25 December 2006, Volume 28 Issue 6
    

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  • CHENG Guo-dong, SUN Zhi-zhong, NIU Fu-jun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 797-808. https://doi.org/10.7522/j.issn.1000-0240.2006.0117
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    About one-half of the permafrost area traversed by the Qinghai-Tibet Railway is warm permafrost with a mean annual ground temperature of 0 ~-1℃,and around 40% is ice-rich permafrost.The railway is expected to operate over 50~100 years,therefore,climate change for the next 50~100 years must be considered seriously.Traditionally,road constructions in permafrost regions rely passively on thermal resistance methods such as increasing embankment height and/or using thermal resistant materials to protect permafrost under roadbed from thawing.Under the global warming scenario,it is needed to take proactive methods to cool down the roadbed temperatures in order to maintain railway stability.Various roadbed cooling approaches have been adopted in the construction of the Qinghai-Tibet Railway,such as,shading board to reduce solar radiation,ventilated duct,thermosyphon,crushed rock interlayer and revetment to control thermal convection,"thermal diode" material to control thermal conduction,and the combination of above methods to enhance the cooling effect.Observational data have shown that all these roadbed cooling approaches can ensure the stability of railroad.
  • Max Clifton Brewer, JIN Hui-jun, HU Wan-zhi, ZHANG Xin-jia, CHEN Jian-feng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 809-817. https://doi.org/10.7522/j.issn.1000-0240.2006.0118
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    Alyeska had developed or used three major modes in the construction: conventional burial,special burial,and above ground modes.Conventional burial depths of the pipeline top vary from 0.9 to 2.7 m in accommodationto topography,but not soil conditions.Circulating coolant system and/or thermosyphons were equipped for the special burial at the animal passage sections where the pipeline has to be buried.The above ground mode include the pile bent and above ground gravel berms.The later was used only when the pipeline dips into ground and comes out of the ground.The elevated pile bent uses the vertical support member (VSM),with or without thermosyphons.During the initial planning and design phases,the owner companies,the Trans-Alyeska Pipeline System (TAPS),and later Alyeska Pipeline Service Company (APSC),staunchly demanded 100% burial.However,with the progress of survey and elaboration of designs,the construction modes had been changing all the time.When the construction was completed in 1977,only 57% of pipeline was buried,and some experienced engineers prefer 53% of burial after 30 years of operations.The "reasons" for the changes of construction modesinclude: 1) that they had to change in order to get the permit to cross Federal lands;2) they performed actual field investigations and participated in the development of the detailed engineering;and 3) National Environmental Policy Act (NEPA).Alyeska was the agent for the seven oil companies,and uncharacteristically,because of the size and costs of the project,the oil companies’ engineers individually participated to an unusual extent.In this paper,the authors present the organizational history of Alyeska and the US Federal and Alaska State governments as regards to the construction of the Alyeska Oil Pipeline,the process how the design was evolvedand the reasons and the philosophy behind them,and experiences and lessons learned from the Alyeska project.
  • DENG You-sheng, HE Ping, ZHOU Cheng-lin, LI Yi-chi, FANG Jian-hong, HUANG Shi-jing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 818-822. https://doi.org/10.7522/j.issn.1000-0240.2006.0119
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    Hydraulic diffusivities of unsaturated soil with the different salt contents,saline concentrations and dry densities were experimental studied by means of wet front advancing in a horizontal soil column.It is found that: 1) The hydraulic diffusivity of soil water or saline is an exponential function of water content,and decreases with decreasing water content;2) For the same type of soil when dry density and water content are the same,the hydraulic diffusivity of soil water increases with salt content,especially,for the coarse-grained soil;3) When saline migrates in the soil,the hydraulic diffusivity of saline decreases with saline concentration.
