Articles | Volume 20, issue 11
https://doi.org/10.5194/cp-20-2455-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-20-2455-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Nov 2024
Research article |
| 08 Nov 2024
| 08 Nov 2024
Processes, spatial patterns, and impacts of the 1743 extreme-heat event in northern China: from the perspective of historical documents
Le Tao
Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China
Key Laboratory of Environmental Change and Natural Disaster, Ministry of Education, Beijing Normal University, Beijing, 100875, China
Yun Su
CORRESPONDING AUTHOR
Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China
Key Laboratory of Environmental Change and Natural Disaster, Ministry of Education, Beijing Normal University, Beijing, 100875, China
Xudong Chen
Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China
Key Laboratory of Environmental Change and Natural Disaster, Ministry of Education, Beijing Normal University, Beijing, 100875, China
Fangyu Tian
Faculty of Geographical Science, Beijing Normal University, Beijing, 100875, China
Key Laboratory of Environmental Change and Natural Disaster, Ministry of Education, Beijing Normal University, Beijing, 100875, China
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The Thirty Years' War (from 1618 to 1648 CE), an armed military conflict in Europe, brought extensive devastation to Europe. The paper analyses annual and seasonal temperature, precipitation, and drought patterns, as well as severe weather extremes, based particularly on documentary data, during this event in central Europe to demonstrate their broad impacts on human society and human responses in coincidence with weather and climate during this period of hardship.
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Gregory Burris, Jane Washburn, Omar Lasheen, Sophia Dorribo, James B. Elsner, and Ronald E. Doel
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Jingyun Zheng, Yingzhuo Yu, Xuezhen Zhang, and Zhixin Hao
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We investigated the decadal variations of extreme droughts and floods in North China using a 17-site seasonal precipitation reconstruction from a unique historical archive. Then, the link of extreme droughts and floods with ENSO episodes and large volcanic eruptions was discussed. This study helps us understand whether the recent extreme events observed by instruments exceed the natural variability at a regional scale, which may be useful for adaptation to extremes and disasters in the future.
Alvaro Guevara-Murua, Caroline A. Williams, Erica J. Hendy, and Pablo Imbach
Clim. Past, 14, 175–191, https://doi.org/10.5194/cp-14-175-2018, https://doi.org/10.5194/cp-14-175-2018, 2018
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This study reconstructs a new semi-quantitative rainfall index for the Pacific coast of Central America using documentary sources for the period 1640 to 1945. In addition, we explore the various mechanisms and processes that may explain inter-annual and inter-decadal rainfall variability over the Pacific coast of Central America.
Feng Shi, Sen Zhao, Zhengtang Guo, Hugues Goosse, and Qiuzhen Yin
Clim. Past, 13, 1919–1938, https://doi.org/10.5194/cp-13-1919-2017, https://doi.org/10.5194/cp-13-1919-2017, 2017
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We reconstructed the multi-proxy precipitation field for China over the past 500 years, which includes three leading modes (a monopole, a dipole, and a triple) of precipitation variability. The dipole mode may be controlled by the El Niño–Southern Oscillation variability. Such reconstruction is an essential source of information to document the climate variability over decadal to centennial timescales and can be used to assess the ability of climate models to simulate past climate change.
Rudolf Brázdil, Ladislava Řezníčková, Hubert Valášek, Lukáš Dolák, and Oldřich Kotyza
Clim. Past, 12, 1361–1374, https://doi.org/10.5194/cp-12-1361-2016, https://doi.org/10.5194/cp-12-1361-2016, 2016
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The paper deals with climatic and human impacts of the strong Tambora (Indonesia) volcanic eruption in April 1815 over the Czech Lands territory based on analysis of documentary data and instrumental records. While climatic effects were related particularly to summers 1815 and 1816 (1816 is known as "a Year Without Summer"), quite important were societal impacts represented after bad harvest by steep increase in prices and shortages of food.
C. Camenisch
Clim. Past, 11, 1049–1066, https://doi.org/10.5194/cp-11-1049-2015, https://doi.org/10.5194/cp-11-1049-2015, 2015
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This paper applies the methods of historical climatology to present a climate reconstruction for the area of the Burgundian Low Countries during the 15th century. The results are based on documentary evidence. Approximately 3000 written records derived from about 100 different sources were examined and converted into seasonal seven-degree indices of temperature and precipitation.
A. Guevara-Murua, C. A. Williams, E. J. Hendy, A. C. Rust, and K. V. Cashman
Clim. Past, 10, 1707–1722, https://doi.org/10.5194/cp-10-1707-2014, https://doi.org/10.5194/cp-10-1707-2014, 2014
A. J. Berland, S. E. Metcalfe, and G. H. Endfield
Clim. Past, 9, 1331–1343, https://doi.org/10.5194/cp-9-1331-2013, https://doi.org/10.5194/cp-9-1331-2013, 2013
O. Wetter and C. Pfister
Clim. Past, 9, 41–56, https://doi.org/10.5194/cp-9-41-2013, https://doi.org/10.5194/cp-9-41-2013, 2013
H. Castebrunet, N. Eckert, and G. Giraud
Clim. Past, 8, 855–875, https://doi.org/10.5194/cp-8-855-2012, https://doi.org/10.5194/cp-8-855-2012, 2012
F. S. Rodrigo, J. J. Gómez-Navarro, and J. P. Montávez Gómez
Clim. Past, 8, 117–133, https://doi.org/10.5194/cp-8-117-2012, https://doi.org/10.5194/cp-8-117-2012, 2012
O. Wetter and C. Pfister
Clim. Past, 7, 1307–1326, https://doi.org/10.5194/cp-7-1307-2011, https://doi.org/10.5194/cp-7-1307-2011, 2011
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Short summary
Our study collected 63 historical documents on the extreme heat of 1743 from three kinds of historical materials. Using text analysis methods, such as keyword extraction, grading, and classification, we reconstructed the 1743 extreme heat event. This heat event developed cumulatively, and the key areas affected are consistent with those impacted in modern times. Timely cooling and reducing exposure have been limited but necessary means of addressing extreme heat in both ancient and modern times.
Our study collected 63 historical documents on the extreme heat of 1743 from three kinds of...
