间冰期的 meaning in Chinese
interglacial
Examples
- 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
今后的气候营力每平方公尺只要增加一瓦特，就会使全球气温达到艾姆间冰期的最高水准。 - 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
虽然二氧化碳的变化受到三种轨道周期的复杂组合所控制，但先前各个间冰期的趋势都非常相似。 - 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
青藏高原的横空崛起以及第四纪冰期间冰期的循环往复，导致该地区生境千差万别，使蝇科区系不仅有地域分异，且垂直差异显著。 - 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阶段的气候在我国，尤其是青藏高原地区表现出明显不同于深海沉积物和极地冰芯记录的特征：青藏高原古里雅冰芯的~ ( 18 ) o曲线表明3阶段存在特强夏季风事件，其气温和降水接近于末次间冰期5e阶段，超过全新世，其暖湿程度已经达到间冰期的程度；而深海氧同位素3阶段在深海、南极、格陵兰冰芯的氧同位素记录中均为弱暖期，虽较2阶段、 4阶段温暖，但显著低于全新世大暖期和末次间冰期。