Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-201-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-201-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
05 Feb 2016
Research article |
| 05 Feb 2016
Significant recent warming over the northern Tibetan Plateau from ice core δ18O records
W. An
Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing
100101, China
W. Zhang
Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
College of Population, Resources and Environment, Shandong Normal
University, Jinan 250014, China
Y. Liu
State Key Laboratory of Cryospheric Science, Cold and Arid Regions
Environmental and Engineering Research Institute, Chinese Academy of
Sciences, Lanzhou 730000, China
S. Wu
Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
Geology Department, University of Dayton, Ohio 45469-2364, USA
H. Pang
Key Laboratory of Coast and Island development of Ministry of Education,
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing
210093, China
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Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2024-151, https://doi.org/10.5194/amt-2024-151, 2024
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We developed and validated a theoretical model for water vapor diffusion through sampling bags. This model accurately reconstructs the initial isotopic composition of the vapor samples. When applied to upper troposphere samples, the corrected data aligned closely with IASI satellite observations, enhancing the accuracy of drone-based measurements.
Zehua Chang, Hongkai Gao, Leilei Yong, Kang Wang, Rensheng Chen, Chuntan Han, Otgonbayar Demberel, Batsuren Dorjsuren, Shugui Hou, and Zheng Duan
Hydrol. Earth Syst. Sci., 28, 3897–3917, https://doi.org/10.5194/hess-28-3897-2024, https://doi.org/10.5194/hess-28-3897-2024, 2024
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An integrated cryospheric–hydrologic model, FLEX-Cryo, was developed that considers glaciers, snow cover, and frozen soil and their dynamic impacts on hydrology. We utilized it to simulate future changes in cryosphere and hydrology in the Hulu catchment. Our projections showed the two glaciers will melt completely around 2050, snow cover will reduce, and permafrost will degrade. For hydrology, runoff will decrease after the glacier has melted, and permafrost degradation will increase baseflow.
Yetang Wang, Xueying Zhang, Wentao Ning, Matthew A. Lazzara, Minghu Ding, Carleen H. Reijmer, Paul C. J. P. Smeets, Paolo Grigioni, Petra Heil, Elizabeth R. Thomas, David Mikolajczyk, Lee J. Welhouse, Linda M. Keller, Zhaosheng Zhai, Yuqi Sun, and Shugui Hou
Earth Syst. Sci. Data, 15, 411–429, https://doi.org/10.5194/essd-15-411-2023, https://doi.org/10.5194/essd-15-411-2023, 2023
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Here we construct a new database of Antarctic automatic weather station (AWS) meteorological records, which is quality-controlled by restrictive criteria. This dataset compiled all available Antarctic AWS observations, and its resolutions are 3-hourly, daily and monthly, which is very useful for quantifying spatiotemporal variability in weather conditions. Furthermore, this compilation will be used to estimate the performance of the regional climate models or meteorological reanalysis products.
Jiajia Wang, Hongxi Pang, Shuangye Wu, Spruce W. Schoenemann, Ryu Uemura, Alexey Ekaykin, Martin Werner, Alexandre Cauquoin, Sentia Goursaud Oger, Summer Rupper, and Shugui Hou
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2022-384, https://doi.org/10.5194/essd-2022-384, 2022
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Stable water isotopic observations in surface snow over Antarctica provide a basis for validating isotopic models and interpreting Antarctic ice core records. This study presents a new compilation of Antarctic surface snow isotopic dataset based on published and unpublished sources. The database has a wide range of potential applications in studying spatial distribution of water isotopes, model validation, and reconstruction and interpretation of Antarctic ice core records.
Wangbin Zhang, Shugui Hou, Shuang-Ye Wu, Hongxi Pang, Sharon B. Sneed, Elena V. Korotkikh, Paul A. Mayewski, Theo M. Jenk, and Margit Schwikowski
The Cryosphere, 16, 1997–2008, https://doi.org/10.5194/tc-16-1997-2022, https://doi.org/10.5194/tc-16-1997-2022, 2022
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This study proposes a quantitative method to reconstruct annual precipitation records at the millennial timescale from the Tibetan ice cores through combining annual layer identification based on LA-ICP-MS measurement with an ice flow model. The reliability of this method is assessed by comparing our results with other reconstructed and modeled precipitation series for the Tibetan Plateau. The assessment shows that the method has a promising performance.