  • LI Shuang-yang, ZHANG Ming-yi, GAO Zhi-hua, ZHANG Shu-juan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 823-832. https://doi.org/10.7522/j.issn.1000-0240.2006.0120
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    In this paper,a subway tunnel in Guangzhou constructed by employing artificial freezing method is taken as an engineering example.Firstly,based on the governing differential equations of the transient temperature field with phase change and heat of hydration of lining cement,the temperature fields are analyzed through using finite element formulae deduced by Galerkin method.Then,according to the features of the temperature field,a frozen wall is determined,and the stresses and displacements of soils are computed and analyzed through using creep constitutive model for frozen soil and elastoplastic constitutive model for unfrozen soil.The results show that,as an auxiliary method to construct a tunnel,applying artificial freezing method to construct tunnel can satisfy not only the strength requirement of structures but also the requirement of settlements of ground surface.
  • LIU Guo-yu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 833-837. https://doi.org/10.7522/j.issn.1000-0240.2006.0121
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    Dabanshan highway tunnel,a highest tunnel in the world,is located in the cold region.The natural conditions are very special, for example,high altitude,cold climate,low oxygen content,more precipitation,relatively long winter,and so on.The annual mean air temperature is-3.1℃.The key engineering measures to keep the tunnel in normal work is how to control the damages caused by frost and water. Therefore,hard work was done by scientists from institutions of research,design and construction for reasonable engineering measures,prevention countermeasures and construction methods in order to assure the tunnel to work normally.
  • JIN Hui-jun, MA Wei, LAI Yuan-ming, WU Qing-bai, WANG Gui-rong, NIU Fu-jun, SHEN Yong-ping, ZHAO Shu-ping, Jerry Brown, Max C. Brewer
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 838-843. https://doi.org/10.7522/j.issn.1000-0240.2006.0122
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    Under the auspices of the Geographical Society of China and the International Permafrost Association,organized and hosted by the State Key Laboratory of Frozen Soils Engineering,Cold and Arid Region Environmental and Engineering Research Institute,Chinese Academy of Sciences,the First Asian Conference on Permafrost (ACOP) was successfully held in Lanzhou,along the Qinghai-Tibet Highway/Railway (QTH/R),and in Lhasa during 5~16 August 2006.Two hundred fifty three participants (99 overseas scholars) from 16 countries presented 128 papers on permafrost and cold regions science,engineering and technology in oral (90) and/or posters (38) formats.The ACOP themes ranged widely in the following five aspects: 1) permafrost engineering;2) frost hazards and periglacial environments in mountain and plateau areas;3) climate and environments in the cryosphere;4) permafrost hydrology,cold regions water resources and land use;and 5) monitoring,mapping and modeling of permafrost.The majority of the Chinese papers were more concentrated on the various scientific and innovative engineering of the QTR design construction.The Conference was preceded by an 1.5 day Workshop on the Classification,Mapping and Monitoring of Permafrost in Central Asia,attempting to develop a uniform classification system and mapping legend of permafrost in Central Asia and to uniformly map the permafrost in Central (High)-Middle Asia.Fifteen world leading geocryologists and foremost cold regions engineers were interviewed by the Xinghua News Agency,Science Times and local news media during the ACOP.More than 80 experts inspected the recently completed and operating QTR,and the QTH which have been in operation for more than 40 years.The filed-trip participants lively discussed the innovative permafrost engineering techniques applied by the QTR during the Workshop on Engineering and Environments along the QTH/R on 15 August.It is agreed that the permafrost engineering approaches and techniques are proper and effective,and therefore can ensure the long-term roadbed stability of the QTR.However,the cold regions environmental protection and management have a long problematic history;only the timely and comprehensive environmental mitigation and management under a logical legal system and powerful enforcement of environmental acts,stipulations and regulations can attain the objective of a concordant and sustainable development of socio-economical community and natural ecosystems in the interior of the Qinghai-Tibetan Plateau.
