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| 1 | Amplitude of climatic changes in Qinghai-Tibetan Plateau显示文摘On the basis of ice core and meteorological data from the Qinghai-Tibetan (Q-l) Plateau, this article focuses on the discussion of the problems related to the sensitivity of temporal and spatial changes of the climate in high-altitude regions, particularly in the Q-T Plateau. The features of abrupt climatic changes of the past 100 ka, 2 000 a and recent years indicate that the amplitude of these changes in the Q-T Plateau was obviously larger than that in low-altitude regions. The scope of temperature change above 6 000 m in the Q-T Plateau between glacial and interglacial stages could reach over 10C℃, but only about 4℃ in low-elevation regions close to sea level. During the last 2 000 a, the amplitude of temperature changes at Guliya (over 6 000 m a.s.l.) in the Q-T Plateau reached 7℃, in comparison with 2℃ in eastern China at low altitude. In the present age, apparent differences of climatic warming have been observed in the Q-T Plateau, indicating that the warming in high-elevation regions is | YAO Tandong LIU Xiaodong WANG Ninglian SHI Yafeng | 2000 | Chinese Science Bulletin2000，45，13： | 47 |
| 2 | Evidence for cold events in the early Holocene from the Guliya ice core, Tibetan Plateau,China显示文摘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 evidence for the '8.2 ka cold event' from the Guliya ice core in the northwest Tibetan Plateau, and it was found that the peak cooling (-8.3-8.2 ka) in this ice core was about 7.8-10°C, which was larger than the cooling in the North Atlantic region. The primary causes for this episode were diminished solar activity and weakened thermohaline circulation. Moreover, another weak cold event, centered about 9.4 ka, was also recorded in the Guliya ice core record. These two cold events were concurrent with the ice-rafting episodes in the North Atlantic during the early Holocene, which implies that the millennial-scale climatic cyclicity might exist in the Tibetan Plateau as well as in the North Atlantic. | WANG Ninglian YAO Tandong L.G.Thompson K.A.Henderson M.E.Davis | 2002 | Chinese Science Bulletin2002，47，17： | 23 |
| 3 | Variations in equilibrium line altitude of the Qiyi Glacier,Qilian Mountains,over the past 50 years显示文摘Based on observations of the equilibrium line altitude(ELA)of the Qiyi Glacier in the Qilian Mountain,we established a statistical model between ELA and its major influencing factors,warm season air temperature(air temperature averages for September,July and August)and cold season precipitation(total precipitation in the period January through March).Warm season air temperature was the leading climatic factor influencing ELA variations.The glacier ELA ascends(descends)172 m when warm season air temperature increases(decreases)by 1°C,and ascends(descends)62 m when cold season precipitation decreases(increases)by 10%.In the period 1958-2008,the glacier ELA showed a general increasing trend,ascending 230 m and reaching its highest altitude in 2006 at 5131 m a.s.l.,close to the glacier summit.If future climate is similar to that in the period 2001-2008,the Qiyi Glacier will not stabilize until it retreats by 2.08 km. | WANG NingLian HE JianQiao PU JianChen JIANG Xi JING ZheFan | 2010 | Chinese Science Bulletin2010，55，33： | 22 |
| 4 | Variations in air temperature during the last 100 years revealed by δ^(18)O in the Malan ice core from the Tibetan Plateau显示文摘By comprehensive analyses, it was found that the variations in d 18O recorded in Malan ice core from theKekexili Region on the Tibetan Plateau could represent thechanges in air temperature during the summer half year (from May to October) over the Kekexili Region and the northern margin of the Tibetan Plateau. The general increase trend in d18O in this ice core during the past century indicated climate warming, and it was estimated that air temperature during the summer half-year rose about 1.2C over there then. However, this ice core record documented that the study area has been cooling while most of the world has been dramatically warming since the late 1970s. A teleconnection was foundbetween the variations in d 18O in the Malan ice core and the North Atlantic Oscillation. Moreover, the variations in d 18O in this ice core were similar to that in the summer half-year air temperature over the southern Tibetan Plateau on thecenturial time scale, but opposite on the multidecadal timescale. | WANG Ninglian, YAO Tandong, PU Jianchen, ZHANG Yongliang, SUN Weizhen & WANG Youqing Key Laboratory of Ice Core and Cold Regions Environment, Cold and Arid Regions Environmental and Engineering Research Institute, ChineseAcademy of Sciences, Lanzhou 730000, China | 2003 | Chinese Science Bulletin2003，48，19： | 19 |