Tao Xu, Hongxi Pang, Zhaojun Zhan, Wangbin Zhang, Huiwen Guo, Shuangye Wu, and Shugui Hou
Hydrol. Earth Syst. Sci., 26, 117–127, https://doi.org/10.5194/hess-26-117-2022, https://doi.org/10.5194/hess-26-117-2022, 2022
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In this study, we presented stable isotopes in atmospheric water vapor and precipitation for five extreme winter precipitation events in Nanjing, southeastern China, from December 2018 to February 2019. Our results imply that multiple moisture sources and the rapid shift among them are important conditions for sustaining extreme precipitation events, especially in the relatively cold and dry winter.
Yetang Wang, Minghu Ding, Carleen H. Reijmer, Paul C. J. P. Smeets, Shugui Hou, and Cunde Xiao
Earth Syst. Sci. Data, 13, 3057–3074, https://doi.org/10.5194/essd-13-3057-2021, https://doi.org/10.5194/essd-13-3057-2021, 2021
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Accurate observation of surface mass balance (SMB) under climate change is essential for the reliable present and future assessment of Antarctic contribution to global sea level. This study presents a new quality-controlled dataset of Antarctic SMB observations at different temporal resolutions and is the first ice-sheet-scale compilation of multiple types of measurements. The dataset can be widely applied to climate model validation, remote sensing retrievals, and data assimilation.
Shugui Hou, Wangbin Zhang, Ling Fang, Theo M. Jenk, Shuangye Wu, Hongxi Pang, and Margit Schwikowski
The Cryosphere, 15, 2109–2114, https://doi.org/10.5194/tc-15-2109-2021, https://doi.org/10.5194/tc-15-2109-2021, 2021
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We present ages for two new ice cores reaching bedrock, from the Zangser Kangri (ZK) glacier in the northwestern Tibetan Plateau and the Shulenanshan (SLNS) glacier in the western Qilian Mountains. We estimated bottom ages of 8.90±0.57/0.56 ka and 7.46±1.46/1.79 ka for the ZK and SLNS ice core respectively, constraining the time range accessible by Tibetan ice cores to the Holocene.
Ling Fang, Theo M. Jenk, Thomas Singer, Shugui Hou, and Margit Schwikowski
The Cryosphere, 15, 1537–1550, https://doi.org/10.5194/tc-15-1537-2021, https://doi.org/10.5194/tc-15-1537-2021, 2021
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The interpretation of the ice-core-preserved signal requires a precise chronology. Radiocarbon (14C) dating of the water-insoluble organic carbon (WIOC) fraction has become an important dating tool. However, this method is restricted by the low concentration in the ice. In this work, we report first 14C dating results using the dissolved organic carbon (DOC) fraction. The resulting ages are comparable in both fractions, but by using the DOC fraction the required ice mass can be reduced.
Shugui Hou, Wangbin Zhang, Hongxi Pang, Shuang-Ye Wu, Theo M. Jenk, Margit Schwikowski, and Yetang Wang
The Cryosphere, 13, 1743–1752, https://doi.org/10.5194/tc-13-1743-2019, https://doi.org/10.5194/tc-13-1743-2019, 2019
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The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice cores may be attributed to a possible misinterpretation of the Guliya ice core chronology.
Shugui Hou, Theo M. Jenk, Wangbin Zhang, Chaomin Wang, Shuangye Wu, Yetang Wang, Hongxi Pang, and Margit Schwikowski
The Cryosphere, 12, 2341–2348, https://doi.org/10.5194/tc-12-2341-2018, https://doi.org/10.5194/tc-12-2341-2018, 2018
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We present multiple lines of evidence indicating that the Chongce ice cores drilled from the northwestern Tibetan Plateau reaches back only to the early Holocene. This result is at least, 1 order of magnitude younger than the nearby Guliya ice core (~30 km away from the Chongce ice core drilling site) but similar to other Tibetan ice cores. Thus it is necessary to explore multiple dating techniques to confirm the age ranges of the Tibetan ice cores.