  • YU Qi-hao, Kurt Roth, JIN Hui-jun, PAN Xi-chai, Schiwek Philip Martin, SHEN Yu, WEI Zhi, WU Ji-chun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 844-849. https://doi.org/10.7522/j.issn.1000-0240.2006.0123
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    The Sino-German joint expedition from the Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences and the Institute of Environmental Physics,University of Heidelberg,Germany,conducted investigation and preliminary research on the degradation of permafrost on the Tibetan Plateau and its environmental impacts in the source regions of the Yangtze,Yellow and Lancang-Mekong Rivers in the eastern plateau and in the Tianshuihai area in the West Kunlun Mountains.Three long-term monitoring stations were established along the road from Yushu to Budongquan in Qinghai Province.In addition to conventional exploratory methods,such as hand pits,water and soil sampling,in situ measurements of soil moistures and temperatures,and surface surveys,new multi-channel ground penetrating radar (GPR) was applied for investigating structures of the active layer,permafrost,cryogenic phenomena and vegetation differentiations,ground water tables and soil moistures,and migration of salts.The preliminary research shows that the characteristics of surface landscapes have pronounced influences on the heat and mass transfers in soils.Major differences between cold (<-4℃) permafrost in the Tianshuihai area and warm (>-1℃) permafrost in the interior and eastern plateau can be seen in their tectonics and ground ice development,as well as ground temperatures.The ecological environments in the Tianshuihai area have changed greatly during the past 30 years: vegetation has degenerated or vanished in a large scale,together with considerable surface soil salinization.In the Tianshuihai area, small pingos,unsorted circles,sand wedges and polygons,and other periglacial phenomena were identified.GPR survey indicates that topography,vegetation,and surface moisture conditions have substantial impacts on the permafrost table and ground ice.
  • YANG Si-zhong, JIN Hui-jun, Bernhard Diekmann, Bernd Wünnemann, Steffen Mischke, JI Yan-jun, CHEN Jian-hui, YANG Qi-li
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 850-853. https://doi.org/10.7522/j.issn.1000-0240.2006.0124
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    Inland lakes and lacustrine sediments on the Qinghai-Tibet Plateau can provide reliable proxy records for paleoenvironmental reconstruction and are therefore studied by increasingly more researchers.A SinoGermany joint team investigated topography,geomorphology and sedimentology in the Donggi Conag Lake (220 km2;98°21’~98°43’E,35°13’~35°23’N;4081m) area on northeastern Qinghai-Tibet Plateau from 15 August to 10 September 2006. The lake terraces were analyzed by digital elevation model (DEM).The lake bottom profiles were preliminarily studied using shallow seismic,sonar and GPS instruments and several core samples of lake sediments up to 1.9 m in length were taken for further analyses.Permafrost was found along the eastern and western banks of this lake.Sediment analysis and geomorphology indicate the existence of Quaternary glaciations in a valley to the northeast of the Lake.It is preliminarily concluded that the Donggi Conag Lake was formed by fault settlement.To further understand climatic and environmental changes in this area,the Sino-German joint research team is planning to core lake sediments in March 2007.
  • WANG Guo-ya, SHEN Yong-ping, QIN Da-he
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 854-860. https://doi.org/10.7522/j.issn.1000-0240.2006.0125
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    The data of Issyk-Kul Lake level from 1860 to 2005 and the Tuyuksu Glacier snowline and air temperature in Karakol Station from 1879 to 1998 were analyzed,and the relationship between lake level fluctuation and regional climate change was revealed in the Issyk-Kul region over the past 145 years.It is found that a cold-humid climate occurred in the end of 19th and the beginning of 20th century,a cold-dry climate occurred from 1915 to 1962,and a warm-dry climate occurred from 1963 to 1986.The changes of lake level and glacier snowline indicated that the climate has shifted to warm-humid since 1986.By comparing the lake level of Issyk-Kul with Bosten Lake level,and the snowline altitudes of Tuyuksu Glacier with that of Glacier No.1,it is expected that the warm-humid climate will extend westwards from Northwest China to Issyk-Kul area.It is believed that this is a result of water cycle accelerating due to global warming.The increases of water vapor transported by westerly and Indian Ocean circulation or regional evaporation will result in precipitation increasing.