| 5 | Tracing the major source area of the mountainous runoff generation of the Heihe River in northwest China using stable isotope technique显示文摘Based on the data of δ18O in precipitation during the period of April 2006 through May 2007 in the upper catchment of the main stream of the Heihe River in the Qilian Mountains, we found that there existed an evident altitude effect on δ18O in precipitation, and the δ18O-altitude gradient was _0.18‰/100 m. When δ18O in river water at the outlet of the mountainous drainage area of the main stream of the Heihe River was combined with the δ18O-altitude relation, it was realized that the mountainous runoff was generated mostly at high altitudes. Using two component models, we revealed that 80.2% of the annual total mountainous runoff amount was generated at the alpine permafrost-snow-ice zone with an altitude of above 3600 m a.s.l. | WANG NingLian ZHANG ShiBiao HE JianQiao PU JianChen WU XiaoBo JIANG Xi | 2009 | Chinese Science Bulletin2009，54，16： | 16 |
| 6 | A distributed surface energy and mass balance model and its application to a mountain glacier in China显示文摘Based on the field observations on Qiyi Glacier during the warm season of 2007,using a digital elevation model(DEM,15 m resolution),we developed a distributed surface energy-and mass-balance model with an hourly resolution.The model described the effect of topography on shortwave solar radiation,and used a new parameterization for glacier albedo.The model was applied to Qiyi Glacier in the Qilian Mountain,China,for the period 20:00 30 June to 12:00 10 October 2007,to simulate the firn-line changes,the temporal and spatial variations of mass balance,and the glacial meltwater runoff.The results indicated that the patterns of altitudinal profile of glacier mass-balance were affected mainly by the altitudinal profile of albedo,and the status of the glacier mass balance was influenced directly by the values of albedo.The parameter sensitivity test showed that the model was sensitive to the air temperature lapse rate and precipitation gradient,and also sensitive to the threshold temperature for solid/liquid precipitation.Furthermore,the climate sensitivity test showed that the mass balance was more sensitive to air temperature than precipitation,and the response of mass balance to air temperature change was nonlinear while the response to precipitation change linearly.The negative mass balance trend of the glacier can not be reversed when precipitation increases by 20%and meanwhile air temperature rises by 1°C. | JIANG Xi WANG NingLian HE JianQiao WU XiaoBo SONG GaoJu | 2010 | Chinese Science Bulletin2010，55，20： | 11 |
| 7 | Climate change and its impacts on mountain glaciers during 1960–2017 in western China显示文摘Mountain glaciers are highly sensitive to climate change. In this paper, we systematically analyzed and discussed the responses of glaciers to climate change during 1960–2017 in western China by the methods of least squares and correlation analysis. Results show that the maximum temperature, minimum temperature, average temperature, and precipitation significantly increased in western China at the rates of 0.32°C/10 a, 0.48°C/10 a, 0.39°C/10 a, and 11.20 mm/10 a, respectively. However, the wind speed, hours of sunshine, snowfall, and snowy days displayed decreasing trends at the rates of –0.53 m/(s·10 a), 3.72 h/10 a, –2.90 mm/10 a, and –0.10 d/10 a, respectively. The annual percentage of glacier area decreased by approximately 0.42%, and the average glacier area decreased by 2.76 km^2/a. Meanwhile, glacial shrinkages were greater in the Altay Mountains, Tanggula Mountains, and Qilian Mountains than in the other mountainous regions. Glacier accumulation decreased while melt volume increased at a rate of 2.7×10~4 m^3/a. The area of melt volume was 1.3 times that of the glacier accumulation area. The glacier mass balance(GMB) decreased substantially at a rate of –14.0 mm/a, whereas the equilibrium line altitude(ELA) showed an increasing trend at a rate of 0.5 mm/a. After 1997, the mass was