significant recent warming over the northern tibetan plateau from ice core δ18o records
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2016
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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.
| Reference Key |
an2016climatesignificant
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|---|---|
| Authors | ;W. An;S. Hou;W. Zhang;Y. Wang;Y. Liu;S. Wu;H. Pang |
| Journal | proceedings - 16th ieee/acis international conference on computer and information science, icis 2017 |
| Year | 2016 |
| DOI |
10.5194/cp-12-201-2016
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| URL | |
| Keywords |
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