  • PU Jian-chen, YAO Tan-dong, TIAN Li-de
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 861-864. https://doi.org/10.7522/j.issn.1000-0240.2006.0126
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    Gurenhekou Glacier lies in the Yangbajain area of Nyainqêntanglha Range,variation of which was monitored during the period 2004-2006.The locations of glacier terminus in different periods were measured using the Global Position System (GPS).Combined with the topographic maps and aerophotos,it is concluded that the glacier retreating is distinct considerably from the Little Ice Age (LIA).In the maximum of the Little Ice Age,the altitude of glacier terminus was 100 m lower than that of present;the glacier shrinking rate was about 7.0 m·a-1 from the last of Little Ice Age to 1970 and 8.3 m·a-1 from 1970 to 2004,respectively.The shrinking rate was measured to be about 9.5 m·a-1 for the periods 2004-2005 and 17.0 m·a-1 for the period of 2005-2006,respectively.It is clear that under global warming,the glacier water resources will decrease considerably with the pronounced retreat of Gurenhekou Glacier in the Yangbajain area,Nyainqêntanglha Range.
  • DENG Yu-wu, XIE Zi-chu, QIN Jian-xin, WANG Xin, LI Qiao-yuan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 865-872. https://doi.org/10.7522/j.issn.1000-0240.2006.0127
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    On the basis of the glacier inventory of China,the calculated snow line (ELAhc) can be obtained,based on the linear relationship between ELAh and Hme.It is revealed that the more number of the data of ELAh,the more sound linear relationship between ELAh and Hme in a glacier system is.In order to minimize the influence of topographical snow-line and other uncertain error,a method is adopted that to overlay the data points with a graticule mesh of 10’×10’,and then to calculate arithmetic average values of all the data points’ longitude,latitude and ELAhc in every square,utilizing such software as ArcGIS 9,etc.Then an ELAhc distribution map,namely,the field of equilibrium line attitude,with an interval of 100 m,is produced by ordinary Kriging interpolation.In this paper it is found that: 1) The result in the recent equilibrium line attitude field is different from the previous ones from others,and shows more detail of glacier distribution in the southern Tibet glacier system,besides some common understanding;2) The field gradient of ELAhc is greater in the south than in the north of the Ganga-Yarlung Zangbo Rivers system,with 5 m·km-1 in the south and 0.5 m·km-1 in the north.Furthermore,the distribution of ELAhc is more complicated and the high ELAhc values and low ELAhc values appear alternative; 3) In this region the influence of precipitation on the distribution of ELAhc is more evident than the influence of temperature,because precipitation decreases westwards,and the ELAhc increases westwards,with a gradient of ELAhc varying from 2.5 m·km-1 to 4~6 m·km-1 from east to west.
  • LI Yong-neng, YANG Yang, HAN Jian-kang, XIE Zi-chu, Masayoshi Nakawo, Kumiko Goto-Azuma
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 873-878. https://doi.org/10.7522/j.issn.1000-0240.2006.0128
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    An ice core of 18.7 m long from Chongce Ice Cap (at an elevation of 6350 m),West Kunlun Mts.,China,showed an overall decrease in magnitude of the total particle content for about 100 years from the beginning of the 20 century.Three phases could be identified approximately: before 1930 (going back to 1903),1931-1960,and 1961-1992.The conspicuous periods include the early 1900s,1910s,late 1920s and early 1940s,of which the dust level was much higher,and the early 1970s,of which the dust level was relatively low.The dust deposit rate at the altitude was built up for the past 60 years.The mean is 1106 μg·cm-2·yr-1 with the maximum and minimum of 3462 and 77 μg·cm-2·yr-1,respectively. Analyzing the volume distribution of micro-particles obtained from size measurement,it is estimated that contribution of the local component is 17% of the total dust input.The rest could be taken as long-range transportation,i.e,the deposit of atmospheric dust burden in meso-large scale.Thus,the changing trend of dust flux at the troposphere altitude over the southern Taklimakan Desert is known.The calculated deposited dust flux for the 60 years before 1992 is 913 μg·cm-2·yr-1 in average,with a decreasing rate of-120 μg·cm-2 in a decade.This could be a representative of the regional record of the mid-upper troposphere dust burden in temporal tendency.
