Ring-widths of Abies at tree-line ecotone reveal three centuries of early winter season temperature changes in Yunnan, China
Creators
- 1. Yunnan Key Laboratory for Wild Plant Resources (China)
- 2. Chinese Academy of Sciences. Key Laboratory of Economic Plants and Biotechnology, Kunming Institute of Botany (China)
- 3. Chinese Academy of Sciences. Key Laboratory for Plant Diversity and Biogeography of East Asia, Kunming Institute of Botany (China)
- 4. University of Bonn. Institute of Crop Science and Resource Conservation (INRES), Department Horticultural Sciences/ Center for Development Research ZEF (Germany)
- 5. Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences. Key Laboratory of Tropical Forest Ecology (China)
- 6. Kunming Institute of Survey and Design. State Forestry and Grassland Administration (China)
- 7. Guizhou University of Traditional Chinese Medicine (China)
- 8. Southeast Asia Biodiversity Research Institute, Chinese Academy of Sciences (China)
Description
Variation in winter temperature is less well understood than in annual and summer temperatures over long timescales, particularly in low-latitude (0–30° N) montane regions with large spatial and topographic heterogeneity. Understanding these variations could be critical for forest manageemnt in these important tree growing regions. We collected tree-ring cores from Yunnan Province in montane southwest China, to determine how winter temperature has varied in the past and to explore its possible drivers in this region. Six highly correlated site chronologies were combined into a long and well-replicated regional composite (RC) chronology. The RC chronology correlated strongest with mean early winter season temperature (EWST) from November to January during 1959–2015. We applied RC chronology to reconstruct EWST from 1653 to 2015. The reconstruction shows five relatively warm historic intervals (1658–1718, 1743–1755, 1771–1791, 1929–1959, and 1995–2015) and cold intervals (1720–1742, 1792–1852, 1860–1883, 1905–1928, and 1960–1994). The 1950s with six anomalous warm seasons and 1980s with five anomalous cold seasons were the warmest and coldest decades, respectively. The EWST reconstruction generally agreed with other winter temperature reconstructions from nearby areas and with historical documents. Atlantic Multidecadal Oscillation (AMO) might be a key forcing of multidecadal winter temperature variations in montane southwest China over the past three and half centuries. Both warm and cold temperature periods coincide with respective positive and negative phases of AMO. Besides, the cold intervals during the nineteenth and twentieth centuries may also have been influenced by large volcano eruptions in low-latitude regions of south and east Asia. Our EWST reconstruction not only improves our understanding of the trends and variations of winter climate history, but also supports planning for resilience in conservation, agriculture, and forestry management in montane southwest China into the future.
Additional details
Identifiers
Publishing Information
- Journal Title
- Climate Dynamics
- Journal Volume
- 55
- Journal Issue
- 3-4
- Journal Page Range
- p. 945-959
- ISSN
- 0930-7575
- CODEN
- CLDYEM
INIS
- Country of Publication
- Germany
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 55062227
- Subject category
- S54: ENVIRONMENTAL SCIENCES; S09: BIOMASS FUELS;
- Descriptors DEI
- AGRICULTURE; ASIA; CHINA; CLIMATIC CHANGE; CLOUD COVER; ERUPTION; FORESTS; MICROCLIMATES; OSCILLATIONS; PLANNING; SEASONAL VARIATIONS; SEASONS; SOUTHERN OSCILLATION; TREE RINGS
- Descriptors DEC
- ASIA; CLIMATES; VARIATIONS
Optional Information
- Copyright
- Copyright (c) 2020 © The Author(s) 2020