Geology Faculty Publications

Document Type

Article

Publication Date

2-5-2016

Publication Source

Climate of the Past

Abstract

Stable oxygen isotopic records in ice cores provide valuable information about past temperature, especially for regions with scarce instrumental measurements. This paper presents the δ18O result of an ice core drilled to bedrock from Mt. Zangser Kangri (ZK), a remote area on the northern Tibetan Plateau (TP). We reconstructed the temperature series for 1951–2008 from the δ18O records. In addition, we combined the ZK δ18O records with those from three other ice cores in the northern TP (Muztagata, Puruogangri, and Geladaindong) to reconstruct a regional temperature history for the period 1951–2002 (RTNTP). The RTNTP showed significant warming at 0.51 ± 0.07 °C (10 yr)−1 since 1970, a higher rate than the trend of instrumental records of the northern TP (0.43 ± 0.08 °C (10 yr)−1) and the global temperature trend (0.27 ± 0.03°C (10 yr)−1) at the same time. In addition, the ZK temperature record, with extra length until 2008, seems to suggest that the rapid elevation-dependent warming continued for this region during the last decade, when the mean global temperature showed very little change. This could provide insights into the behavior of the recent warming hiatus at higher elevations, where instrumental climate records are lacking.

Inclusive pages

201-211

ISBN/ISSN

1814-9324

Document Version

Published Version

Comments

This document, published under a Creative Commons Attribution 3.0 License, has been made available for download in accordance with the license and the publisher's policy on open-access.

Permission documentation on file.

DOI: https://doi.org/10.5194/cp-12-201-2016

Publisher

Copernicus Publications

Volume

12

Issue

2

Peer Reviewed

yes

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