阿尔泰山北部过去2 000 a来的气候记录集成

Abstract

Abstract: This study firstly reviewed the achievements about climate change in the north Altay Mountains over the past 2 000 years, and then summarized the geographical consistency of climate information contained in these documents. Mutil proxies (lake cores, tree rings and ice cores) recorded the five important climatic events in the Northern Hemisphere, including the Roman Optimum (0-400 AD),Dark Age Cold Period (400-600 AD),Medieval Warm Period (800-1200 AD),Little Ice Age (1400-1860 AD),and recent warming period (since 1860 AD).These climatic events were mainly modulated by solar activity dominated solar radiation variations in the past 2 000 years and recent warming period since 1860 AD, which were largely attributable to an increase of CO₂ concentration in the past 150 years. The precipitation history in the north Altay Mountains over the past 2 000 years indicated that these periods including 0-450,600-800,1050-1300,1650-1860 AD were characterized by high precipitation, and those including 450-600,800-1050,1300-1650,1860-2000 AD were featured by low precipitation. In addition, the combination of temperature and precipitation in the north Altay Mountains over the past 2 000 years did not supported the “cold wet and warm dry” hydrothermal configuration in the arid zone in Central Asia.

Key words: climate change')">

climate change, tree ring, lake core, ice core, Altay Mountains

ZHANG Dong-liang, LI Yin-bo, YANG Yun-peng, LAN Bo. Synthesized Climate Change in the North Altay Mountains in the Past 2 000 Years[J].Arid Zone Research, 2019, 36(1): 176-185.

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Synthesized Climate Change in the North Altay Mountains in the Past 2 000 Years

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