Articles | Volume 14, issue 12
https://doi.org/10.5194/cp-14-1869-2018
https://doi.org/10.5194/cp-14-1869-2018
Research article
 | 
30 Nov 2018
Research article |  | 30 Nov 2018

Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India

Gayatri Kathayat, Hai Cheng, Ashish Sinha, Max Berkelhammer, Haiwei Zhang, Pengzhen Duan, Hanying Li, Xianglei Li, Youfeng Ning, and R. Lawrence Edwards

Viewed

Total article views: 4,779 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,231 1,474 74 4,779 68 105
  • HTML: 3,231
  • PDF: 1,474
  • XML: 74
  • Total: 4,779
  • BibTeX: 68
  • EndNote: 105
Views and downloads (calculated since 16 Aug 2018)
Cumulative views and downloads (calculated since 16 Aug 2018)

Viewed (geographical distribution)

Total article views: 4,779 (including HTML, PDF, and XML) Thereof 4,310 with geography defined and 469 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 24 Apr 2024
Download
Short summary
The 4.2 ka event is generally characterized as an approximately 300-year period of major global climate anomaly. However, the climatic manifestation of this event remains unclear in the Indian monsoon domain. Our high-resolution and precisely dated speleothem record from Meghalaya, India, characterizes the event as consisting of a series of multi-decadal droughts between 3.9 and 4.0 ka rather than a singular pulse of multi-centennial drought as previously thought.