loading page

Temperature Variability in Northeast China over the Past Two Millennia and Linkages with the Arctic Oscillation
  • +7
  • Nan Zhan,
  • Qi Li,
  • Manman Xie,
  • Ruilin Wen,
  • Luo Wang,
  • RuiXia Hao,
  • Chunqing Sun,
  • Guoping Zhang,
  • Qing Sun,
  • Guoqiang Chu
Nan Zhan
National Research Center for Geoanalysis

Corresponding Author:[email protected]

Author Profile
Qi Li
Institute of Geology and Geophysics
Author Profile
Manman Xie
National Research Center for Geoanalysis
Author Profile
Ruilin Wen
Institute of Geology and Geophysics
Author Profile
Luo Wang
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences
Author Profile
RuiXia Hao
School of Earth and Space Sciences, Peking University
Author Profile
Chunqing Sun
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences
Author Profile
Guoping Zhang
CMA Public Meteorological Service Center
Author Profile
Qing Sun
National Research Center of Geoanalysis
Author Profile
Guoqiang Chu
Institute of Geology and Geophysics, Chinese Academy of Sciences
Author Profile

Abstract

Temperature reconstruction over the past two millennia has created a crucial database for global networks and for evaluating and predicting global climate change. Here, we present a high-resolution (~5-25 years) temperature reconstruction over the past 2000 years using branched glycerol dialkyl glycerol tetraethers (brGDGTs) from laminated sediments in a crater lake located in Northeast China. The brGDGT-derived proxies accurately represented the month-above-freezing temperatures (MAFT) within our study region. Our temperature reconstruction exhibited distinct decadal-to-centennial variability and showed rough correspondence with the AO/NAO index and solar activity. Furthermore, the spectral analysis identified two quasi-periodicities of 55-57 and 66-67 years within the MAFTs time series at a 99% confidence level, suggesting possible associations with solar activity. These findings imply that long-term temperature variability in Northeast China is mainly regulated by a combination of the AO, NAO, and solar activity.
07 Mar 2024Submitted to ESS Open Archive
15 Mar 2024Published in ESS Open Archive