1Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
2College of Population, Resources and Environment, Shandong Normal
University, Jinan 250014, China
3State Key Laboratory of Cryospheric Science, Cold and Arid Regions
Environmental and Engineering Research Institute, Chinese Academy of
Sciences, Lanzhou 730000, China
4Geology Department, University of Dayton, Ohio 45469-2364, USA
5CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing
100101, China
1Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
2College of Population, Resources and Environment, Shandong Normal
University, Jinan 250014, China
3State Key Laboratory of Cryospheric Science, Cold and Arid Regions
Environmental and Engineering Research Institute, Chinese Academy of
Sciences, Lanzhou 730000, China
4Geology Department, University of Dayton, Ohio 45469-2364, USA
5CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing
100101, China
Received: 13 May 2015 – Discussion started: 02 Jul 2015 – Revised: 19 Nov 2015 – Accepted: 19 Jan 2016 – Published: 05 Feb 2016
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.
This paper presents the δ18O result of an ice core recovered from Mt. Zangser Kangri (ZK), a remote area on the northern Tibetan Plateau (TP). We combined the δ18O series of ZK and three other nearby Tibetan ice cores to reconstruct a regional temperature history of 1951–2008, which captured the continuous rapid warming since 1970, even during the global warming hiatus period. It implied that temperature change could have behaved differently at high elevations.
This paper presents the δ18O result of an ice core recovered from Mt. Zangser Kangri (ZK), a...
