A 1000-year hydroclimate record from the Asian summer monsoon-Westerlies transition zone in the northeastern Qinghai-Tibetan Plateau
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science,Global and Planetary Change
Link
https://link.springer.com/content/pdf/10.1007/s10584-023-03497-1.pdf
Reference102 articles.
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2. Bard E, Raisbeck G, Yiou F, Jouzel J (2000) Solar irradiance during the last 1200 years based on cosmogenic nuclides. Tellus B 52(3):985–992. https://doi.org/10.1034/j.1600-0889.2000.d01-7.x
3. Benson L (1993) Factors affecting 14C ages of lacustrine carbonates: timing and duration of the last high stand lake in the lahontan basin. Quat Res 39(2):163–174. https://doi.org/10.1006/qres.1993.1020
4. Blaauw M, Christen JA (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Anal 6(3):457–474. https://doi.org/10.1214/11-BA618
5. Cao J, Zhang J, Zhang C, Chen F (2007) Environmental change during the past 800 years recorded in lake sediments from Hala Lake on the northern Tibetan Plateau. Quaternary Sci 27(1):100–107. (in Chinese with English abstract) https://doi.org/10.3321/j.issn:1001-7410.2007.01.012
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