  • HAN Hai-dong, LIU Shi-yin, DING Yong-jian, XIE Chang-wei, ZHANG Yong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 879-884. https://doi.org/10.7522/j.issn.1000-0240.2006.0129
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    In this paper,investigation of scale and shape of 20 random selected ice cliffs in the debris-covered area of Koxkar Glacier is presented to explore the basic characteristics of ice cliffs.Tapelines,together with GPS equipments,are used in length and height measures of ice cliffs,and geological compass is utilized to survey orientation and slope angle of ice cliffs.Bare ice area of the ice cliffs is calculated from the length and height data.Analysis on these basic conformation data of ice cliffs shows that the scale of ice cliffs varies dramatically.The ice cliffs present a trend of decrease in size with altitude.The mechanism is the hypsography changing with altitude and the ice ablation decreasing from the lower ablation area to the upper ablation area.Moreover,investigation on the relationship between orientation and scale of the ice cliffs indicates that orientations of most ice cliffs are NW and NNE,along which ice cliffs also have the great scale.Analysis suggests that the direct solar radiation is the dominant factor that governs the distribution and evolution of ice cliffs.
  • NING Bao-ying, HE Yuan-qing, HE Xiao-zhong, PANG Hong-xi, YUAN Ling-ling, ZHAO Jing-dong, LU Ai-gang, SONG Bo
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 885-892. https://doi.org/10.7522/j.issn.1000-0240.2006.0130
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    The southernmost temperate glaciers in China located at Mt.Yulong are extremely sensitive to climate change,because of the unique geographical location and the glacier characteristics,such as overall shrinkage since the 20th century.Due to these characteristics,they are also attractive scenic spots and become important tourism resources in Lijiang.By the analysis on statistical data and investigation data,it is revealed that glacier retreat has evident influence on the local socio-economy,especially on Lijiang tourism,and residents’ life style.
  • GU Liang-lei, HU Ze-yong, LÜ Shi-hua, YAO Ji-min
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 893-899. https://doi.org/10.7522/j.issn.1000-0240.2006.0131
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    By using the radiosonde data,the temporal and spatial distributions and characteristics of wind velocity,potential temperature and specific humidity over North Tibet Plateau during summer were analyzed.It is found that the zonal wind components (meridional wind components) and the shears are smaller (greater) in clear day than those in cloudy day in August.The prevailing wind direction is west in Amdo and east in Naqu.Besides,the depths of SBL and the height of CBL are higher in clear day than in cloudy day.The specific humidity of the night is greater than that of the daytime,and also the specific humidity of the cloudy day is greater than that of the clear day.There are humidity inversion phenomena over the Tibet Plateau.The strong humidity inversion phenomena appear in night or noon.
  • HOU Yi-ling, LI Dong-liang, SHI Ya-feng, SHEN Yong-ping
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 900-908. https://doi.org/10.7522/j.issn.1000-0240.2006.0132
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    The climatic decadal variation in Northeast China and its responding to the Northern Hemisphere warming and snow cover area changing in Eurasia are analyzed and studied by using the observational data of 195 stations in Northeast China and 6 stations in Mongolia with EOF analyses and the means of separated time interval linear fitting.The results show that there are two temperature changing pattern in the studied regions.One is the consistent pattern in all of their sub-regions and one is the spatially-opposite pattern between the north and the south.In the recent 50 years,the mean temperature in Northeast China performed the course of increasing,especially in the 1990s,showing that the northern part of Northeast China was changing from cold-dry to warm-humid and the North China was changing form warm-humid to warm-dry.It was found that the mean temperature had two abrupt events in 1968 and 1985 in the southern part,while it was increasing in evidence in the northern part of Northeast China.It is considered that the warming of Northeast China was according to the Northern Hemisphere warming,and also responded to snow cover area changing in Eurasia.
