中文摘要：

活动吸引了的台风(热带气旋) 的最近的增加它是否被连接到到著名多十的可变性的一个活跃阶段的全球温暖或仅仅回来的大兴趣和导致的激烈的争论。由于短仪器的记录，我们的知识在台风产生，开发，和进化的多相过程和机制上是相当少见的，为特别稀罕却高度破坏超级台风。扩大台风活动记录的时间跨度因此是很重要的。Paleotempestology，出现在 1990 年代初的一门年轻科学，通过地质的代理和历史的记录片的使用在仪器的时代前跨越几个世纪到几千年的研究过去台风活动记录。这篇论文在代理技术开发和应用与一个重音在主要研究进展和 paleotempestology 的调查结果上论述简短评论和合成。方法论由集成微化石，沉积器官的元素的比率，和稳定的同位素从单个地质的代理一直在演变到多代理技术，和典型沉积质地和结构，为暴风雨存款的诊断。一种最新开发的代理技术正在采用在种诊断台风雨水影响的树戒指，洞石笋，和礁石珊瑚的薄片保存的氧同位素。历史的记录片记录系统地被编了并且分析了重建在一些区域的台风活动的历史。在台风频率和 Holocene 气候(温度) 之间的一种简单线性关系改变的在那里不存在的提取台风代理数据表演。台风活动应该与 ENSO 变化有一个世俗、经常的连接，因为更多的台风和飓风在中国做 landfalls，中央并且北美洲在拉·尼娜年期间比 El Nino 年。这发现与那源于最近的仪器的数据一致。在副热带的高度的位置的移动对暴风雨轨道，而是他们的长期的关系施加大影响仍然不好被理解。所有这些调查结果在在全球温暖的情形下面投射台风趋势是重要的。在 paleotempestology 的未来开发应该加强下列研究领域：(1 ) 代理产生机制和保藏潜力，(2 ) 不同代理数据内部确认，(3 ) 暴风雨和海啸的识别扔，(4 )paleo 台?

英文摘要：

The recent increase in typhoon （tropical cyclone） activity has attracted great interest and induced heated debates over whether it is linked to global warming or only a return to an active phase of the well-known multi-decadal variability. Due to the short instrumental record, our knowledge is quite scarce on the complex processes and mechanism of typhoon generation, development, and evolution, especially for the rare but highly destructive super-typhoons. It is therefore very important to extend the time span of typhoon activity records. Paleotempestology, a young science that emerged in the early 1990s, studies past typhoon activity spanning several centuries to millennia before the instrumental era through the use of geological proxies and historical documentary records. This paper presents a brief review and synthesis on the major research advances and findings of paleotempestology with an emphasis on proxy technique development and applications. The methodology has been evolving from single geologic proxy to multi-proxy techniques by integrating microfossils, sedimentary organic elemental ratios, and stable isotopes, together with typical sedimentary textures and structures, for the diagnosis of storm deposits. A newly-developed proxy technique is employing oxygen isotopes preserved in growing laminae of tree rings, cave stalagmites, and reef corals to diagnose typhoon rainwater impacts. Historical documentary records have been systematically compiled and analyzed to reconstruct the history of typhoon activity in some regions. The extracted typhoon-proxy data show that there does not exist a simple linear relationship between typhoon frequency and Holocene climate （temperature） change. Typhoon activity should have a secular and constant linkage with ENSO fluctuations, in that more typhoons and hurricanes make landfalls in China, Central and North America during La Ni~↑na years than El Ni~↑no years. This finding is consistent with that derived from recent instrumental data. Shifts in positions of