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1.Researches on Coastal Storm Surge Frequency during the Warm Period of Middle Holocene in Middle Jiangsu Province
江苏中部海岸全新世中期温暖期风暴潮频率的研究收藏指正
2.Study on the transition form ! Dark Ages" to Medieval Warm Period will provide us some valuable references to understand the climate change from Little Ice Age to the 20th Century warming.
气候总是在冷暖波动中前进的, 结合紧随其后的中世纪暖期(MWP), 由“Dark Ages”向“MWP”的过渡可以为认识由小冰期(LIA)向20世纪全球变暖的转变提供借鉴.收藏指正
3.So, it can be concluded that sand drift activity and aeolian landform forming are mainly taking place in warm dry period.
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。收藏指正
4.the mid-Holocene(8 240～3 200 cal.aBP),which was warm and wet in early period and cool and dry in late period;
aBP,中全新世较为暖湿期,年代为8240-3200 cal.收藏指正
5.The source of the Tsushima Warm Current during the period of June, 1986 to December, 1988 has been primarily studied with a two dimensional numerical model. The simulation results show three basic patterns for the source of the Tsushima Warm Current: 1. the water of the Tsushima Warm Current in the East China Sea is composed mainly of the part of the Kuroshiogoing northward;
本文通过二维数值模拟对1986年6月～1988年12月东海对马暖流水的来源问题进行了初步探讨,结果得出东海对马暖流水的来源基本上分为三种类型:(1)东海对马暖流水主要为东海黑潮水继续北上部分构成;收藏指正
6.お?he bigger amplitude anomalies of Tainan warm spring well outflow in three period for 13 years are presented in detail, which responded to four earthquakes of ?M??s 4.6～6.3 occurred in 1°×1° in the south Yellow Sea.
江苏省东台市台南温泉井13年来共有三个时段的流量有较大幅度的异常都对应了南黄海一平方度内发生的4次4?6～6?3级地震。收藏指正
7.the thickness of South China Sea warm pool reaches 55 m in its strong period, its main axis is from southwest to northeast and locates alone the steep slope area of west off shore of North Kalimantan Palawan island;
在南海暖池盛期，其高于28℃的暖水最大厚度达55m，暖池轴线呈西南一东北向，主轴位于北加里曼丹－马拉望岛西侧海域陡坡区：南海暖池、西太平洋暖池和印度洋暖池处于同一大尺度海气耦合系统中，有4．8年左右的长周期振荡；收藏指正
8.Object: observed the clinic effect of warm needling, which treated the arteriosclotic cerebral infarction(ACI) patients of the acute period and convalescence .
目的：观察了温针灸治疗风痰瘀阻型动脉硬化性脑梗死(arteriosclotic cerebral infarction)急性期及恢复期的临床疗效。收藏指正
9.Comparison and study of the biotic characters in the Jinggu and Longchuan basins in Yunnan Province show that: (1)the two basins underwent the developing period, expanding period and shrinking period from early Miocene Epoch to Pliocene Epoch; (2)the climate in the region was dry in early Miocene Epoch, warm and humid in middle-late Miocene Epoch and dry in Pliocene period; (3)the basins expanding in middle-late Miocene Epoch formed a semi-deep-lake to deep-lake environment.
通过对云南景谷盆地及陇川盆地新生代生物群特征的对比，探讨了新生代两大盆地环境演变：早中新世到上新世为湖盆发展期→湖盆扩大→萎缩期，气候为早期的千燥→中新世早期的温暖湿润→中新世中晚期的寒冷阴湿→上新世的干燥，而中新世中晚期湖盆的扩大形成的半深湖－深湖环境为油气的形成提供了有利条件。收藏指正
10.Abstract: Comparison and study of the biotic characters in the Jinggu and Longchuan basins in Yunnan Province show that: (1)the two basins underwent the developing period, expanding period and shrinking period from early Miocene Epoch to Pliocene Epoch; (2)the climate in the region was dry in early Miocene Epoch, warm and humid in middle-late Miocene Epoch and dry in Pliocene period; (3)the basins expanding in middle-late Miocene Epoch formed a semi-deep-lake to deep-lake environment.
文摘:通过对云南景谷盆地及陇川盆地新生代生物群特征的对比，探讨了新生代两大盆地环境演变：早中新世到上新世为湖盆发展期→湖盆扩大→萎缩期，气候为早期的千燥→中新世早期的温暖湿润→中新世中晚期的寒冷阴湿→上新世的干燥，而中新世中晚期湖盆的扩大形成的半深湖－深湖环境为油气的形成提供了有利条件。收藏指正
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