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The Cryosphere, 12, 163–168, https://doi.org/10.5194/tc-12-163-2018, https://doi.org/10.5194/tc-12-163-2018, 2018
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We provide the first luminescence dating of the basal sediment of the Chongce ice cap in the western Kunlun Mountains on the north-western Tibetan Plateau (TP), which gives an upper constraint for the age of the bottom ice at the drilling site. The age is more than 1 order of magnitude younger than the previously suggested age of the basal ice of the nearby Guliya ice cap (~ 40 km away from the Chongce ice cap). This work provides an important step towards better understanding the TP ice cores.
Shuang-Ye Wu and Shugui Hou
The Cryosphere, 11, 707–722, https://doi.org/10.5194/tc-11-707-2017, https://doi.org/10.5194/tc-11-707-2017, 2017
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The primary productivity in the Southern Ocean (SO) is limited by the amount of iron available for biological activities. Recent studies show that icebergs could be a main source of iron to the SO. Based on remote sensing data, our study shows that iceberg presence is associated with elevated levels of ocean productivity, particularly in iron-deficient regions. This impact could serve as a negative feedback to the climate system.
Yetang Wang, Shugui Hou, Wenling An, Hongxi Pang, and Yaping Liu
The Cryosphere Discuss., https://doi.org/10.5194/tc-2016-165, https://doi.org/10.5194/tc-2016-165, 2016
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This study further confirms "Pamir–Karakoram–Western-Kunlun-Mountain (northwestern Tibetan Plateau) Glacier Anomaly". Slight glacier reduction over the northwestern Tibetan Plateau may result from more accumulation from increased precipitation in winter which to great extent protects it from mass reductions under climate warming during 1961–2000. Warming slowdown since 2000 happening at this region may further mitigate glacier mass reduction.
Y. Tang, H. Pang, W. Zhang, Y. Li, S. Wu, and S. Hou
Hydrol. Earth Syst. Sci., 19, 4293–4306, https://doi.org/10.5194/hess-19-4293-2015, https://doi.org/10.5194/hess-19-4293-2015, 2015
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We examined the variability of daily stable isotopic composition in precipitation in Nanjing, eastern China. We found that both the upstream rainout effect on stable isotopes related to changes in the Asian summer monsoon and the temperature effect of precipitation stable isotopes associated with the Asian winter monsoon should be taken into account when interpreting the stable isotopic composition of speleothems in the Asian monsoon region.
H. Pang, S. Hou, S. Kaspari, and P. A. Mayewski
The Cryosphere, 8, 289–301, https://doi.org/10.5194/tc-8-289-2014, https://doi.org/10.5194/tc-8-289-2014, 2014
S. Hou, J. Chappellaz, D. Raynaud, V. Masson-Delmotte, J. Jouzel, P. Bousquet, and D. Hauglustaine
Clim. Past, 9, 2549–2554, https://doi.org/10.5194/cp-9-2549-2013, https://doi.org/10.5194/cp-9-2549-2013, 2013
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Ice Cores | Timescale: Centennial-Decadal
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This study presents organic acid levels in an ice core from Svalbard over the past 800 years. These acids are produced from wildfire emissions and transported as aerosol. Organic acid levels are high early in the record and decline until the 20th century. Siberia and Europe are likely the primary source regions of the fire emissions. The data are similar to those from a Siberian ice core prior to 1400 CE. The timing of the divergence after 1400 CE is similar to a shift in North Atlantic climate.
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Mana Inoue, Mark A. J. Curran, Andrew D. Moy, Tas D. van Ommen, Alexander D. Fraser, Helen E. Phillips, and Ian D. Goodwin
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A 120 m ice core from Mill Island, East Antarctica, was studied its chemical components. The Mill Island ice core contains 97 years of climate record (1913–2009) and has a mean snow accumulation of 1.35 m yr−1 (ice equivalent). Trace ion concentrations were generally higher than other Antarctic ice core sites. Nearby sea ice concentration was found to influence the annual mean sea salt record. The Mill Island ice core records are unexpectedly complex, with strong modulation of the trace chemistry.
