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| 1 | AMS dating on glacial tills at the source area of the Urumqi River in the Tianshan Mountains and its implications显示文摘Using accelerating mass spectrometry (AMS) dating method, a dating has been made on the primary calcium carbonate in tills and secondary calcium carbonate coating on till gravel and the roche moutonnee formed since the Last Glaciation at the source area of the Urumqi River valley in the Tianshan Mountains, northwestern China. The results reveal that the carbonate content in the tills in this noncarbonate area is high enough to date by AMS, that the carbon in the coatings on the newly exposed roche moutons and in the modern till is modern carbon and so the 14 C dating results in the ancient till can represent the actual ages of the till formation, and that the warm period during the Holocene began as early as 6 500 a B.P. and lasted to 1 800 a B.P. | Chaolu Yi Kexing Liu Zhijiu Cui | 1998 | Chinese Science Bulletin1998，43，20： | 15 |
| 2 | Late Pleistocene glaciation of the Hulifang Massif of Gongwang mountains in Yunnan Province显示文摘Late Pleistocene glaciation was restricted to only a few high mountains in eastern China. The Gongwang mountainsconstitute one ofthe typicalplacesonce glaciated.Geomorphic mapping of the area and the TL dating provides evidence for at least four distinct glaciations. YJT-I glacial advance occurred about100 ka BP and two TL absolute ages(101,100 ±7780 a BP;104,000±8300 a BP)indicate thisadvance happened during the Penultimale Glaciation.The early stage glacialadvance (YJT-II advance) during the last glaciation occurred about 40,920±3400 a BP. The last glacial maximum advance (YJT-IIIadvance)about18-25 ka BP,which sustained by two TL ages(18,230 ± 1420 a BP;25,420 ±2110 a BP).The Penultimale and the early stage glaciationswere more extensive and the lastglacialmaximum (LGM )and the late-glacialperiod (YJT-IV advance,10 ka BP) were progressively less extensive. Correlated with the other mountains in eastern China, these glacial advances in the Gongwang mountains justlike the advances in the western partsuch as Diancang mountains,Yulong mountains ofYunnan Province and the glacierseries are more complete than the adjacent mid-latitude regions such as Taibai mountain and Taiwan mountains and are roughly representativeofclimatechangesduring thelastglacialcyclein Yunnan Province. | ZHANG Wei CUI Zhijiu FENG Jinliag YI Chaolu YA NG Jianqiang | 2005 | Journal of Geographical Sciences2005，15，4： | 13 |
| 3 | ^(10)Be dating of boulders on moraines from the last glacial period in the Nyainqentanglha mountains,Tibet显示文摘Chronologies of glacial advances during the last glacial period in the Nyainqentanglha mountain range may provide constraints on the past climate in a transition zone of the Asian monsoon.We present 15 new10Be exposure ages from two moraines in the Payuwang valley,on the north slope of the range.The inner moraine has exposure ages ranging from 18.0±1.7 to 30.6±2.8 ka(n=10),with a mean age of 23.8±4.0 ka,corresponding to the global Last Glacial Maximum(LGM).The outer moraine yields exposure ages ranging from 18.0±1.6 to 39.9±3.7 ka(n=5).Evidence for weathering leads us to view the oldest age as a minimum age,placing moraine formation during MIS3.Chronologies from the last glacial period from south slope of the Nyainqentanglha support this interpretation.Thus,there appears to have been a local LGM(LLGM)during MIS3 and a more limited glacial advance during the global LGM.Glacial advances during MIS3 in the Nyainqentanglha may correlate with millennial-scale climate change(Heinrich events). | DONG GuoCheng YI ChaoLu Marc CAFFEE | 2014 | Science China Earth Sciences2014，57，2： | 10 |
| 4 | Evolution of permafrost in China during the last 20 ka显示文摘The formation and evolution of permafrost in China during the last 20 ka were reconstructed on the basis of large amount of paleo-permafrost remains and paleo-periglacial evidence, as well as paleo-glacial landforms, paleo-flora and paleofauna records. The results indicate that, during the local Last Glacial Maximum(LLGM) or local Last Permafrost Maximum(LLPMax), the extent of permafrost of China reached 5.3×106-5.4×106 km2, or thrice that of today, but permafrost shrank to only0.80×106-0.85×106 km2, or 50% that of present, during the local Holocene Megathermal Period(LHMP), or the local Last Permafrost Minimum(LLPMin). On the basis of the dating of periglacial remains and their distributive features, the extent of permafrost in China was delineated for the two periods of LLGM(LLPMax) and LHMP(LLPMin), and the evolution of permafrost in China was divided into seven periods as follows:(1) LLGM in Late Pleistocene(ca. 20000 to 13000-10800 a BP)with extensive evidence for the presence of intensive ice-wedge expansion for outlining its LLPMax extent;(2) A period of dramatically changing climate during the early Holocene(10800 to 8500-7000 a BP) when permafrost remained relatively stable but with a general trend of shrinking areal extent;(3) The LHMP