25 August 1998, Volume 20 Issue 3
    

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  • SHI Ya-Feng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 197-208. https://doi.org/10.7522/j.issn.1000-0240.1998.0041
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    This paper defines the implication and composition of the cryosphere and presents the process of the cryospheric evolution in a very long period from the appearance of ice cover in Antarctic about 42 Ma ago to the mid Pleistocene During the early Pleistocene, there were only a few peaks of glaciation occurred in the Himalayas Until the orogenic movement of Kun-huang from 1.1 to 0.6 Ma BP, the plateau ground lifted up to about 3500 m, resulting in the plateau’s cooling; and at the same time, the control of the earth orbit taking in solar insolation changed from the orbital incline rate of 41 ka in a cycle to the eccentricity of 100 ka in a cycle, concomitantly resulting in the Plateau’s cooling as well Because the events mentioned above were coupled, the third glaciation from the last or the maximum glaciation occurred in 0.6 to 0.8 Ma BP The period when the maximum glaciation occurred was comparable with MIS16 Period, with the total glacier area more than 5×105 km2 Air temperature in summer at the equilibrium line of glaciers was 1~2℃ higher than that at present Precipitation in four mountainous areas of the mid and east plateau was 1.8~3.2 times as much as that at present, while precipitation in the arid West Kunlun Mountains was only 30% more than the present one Permafrost grew at a large scale in the west plateau and stable snow cover existed with different depths in the plateau, except for summer Consequently, the albedo was greatly increased on one hand and the snow melting consumed a large amount of heat energy on the other hand, resulting in the plateau’s effect changing from a heat source of a year-round to a cold source of most months in a year and furthermore resulting in a decrease in air temperature The winter monsoon to the outside was enhanced and as a result, summer precipitation from the southwest monsoon decreased However, precipitation was still rich and climate was relatively cool and humid in the mid and east plateau where climate constantly affected by the south branch of the west jet stream and by the hot low in summer, which in turn had an important impact on climate of the plateau itself and its nearby areas The interglacial between the last but one and the last but two glaciations was symbolized by MIS13 period During the interglacial, climate was much warmer than that in glaciation Forestry was distributed near what is now called Qinghai-Xizang Highway and the laterite crust of weathering grew in the south plateau The plateau’s role as a heat source was strengthened, resulting in an enhancement of summer monsoon Except for existence of a small number of high-elevation glaciers, such as the Guliya Glacier, a large part of glaciers and permafrost areas might be fully depleted and disappeared.
  • JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 209-212. https://doi.org/10.7522/j.issn.1000-0240.1998.0042
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  • CHENG Guo-Dong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 213-226. https://doi.org/10.7522/j.issn.1000-0240.1998.0043
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    In the past 40 years, significant progress has been achieved in glaciology and geocryology of China from a blank The interaction between the cryosphere and climatic change is concerned at present Consequently, studies on the water resources in arid and cold regions, the cold regions engineering and the hazard prevention under a warming climate are essential to the sustainable and concordant development of regional economy and ecosystems As a tool and key for the above topics, the geographic information sciences should be speeded up urgently.
  • QIN Da-He, REN Jia-Wen, KANG Shi-Chang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 227-232. https://doi.org/10.7522/j.issn.1000-0240.1998.0044
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    The history of Antarctic glaciology in China is reviewed with the emphasis on the past decade Much progress has been made both in investigation of physical characteristics of the Antarctic ice sheet and caps and in study of climatic and environmental records in Antarctic snow and ice Through the observation of snow profiles of numerous snow-pits and shallow cores over Wilkes Land and Lambert Glacier basin and along the route of the 1990 International Trans-Antractica Expedition (ITAE), regional features of snow deposition and densification over Antarctica were revealed The Nelson Island ice cap in South Shetland Islands was investigated in detail, which has enriched knowledge of glaciers in sub-Antarctic maritime climate From shallow ice core study and chemical analyses of surface snow samples, in particular those taken along the ITAE route, most systematic data has been obtained for distribution of stable isotopes, soluble impurities and heavy metal Pb in modern precipitation over Antarctica After discussing the international hot pots at present and the trend in near future, some suggestions are proposed.
  • YAO Tan-Dong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 233-237. https://doi.org/10.7522/j.issn.1000-0240.1998.0045
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    Ice core study is one of the important parts in the global change studies Due to its high resolution, more information, high quality, long time series and purity, ice core is the best media to study the biology, chemistry and physics processes in the global system Firstly, the main aspects of the Tibetan Plateau ice core studies, namely, the processes relating to the ice core and the ice core records are discussed in this paper Then, the main results in the Tibetan Plateau ice core studies in the last decade are summarized and it is pointed out that the main results can be concluded as five aspects It is also pointed out that the Tibetan Plateau ice core studies have acquired breakthrough progress in eight aspects Lastly, the strategies of the future Tibetan Plateau ice core study is proposed for both the field work and laboratory work.
