By the analyses of Guliya ice core on the Ti-betan Plateau, it was found that the calcium (Ca2+) origi-nated from the terrestrial source is the main cation of soluble aerosol and a good proxy of the atmospheric compon...
Based on the study of oxygen isotope and mi-croparticle in the Guliya ice core, atmospheric dust and en-vironmental changes in the northwest Tibetan Plateau since the last interglacial were revealed. The microparticle...
This work was supported by the Chinese National Committee of Science and Technology (Grant No. G1998040800);the Chinese Academy of Sciences (Grant No. KZCX1-10-02); the National Natural Science Foundation of China (Grant No. 49801004); the US NSF-ESH
Evidence for the '8.2 ka cold event' has been provided mostly from the circum-North Atlantic area. However, whether this cold event occurred in other places is a key to understanding its cause. Here, we provide the ev...
the National Key Project for Basic Research (Grant No. G1998040800) and the Chinese Academy of Sciences (Grant No. KZCX2-301).
Based on ice core records in the Tibetan Plateau and Greenland, the features and possible causes of climatic changes on orbital and sub-orbital time scale were discussed. Orbital time scale climatic change recorded in...
Under the auspices of the G1998040802; BX2001-03 and KXCX2-301 programs
The correlations of the d18Omax in the shallow ice core from the Guliya ice cap on the Tibetan Plateau with the global sea surface temperatures (SST) and height at the 500 hPa over the Northern Hemisphere were analyze...
Whether the solar activity was very low, and especially whether the solar cycle existed, during the Maunder Minimum (1645-1715 AD), have been disputed for a long time. In this paper we use the Guliya NO3 data, which c...
Project supported by Chinese Academy of Sciences (Grant No. G1998040800, KZ951-A1-402-03, KZ951-A1-204-02 and KZ951-B1-212).
Based on the Guliya ice core records, the precipitation in the past 400 years was retrieved. Its relations with other regions were also analyzed. The results demonstrated that there were two high-precipitation periods...
G1998040800,KZ951-A1-204-02,KZ951-A1-402 and 95-Yu-24.
Examination of ENSO events and the accumulated precipitation and δ^(18)O values recorded in the Guliya ice core,China,shows that the relationship between the occurrence of ENSO events and the precipitation anomaly in...
A 36CI peak was found in the predicted section of Guliya ice core, from the Qinghai-Tibetan Plateau, at about 37 kaBP. This cannot be interpreted by means of changes in the accumulation rate, but by the enhanced cosmo...
Project supported by the Ministry of Science and Technology of China and the KZ 951-A1-202-04 project of the Chinese Academy of Sciences.
The high-resolution records of δ18O and snow accumulation variations from the Guliya ice core provide valuable data for research on climatic variations at a decadal resolution during the past 2000 years in China. Bas...