Titlebook: Droughts, Floods, and Global Climatic Anomalies in the Indian Ocean World; Philip Gooding Book 2022 The Editor(s) (if applicable) and The

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Palgrave Series in Indian Ocean World Studieshttp://image.papertrans.cn/e/image/282994.jpg

Ceremony

Droughts, Floods, and Global Climatic Anomalies in the Indian Ocean World978-3-030-98198-3Series ISSN 2730-9703 Series E-ISSN 2730-9711

anachronistic

Introduction: Droughts, Floods, and Global Climatic Anomalies in the Indian Ocean World,triggered by global climatic anomalies associated with, for example, the El Ni?o Southern Oscillation, the Indian Ocean Dipole, volcanism, and sunspot activity, are crucial to the conception of the Indian Ocean World. It does so by engaging with the Braudelian concept of ‘deep structure.’ In Indian

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,The Economy of Floods and Inundations in the Southern Song Capital Prefecture Lin’an (Hangzhou) on , were situated on the Zhe River’s northern shore debouching into Hangzhou Bay. They drew their fresh water from a reservoir west of the city, then called West Lake (Xihu 西湖). However, the sedimentation of Hangzhou Bay intensified tidal inundations with ensuing salination, probably also due to clima

歹徒

,Epidemic and Environmental Change in China’s Early Modern Maritime World During the ‘Little Ice Agemensions. Such catastrophes constituted a perpetual problem in China’s past. This chapter analyses potential answers to the question of if significant climate changes, such as the rise or drop of temperatures, decisively influenced typhoons, floods, or droughts, and how these broader climatic anomal

avarice

,The El Nino of 1685–1687 in Golconda and Northern Coromandel, South Asia: Drought, Famine, and Mughclimatic anomalies across South-and-South-East Asia to analyse the impact of the 1685–1687 ENSO in northern Coromandel (South Asia) that coalesced with the Mughal emperor Aurangzeb’s southern campaigns (1682–1707). The chapter argues that while crop failures could often briskly affect non-combatants

inspired

Rainfall and Floods in the Upper Zambezi Basin, 1680s to 1910s,ng northwest to southeast configuration. Long-term average rainfall has been roughly stable for centuries, but conditions in the Indian Ocean, rather than in the Atlantic Ocean, affect variations between years and decades. Written sources exist 1680s–1830s for Angola, whose rivers supply most of the

Malcontent

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The Great Ilocos Flood of 1867,h-century inhabitants of the Ilocos region occurred on 25–27 September 1867. The typhoon sent a huge amount of water rushing down the hills of the Abra Valley. This extraordinary flood, with waters reaching a height of 25 meters (82 feet) above normal level, killed 1800 persons and many thousands mo

Resistance

,El Ni?o and the Human–Environment Nexus: Drought and Vulnerability in Singapore, 1877–1911,7, 1902 and 1911. The narrative focuses on unpacking the nexus of nature-inspired versus human-induced vulnerability to drought within the contexts of colonial urbanisation and looks at the short-to medium-term impacts of the events on society. It also explores how such events inspired new questions