  • KANG Er-Si
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 238-244. https://doi.org/10.7522/j.issn.1000-0240.1998.0046
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    For studying the hydrology of cold and dry regions, a relatively comprehensive system of measurements, experiments and a investigation has been basically formed in the areas of glaciers, snow cover, permafrost, high moutainous watersheds and the low land area in front of the mountains in the arid area of northwest China Since the 1980′s, achievements of scientific researches have been obtained on glacial meltwater runoff, measurements and experiments of runoff generation from mountainous watersheds of inland river basins, hydrological processes in cold regions, interrelationship between hydrological processes and atmospherical processes in glacierized basins, water resources in the Urumqi Prefecture of Xinjiang Autonomous Region, impacts of climate changes on water resources, hydrology of the High-Asia cryosphere, glalcier lake outburst floods, snowmelt runoff, and hydrology in arid regions For recent years, in the studies of hydrology and water resources in cold and dry regions, new projects have been initiated on the rational exploitation and utilization of water resources, on the coordinate development of society and ecotope, on the prediction of changing trends of snow and ice water resources and runoff from the mountainous watershes under global warming, and on the basic researches on the generation and variation of water resources in inland river basins It can be foreseen that, in the next ten years or more, the studies of hydrology in cold and dry regions will develop to a new stage of comprehensive researches, which are centralized by hydrosphere, on the spatial and temperal interactions among the hydrosphere, atmosphere, cryosphere, lithosphere and biosphere It is expected that a breakthrough progress will be achieved in the studies on water resources and hydro-environment All the achievements will serve the foundations of the decision making for the sustainable economic development of the arid northwest China.
  • FENG Xue-Zhi, CHEN Xian-Zhang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 245-248. https://doi.org/10.7522/j.issn.1000-0240.1998.0047
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    As a summary, in this paper a brief review of themain research works on the remote sensing of snow and ice in the institute is given, with the focus on discribing the research results and the application effect of the remot sensing monitoring of snow and ice and the model of snow meltweaer runoff, snow disaster remote sensing and the evaluation of disaster loss ect In the prevailing circumstance, a brief analysis and a prospect for the future about snow and ice remote sensing in the institute is also made inthis paper.
  • QI Long
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 249-257. https://doi.org/10.7522/j.issn.1000-0240.1998.0049
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    The 40-year achievement and progress of studies on glacier, snow and debris flow disasters by LIGG is summarized and the situation of glacier, snow, permafrost and debris flow disasters is reviewed An orientation of the disaster research is suggested, which includes the impact of global change on formation and development of disasters and the hazards triggered by human activities after national economic developing focus moving to the west At last, some preventional countermeasures of disasters are put forward.
  • HE Xing, XU Yue-Zhen, ZHU Guo-Cun, LIANG Hong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 258-263. https://doi.org/10.7522/j.issn.1000-0240.1998.0050
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    Since its starting in 1979, 87 issues of the Journal of Glaciology and Geocryology have been delivered, including 1 331 papers or 14 110 000 words during the past 20 years Under the profound concern and full support of the leaders of Chinese Academy of Sciences and Lanzhou Institute of Glaciology and Geocryology, CAS, the journal has made excellent progress In 1996, it was recognized as the eighth distinguished geoscience periodical in China, based on the quote ratio The achievement is also owed to the authors and editors The aim of the journal is to be an outstanding international geoscience periodical in the next century.
  • MA Wei, ZHU Yuan-Lin, XU Xiao-Zu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 264-272. https://doi.org/10.7522/j.issn.1000-0240.1998.0051
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    The State Key Laboratory of Frozen Soil Engineering is an unique comprehensive laboratory which carries out the study of frozen soil engineering in China Its construction and development will have very important significance for developing Geocryology in China On the occasion of greeting the 40th anniversary of the Lanzhou Institute of Glaciology and Geocryology, the State Key Laboratory of Frozen Soil Engineering has made its way for 9 years Looking before and behind, it is clear that only by grasping closely the frontier of Geocryology and solving the fundamental, crucial and integrated problems of engineering, resources and environment in the economic and social development of cold regions in China can we establish the most advanced state key laboratory and make the study of frozen soil engineering of China be in the lead of the world.
  • QIN Da-He, YAO Tan-Dong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 273-279. https://doi.org/10.7522/j.issn.1000-0240.1998.0052
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    The history and the present situation of the international and domestic studies on ice cores are reviewed in this paper The summary of the Laboratory of Ice Core and Cold Regions Environment is given in two aspects: 1) hardware, such as establishing of the laboratory and equipment; 2) software, such as stuff in the laboratory At present, there are three research field: 1) The interaction processes between glacier and atmosphere; 2) The ice core records; 3) The physics of snow and ice Thirty-two projects have been finished or are being carried out More than 300 papers and 9 monographs have been published There are 4 achievements in scientific research were awarded Cooperation have been hold between some high level scientific departments and the laboratory In the future, the research goal of the laboratory will be focused on the climatic and environmental records and modern processes in cold regions It is urgent to cultivate and recruit more qualified researchers.
  • LI Zhong-Qin, YE Bai-Sheng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 280-286. https://doi.org/10.7522/j.issn.1000-0240.1998.0053
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    This paper presents rivew of the scientific works in the Tianshan Glaciological Station over the past 10 years The progress of scientific research, student training and construction of the station is summarized In addition a prospect is also given.
  • ZHAO Lin, GUO Dong-Xin, LI Shu-Xun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1998, 20(3): 287-292. https://doi.org/10.7522/j.issn.1000-0240.1998.0054
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    The Observation and Research Station of the Qinghai-Tibet Plateau have made great progress in the past decade The development of research in entrusted productive projects not only solved many problems for the local and military, but also, in some degrees, the funding problem of the station In the meantime, it provided many chances to practice for scientists in the institute The progress in the research of basic sciences was remarkable Funded by the National Nature Science Foundation, "Foundational research on cryosphere dynamic variation" of Chinese Academy of Sciences (CAS), Major Projects of CAS and national Climbing Programme, gratifying achievements have been made in many subjects, such as changes of permafrost and climate on the Tibetan Plateau, water and heat balance in the active layer, the relationship between desertification and permafrost in permafrost regions, the interaction between permafrost and atmosphere and the dynamics of frost weathering International co-operation and scientific exchanges have been enhanced To look forward to the future, aimed at the research on so-called the third polar in the earth, it is believable for the station to make great success and play more important role in the research on the Tibetan Plateau.