間冰期的 的英文怎麼說
中文拼音 [jiānbīngqīde]
間冰期的
英文
interglacial-
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冰川期和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。These ice ages are also called glaciations and the periods of relative warmth between them are called interglacials.
這些冰期也叫冰河期,在各冰期間的相對溫暖時期就叫間冰期。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冰期和間冰期。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。There is no conclusive evidence about the relative length, complexity, and temperatures of the various glacial and interglacial periods
還無法確證不同冰川期與間冰期之間的相對長度、復雜性及溫度。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冰芯記錄的末次間冰期以來氣候環境變化過程的對比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年前達預期的高峰,然後也如預期的開始下降。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冰期間冰期的循環往復,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。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冰河研究的范圍、盆地分析、植物變化等。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)最近的千年氣候周期的傑作。這種常見周期(刪- -的運行)是獨立於冰期-間冰期交替氣候的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。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期的復雜組合所控制,但先前各個間冰期的趨勢都非常相似。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?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,且冰期和間冰期都有塵暴堆積。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。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
末次冰期中期,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冰芯記錄的特徵:青藏高原古里雅冰芯的~ ( 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、格陵蘭冰芯的氧同位素記錄中均為弱暖期,雖較2階段、 4階段溫暖,但顯著低於全新世大暖期和末次間冰期。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冰期時的平均沉積速率。Over the past three million years, these regular changes in the amount of sunlight reaching the planet ' s surface have produced a long sequence of ice ages ( when great areas of northern hemisphere continents were covered with ice ) separated by short, warm interglacial periods
過去300萬年間,陽光抵達地表的規律變化造就了一系列的冰期(北半球陸地大部份都由冰覆蓋) ,間隔著短暫、溫暖的間冰期。During the quaternary period, spanning the last 2 million years, major glaciations in polar regions affected global sea level, which fell to 120metres below present level, leaving the site of present - day hong kong as much as 130 kilometres from the coast
長達200萬年的第四紀期間,全球海平面受到兩極地區幾次大冰期的影響,曾下降至現時海平面之下120米,當時的海岸線離開現時本港海岸達130公里。分享友人