smaller than –500.0 mm, indicating a huge loss in glaciers. Furthermore, relationships between ELA and GMB and various climatic factors were established. Temperature and precipitation demonstrated a significantly negative correlation, whereas wind speed and snowy days had significantly positive correlations with GMB. Snowy days also exhibited a remarkably negative correlation with ELA. The strong warming trend and less snowy days were thought to be the main factors leading to glacial melting, whereas the increase in precipitation, and reductions of sunshine hours and wind speed might slow glacial melting. | LIU Yinge WANG Ninglian ZHANG Junhui WANG Lingang | 2019 | Journal of Arid Land2019，11，4： | 8 |
| 8 | Accumulation in Dasuopu ice core in Qinghai-Tibet Plateau and solar activity显示文摘The time series of accumulation in recent 300 years correlated well with solar activity in Dasuopu ice core. Results of spectrum analysis on the accumulation time series of the Dasuopu ice core shows that there are some periods that coincide with the periods of solar activity. By comparing the long-time change trend of the accumulation in the Dasuopu ice core with various kinds of indexes of solar activity intensity, a negative correlation is found between the trend and solar activity. | Keqin Duan Ninglian Wang Yuefang Li Weizheng Sun | 2000 | Chinese Science Bulletin2000，45，11： | 8 |
| 9 | Numerical simulation of Urumqi Glacier No.1 in the eastern Tianshan,central Asia from 2005 to 2070显示文摘Due to climate changes, most of the alpine glaciers have retreated dramatically during the past decades. Thus it is significant to predict the alpine glacier variability in the future for a better understanding of the impact of climate changes on water resource. In this paper, we perform the numerical simulation on Urumqi Glacier No.1 in the eastern Tianshan, central Asia (hereafter Glacier No.1 for short) by considering both the mass balance and ice flow. Given the shape of the Glacier No.1, the velocity of the glacier is obtained by solving a two-dimensional nonlinear Stokes equation and simulated result is in agreement with the observation. In order to predict the variability of Glacier No.1 in the next decades, a climatic scenario is constructed with a temperature rise rate as 0.17°C/10 a and precipitation as constant during the period of 2005-2070. The simulation shows that, the glacier terminus will retreat slowly and the glacier will thin dramatically before 2040, while after year 2040, the glacier terminus retreat will accelerate. This study confirms the increasing retreat rate of alpine glaciers under global warming. | DUAN KeQin YAO TanDong WANG NingLian LIU HuanCai | 2012 | Chinese Science Bulletin2012，57，34： | 7 |
| 10 | Compositional characteristics of n-alkanes of the glaciers over the Tibetan Plateau and their environmental and climatic significances显示文摘We report on the concentration and compositional features of n-alkanes of natural and anthropogenic origins in the snow samples collected from the Qiyi glacier in the Qilian Mountains, the Yuzhufeng glacier in eastern Kunlun Mountains, the Xiaodongkemadi glacier in the Tanggula Mountains, and the Gurenhekou glacier in the Nyainqêntanglha Range. The results indicate a decrease in the total n-alkane concentration (T-HCs) from the northeast to the south over the Tibetan Plateau. The T-HCs in these studied areas were close to those in the Belukha and Sofiyskiy glacier, Russian Alati Mountains and the Dasuopu glacier in the Himalaya but were much higher than those in the Greenland ice sheet, suggesting that the mountain glaciers in the Asian continent may receive a higher loading of n-alkanes than the Greenland ice core. Moreover, the compositional characteristics of n-alkanes indicated that the n-alkanes in the studied areas were probably originated from the plant waxes as well as the fossil-fuel combustion exhaust, whereas the contribution from the lower organisms was small. In addition, the plant wax (Cn(wax)) and anthropogenic (non-Cn(wax)) contributions revealed that fast industrialization may have significant effects on the organic pollutant composition in glacier over the Tibetan Plateau and its circumference environment. Particularly, except for the Yuzhufeng glacier, the ΣnC21-/ΣnC22+ and (nC15+nC17+nC19)/(nC27+nC29+nC31) ratio decreased from the Qiyi glacier to the Gurenhekou glacier over the Tibetan Plateau, while the carbon preference index (CPI) values increased. These results indicate a decrease in terrigenous input while an increase in marine input from the northeast to the south over the Tibetan Plateau. These two ratios can be used as the climatic and environmental change indicators. | LI QuanLian WANG NingLian WU XiaoBo PU JianChen HE JianQiao XIE Jun | 2009 | Science China Earth Sciences2009，52，11： | 6 |