  • XIE Ai-hong, REN Jia-wen, QIN Xiang, JIANG You-yan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 909-917. https://doi.org/10.7522/j.issn.1000-0240.2006.0133
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    An automatic weather station was set up on April 27 2005 at the Ruopula Pass (6523 m a.s.l.) on the northern slope of Mt.Qomolangma (Everest) by the team of integrated scientific expedition to Mt.Qomolangma.In this paper the meteorological features were analyzed based on the 10-minute-averaged and 24-hour records of air temperature,relative humidity,saturated vapor pressure,air pressure and wind from May 1 to July 22 in 2005.It is shown that at 6523 m a.s.l.of Mt.Qomolangma,these meteorological elements display very obvious diurnal variations,and the averaged diurnal variation was one-peak-one-vale for air temperature and saturated vapor pressure, one-vale for relative humidity,two-peak-two-vale for air pressure,and one-peak in an asymmetrical way for wind speed.In the 83 days,all the air temperature,relative humidity,saturated vapor pressure and air pressure increased with some fluctuations,while wind speed decreased gradually,and frequency of calm wind went up and wind direction turned from north to south.Variations of relative humidity and saturated vapor pressure have great fluctuation and obvious local difference.Finally,the reasons of the diurnal and daily variations are discussed.Compared with the records of May in 1960,the 5-day maximum,minimum and averaged values of air temperature in May 2005 were apparently lower.
  • YIN Chang-liang, TIAN Li-de, YU Wu-sheng, GONG Tong-liang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 918-924. https://doi.org/10.7522/j.issn.1000-0240.2006.0134
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    In this paper,the variations of δ18O of precipitation and the relationships between δ18O in precipitation and temperature and precipitation amount are analyzed by using the meteorological data observed in the summer of 2004 at Baidi,Wengguo and Duixiang Hydrographic Stations around the Yamzho Lake on the Tibetan Plateau.Precipitations at the three stations almost exhibit the same changing trend,showing a notable seasonal variation.Moreover,most of the precipitation events occur in summer,especially from June to September.The δ18O values in precipitation at the three stations also exhibit the same changing trend and they are high before the southwest monsoon onset,but begin to decrease when the southwest monsoon onset and then increase after the southwest monsoon retreat.The characteristic of low δ18O values in precipitation at the three stations correlates with southwest monsoon activity in summer.Affected by the southwest monsoon,the relationships between δ18O in precipitation and temperature are poor,It is found that the more precipitation amount is, the more depleted the δ18O is,which can be described as a precipitation amount effect that results in a poor δ18O-T relationship.The variations of δ18O in precipitation around the Yamzho Lake are similar to those in Lhasa.
  • MING Qing-zhong, SHI Zheng-tao, DENG Ya-jing, DONG Ming
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 925-930. https://doi.org/10.7522/j.issn.1000-0240.2006.0135
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    Mountain regions were 3-D landforms on the earth,which have obvious undulation and gradient.Because the natural factors and their consequent human activities vary with elevation and relative height,the high gradient effects of mountain regions appear.That is to say,the high gradient effects of mountain regions exhibit the natural factors and human dimension changing with elevation and relative height.These are integrated effects of evolution in the mountain system.The Hengduan Mountains are the typical upland-valley areas,where the high gradient effects of mountain regions are notable.The meaning of the high gradient effects includes high gradient effect about energy, precipitation, temperature, climate, climatic landforms, natural belts, social and economic activities and habitation etc.The energy includes gravity potential energy,heat energy and biomass etc.Research on the high gradient effects of mountain regions is the important activities responding to the "Global Change and Mountain Regions" which is put forward by IGBP,IHDP and GTOS.The study on the high gradient effects is an important method to go through the complex research on the mountains.It has great significance in the use of natural resources in the mountains,social economy development,ecological construction and regionally sustainable development.
