Altman Jan, Ukhvatkina Olga N, Omelko Alexander M, Macek Martin, Plener Tomas, Pejcha Vit, Cerny Tomas, Petrik Petr, Srutek Miroslav, Song Jong-Suk, Zhmerenetsky Alexander A, Vozmishcheva Anna S, Krestov Pavel V, Petrenko Tatyana Y, Treydte Kerstin, Dolezal Jiri
Institute of Botany, Czech Academy of Sciences, 252 43 Pruhonice, Czech Republic;
Research Unit Forest Dynamics, Swiss Federal Institute for Forest, Snow and Landscape Research WSL, CH-8903 Birmensdorf, Switzerland.
Proc Natl Acad Sci U S A. 2018 Nov 6;115(45):11543-11548. doi: 10.1073/pnas.1808979115. Epub 2018 Oct 22.
Determination of long-term tropical cyclone (TC) variability is of enormous importance to society; however, changes in TC activity are poorly understood owing to discrepancies among various datasets and limited span of instrumental records. While the increasing intensity and frequency of TCs have been previously documented on a long-term scale using various proxy records, determination of their poleward migration has been based mostly on short-term instrumental data. Here we present a unique tree-ring-based approach for determination of long-term variability in TC activity via forest disturbance rates in northeast Asia (33-45°N). Our results indicate significant long-term changes in TC activity, with increased rates of disturbances in the northern latitudes over the past century. The disturbance frequency was stable over time in the southern latitudes, however. Our findings of increasing disturbance frequency in the areas formerly situated at the edge of TC activity provide evidence supporting the broad relevance of poleward migration of TCs. Our results significantly enhance our understanding of the effects of climate change on TCs and emphasize the need for determination of long-term variation of past TC activity to improve future TC projections.
确定长期热带气旋(TC)变化对社会具有极其重要的意义;然而,由于各种数据集之间存在差异以及仪器记录的时间跨度有限,人们对热带气旋活动的变化了解甚少。虽然此前已利用各种代用记录在长期尺度上记录了热带气旋强度和频率的增加,但其向极地迁移的确定大多基于短期仪器数据。在此,我们提出一种独特的基于树木年轮的方法,通过东北亚(北纬33 - 45°)的森林干扰率来确定热带气旋活动的长期变化。我们的结果表明热带气旋活动存在显著的长期变化,过去一个世纪北纬地区的干扰率有所增加。然而,南纬地区的干扰频率随时间保持稳定。我们发现在以前位于热带气旋活动边缘的地区干扰频率增加,这为热带气旋向极地迁移的广泛相关性提供了证据支持。我们的结果显著增强了我们对气候变化对热带气旋影响的理解,并强调需要确定过去热带气旋活动的长期变化,以改进未来热带气旋的预测。