The ‘4.2 ka drought event’ and the fall of the Harappan Civilization: A critical review

IF 16.4 1区 化学 Q1 CHEMISTRY, MULTIDISCIPLINARY Accounts of Chemical Research Pub Date : 2024-09-03 DOI:10.1016/j.revpalbo.2024.105187
Tarannum Jahan , Mohammad Firoze Quamar
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Abstract

The role of climate variability in the expansion and collapse of the Harappan Civilization in South Asia has been a subject of intense research and debate among archaeologists, Quaternary climate scientists, meteorologists, climatologists, historians, geographers, archaeobotanists, and anthropologists. Moreover, high-resolution palaeoclimatic studies have challenged the previous perspectives attributing societal collapses solely to socio-political and economic factors. These studies have revealed that periods of abundant rainfall, resulting from climate amelioration and/or due to seasonality: Winter vs. Summer precipitation, often coincided with the peak of socio-economic, cultural, and technological advancements in various civilizations. Conversely, abrupt climatic changes or rapid climatic changes, such as prolonged droughts, led to the destruction of irrigation systems, agricultural devastation, and widespread famines. These climatic disruptions triggered cultural adaptations, migrations, and sometimes even the collapse of entire civilizations. Climate forcing, particularly solar variability, played a primary role in repeated societal displacements, migrations, and deurbanization across different regions in the past. Additionally, the intensified El Niño-Southern Oscillation, a shift of the Indian Ocean Dipole to a strong negative state, and the southward migration of the Inter-Tropical Convergence Zone contributed to an extended period of weakened Summer Monsoons of South Asia and increased aridity. This depletion of water resources triggered the general demographic shift vis-à-vis the 4.2 ka event. The displacement was a response to a weakened Summer Monsoons of South Asia. In this research review article, we aim to understand the role of climate variability and explore the complex socio-climatological linkages in the mysterious displacement of once-thriving, highly advanced, widespread, and urbanized Harappan Civilization at the 4.2 ka.

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4.2 ka干旱事件 "与哈拉帕文明的衰落:批判性评论
气候变异在南亚哈拉帕文明的扩张和崩溃中所扮演的角色一直是考古学家、第四纪气候科学家、气象学家、气候学家、历史学家、地理学家、考古植物学家和人类学家激烈研究和争论的主题。此外,高分辨率古气候研究对以往将社会崩溃完全归因于社会政治和经济因素的观点提出了挑战。这些研究表明,气候改善和(或)季节性因素导致了降雨量丰富的时期:冬季降水量与夏季降水量的对比往往与各种文明的社会经济、文化和技术进步的高峰期相吻合。相反,气候突变或气候急剧变化(如长期干旱)则会导致灌溉系统被破坏、农业遭到破坏以及大范围的饥荒。这些气候破坏引发了文化适应、迁徙,有时甚至导致整个文明的崩溃。气候强迫,特别是太阳变率,在过去不同地区反复出现的社会迁移、移民和非城市化中发挥了主要作用。此外,厄尔尼诺-南方涛动的加剧、印度洋偶极子向强负状态的转移以及热带辐合带的南移,导致南亚夏季季风长期减弱,干旱加剧。水资源的枯竭引发了相对于 4.2 ka 事件的人口迁移。人口迁移是对南亚夏季季风减弱的回应。在这篇研究综述文章中,我们旨在了解气候多变性的作用,并探讨 4.2 ka 期间曾经繁荣、高度发达、广泛分布和城市化的哈拉帕文明神秘迁移过程中复杂的社会-气候联系。
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来源期刊
Accounts of Chemical Research
Accounts of Chemical Research 化学-化学综合
CiteScore
31.40
自引率
1.10%
发文量
312
审稿时长
2 months
期刊介绍: Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance. Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.
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