Abstract

This article analyzes the effect of climate extremes on the historical processes that took place (AD 536, 581, 601, 626 and 679) in the Eastern Turk Empire (AD 534–745) in Inner Asia. Climate extremes are sharp, strong and sometimes protracted periods of cooling and drought caused by volcanic eruptions that in this case resulted in a negative effect on the economy of a nomadic society and were often accompanied by famine and illness. In fact, many of these natural catastrophes coincided with the Black Death pandemics among the Eastern Turks and the Chinese living in the north of China. The Turk Empire can be split into several chronological periods during which significant events that led to changes in the course of history of the nomadic state took place: AD 534–545—the rise of the Turk Empire; AD 581–583—the division of the Turk Empire into the Western and the Eastern Empires; AD 601–603—the rise of Qimin Qaghan; AD 627–630—the Eastern Turks are conquered by China; AD 679–687—the second rise of the Eastern Turk Empire. The research shows that there is clearly-discernable interplay between important historical events and climate extremes in the history of the Turk Empire. This interplay has led us to the conclusion that the climatic factor did have an impact on the historical processes that took place in the eastern part of Inner Asia, especially on the territories with a nomadic economy.

Highlights

  • The material presented here demonstrates that there is a definite interplay between the historical events and the climate extremes on the territory of Inner Asia, and that these events coincide with other climate anomalies in Europe and China

  • It has been proved that such coincidences come parallel with the key events in the Turk Empire and with those in Northern China in the following years: AD 535–545—the rise of the Turk Empire; AD 581–583—the division of the Turk Empire into the Western and the Eastern Empires; AD 599–603—the strengthening of the Eastern Turks under the leadership of Qimin Qaghan; AD 627–630—the collapse of the Turk Empire; in AD 679–685—the second rise of the Turk Empire (Table 8.1)

  • Most climatologists believe that the reason for such phenomena is a large explosive volcanic eruption

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Summary

Introduction

The Turks played a significant role in the cultural interaction of the West and the East. They furthered the development of trade along the Great Silk Road and established trade relations with the leading empires of the time (Sasanian Empire, Byzantium and China). In AD 581, the Turk Empire broke up into two parts—the Western one and the Eastern one. Its northern borders spread out to Lake Baikal, the southern to North China (the Great Wall), the western to Eastern Kazakhstan, including Tuva and the Altai, the eastern to the Greater Khingan Range (Fig. 8.1)

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