Mackenzie M. Grieman, Murat Aydin, Diedrich Fritzsche, Joseph R. McConnell, Thomas Opel, Michael Sigl, and Eric S. Saltzman
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Wildfires impact ecosystems, climate, and atmospheric chemistry. Records that predate instrumental records and industrialization are needed to study the climatic controls on biomass burning. In this study, we analyzed organic chemicals produced from burning of plant matter that were preserved in an ice core from the Eurasian Arctic. These chemicals are elevated during three periods that have similar timing to climate variability. This is the first millennial-scale record of these chemicals.
Olivia J. Maselli, Nathan J. Chellman, Mackenzie Grieman, Lawrence Layman, Joseph R. McConnell, Daniel Pasteris, Rachael H. Rhodes, Eric Saltzman, and Michael Sigl
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Alexey A. Ekaykin, Diana O. Vladimirova, Vladimir Y. Lipenkov, and Valérie Masson-Delmotte
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Michel Legrand, Joseph McConnell, Hubertus Fischer, Eric W. Wolff, Susanne Preunkert, Monica Arienzo, Nathan Chellman, Daiana Leuenberger, Olivia Maselli, Philip Place, Michael Sigl, Simon Schüpbach, and Mike Flannigan
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A. Tsushima, S. Matoba, T. Shiraiwa, S. Okamoto, H. Sasaki, D. J. Solie, and K. Yoshikawa
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A 180.17-m ice core was drilled at Aurora Peak in the central part of the Alaska Range, Alaska, in 2008. The ice core age was determined by annual counts of δD and seasonal cycles of Na+. Here, we show that the chronology of the Aurora Peak ice core from 95.61 m to the top corresponds to the period from 1900 to the summer season of 2008, with a dating error of ±3 years. Our results suggest that temporal variations in δD and annual accumulation rates are strongly related to shifts in PDO Index.
P. Zennaro, N. Kehrwald, J. R. McConnell, S. Schüpbach, O. J. Maselli, J. Marlon, P. Vallelonga, D. Leuenberger, R. Zangrando, A. Spolaor, M. Borrotti, E. Barbaro, A. Gambaro, and C. Barbante
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B. G. Koffman, K. J. Kreutz, D. J. Breton, E. J. Kane, D. A. Winski, S. D. Birkel, A. V. Kurbatov, and M. J. Handley
Clim. Past, 10, 1125–1144, https://doi.org/10.5194/cp-10-1125-2014, https://doi.org/10.5194/cp-10-1125-2014, 2014
T. Sato, T. Shiraiwa, R. Greve, H. Seddik, E. Edelmann, and T. Zwinger
Clim. Past, 10, 393–404, https://doi.org/10.5194/cp-10-393-2014, https://doi.org/10.5194/cp-10-393-2014, 2014
S. Brönnimann, I. Mariani, M. Schwikowski, R. Auchmann, and A. Eichler
Clim. Past, 9, 2013–2022, https://doi.org/10.5194/cp-9-2013-2013, https://doi.org/10.5194/cp-9-2013-2013, 2013
S. Preunkert and M. Legrand
Clim. Past, 9, 1403–1416, https://doi.org/10.5194/cp-9-1403-2013, https://doi.org/10.5194/cp-9-1403-2013, 2013
R. H. Rhodes, N. A. N. Bertler, J. A. Baker, H. C. Steen-Larsen, S. B. Sneed, U. Morgenstern, and S. J. Johnsen
Clim. Past, 8, 1223–1238, https://doi.org/10.5194/cp-8-1223-2012, https://doi.org/10.5194/cp-8-1223-2012, 2012
Cited articles
Araguás-Araguás, L., Froehlich, K., and Rozanski, K.: Stable
isotopic composition of precipitation over southeast Asia, J. Geophys. Res.,
103, 28721—28742, https://doi.org/10.1029/98JD02582, 1998.
Dansgaard, W.: Stable isotopes in precipitation, Tellus, 16, 436–468,
https://doi.org/10.1111/j.2153-3490.1964.tb00181.x, 1964.
