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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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;
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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