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    30 September 2002, Volume 14 Issue 3 Previous Issue    Next Issue

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    PALAEOENVIRONMENTAL RECORDS FROM PALAEOGOE SEDIMENTS ON FILDES PENINSULA, ANTARCTICA
    2002, 14 (3):  163-173. 
    Abstract ( 1632 )   PDF (525KB) ( 2522 )  

    A great deal of palaeogoes have been found in the area around the Great Wall Station located on Fildes Peninsula in west Antarctica, in which intact sedimental sections are preserved. By the analysis of the grain size characteristics and elemental composition in sediments collected from one of those sections, we can affirm that the sedimental section is composed of lake sediments , by which the evolutional history of paleoenviroment in this area since 4600aBP has been reconstructed. The results indicate that chemical weathering of rocks on the earth surface in the Gread Wall Station area is relatively strong from 4000 to 3000aBP, which is suggestive of a comparatively warm period, and this warm period is also imprinted in some sedimental records such as lake and marine sediments. It is proved that palaeogoe sediments can be regarded as a new geological carrier by which we can research palaeoenvironmental evolution history in the ice-free and periglacial area, Antarctica.

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    INSPIRATION FROM STUDY OF ANTARCTIC METEORITES-X:TERRESTRIAL AGES OF ANTARCTIC METEORITES
    2002, 14 (3):  174-185. 
    Abstract ( 1412 )   PDF (396KB) ( 1255 )  

    Up to date, meteorite scientists have searched about 2500km 2 of blue ice and recovered more than 30000 meteorite specimens from different locations on the Antarctic ice sheet. In the past two decades ,terrestrial ages of a few hundred meteorites were determined, mainly on the basis of the 36 Cl or 14 C concentrations. Each stranding area shows a different terrestrial age distribution and provides the information of the local accumulation mechanisms. The Antarctic meteorite density on the blue ice surface are determined by many factors, such as the meteorite fall rate, the ice ablation rate and the snow accumulation rate. Meteorites from Yamato Mountains Icefields have ages up to 200ka,whereas Lewis Cliff and Allan Hills specimens have ages up to 500ka and 1Ma, respectively. Recently, two meteorites have been discovered with exceptional ages of about 2Ma from Allan Hills and 2.35Ma from Lewis Cliff, which indicate that they are deeply inside the ice, near the base of glacier and ice flow rates are much lower than at surface. Their terrestrial ages also indicate the process of meteorite accumulation into present day stranding areas started at least 2 million years ago and the long terrestrial ages are consistent with an assumption concerning the stability and persistence of the East Antarctic ice sheet. The residence time on the surface is an important parameter in determining the history of the meteorite. In addition, terrestrial ages can be used to estimate the average transport time of meteorites from accumulation to ablation area and the mean weathering lifetime.

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    DISTRIBUTION OF CHAETOGNATHA IN CHUKCHI SEA AND BERING SEA
    2002, 14 (3):  186-194. 
    Abstract ( 1686 )   PDF (407KB) ( 1305 )  

    The data used in this paper was obtained from the comprehensive oceanographic survey during the First Chinese National Arctic Research Expedition in Chukchi Sea and Bering Sea in July and August 1999. The characteristics of ecological groups, species composition, horizontal and vertical distribution of Chaetognatha in both Chukchi Sea and Bering Sea are described and the relationships of Chaetognatha density and some other environmental factors are discussed. The results show that seven species of Chaetognatha were recorded which belongs to 3 ecological groups. The number of Chaetognatha was higher in Bering Sea than in Chukchi Sea. The density of dominant species determined the total Chaetognatha abundance and it was higher in south than in north. The density was high in water layer of 50-200m and low in water layer of 500 -800m in Chukchi Sea. In the other hand, the density was comparatively high in layers of 200-500m in Bering Sea during the daytime and aggregated in water layers 0-100m, particularly in 0-50m during the night, showing a pattern of up and down migrations in day and night, respectively.

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    THE CHARACTERISTICS OF TEMPERATURE CHANGE OVER PRYDZ BAY IN RECENT 10 YEARS
    2002, 14 (3):  195-202. 
    Abstract ( 1335 )   PDF (222KB) ( 1292 )  

    The characteristics of temperature change of Prydz Bay in recent 10 years is analysed based on observational meteorological data from Zhongshan Station and Davis Station since 1989. The results show that the time change trend of monthly mean temperature for the both stations is negative with -0.066℃/a which is opposite to Antarctic mean warming trend. The main feature of seasonal change is most cooling trend appeared in autumn and warming trend in summer. The variation of monthly mean maximum temperature is also warming with time and contrasts with minimum temperature in the both stations. The fluctuation of the temperature of Prydz Bay is very larger with extremity abnormal values of about ±10℃, Such events are closely connected with abnormal positions distribution of Antarctica continent high pressure system and locations of low pressure centers of surrounding polar.

