间冰期的

基本解释 (translations)

interglacial

与间冰期的相关的网络例句 [注：此内容来源于网络，仅供参考]

The tuned Brunhes/Matuyama paleomagnetic polarity reversal agrees well with an age of 0.78 Ma dated previously. The tuned ages for several planktonic foraminifer Mo-events also agree well with published dates, and new ages for some other bin events in the South China Sea are also estimated.

调谐结果显示，1143站190.77m、191个冰期、间冰期的深海沉积记录了5.02Ma的南海古海洋学历史；1143站布容／松山磁性反转事件的年龄为0.78Ma，与前人研究结果一致；15个识别出的浮游有孔虫生物事件年龄部分与已经发表过的年龄相吻合，部分为该生物事件在南沙海区的新年龄。

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。

We suggested that, in the last 130ka, the prominently lake expanding period i.e. the pan-lake period, probably have come into being at MIS5e、MIS5c、MIS5a、 MIS3c、MIS3a, corresponding to high summer solar radiation stages of middle and low latitude in northern Hemisphere, which were in phased with 20ka-cycle. MIS5e was the warmest and wettest stage of the last interglacial, and the other stages were the interstadial of the last interglacial.

对青藏高原及上述诸地区末次间冰期以来气候记录的对比分析揭示：末次间冰期以来，青藏高原湖泊淡化、湖面显著扩涨期，即泛湖期，可能对应于MIS5e、MIS5c、MIS5a、MIS3c、MIS3a，即末次间冰期各暖湿期，末次冰期间冰阶；其分别产生于北半球中、低纬度夏季高太阳辐射阶段，具有准20ka周期演化特征，夏季风降水是造成湖泊扩涨的控制因素。

Theδ〓O fluctuation showed that during the Last Glaciation there existed at least seven warm and five cold climatic fluctuations or events in the east Tibetan plateau, and that during the Last Interglacial Age there existed clearly 5 climatic substages, namely 5a to 5e, among which substage 5e was the warmest climate period, but 5a was an optimum episode of moisture and heat combination.

对末次间冰期及末次冰期气候特征研究表明，青藏高原东部末次间冰期内部存在着5个十分清晰的气候亚期，其中5a、5c、5e三次暖事件以5e温度最高，但水热配置最好的是5a。

Although significant uncertainties remain about both the cause and the scale of the impact of these abrupt climatic events, there is growing general knowledge of change process in climate during the past 13 000 years based on the studies of some important rapid climatic oscillations, such as a cold and dry event near the middle of the last interglacial, Dansgaard-Oeschger cycles, Heinrich events and Younger Dryas event during the last glacial and some cooling events during the Holocene.

尽管末次间冰期以来这些数百年－千年时间尺度气候突变事件的成因和影响范围还存在明显的不确定性，但已从诸如末次间冰期(MIS 5e)中期的干冷事件、末次冰期的Dansgaard-Oeschger旋回、Heinrich事件和Younger Dryas事件以及发生在全新世冰后期的一些降温事件的研究中。获得对过去130ka来气候变化过程总体上的认识知理解。

They have several meters of paleosol developed on the top of overbank silt, suggesting that the abandonment of each terrace due to river incision occurs during the transition from glacial to interglacial climates and there may be a link between the production of terraces and glacial-interglacial climatic cycles. However, it is not every glacial-interglacial transition during the last 1,240ka that terrace can form and preserve.

黄河各阶地河漫滩顶部都有一层古土壤发育表明黄河下切形成阶地发生在古土壤开始发育的冰期向间冰期的过度阶段，但是并非1，240ka以来的每次冰期—间冰期的气候交替都能引起黄河下切形成阶地。

In 1956 Gilbert Plass was heir to a century of work that identified variations in the trace amounts of carbon dioxide in the atmosphere as a possible cause of ice ages and interglacial periods.

1956年的吉尔伯特·普拉斯深受一个世纪以来科学工作的影响，当时认为大气中微量二氧化碳的变化是引起冰川期和间冰期的因素之一。1861年约翰·丁达尔写道，大气中任何有放射活性的物质（水蒸气、二氧化碳、臭氧或烃类）数量发生微小的变化，都可能引起&地质研究所发现的各种气候变化……它们是真正的原因，只是有多大范围的影响还存在疑问。&

The down core changes of Florisphaera profunda percentage content implied that the thermocline was shallower in glacial periods and deeper in interglacial periods, which might be the direct controlling factors of WPWP productivity changes. It is speculated that the glacial-interglacial fluctuation of the depth of thermocline was induced by the super-ENSO variation.

钙质超微化石下透光带属种Florisphaeva profunda百分含量指示的温跃层深度变化表明冰期温跃层浅、间冰期温跃层加深，这说明类ENSO式变化导致的冰期-间冰期温跃层深度波动可能是MIS7期以来暖池核心区古生产力在冰期高而在间冰期显著降低的直接控制因素。

This paper presents the high-resolution sequence of vegetation change of the last inter-glacial period in Xishan Mountain,Beijing by pollen analysis and thermoluminescent dating technology with reconstruction of the palaeo-vegetation and palaeo-environment of this region.

末次冰期—间冰期气候旋回研究是过去的全球变化研究的三大重点之一，通过孢粉分析和热释光断代建立了北京西山末次间冰期植被的演化序列，研究了该地区古植被与古环境的演化规律。

These ice ages are also called glaciations and the periods of relative warmth between them are called interglacials.

这些冰期也叫冰河期，在各冰期间的相对温暖时期就叫间冰期。

与间冰期的相关的网络解释 [注：此内容来源于网络，仅供参考]

interformational foliation：层间面理

interferometry 干涉量度法 | interformational foliation 层间面理 | interglacial 间冰期的

glacial period：冰期

两个冰期(glacial period)之间的时期,称为间冰期. 间冰期的气候较冰期温暖,因此冰川融化退缩,海面上升. 间冰期的时间也长於冰期,通常说,更新世(pleistocene)有四个冰期和三个间冰期,目前我们的时代为后冰期,若在未来又有一次冰期,则我们这个时代也是个间冰期了

interglacial：间冰期的

intergeneric 属间的 | interglacial 间冰期的 | intergradation 间渡

interglacial period：间冰期

俄罗斯真理报(Pravda)报导,科学家根据南极冰河冰核、海洋沉积物、地质纪录分析和古生物研究,发现地球气候有循环模式,约10万年的冰河期结束后,就进入约1万2000年的间冰期(interglacial period),然后再变冷,进入另一个冰河期.

interglacial epoch：间冰期

它提供相当多种类的金属与非金属矿...时间第四纪大冰期的全球性冰川活动约从距今200万年前开始直到现在,是地质史上距今最近的一次大冰期. 在这次大冰期中,气候变动很大,冰川有多次进退,分别被称为冰期(glacial epoch)和间冰期(interglacial epoch). 第四纪大冰期比以前的冰...

intergradation：间渡

interglacial 间冰期的 | intergradation 间渡 | intergrade 逐渐合一

intergranular：间粒状的

interglacial epoch 间冰期 | intergranular 间粒状的 | intergranular diffusion 粒间扩散

interstadial：小间冰期的

小间冰期 interstade | 小间冰期的 interstadial | 小间断 diastem

interglobular：球间

interglacial 间冰期的 | interglobular 球间 | intergroove 间沟

Sangamon：散加蒙间冰期

Sandusky 桑达斯基 | Sangamon 散加蒙间冰期 | Sanskrit 梵语的