  • ADILI·Azizi, WANG Jian-wen, ZHANG Jian-gang, MAO Wei-yi, ZHANG Li-ping, SHEN Yong-ping, WANG Shun-de, WANG Gang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 931-940. https://doi.org/10.7522/j.issn.1000-0240.2006.0136
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    The Tarim Basin is the biggest arid inland basin in China.The Aksu,Hotan,Yarkant and Kaidu-Konque Rivers are four source rivers of Tarim River drainage.The three tributary river systems (Aksu,Hotan and Yarkant) that contribute flows to the Tarim River join just above the Aler gauging station where the Tarim River begins.From the confluence of its three main contributing tributaries,the Tarim River mainstream extends 1 321 km to Taitema Lake.In addition the Kaidu-Konque River Basin,which is hydrologically separate from the Tarim River,contributes water to the Tarim River by means of a man-made transfer channel.The annual mean air temperature was unusual high in plain,but was slight higher in mountain regions in Tarim River Basin in 2004.Both precipitations in plain and mountains were a little more than normal.The 0℃ level height was lower in spring and summer in Tarim River Basin.In 2004,total annual virgin flow of 224.0×108m3 from four mountains basins of Aksu,Hotan,Yarkant and Kaidu-Konque Rivers drain into the Tarim basin,is an normal hydrological year.The Aksu River and Kaidu-Konque Rivers from the south slope of Tianshan Mountains have a large runoff rising comparing with average annual runoff,Aksu River,increasing by 15.9%,was an abundant hydrological year;Kaidu-Konque Rivers,increasing by 4.2%,was a slight abundant hydrological year.But the runoff in Yarkant River from the Karakorum and Hotan River from the West Kunlun Mountains were less than average annual runoff,Yarkant River,decreasing by 10.8%,was a little shortage of water year;Hotan River,decreasing by 17.9%,was a shortage of water year.The total discharge of the four source rivers,which are Aksu,Hotan,Yarkant and Kaidu-Konque Rivers,drain into Tarim River is 27.02×108m3 in 2004,occupy up 12.1% of annual virgin flow from mountains basin.The Yarkant River is the only river no water drain into the mainstream of Tarim Rive.The interzone consumed water of the Tarim River mainstream are estimated to be 19.19×108m3 for the upper course from Aler to Yingbazha,the largest consumed section of the Tarim River mainstream;7.530×108m3 for the middle course from Yingbazha to Qiala,occupy up 30.3% of the consumption that before harness.The proportion of consumed water of upper,middle and downstream occupy the whole consumed water of Tarim River mainstream comparing with their own woodland proportion respectively,the proportion of consumed water was more in the upper stream course,was a little in the middle streams course,and was correspond in the lower course.During April 22 to June 25,2004,the sixth ecological emergency water diversion project was carried out in the lower reaches of Tarim River,transfer water 1.600×108m3 from Bosten Lake,outflow 1.020×108m3 drains into Taitema Lake,from Daxihaizi Reservoir,and water reached in Taitema Lake again in 2004.