Duan, A. M. and Xiao, Z. X.: Does the climate warming hiatus exist over the
Tibetan Plateau?, Scientific Reports, 5, 13711, https://doi.org/10.1038/srep13711,
2015.
Easterling, D. R. and Wehner M. F.: Is the climate warming or cooling?,
Geophys. Res. Lett., 36, L08706, https://doi.org/10.1029/2009GL037810, 2009.
Ghatak, D., Sinsky, E., and Miller. J.: Role of snow-albedo feedback in
higher elevation warming over the Himalayas, Tibetan Plateau and Central
Asia, Environ. Res. Lett., 9, 114008, https://doi.org/10.1088/1748-9326/9/11/114008,
2014.
Guo, D. L. and Wang, H. J.: The significant climate warming in the northern
Tibetan Plateau and its possible causes, Int. J. Climatol., 32, 1775–1781,
https://doi.org/10.1002/joc.2388, 2011.
He, Y., Risi, C., Gao, J., Masson-Delmotte, V., Yao, T. D., Lai, C. T., Ding,
Y. J., Worden, J., Frankenberg, C., Chepfer, H., and Cesana, G.: Impact of
atmospheric convection on south Tibet summer precipitation isotopologue
composition using a combination of in situmeasurements, satellite data, and
atmospheric general circulation modeling, J. Geophys. Res., 120, 3852–3871,
https://doi.org/10.1002/2014JD022180, 2015.
He, Y. X., Zhao, C., Wang, Z., Wang, H. Y., Song, M., Liu, W. G., and Liu,
Z. H.: Late Holocene coupled moisture and temperature changes on the
northern Tibetan Plateau, Quaternary Sci. Rev., 80, 47–57,
https://doi.org/10.1016/j.quascirev.2013.08.017, 2013.
Herzschuh, U., Mischke, H. J. S., Zhang, C. J., and Böhner,
J.: A modern pollen-climate calibration set based on lake sediments from the
Tibetan Plateau and its application to a Late Quaternary pollen record from
the Qilian Mountains, J. Biogeogr., 37, 752–766,
https://doi.org/10.1111/j.1365-2699.2009.02245.x, 2010.
Hou, S. G., Ren, J. W., and Qin, D. H.: Modification of three ice-core
δ18O records from an area of high melt, Ann. Glaciol., 43,
172–176, https://doi.org/10.3189/172756406781812140, 2006.
Joswiak, D. R., Yao, T., Wu, G., Xu, B., and Zheng, W.: A 70-yr record of
oxygen-18 variability in an ice core from the Tanggula Mountains, central
Tibetan Plateau, Clim. Past, 6, 219–227, https://doi.org/10.5194/cp-6-219-2010, 2010.
Joswiak, D. R., Yao, T., Wu, G., Tian, L., and Xu, B.: Ice-core evidence of
westerly and monsoon moisture contributions in the central Tibetan Plateau,
J. Glaciol., 59, 56–66, https://doi.org/10.3189/2013JoG12J035, 2013.
Kang, S. C., Zhang, Y. J., Qin, D. H., Ren, J. W., Zhang, Q. G., Bjorn, G.,
and Mayewski, P. A.: Recent temperature increase recorded in an ice core in
the source region of Yangtze River, Chinese Sci. Bull., 52, 825–831,
https://doi.org/10.1007/s11434-007-0140-1, 2007.
Lang, T. J. and Barros, A. P.: Winter storms in the central Himalayas, J.
Meteorol. Soc. Jpn., 82, 829–844, https://doi.org/10.2151/jmsj.2004.829, 2004.
Liu, X. D. and Chen, B. D.: Climatic warming in the Tibetan Plateau during
recent decades, Int. J. Climatol., 20, 1729–1742,
https://doi.org/10.1002/1097-0088(20001130)20:14<1729::AID-25JOC556>3.0.CO;2-Y, 2000.
Mitchell, T. D. and Jones, P. D.: An improved method of constructing a
database of monthly climate observations and associated high-resolution
grids, Int. J. Climatol., 25, 693–712, https://doi.org/10.1002/joc.1181, 2005.
