A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China

Liya Jin; Fahu Chen; Xiaojun Ding; Yan Zhu

doi:10.1007/s00343-007-0149-y

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A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China

OriginalPaper | Updated：2023-05-16

- A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China
- A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China
- 海洋湖沼学报（英文） 2007年25卷第2期页码：149-156
- Affiliations：
  
  1. Key Laboratory of Western China’s Environmental Systems The Ministry of Education China
  2. Center for Arid Environment and Paleoclimate Research Lanzhou University
  3. College of Atmospheric Sciences Lanzhou University
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China (NSFC) (No. 40571169), the NSFC’s Innovation Team Project (No. 40421101), and the NSFC’s Key Program Project (No. 90502008).
- DOI：10.1007/s00343-007-0149-y
  中图分类号：
- 纸质出版：2007
- Accepted：
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A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China[J]. 海洋湖沼学报（英文）, 2007,25(2):149-156.

Jin, L., Chen, F., Ding, X. et al. A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China., Chin. J. Ocean. Limnol. 25, 149–156 (2007). https://doi.org/10.1007/s00343-007-0149-y
A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China[J]. 海洋湖沼学报（英文）, 2007,25(2):149-156. DOI： 10.1007/s00343-007-0149-y.

Jin, L., Chen, F., Ding, X. et al. A singular spectrum analysis on holocene climatic oscillation from lake sedimentary record in Minqin Basin, China., Chin. J. Ocean. Limnol. 25, 149–156 (2007). https://doi.org/10.1007/s00343-007-0149-y DOI：

摘要

Abstract

The total organic carbon (TOC) content series from the lake sediment of Minqin Basin (100°57′–104°57′E

37°48′–39°17′N) in northwestern China

which has a 10 000-year-long paleo-climatic proxy record

was used to analyze the Holocene climate changes in the local region. The proxy record was established in the Sanjiaocheng (SJC)

Triangle Town in Chinese

Section (103°20′25″E

39°00′38″N)

which is located at the northwestern boundary of the present Asian summer monsoon in China

and is sensitive to global environmental and climate changes. Applying singular spectrum analysis (SSA) to the TOC series

principal climatic oscillations and periodical changes were studied. The results reveal 3 major patterns of climate change regulated by reconstructed components (RCs). The first pattern is natural long-term trend of climinatic change in the local area (Minqin Basin)

indicating a relatively wetter stage in early Holocene (starting at 9.5 kaBP)

and a relatively dryer stage with a strong lake desiccation and a declined vegetation cover in mid-Holocene (during 7-6 kaBP). From 4.0 kaBP to the present

there has been a gradually decreasing trend in the third reconstructed component (RC3) showing that the local climate changed again into a dryer stage. The second pattern shows millennial-centennial scale oscillations containing cycles of 1 600 and 800 years that have been present throughout almost the entire Holocene period of the last 10 000 years. The third pattern is a millennial-centennial scale variation with a relatively smaller amplitude and unclear cycles showing a nonlinear interaction within the earth’s climate systems.

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references

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