、盆地分析、植物變化等。
  13. The holocene events, therefore, appear to be the most recent manifestation of a pervasive millennial - scale climate cycle operating independently of the glacial - interglacial climate state

    所以,全新世事件似乎是(距今)最近的千年氣候周的傑作。這種常見周(刪- -的運行)是獨立於-間冰期交替氣候的
  14. The most plausible “ new factor ” operating in the climate system during the present interglaciation is farming

    在目前的間冰期,最可能作用於氣候系統的新因素,就是農業。
  15. Although a complex combination of all three orbital cycles controls co2 variations, the trends during previous interglacial intervals were all surprisingly similar to one another

    雖然二氧化碳的變化受到三種軌道周的復雜組合所控制,但先前各個間冰期的趨勢都非常相似。
  16. Why, then, would the gas concentrations have fallen during the last four interglaciations yet risen only during the current one

    那麼,為何過去四個間冰期時,溫室氣體濃度都是下降,卻只有目前是上升的?
  17. The substances making up of loess on the northern slop of tian shan mountains and iii basin are carried by dust storm not only in glacial but in inter - glacial

    形成黃土的粉塵主要是以塵暴方式搬運,且間冰期都有塵暴堆積。
  18. One additional watt per square meter of forcing, over and above that today, will take global temperature approximately to the maximum level of the eemian

    今後的氣候營力每平方公尺只要增加一瓦特,就會使全球氣溫達到艾姆間冰期的最高水準。
  19. The climate of this period is almost as warm and wet as the stage 5e of the last interglacial. the mean temperature is 2 - 4 c higher and the precipitation is much larger than that of the today, the holocene which we live in. while in the climatic records of deep ocean, antarctic and greenland ice - core, marine isotope stage ( mis ) 3 is a weakly warm period, though a little warmer than marine isotope stage ( mis ) 2 and marine isotope stage ( mis ) 4, evidently colder than the last interglacial and holocene favorable period

    末次,即深海氧同位素第3階段的氣候在我國,尤其是青藏高原地區表現出明顯不同於深海沉積物和極地芯記錄的特徵:青藏高原古里雅芯的~ ( 18 ) o曲線表明3階段存在特強夏季風事件,其氣溫和降水接近於末次間冰期5e階段,超過全新世,其暖濕程度已經達到間冰期的程度;而深海氧同位素3階段在深海、南極、格陵蘭芯的氧同位素記錄中均為弱暖,雖較2階段、 4階段溫暖,但顯著低於全新世大暖和末次間冰期
  20. In addition the average sedimentation rate was obviously higher in the interglacial period than in the glacial period in the drilling core ey02 - 1 in the north of mid - shelf

    而東海中陸架北部ey02 - 1孔間冰期時的平均沉積速率明顯高於時的平均沉積速率。
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