Pang, H., Hou, S., Kaspari, S., and Mayewski, P. A.: Influence of regional
precipitation patterns on stable isotopes in ice cores from the central
Himalayas, The Cryosphere, 8, 289–301, https://doi.org/10.5194/tc-8-289-2014, 2014.
Pepin, N. and Lundquist, J.: Temperature trends at high elevations: patterns
across the globe, Geophys. Res. Lett., 35, L14701, https://doi.org/10.1029/2008GL034026,
2008.
Pu, Y., Zhang, H. C., Wang, Y. L., Lei, G. L., Nace, T., and Zhang, S. P.:
Climatic and environmental implications from n-alkanes in glacially eroded
lake sediments in Tibetan Plateau: An example from Ximen Co, Chinese Sci.
Bull., 56, 1503–1510, https://doi.org/10.1007/s11434-011-4454-7, 2011.
Qin, D. H., Hou, S. G., Zhang, D. Q., Ren J. W., and Kang, S. C.: Preliminary
results from the chemical records of an 80.4 m ice core recovered from East
Rongbuk Glacier, Qomolangma (Mount Everest), Ann. Glaciol., 35, 278–284,
https://doi.org/10.3189/172756402781816799, 2002.
Qu, B.: Albedo changing and its impact factors in the glacier area of Mt.
Nyainquentanglha region, Beijing, University of Chinese Academy of Sciences,
35–36, 2013.
Rangwala, I. and Miller, J.: Climate change in mountains: a review of
elevation dependent warming and its possible causes, Climatic Change, 114,
527–547, https://doi.org/10.1007/s10584-012-0419-3, 2012.
Risi, C., Bony, S., Vimeux, F., and Jouzel, J.: Water-stable isotopes in the
LMDZ4 general circulation model: Model evaluation for present – day and past
climates and applications to climatic interpretations of tropical isotopic
records, J. Geophys. Res., 115, D12118, https://doi.org/10.1029/2009JD013255, 2010.
Rowley, D. B., Pierrehumbert, R. T., and Currie, B. S.: A new approach to
stable isotope-based paleoaltimetry: implications for paleoaltimetry and
paleohypsometry of the High Himalaya since the Late Miocene, Earth Planet.
Sc. Lett., 188, 253–268, https://doi.org/10.1016/S0012-821X(01)00324-7, 2001.
Shi, Y. F.: Concise Glacier Inventory of China, Shanghai Science Press,
Shanghai, 2008.
Tang, Y., Pang, H., Zhang, W., Li, Y., Wu, S., and Hou, S.: Effects of
changes in moisture source and the upstream rainout on stable isotopes in
precipitation – a case study in Nanjing, eastern China, Hydrol. Earth Syst.
Sci., 19, 4293–4306, https://doi.org/10.5194/hess-19-4293-2015, 2015.
Thompson, L. G., Yao, T., Mosley-Thompson, E., Davis, M .E., Henderson, K.
A., and Lin, P. N.: A high-resolution millennial record of the South Asian
monsoon from Himalayan ice cores, Science, 289, 1916–1919,
https://doi.org/10.1126/science.289.5486.1916, 2000.
Tian, L. D., Yao, T. D., Li, Z., MacClune, K., Wu, G. J., Xu, B. Q., Li, Y.
F., Lu, A. X., and Shen, Y. P.: Recent rapid warming trend revealed from the
isotopic record in Muztagata ice core, eastern Pamirs, J. Geophys. Res., 111,
D13103, https://doi.org/10.1029/2005JD006249, 2006.
Wang, J., Ye, B. S., Cui, Y. H., He, X. B., and Yang, G. J.: Spatial and
temporal variations of albedo on nine glaciers in western China from 2000 to
2011, Hydrol. Process, 28, 3454–3465, https://doi.org/10.1002/hyp.9883, 2014.
Wang, N., Yao, T. D., Pu, J. C., Zhang, Y. L., Sun, W. Z., and Wang, Y. Q.:
Variations in air temperature during the last 100 years revealed by δ18O in the Malan ice core from the Tibetan plateau, Chinese Sci. Bull.,
48, 2134–1238, https://doi.org/10.1360/02wd0539, 2003.