in the Mid-Holocene(8500-7000 to 4000-3000 a BP)when permafrost degraded intensively and extensively, and shrank to the LLPMin;(4) Neoglaciation during the late Holocene(4000-3000 to 1000 a BP, when permafrost again expanded;(5) Medieval Warming Period(MWP) in the late Holocene(1000-500 a BP) when permafrost was in a relative decline;(6) Little Ice Age(LIA) in the late Holocene(500-100 a BP), when permafrost relatively expanded, and;(7) Recent warming(during the 20 th century), when permafrost continuously degraded and still is degrading. The paleo-climate, geography and paleopermafrost extents and other features were reconstructed for each of these seven periods. | Huijun JIN Xiaoying JIN Ruixia HE Dongliang LUO Xiaoli CHANG Shaoling WANG Sergey S MARCHENKO Sizhong YANG Chaolu YI Shijie LI Stuart A HARRIS | 2019 | Science China Earth Sciences2019，62，8： | 6 |
| 5 | Classical and nonclassical symmetry classifications of nonlinear wave equation with dissipation显示文摘A complete classical symmetry classification and a nonclassical symmetry classification of a class of nonlinear wave equations are given with three arbitrary parameter functions.The obtained results show that such nonlinear wave equations admit richer classical and nonclassical symmetries,leading to the conservation laws and the reduction of the wave equations.Some exact solutions of the considered wave equations for particular cases are derived. | Yinshan YUN Chaolu TEMUER | 2015 | Applied Mathematics and Mechanics(English Edition)2015，36，3： | 4 |
| 6 | On the Unusual Holocene Carbonate Sediment in Lake Nam Co,Central Tibet显示文摘In lacustrine sediments,aragonite is a widespread mineral,whereas monohydrocalcite is a rare carbonate mineral. In the cold and high-attitude Xizang (Tibetan) Plateau,where aragonite has been commonly found in lacustrine sediments,there is no aragonite,but low-Mg calcite,monohydrocalcite and trace dolomite. The lake receives solutes primarily from surface runoffs and remains fairly constant water chemistry for a long time. The total CaCO3 percentage in sediments could be controlled by evaporation and inflow of detrital materials. The absence of aragonite is unusual when compared to other lacustrine sediments from the Tibetan Plateau. This could be due to low Ca/Mg ratio,low salinity,low Mg and Ca concentration. Monohydrocalcite might precipitate from the lake water mediated by biological activities. Low-Mg calcite originated from minor ostracoda shell and the precipitation of lake water with biological activities. | LI Minghui KANG Shichang ZHU Liping WANG Feiyue WANG Junbo YI Chaolu FANG Xiaomin XIE Manping | 2009 | Journal of Mountain Science2009，6，4： | 3 |
| 7 | Late Glacial glacier-climate modeling in two valleys on the eastern slope of Samdainkangsang Peak, Nyaiqentanggulha Mountains显示文摘Well-preserved Late Glacial moraines in the Barenduo and Yuqiongqu valleys on the eastern slope of the Samdainkangsang Peak present an opportunity to reconstruct glacier extents and examine the character of the climate during the Late Glacial stage in the Nyaiqentanggulha Mountains.This study employs a coupled mass-balance and ice-flow model to reconstruct the glacier extents in the two valleys and assess the magnitudes of temperature and precipitation change during the Late Glacial period.Model results indicate that during the Late Glacial,the Barenduo valley contained an ice volume of 1.67×10~8m^3,with the equilibrium-line altitude(ELA)being^5500 m asl;and the Yuqiongqu valley had an ice volume of 5.56×10~8 m^3,with the ELA being^5470 m asl.A climate scenario,temperature depression of 2.6-2.8℃and 60-70%,percent of modern(1981-2010)precipitation,can sustain both of the Late Glacial glacier extents in the two valleys.A 50%increase or decrease from modern precipitation would have been coupled with the respective Late Glacial temperature depressions of 1.6 and 3.0℃in the Barenduo valley,and 2.1 and 2.8℃in the Yuqiongqu valley. | XU XiangKe DONG GuoCheng PAN BaoLin HU Gang BI WeiLi LIU JinHua YI ChaoLu | 2017 | Science China Earth Sciences2017，60，1： | 3 |
| 8 | Evaporite minerals and geochemistry of the upper 400<ce:hsp sp='0.25'/>m sediments in a core from the Western Qaidam Basin, Tibet显示文摘 | Minghui Li Xiaomin Fang Chaolu Yi Shaopeng Gao Weilin Zhang Albert Galy | 2009 | Quaternary International2009，，1： | 2 |
