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Severe multi-year drought coincident with Hittite collapse around 1198-1196 BC
Sturt W Manning1,2, Cindy Kocik3, Brita Lorentzen4,5
1Cornell Tree-Ring Laboratory, Department of Classics and Cornell Institute of Archaeology and Material Studies, Cornell University, Ithaca, NY, USA. sm456@cornell.edu.
Climate change significantly impacted ancient civilizations. A severe, multi-year drought around 1198 BC likely caused the Hittite Empire
Area of Science:
- Paleoclimatology and Archaeology
- Ancient Near Eastern Studies
- Climate Change Impacts on Civilizations
Background:
- Climate change poses a significant threat to human history, yet specific impacts remain unclear.
- Past civilizations have faced climate shifts, but precise links between climate events and societal collapse are often missing.
- The Hittite Empire, a major ancient power, was centered in a vulnerable semi-arid region.
Purpose of the Study:
- To investigate the precise climate conditions and their correlation with the collapse of the Hittite Empire around 1200 BC.
- To understand how extreme climate events can overwhelm societal adaptation and resilience.
Main Methods:
- Analysis of high-resolution dryness records using tree ring width and stable isotope data from contemporary juniper trees in Anatolia.
- Correlation of paleoclimatic data with the archaeological and historical timelines of the Hittite Empire.
Main Results:
- Identification of an exceptionally severe and continuous dry period in central Anatolia from approximately 1198 to 1196 BC (±3 years).
- This intense drought event is pinpointed as a potential tipping point for the Hittite civilization.
- The findings suggest that consecutive extreme climate events can exceed the adaptive capacity of even resilient societies.
Conclusions:
- A severe multi-year drought around 1198 BC was a critical factor in the collapse of the Hittite Empire.
- This study highlights the vulnerability of ancient societies to abrupt and extreme climate shifts.
- Understanding past climate-society interactions is crucial for assessing future climate change risks.
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