| 11 | Sources and distribution of polycyclic aromatic hydrocarbons of different glaciers over the Tibetan Plateau显示文摘Twenty snow samples were collected from the Qiyi glacier in Qilian Mountains,the Yuzhufeng glacier in eastern Kunlun Mountains,the Xiaodongkemadi glacier in Tanggula Mountains,and the Gurenhekou glacier in Nyainqêntanglha Range over the Tibetan Plateau.The concentration and distribution features of sixteen priority Polycyclic Aromatic Hydrocarbons (PAHs) were determined by gas chromatography equipped with a mass spectrometry detector (GC-MS).The sources of these PAHs were explored as well.Our results indicated that the average concentrations of PAHs in snow were in the range of 20.45 60.57 ng/L.Maximum PAHs levels were found in the YZF glacier andminimum in the XDKMD glacier.However,no apparent regional distribution pattern of PAHs was found in the glaciers over the Tibetan Plateau.Moreover,the 2 4 ring low molecular weight PAHs predominated in snow samples and the concentrations of phenanthrene was the highest.Integrated factor analysis and isomer pair ratios suggested that PAHs of glaciers over the Tibetan Plateau were derived from low temperature combustion of coal and biomass,and partially from the exhaust gas of locomotives.Air mass back trajectory indicated that organic compounds detected in snowpit of these four glaciers,in the period of time they represented,mainly came from Central Asia and the arid area of Northwest China by westerly wind circulation. | LI QuanLian WANG NingLian WU XiaoBo PU JianChen HE JianQiao ZHANG ChunWen | 2011 | Science China Earth Sciences2011，54，8： | 5 |
| 12 | Concentration of nitrate in the Guliya ice core from theQinghai-Xizang Plateau and the solar activity显示文摘The variations of NO\+-\-3 concentration in the Guliya ice core are reconstructed for recent about 1 000 a. Spectrum analysis of NO\+-\-3 indicates significant periodicities in the variations of NO\+-\-3 concentration, which coincide with the periodicities of the solar activity. Therefore, a positive correlation between the variations of NO\+-\-3 concentration and the solar activity is found. | Ninglian Wang Tandong Yao L. G. Thompson | 1998 | Chinese Science Bulletin1998，43，10： | 5 |
| 13 | Events of abrupt change of Indian monsoon recorded in Dasuopu ice core from Himalayas显示文摘Three ice cores distributed across Dasuopu glacier in Himalayas were recovered. A 400-year net annual accumulation record reconstructed from one of the cores reflects the major precipitation trend in the central Himalayas. This record is related closely to the Indian monsoon precipitation. Wavelet and moving T-test were applied to the 400-year-long Dasuopu accumulation record, and significant staggered variability and abrupt change of the record on interannual to centennial time scales are identified. Finally the possible reason for abrupt change of the accumulation record is discussed. | Keqin Duan Ninglian Wang Jianchen Pu | 2002 | Chinese Science Bulletin2002，47，8： | 5 |
| 14 | Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau显示文摘By analyses of the dust layers in the Malan ice core from the northern Tibetan Plateau, it was found that dirty ratio in this core might be a good proxy for dust event frequency. The variations in the dirty ratio displayed a de- crease trend over the past 200 years, which implies that dust events became less frequent during the study period. The decrease trend in the variations in dust event frequency might be caused mostly by the natural processes, including increasing precipitation and weakening westerly which might be related with global warming. Furthermore, significant negative correlation was found between the dirty ratio and δ 18O in the Malan ice core. This is highly important for studying the effect of atmospheric dust on climate change. | WANG Ninglian Key Laboratory of Cryosphere and Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 73000, China Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China | 2005 | Chinese Science Bulletin2005，50，24： | 5 |