  • SU Hong-chao, BAYIN Cha-han, PANG Chun-hua, JI Jin-huan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 941-949. https://doi.org/10.7522/j.issn.1000-0240.2006.0137
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    The Ebinur Lake (44°30’N,82°25’E) at the north piedmont of west Tianshan Mountains is characterized by its wide area and shallow depth,thus its area change is extremely sensitive to the climate change. Ebinur Lake was a great well freshwater lake with an area of 3000 km2 and a volume of 700×108 m3 in the middle Pleistocene period.Because of tectonically movement of the Earth and warm-dry climate change,the lake area shrank to 1070 km2 at the beginning of 1950s.The inflow runoff to Ebinur Lake decreased sharply as large increase of water consumption since 1950s,because of large-scale water and soil development,the increase of population and irrigation area in the watershed.From 1950s to the late of 1980s,the population had increased by 59.3×104,the irrigation area increased by 16.43×104 km2,net consumed water increased by 8.13×108m3,and result in the lake area was reduced to 499 km2 and the water salinity reached about 100 g·L-1 in 1987.The shrinking of the lake would result in eco-environmental deterioration: accelerated the extent of desertification,floating dust and sandstorm increasing;the number of wild animals decreasing.After 1987,the increasing of precipitation and river runoff as climate change from warm-dry pattern to warm-wet pattern,and using measurements of water-saving irrigation technology and the development of ecological forests and returning farmland to forest,the inflow runoff to the lake increased rapidly,and the lake area was enlarged to 1096 km2 in May 2000,to restore to about the water level in 1957.Especially in years of 2001-2005,the mean annual runoff of inflowing into Ebinur Lake reached 7.7×108m3,increased by 76% than 1989,and the lake water kept in an area of 800-950 km2.The ecological environment has been restored and improved,the desert vegetation has been partly restoration,dust weather has significantly decreased,and wildlife animals have appeared there.
  • LAN Yong-chao, SHEN Yong-ping, LIN Shu, ZHANG Shi-qian, CHANG Jun-jie
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 950-955. https://doi.org/10.7522/j.issn.1000-0240.2006.0138
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    The changing characteristics of high and low flows of the runoff in the upper reaches of Yellow River and the circumfluence backdrop corresponding with the typical high and low flow years were analyzed according to some relational hydrologic and meteorological data,aimed at searching the weather factors that control the flood discharge in flood season,at affording warranty to the long-term and super long-term forecasts of flood discharge rate,and at programming the use of water resources in the upper reaches of Yellow River.It is revealed that cycles of high and low flows in the upper reaches of the river alternately occur,but the time of the high flow is less than that of low flow on the whole,and the period of an integrated high and low flow cycle is about 18 years in the upper reaches.There is a close relation between the high or low flow of the reaches and the abnormity of circumfluence.The subtropical high over the west Pacific extending to west and the westerly trough occurring in the mid and west of the Tibetan Plateau are the two important factors that bring abundant precipitation and more runoff in flood season of the upper reaches.Thus,the flood discharge rate in flood season of the reaches can be forecasted approximately based on the relations between the high or low flow and the abnormity of circumfluence and the characteristics of prophase circumfluence.
  • LU An-xin, DENG Xiao-feng, ZHAO Shang-xue, WANG Li-hong, ZHANG Ying-song, JIANG Xi
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 956-960. https://doi.org/10.7522/j.issn.1000-0240.2006.0139
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    Tibetan Plateau is one of the most serious debris flow hazard regions in China.Debris flow in Guxiang valley in southern Tibet Region is one of the main hazards to Sichuan-Tibet Highway.The Guxiang debris flow was in inactive during the period of 1966 to 2004,and then it broke out at 10 am and night on July 30,and at 8 am on August 6,2005.The deposit on the road caused by the debris had a volume of 20000 m3 with a thickness over 2 m and a width over 20 m,which blocked the road for a long time and caused great loss of local people’s property.The debris flow in 2005 was caused by concentrative rainfall and continuous high temperature,same as that in 1953.
  • YONG Bin, ZHANG Wan-chang, LIU Chuan-sheng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2006, 28(6): 961-970. https://doi.org/10.7522/j.issn.1000-0240.2006.0140
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    As one of the hottest problems in the global change studies,the coupling study of hydrological models and land-surface models has become more and more attractive recently.It has been an important scientific issue how to carry out the intercoupling between distributed hydrological models and land-surface process models,and then embed the two models into the climate models properly in the future GCM or RCM research.After briefly introducing the development of land-surface process models and hydrological models,this paper summarizes the new advances of the intercoupling between hydrological models and land-surface process models and points out the common weakness of all the studies and the research focuses in the future.Finally,it is discussed what kind of role the intercoupling between distributed hydrological models and land-surface models plays in the frame of global change research.At the same time,the main study trends of land-surface hydrological process are also proposed.