• 1850年后,随着现代暖期的开始,全球气温开始缓慢上升。

    Global temperatures began to rise slowly after 1850, with the beginning of the Modern Warm Period.

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  • 我们有过暖期和小冰期;但是变化很小。

    We have had warm periods and little ice ages; but the changes have been small.

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  • 最暖期不是在中全新世,而是在晚全新世。

    The warmest stage was not in Middle Holocene but in Late Holocene.

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  • 从偏冷期到偏暖期,整个热带对流层顶显著变暖。

    The whole tropical tropopause has been warmed up from cold period to warm period.

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  • 他也承认有关中世纪暖期是否比当前阶段更暖的争论还没有定论。

    And he agreed that the debate had not been settled over whether the Medieval warm period was warmer than the current period.

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  • 暖期海洋沉积层样品因含钙微生物在酸性海洋中溶解而呈灰色。

    Warm periods were marked by gray layers in the ocean sediments caused by the calcium-containing microorganisms dissolving into acidic oceans.

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  • 最近的暖期已导致冰川数量从1850年的150个下降到今天的26个。

    The latest warm period has caused the number of glaciers to decrease from 150 in 1850 to 26 today.

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  • 结果显示本区气候总体冷期易旱、暖期易涝,显示季风气候区的特征。

    It is revealed that droughts often occur in the cold periods while floods in the warm, indicating the monsoon climate change.

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  • 许多地质特征像峡谷,干涸的湖和河渠道,显示出了在遥远的过去,可能是火星的暖期有水流流动。

    Many geological features like canyons, dried-up lakes and river channels point to the flow of liquid water in the distant past when Mars may have been warmer.

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  • 由于河流阶地是间歇性新构造抬升的产物,其形成阶段又与气候的冷暖变化相关,即冷期阶地陡坎形成,暖期阶地堆积物形成。

    Because the river terrace is the result of interrupting neotectonic uplift and its forming stages are bound up with the geologic climate cold warm changes, I.

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  • Swetnam博士的工作表明,在气象学家所说的中世纪暖期,即公元900年到1300年,气温的变动和火灾的频率密切相关。

    Dr Swetnam's work suggests that variations in temperature were well correlated with the frequency of fire during what climatologists call the medieval warm period, from 900 to 1300.

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  • 公元前9000年到5000年这段时期被称为全新世气候暖期(Holocene ClimateOptimum),这种气候就像地中海海滨的温暖午后一样惬意。

    The time from 9, 000 to 5, 000 BC is called the Holocene Climate Optimum, which makes it sound like a nice afternoon on a Mediterranean beach.

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  • 冰冻期地面高程等于原地面暖土高程与冻胀量之和。 分析了冻土与暖土高程混用对工程建设的不良结果。

    Some bad results for engineering project have been analyzed due to the mixed usage of altitudes in freezing and warm period.

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  • 可见,区内风沙活动及风成景观的塑造过程,主要是在暖干期进行的。

    So, it can be concluded that sand drift activity and aeolian landform forming are mainly taking place in warm dry period.

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  • 地球历史上曾经出现过的某段暖温期,被认为是地球未来气候可能的写照。

    A warm period in Earth's past thought to be a possible analog to Earth's climate future wasn't stuck in a permanent El nin.

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  • 二者年际变化的负相关关系在长期趋势的冷位相期不显著,而在暖位相期显著。

    The negative correlation between the interannual variability of IODM and that of SCS summer monsoon is significant during the warm phase of long-term trend but insignificant during the cool phase.

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  • 丙二醛(MDA)含量随生育期的推移积累速度也较暖型大豆明显为慢。

    MDA content accumulation rate was slower than warm soybean with the growth moved.

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  • 冷型大豆绿叶功能期均长于暖型大豆,叶片衰老进程也较暖型大豆迟缓;

    The functional period of leaf of cold soybean was longer than warm soybean, and the cosenescence progress of leaf was also slower than warm soybean;

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  • 冷型大豆绿叶功能期均长于暖型大豆,叶片衰老进程也较暖型大豆迟缓;

    The functional period of leaf of cold soybean was longer than warm soybean, and the cosenescence progress of leaf was also slower than warm soybean;

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