Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

SUN Li; BI Shuoben; PAN Wei; CHEN Changchun; XU Zhihui

doi:10.6054/j.jscnun.2019106

Journal of South China Normal University (Natural Science Edition) > 2019 > 51(6): 88-97. > DOI: 10.6054/j.jscnun.2019106

SUN Li, BI Shuoben, PAN Wei, CHEN Changchun, XU Zhihui. Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors[J]. Journal of South China Normal University (Natural Science Edition), 2019, 51(6): 88-97. DOI: 10.6054/j.jscnun.2019106

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Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

1.
School of Geographical Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China
2.
Institute of History of Science and Technology, Nanjing University of Information Science and Technology, Nanjing 210044, China
3.
School of History and Archives, Yunnan University, Yunnan 650091, China

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Received Date: April 23, 2019
Available Online: March 21, 2021

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Abstract

Abstract

Through systematically sorting out the historical data such as the chronicles of prefectures and counties, 1 180 typhoon disasters in the southeast coastal areas during Ming and Qing Dynasties are reconstructued and the frequency sequence of typhoon disasters is established. The temporal and spatial distribution of typhoon disasters in the region and their main factors are analyzed. The results are as follows. The impacts of typhoons concentrate in the coastal areas and decrease from the coastal areas to the inland. The decay of typhoons is a rapid process. The area most seriously affected by the typhoons is South China, of which Guangdong Province suffers the most. The factors for typhoons include temperature changes and sunspot. When temperature changes are stable, the typhoon frequency changes smoothly. The typhoon frequency shows great turbulence when temperature fluctuations are steep. When the sunspot cycle is at a low activity value, the subtropical high pressure moves northward, and the influence of typhoon in the southeast coastal areas increases. When the sunspot cycle enters an active period, the subtropical high pressure moves southward, and the influence of typhoons in the southeast coastal areas decreases.
- Ming and Qing dynasties,
- southeast coastal areas,
- time and space characteristics,
- factors,
- typhoon reconstruction

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References (32)

References

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Reconstructing Typhoons in Southeast Coastal Areas during Ming and Qing Dynasties and Analyzing the Factors

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