Document Type
Article
Publication Title
Climate of the Past
Rights and Access Note
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s).
Publication Date
2007
First Page
89
Last Page
95
Issue Number
1
Volume Number
3
Abstract/ Summary
Two Himalayan ice cores display a factor-two decreasing trend of air content over the past two millennia, in contrast to the relatively stable values in Greenland and Antarctica ice cores over the same period. Because the air content can be related with the relative frequency and intensity of melt phenomena, its variations along the Himalayan ice cores provide an indication of summer temperature trend. Our reconstruction point toward an unprecedented warming trend in the 20th century but does not depict the usual trends associated with "Medieval Warm Period" (MWP), or "Little Ice Age" (LIA).
Repository Citation
Hou, S.; Chappellaz, J.; Jouzel, J.; Chu, P. C.; Masson-Delmotte, V.; Qin, Dahe; Raynaud, D.; Mayewski, Paul Andrew; Lipenkov, V. Y.; and Kang, Shichang, "Summer Temperature Trend Over the Past Two Millennia Using Air Content in Himalayan Ice" (2007). Earth Science Faculty Scholarship. 93.
https://digitalcommons.library.umaine.edu/ers_facpub/93
Citation/Publisher Attribution
Hou, S, Chappellaz, J, Jouzel, J, Chu, PC, Masson-Delmotte, V, Qin, D, Raynaud, D, et al., 2007, Summer Temperature Trend Over the Past Two Millennia Using Air Content in Himalayan Ice: Climate of the Past, v. 3, p. 89-95.
DOI
10.5194/cp-3-89-2007
Version
publisher's version of the published document
Creative Commons License
This work is licensed under a Creative Commons Attribution 3.0 License.