| 15 | Environmental information recorded in shallow ice core of Dasuopu glacier in the Qinghai-Tibetan Plateau显示文摘 | Cuilan Huang Tandong Yao Jianchen Pu Keqin Duan Ninglian Wang Lide Tian | 1998 | Chinese Science Bulletin1998，43，22： | 5 |
| 16 | Responses to climate warming of hydrological processes in the upper Kelan River in the Altay Mountains, Xinjiang, China显示文摘Kelan River is a branch of the Ertix River, originating in the Altay Mountains in Xinjiang, northwestern China. The upper streams of the Kelan River are located on the southern slope of the Altay Mountains; they arise from small glacial lakes at an elevation of more than 2,500 m. The total water-collection area of the studied basin, from 988 to 3,480 m, is about 1,655 km2. Almost 95 percent of the basin area is covered with snow in winter. The westerly air masses deplete nearly all the moisture that comes in the form of snow during the winter months in the upper and middle reaches of the basin. That annual flow from the basin is about 382 mm, about 45 percent of which is contributed by snowmelt. The mean annual precipitation in the basin is about 620 mm, which is primarily concentrated in the upper and middle basin. The Kelan River system could be vulnerable to climate change because of substantial contribution from snowmelt runoff. The hydrological system could be altered significantly because of a warming of the climate. The impact of climate change on the hydrological cycle and events would pose an additional threat to the Altay region. The Kelan River, a typical snow-dominated watershed, has more area at higher elevations and accumulates snow during the winter. The peak flow occurs as a result of snow-melting during the late spring or early summer. Stream flow varies strongly throughout the year because of seasonal cycles of precipitation, snowpack, temperature, and groundwater. Changes in the temperature and precipitation affect the timing and volume of stream-flow. The stream-flow consists of contributions from meltwater of snow and ice and from runoff of rainfall. Therefore, it has low flow in winter, high flow during the spring and early summer as the snowpack melts, and less flows during the late summer. Because of the warming of the current climate change, hydrology processes of the Kelan River have undergone marked changes, as evidenced by the shift of the maximum flood peak discharge from May to June; the largest monthly runoffs also have an increment of about 15 percent related to before 1980; April-June runoff increased from the 60 percent of the annual runoff before 1980 to nearly 70 percent after 1990. The long-term trend shows temperature and precipitation increased mainly in the winter, but the rainfall declined in summer; hydrological process is manifested by the rising runoff in May and decreasing in June. Warming and the increase of winter and spring snowcover would lead to increased snowmelt, increasing the spring-flood hazards and the maximum flood discharge with disastrous consequences. The changed hydrological patterns caused by climate change have already impacted the urban water supply and agricultural and livestock production along the river. | YongPing Shen GuoYa Wang QingBai Wu NingLian Wang WeiYi Mao HongChao Su | 2010 | Research in Cold and Arid Regions2010，2，4： | 3 |
| 17 | Recent advances in precipitation-bias correction and application显示文摘Significant progresses have been made in recent years in precipitation data analyses at regional to global scales. This paper re-views and synthesizes recent advances in precipitation-bias corrections and applications in many countries and over the cold re-gions. The main objective of this review is to identify and examine gaps in regional and national precipitation-error analyses. This paper also discusses and recommends future research needs and directions. More effort and coordination are necessary in the determinations of precipitation biases on large regions across national borders. It is important to emphasize that bias cor-rections of precipitation measurements affect both water budget and energy balance calculations, particularly over the cold regions. | DaQing Yang 1, NingLian Wang 2, BaiSheng Ye 2, LiJuan Ma 3 1. Water and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, Alaska 99775-5860, USA. 2. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China. 3. Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081, China. | 2009 | Research in Cold and Arid Regions2009，1，3： | 3 |