Wang, Y. Q., Pu, J. C., Zhang, Y. L., and Sun, W. Z.: Characteristic of
present warming change recorded in Malan ice core, central Tibetan Plateau,
J. Glaciol. Geocryol., 25, 130–134, 2003 (in Chinese with English
abstracts).
Yang, B., Qin, C., Wang, J. L., He, M. H., Melvin, T. M., Osbornb, T. J., and
Briffa, K. R.: A 3,500-year tree-ring record of annual precipitation on the
northeastern Tibetan Plateau, P. Natl. Acad. Sci. USA, 111, 2903–2908,
https://doi.org/10.1073/pnas.1319238111, 2014.
Yang, K., Wu, H., Qin, J., Lin, C. G., Tang, W. J., and Chen, Y. Y.: Recent
climate changes over the Tibetan Plateau and their impacts on energy and
water cycle: A review, Global Planet. Change, 112, 79–91,
https://doi.org/10.1016/j.gloplacha.2013.12.001, 2014.
Yan, L. B. and Liu, X. D.: Has Climatic Warming over the Tibetan Plateau
Paused or Continued in Recent Years?, J. Earth Ocean Atmos. Sci., 1, 13–28,
2014.
Yang, X. X., Yao, T. D., Joswiak, D., and Yao, P.: Integration of Tibetan
Plateau ice-core temperature records and the influence of atmospheric
circulation on isotopic signals in the past century, Quaternary Res., 81,
520–530, https://doi.org/10.1016/j.yqres.2014.01.006, 2014.
Yao, T. D., Guo, X. J., Lonnie, T., Duan, K. Q., Wang, N. L., Pu, J. C., Xu,
B. Q., Yang, X. X., and Sun, W. Z.: δ18O record and temperature
change over the past 100 years in ice cores on the Tibetan Plateau, Sci.
China Ser. A, 49, 1–9, https://doi.org/10.1007/s11430-004-5096-2, 2006.
Yao, T. D., Thompson, L., Yang, W., Yu, W. S., Gao, Y., Guo, X. J., Yang, X.
X., Duan, K. Q., Zhao, H. B., Baiqing Xu, B. Q., Pu, J. C., Anxin Lu, A. X.,
Xiang, Y., Kattel D. B., and Joswiak, D.: Different glacier status with
atmospheric circulations in Tibetan Plateau and surroundings, Nature Climate
Change, 2, 663–667, https://doi.org/10.1038/nclimate1580, 2012.
Yao, T. D., Masson-Delmotte, V., Gao, J., Yu, W. S., Yang, X. X., Risi, C.,
Sturm, C., Werner, M., Zhao, H. B., He, Y., Ren, W., Tian, L. D., Shi, C. M.,
and Hou, S. G.: A review of climatic controls on δ18O in
precipitation over the Tibetan Plateau: Observations and simulations, Rev.
Geophys., 51, 525–548, https://doi.org/10.1002/rog.20023, 2013.
Yu, W. S., Ma, Y. M., Sun, W. Z., and Wang, Y.: Climatic significance of
δ18O records from precipitation on the western Tibetan Plateau,
Chinese Sci. Bull., 54, 2732–2741, https://doi.org/10.1007/s11434-009-0495-6, 2009.
Zhang, W. B., Hou, S. G., An, W. L., Zhou, L. Y., and Pang, H. X.: Variations
of atmospheric dust loading since 1951 AD recorded in an ice core from the
North Tibet Plateau, Ann. Glaciol., 57, https://doi.org/10.3189/2016AoG71A559, 2016.
Zheng, W., Yao, T. D., Joswiak, D. R., Xu, B. Q., Wang, N. L., and Zhao, H.
B.: Major ions compostion records from a shallow ice core on Mt. Tanggula in
the central Qinghai-Tibetan Plateau, Atmos. Res., 97, 70–79,
https://doi.org/10.1016/j.atmosres.2010.03.008, 2010.
Short summary
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...
