Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 3.536
IF3.536
IF 5-year value: 3.967
IF 5-year
3.967
CiteScore value: 6.6
CiteScore
6.6
SNIP value: 1.262
SNIP1.262
IPP value: 3.90
IPP3.90
SJR value: 2.185
SJR2.185
Scimago H <br class='widget-line-break'>index value: 71
Scimago H
index
71
h5-index value: 40
h5-index40
Download
Short summary
The upper part of stalagmite ky1 (from top to 42.769 mm depth), consisting of 678 laminae, was collected from a cave in northern China, located in the East Asia monsoon area. The time of deposition ranges from AD 1217±20 to 1894±20. The analysis shows that both the variations in the thickness of the laminae themselves and the fluctuating degree of variation in the thickness of the laminae of stalagmite ky1 have obviously staged characteristics and synchronized with climate.
Articles | Volume 12, issue 4
Clim. Past, 12, 871–881, 2016
https://doi.org/10.5194/cp-12-871-2016
Clim. Past, 12, 871–881, 2016
https://doi.org/10.5194/cp-12-871-2016

Research article 08 Apr 2016

Research article | 08 Apr 2016

The climate reconstruction in Shandong Peninsula, northern China, during the last millennium based on stalagmite laminae together with a comparison to δ18O

Qing Wang et al.

Viewed

Total article views: 2,058 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,113 787 158 2,058 93 103
  • HTML: 1,113
  • PDF: 787
  • XML: 158
  • Total: 2,058
  • BibTeX: 93
  • EndNote: 103
Views and downloads (calculated since 02 Oct 2015)
Cumulative views and downloads (calculated since 02 Oct 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 25 Jan 2021
Publications Copernicus
Download
Short summary
The upper part of stalagmite ky1 (from top to 42.769 mm depth), consisting of 678 laminae, was collected from a cave in northern China, located in the East Asia monsoon area. The time of deposition ranges from AD 1217±20 to 1894±20. The analysis shows that both the variations in the thickness of the laminae themselves and the fluctuating degree of variation in the thickness of the laminae of stalagmite ky1 have obviously staged characteristics and synchronized with climate.
Citation