| 18 | Concentration of trace elements and their sources in a snow pit from Yuzhu Peak, north-east Qinghai-Tibetan Plateau显示文摘In order to understand the potential influence of pollution from human activity on the natural cycle of trace elements in the at- mosphere over the eastern Kunlun mountains, north-eastern part of the Qinghai-Tibetan Plateau, concentrations of Al, Fe, Ba, Cd, Co, Cr, Cu, Li, Ni, Zn, Pb, Sb, Sr, U and V in a 75 cm-deep snow pit recovered from 5,800 m a.s.l. of the Yuzhu Peak Glacier on October 25, 2009, were determined by a sector field inductively coupled plasma mass spectrometry. The results indicate that con- centrations of the measured trace elements vary by orders of magnitude from one element to another ranging from the minimum value 1.2 pg/g (U) to the maximum value 293 ng/g (Fe); the value of Max/Min ranges from 7 pg/g (Sd) to 358 pg/g (Li). EFc val- ues of measured trace elements show that there are other important sources except dust for Cd, Sb, Zn, Pb and Cu. Comparison of the concentrations of the measured trace elements with those in other areas in the Tibetan Plateau indicates that trace element con- centrations for Yuzhu Peak are lower than those in east Tianshan and Muztagh Ata (Pamirs). Concentrations of some trace ele- ments are also lower than those in East Rongbuk Glacier. However, concentrations of all measured trace elements are extensively higher than those in Greenland and the Antarctic. | YueFang Li XiaoLan Shi NingLian Wang JianChen Pu TanDong Yao | 2011 | Research in Cold and Arid Regions2011，3，3： | 3 |
| 19 | Diurnal hydrological controls and non-filtration effects on minor and trace elements in stream water draining the Qiyi Glacier, Qilian Mountain显示文摘Diurnal minor and trace elements in glacial outflow water draining the Qiyi Glacier and associated hydrological controls as well as the filtration effects on water chemistry were examined. Results show that major ions, Li, Sr, and Ba are exported predominately as mobile monovalent or divalent ions and are controlled by hydrological variations over the diurnal cycle exhibiting an inverse concentration with discharge, suggesting that Li, Sr, and Ba can be used as tracers in subglacial hydrological investigations. Conversely, other elements (e.g. Fe, Al, and Cr) exhibit variations that are not strongly correlated with the discharge reflecting the physicochemical controls. The non-filtered operation appears not to strongly influence Sr and Ba, but has an effect on some elements such as Fe, Al, V, Ti, and Co, indicating that these changed elements are transported in particulate forms and thus their concentrations are highly dependent on particulate numbers in solutions. This implies that the immediate filtration after sampling is essential in hydrochemical studies at Alpine glacial basins due to subsequent mineral dissolution. | LI XiangYing QIN DaHe JING ZheFan LI YueFang WANG NingLian | 2013 | Science China Earth Sciences2013，56，1： | 3 |
| 20 | Carbonaceous particles in Muztagh Ata ice core,West Kunlun Mountains,China显示文摘Carbonaceous particles concentrations of OC and EC are determined using a two-step gas chroma-tography system in Muztagh Ata ice core covering the time period of 1955―2000.Over the period rep-resented by the core,OC and EC concentrations appear to have changed significantly,varied in the range of 17.7―216.7 and 6.5―124.6,and averaged 61.8,32.9 ng·g-1,respectively.The average concen-tration of EC in Muztagh Ata ice core is much lower than that in an Alpine ice core record(100―300 ng·g-1) during the same period,but it is a factor of 14 in Greenland ice core(2.3 ng·g-1),this may induce a strong impact on the snow albedo in the last 46 years in our study area.Observations indicate two periods with obviously high deposition concentrations(1955―1965 and 1974―1989) and two periods with low concentrations(1966―1973 and 1990―1995),as well as a recent increasing trend.By com-paring EC and SO42- concentration variations and deciphering OC/EC ratios recorded in the same ice core,we can judge roughly that the carbonaceous particles deposited in Muztagh Ata ice core were attributed to fossil fuel combustion sources. | LIU XianQin XU BaiQing YAO TanDong WANG NingLian WU GuangJian | 2008 | Chinese Science Bulletin2008，53，21： | 2 |
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