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    GIS-BASED DATA PROCESS AND ANALYSIS ALONG THE GLACIOLOGICAL TRAVERSE ROUTE FROM ZHONGSHAN STATION TO DOME A
    2002, 14 (3):  203-212. 
    Abstract ( 1372 )   PDF (440KB) ( 1395 )  

    The glaciological traverse route from Zhongshan Station to Dome A is one of the key routes in ITASE project. A preliminary application of GIS for the traverse route has been conducted to display, process, manage and analyze the data obtained by the 3rd Chinese Antarctic Inland Expedition. In this paper, the data sources for our GIS application research include the field data, such as 23 high-resolution GPS data and more than 600 GPS navigator data collected along the 1100 km traverse rate from Zhongshan Station to Dome A by the Chinese Inland Expedition; the surface, sub-ice topographic and ice thickness database provided by Antarctic digital database (ADD) and BEDMAP Project via World Wide Web. The tiling scheme of IMW 1:1 million scale map is adopted for ADD original scale and 1:1 million scale. The data within each IMW sheet boundary are subdivided into feature layers. Therefore, tiles should be first merged according to different features, such as cliff, coast, contour, elevation and so on, then you can clip the region you need using ArcView. In addition, BEDMAP data and field data should be firstly conducted projection transformation before adding them to ADD since ADD uses the Polar Stereographic projection. The major conclusions are achieved as fellows: 1. The route feature is created from GPS navigator data using Arc/Info. Then features defined by measurements along the route can be added to a map. 2. ADD have higher resolution along the route from Zhongshan Station to Dome A by comparing the high-resolution GPS data with the revised GPS navigator data via ADD and ArcView. GPS navigator data can be revised using ADD to promote the resolution. 3. The BEDMAP data along the traverse route is an important reference to our research on ice thickness sounding. The spatial distribution of BEDMAP data can be shown clearly after adding to ADD. 4. The triangulated irregulated network (TIN) of a region including Lambert Glacier Basin is created from the surface topography using 3D Analyst module and Spatial Analyst Module. Then the aspect (slope direction) and slope data along the traverse route can be derived from TIN. 5. It is a convenient and useful tool for us to record, query and display a variety of data in detail along the traverse when we travel inland.

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    ENVIRONMENTAL GEOCHEMICAL INDEX IN POLAR SNOW AND ICE AND ITS SIGNIFICANCE
    2002, 14 (3):  213-225. 
    Abstract ( 1540 )   PDF (232KB) ( 1625 )  

    The geochemical impurities in polar snow and ice can provide information on local or global climate and environment (including human activities, biosphere, volcanic activities and so on) in the past, This paper discusses environmental geochemical indexes, such as, major ions, microparticles as well as the factors that influence their distribution with space and time. The chemical impurities deposited in polar snow mainly include Na + , K + , Ca 2+ , Mg 2+ , Cl - , NO 3 -, SO 4 2- and CH 3SO 3 - , as well as microparticles. There are three sources for the impurities, as, 1) dust emitted by continents under the action of weathering and wind (such as, some of Ca 2+ , SO 4 2- and Mg 2+ ); 2) sea salt (mainly Na + , Cl - and some of Mg 2+ , Ca 2+ , SO 4 2- and K + ); 3) gas-derived aerosol produced by the chemical transformation of atmospheric trace gases (some of Cl - , NO 3 -, SO 4 2- and CH 3SO 3 -). The impurity concentrations derived from continent and marine during the last glacial were higher than that at present in Arctic and Antarctic ice sheet. Human activities have lead to strong increases of sulfate and nitrate in Greenland ice sheet since the late 19 th Century

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    POPULAR MAP PROJECTIONS IN ANTARCTICA AND THEIR APPLICATION
    2002, 14 (3):  226-233. 
    Abstract ( 1546 )   PDF (261KB) ( 1775 )  

    There are three popular map projections in Antarctica-Polar Stereographic Projection, Transverse Mecator Projection and Lambert Conformal Conic Projection. They are all conformal. On the basis of the principal qualification for all conformal projections, the application for the above three projections in Antarctica are specified. Furthermore, the projections for the satellite imagery are referred.

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    POTENTIAL APPLICATION OF COSMOGENIC NUCLIDE ~ 10 BE IN ICE AND SNOW FOR QUATERNARY RESEARCH
    2002, 14 (3):  234-242. 
    Abstract ( 1576 )   PDF (385KB) ( 1500 )  

    The progress in accelerator mass spectrometry made it possible to investigate astronomy, geography and paleoclimate by high precision measurements of cosmogenic 10 Be from various archives. Preceding investigations suggested that the 10 Be concentration could be used to indicate variation in the past precipitation, and its production rate in the atmosphere represented three control factors: primary cosmic ray intensity, solar activity and geomagnetic variations. Moreover,with the help of other cosmogenic nuclides, 10 Be can be used to date old ice layer and provide special information for global comparison. The Qinghai-Xizang plateau in the west china has ample resources of mountainous glacier due to its unique high elevation. For the mid-low- latitude location and peculiar atmospheric circulation pattern, it will be a necessary supplement to the now-existing polar 10 Be datum in providing more detail information of the geomagnetic shielding and climatic influence on the 10 Be.

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