| 9 | Soil Properties in Two Soil Profiles from Terraces of the Nam Co Lake in Tibet,China显示文摘This article investigates the soil properties in two soil profiles from the terraces of the Nam Co Lake in Tibet,China. Profile 1,with a slope aspect to east,is 37 m,and profile 2,to southwest,is 32 m above the lake level. Twelve and nine layers were identified in profile 1 and profile 2,respectively,based on the color,texture,structure,moisture content,presence of carbonate,and root density. Grain sizes and measurements of water content,total organic carbon,total inorganic carbon,total carbon,pH value and electrical conductivity were all analyzed for each sample. The results show that soil is poorly developed because of sparse vegetation coverage and weak chemical weathering in the cold and arid area. The results also indicate that the soil properties are different between the two profiles and suggest that soil is better developed in profile 1 than in profile 2. These differences are ascribed to the dissimilarity of landform,vegetation and timing. Profile 1 faces to east as compared with profile 2 facing to southwest and gets less insolation and therefore less evaporation. Thus,vegetation grows better in profile 1 than in profile 2. Radiocarbon dating and OSL dating show that profile 1 underwent a longer soil forming process than profile 2,which is helpful for the soil development in profile 1. | WANG Liqiang YI Chaolu Brigitta Sehiitt LIU Kexin ZHOU Liping | 2009 | Journal of Mountain Science2009，6，4： | 2 |
| 10 | Symmetry analysis of modified 2D Burgers vortex equation for unsteady case显示文摘In this paper, a symmetry analysis of the modified 2D Burgers vortex equation with a flow parameter is presented. A general form of classical and non-classical symmetries of the equation is derived. These are fundamental tools for obtaining exact solutions to the equation. In several physical cases of the parameter, the specific classical and non-classical symmetries of the equation are then obtained. In addition to rediscovering the existing solutions given by different methods, some new exact solutions are obtained with the symmetry method, showing that the symmetry method is powerful and more general for solving partial differential equations(PDEs). | Lihua LIU Chaolu TEMUER | 2017 | Applied Mathematics and Mechanics(English Edition)2017，38，3： | 2 |
| 11 | Advances in numeri cal dating of Quaternary glaciations in China显示文摘 | Yi Chaolu Zhu Zhiyong Wei Li | 2007 | Zeitschrift fur Geomorpholgie2007，51，2： | 1 |
| 12 | Geomorphology of anomalously high glaciated mountains at the northwestern end of Tibet: Muztag Ata and Kongur Shan显示文摘 | Seong Y B Owen L A Yi Chaolu | 2009 | Geomorphology2009，103，2： | 1 |
| 13 | ANALYTIC SOLUTION AND NUMERICAL SOLUTION TO ENDOLYMPH EQUATION USING FRACTIONAL DERIVATIVE显示文摘In this paper,we study the solution to the endolymph equation using the fractional derivative of arbitrary orderλ(0<λ<1).The exact analytic solution is given by using Laplace transform in terms of Mittag-Leffler functions.We then evaluate the approximate numerical solution using MATLAB. | Duan Junsheng Liu Zhenhang Zhang Fengkuan Temuer Chaolu | 2008 | Annals of Differential Equations2008，24，1： | 1 |
| 14 | Fractal Solitons, Arbitrary Function Solutions, Exact Periodic Wave and Breathers for a Nonlinear Partial Differential Equation by Using Bilinear Neural Network Method显示文摘This paper extends a method, called bilinear neural network method(BNNM), to solve exact solutions to nonlinear partial differential equation. New, test functions are constructed by using this method. These test functions are composed of specific activation functions of single-layer model,specific activation functions of '2-2' model and arbitrary functions of '2-2-3' model. By means of the BNNM, nineteen sets of exact analytical solutions and twenty-four arbitrary function solutions of the dimensionally reduced p-gB KP equation are obtained via symbolic computation with the help of Maple. The fractal solitons waves are obtained by choosing appropriate values and the self-similar characteristics of these waves are observed by reducing the observation range and amplifying the partial picture. By giving a specific activation function in the single layer neural network model, exact periodic waves and breathers are obtained. Via various three-dimensional plots, contour plots and density plots,the evolution characteristic of these waves are exhibited. | ZHANG Runfa BILIGE Sudao CHAOLU Temuer | 2021 | Journal of Systems Science & Complexity2021，34，1： | 1 |
| 15 | An extended simplest equation method and its application to several forms of the fifth-order KdV equation显示文摘 | Sudao Bilige Temuer Chaolu | 2010 | Applied Mathematics and Computation2010，216，： | 1 |
| 16 | Quaternary glaciation of Puruogangri the largest modern ice field in Tibet显示文摘 | Yi Chaolu Li Xiaoze Qu Jianjun | 2002 | Quaternary International2002，9798，： | 1 |
| 17 | Effect of exercise and high - fat diet on plasma adiponeetin and nesfatin levels in mice 显示文摘 | Chaolu H Asakawa A Ushikai M | 2011 | Exp T- her Med2011，2，2： | 1 |
| 18 | ESR dating of the sediments of the Last Glaciation at the source area of the Urumqi River,Tianshan Mountains,China显示文摘 | Yi Chaolu Jiao Keqin Liu Kexin | 2002 | Quaternary International2002，9798，： | 1 |
| 19 | Comparison of the anorexigenic activity of CRF family peptides显示文摘 | Tanaka C Asakawa A Ushikai M Sakoguchi T Amitani H Terashi M Cheng K Chaolu H N | | 0，，： | 1 |
| 20 | Differential Characteristic Set Alogorithm for the Complete Symmetry Classifica- tion of (partial) Differential Equations显示文摘 | Thmuer Chaolu BAI Yu-shan | 2003 | Applied Mathematics And Mechanics2003，32，5： | 1 |
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