Xu Peng

ORCID: 0000-0002-6939-6264
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Cryospheric studies and observations
  • Geological formations and processes
  • Landslides and related hazards
  • Tree-ring climate responses
  • Oceanographic and Atmospheric Processes
  • Cultural Heritage Materials Analysis
  • Environmental Changes in China
  • Climate change and permafrost
  • Building materials and conservation
  • Conservation Techniques and Studies
  • Pleistocene-Era Hominins and Archaeology
  • Environmental and Agricultural Sciences
  • Climate variability and models
  • Ocean Waves and Remote Sensing

Peking University
2018-2024

Chinese Academy of Sciences
2012

Institute of Geographic Sciences and Natural Resources Research
2012

ABSTRACT This study investigates the late Quaternary glacial history of Cogarbu valley on northern slopes Bhutanese Himalaya using 10 Be surface exposure dating. Five major events were constrained based 28 ages. The equilibrium line altitude (ELA) oldest and most extensive event (M5–M9) is ∼489 m lower than present, followed by four other (M4, M3, M2 M1) with ELA depressions ∼452, ∼200, ∼76 ∼42 m, respectively. ages are ∼23.4–19.1 ka, corresponding to global Last Glacial Maximum (gLGM)....

10.1002/jqs.3079 article EN Journal of Quaternary Science 2018-12-14

Abstract Moraines preserved around Mount Xuebaoding (5588 m above sea level) on the eastern margin of Tibetan Plateau, represent past glacial activity in this area. The chronology these moraines was established using 10 Be exposure dating. dating results revealed multiple events prior to late ( > 14.1±2.2 ka), (15.6±1.6 11.2±3.0 early-middle Holocene (9.1±0.9 6.7±0.7 and Neoglacial periods (2.5±0.5 1.5±0.1 ka). These stages are consistent with recalculated ages from surrounding areas...

10.1017/qua.2018.33 article EN Quaternary Research 2018-06-18

This study investigates the sensitivity of Sverdrup transport to NCEP/NCAR, ERA-Interim, CCMP, and QSCAT wind products over tropical North Pacific Ocean during period 2000–2008. Our analyses show that all S-E transports in reanalysis/analysis winds are northward band 7–9° N except wind, which produces more realistic southward as shown meridional geostrophic (MGTs) calculated from WOA13 Argo data. At 24° N, high-resolution can better estimate this region. 8° although CCMP has same high...

10.1007/s10236-019-01260-8 article EN cc-by Ocean Dynamics 2019-03-15
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