全球变化研究

全球变化背景下热带气旋主要变化特征及影响因素

  • 韩岩松 ,
  • 姜伟 ,
  • 肖玉雯 ,
  • 雍阳阳 ,
  • 余克服
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  • 1.广西南海珊瑚礁研究重点实验室/广西大学海洋学院, 广西 南宁 530004
    2.南方海洋科学与工程广东省实验室(珠海), 广东 珠海 519080
韩岩松(1998-),男,甘肃白银人,硕士研究生,主要从事海洋全球变化研究. E-mail:hanyansong1999@163.com
姜伟(1989-),男,河北昌黎人,副教授,主要从事海洋地质与全球变化研究. E-mail:jianwe@gxu.edu.cn

收稿日期: 2022-09-30

  修回日期: 2022-11-30

  网络出版日期: 2023-05-10

基金资助

国家自然科学基金面上项目“南海北部岸礁区海底地下水排泄的高分辨率珊瑚记录”(41976059);国家自然科学基金重点项目“全新世南海珊瑚礁发育的时—空差异及其对全球变暖的适应机制”(42030502)

Main Change Characteristics and Influencing Factors of Tropical Cyclones Under the Background of Global Change

  • Yansong HAN ,
  • Wei JIANG ,
  • Yuwen XIAO ,
  • Yangyang YONG ,
  • Kefu YU
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  • 1.Guangxi Laboratory on the Study of Coral Reefs in the South China Sea/School of Marine Sciences, Guangxi University, Nanning 530004, China
    2.Southern Marine Science and Engineering;Guangdong Laboratory (Zhuhai), Zhuhai Guangdong 519080, China
HAN Yansong (1998-), male, Baiyin City, Gansu Province, Master student. Research area includes ocean global change. E-mail: hanyansong1999@163.com
JIANG Wei (1989-), male, Changli City, Hebei Province, Associate professor. Research areas include marine geology and global change. E-mail: jianwe@gxu.edu.cn

Received date: 2022-09-30

  Revised date: 2022-11-30

  Online published: 2023-05-10

Supported by

the National Natural Science Foundation of China “High-resolution coral records of submarine groundwater discharge in the fringing reefs of the northern South China Sea”(41976059);“The spatial and temporal variations of Holocene coral reef development in the South China Sea and their significance on corals’ adaptation to global warming”(42030502)

摘要

热带气旋是可以影响全球中低纬度海域的气象现象。系统总结和回顾了国内外热带气旋的主要特征、潜在影响因素及影响机制的相关研究进展,并对其在全球变化背景下的变化趋势进行了总结和剖析。全球变暖以来,热带气旋的源地和路径都出现极移的趋势,移动速度略有增加,频率减小并且强度增大,但各大洋存在显著差异。重点回顾了火山活动、厄尔尼诺—南方涛动和太平洋年代际振荡、太阳辐射、热带辐合带以及气溶胶等因素对热带气旋的影响。其中,火山喷发导致平流层存在大量气溶胶,通过降低海表温度对热带气旋产生消极影响,但这种机制存在地域性差异;厄尔尼诺—南方涛动和太平洋年代际振荡以遥相关的方式调制全球热带气旋活动;太阳辐射和热带辐合带的变化与热带气旋频数存在相关性;气溶胶对不同发展阶段的热带气旋存在相反的影响机制。由于器测热带气旋数据在时间长度上和大部分替代指标在分辨率上的不足,严重制约了全球变化背景下热带气旋潜在影响因素的研究。未来可以通过寻找高分辨率记录载体来量化热带气旋活动历史,进一步解析热带气旋与潜在影响因素的关系,完善在气候波动影响下热带气旋活动的变化机制。

本文引用格式

韩岩松 , 姜伟 , 肖玉雯 , 雍阳阳 , 余克服 . 全球变化背景下热带气旋主要变化特征及影响因素[J]. 地球科学进展, 2023 , 38(5) : 515 -532 . DOI: 10.11867/j.issn.1001-8166.2022.079

Abstract

Tropical Cyclones (TCs) are meteorological phenomena that affect middle and low latitudes worldwide. This paper systematically summarizes and reviews the research progress on the main characteristics, potential influencing factors, and influencing mechanisms of TCs at home and abroad, and summarizes and analyzes their changing trends under the climate background of GW. With the significant increase in global temperature, the sources and tracks of global TCs have shifted poleward, with a slight increase in translation speed, decrease in frequency, and increase in intensity; however, there are significant differences in each ocean. This paper focuses on reviewing the effects of volcanic activity, El Ni?o-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), solar radiation, Intertropical Convergence Zone (ITCZ), and aerosols on TC activity. Volcanic eruptions release a large amount of aerosols in the stratosphere, thereby reducing sea surface temperature and negatively affecting TCs. However, there are regional variations in this mechanism. ENSO and PDO modulate the global TC activity through teleconnections, while changes in solar activity and ITCZ are also associated with TC activity. Aerosols have opposite influence mechanisms on TCs at different development stages. Due to the lack of time length and the coarse resolution of most surrogate indicators of instrumental TC data, research on the impact of potential influencing factors on TCs under long-term climate fluctuations is severely restricted. In the future, we should be able to quantify the history of storm activities by finding high-resolution record carriers, thereby further analyzing the relationships between TCs and potential influencing factors, and improving our understanding of the change mechanism in TC activity under the influence of climate fluctuations.

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