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    30 March 2006, Volume 18 Issue 1 Previous Issue    Next Issue

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    ARCTIC GLACIER MOVEMENT MONITORING WITH GPS METHOD IN 2005
    2006, 18 (1):  1-8. 
    Abstract ( 1502 )   PDF (516KB) ( 1646 )  

    During the 2005 Arctic Yellow River Station Expedition, we start to monitor the movement and mass balance of two glaciers around Ny-lesund, Austre Lovénbreen and Pedersenbreen, which were selected in the 2004 Yellow River Station Expedition. This paper analyzes the possibility and advantage in using GPS method to monitor the Arctic glaciers’ movement, estimate the precision of first time measured GPS data and discuss the relevant problems using to survey on the Arctic Glaciers with GPS.

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    STUDY ON MODERN POLLUTION SOURCE AND BIO-INDICATOR IN NY-LESUND, ARCTIC
    2006, 18 (1):  9-19. 
    Abstract ( 1841 )   PDF (1738KB) ( 1871 )  

    We collected three kinds of tundra plants including Dicranum angustum, Puccinellia phryganodes and Salix polaris each on total 12 different sites from a coal-mining gradient profile in Ny-lesund (78°55′N, 11°56′E), Arctic. At the same time, the soil on the profile was also collected. The concentrations of 10 heavy metal elements (Hg, Pb, Cd, Cu, Zn, Ni, Fe, Mn, As, Se) , S and TOC were analyzed in our lab. The results showed that the modern pollution source of Hg, Cd and S in Ny-lesund is the local human's coal-mining activities. The tundra plant Dicranum angustum has the highest ability in absorbing heavy metal elements. The content of heavy metal elements in Dicranum angustum in mining area is much higher than that in non-mining area, which also suggests the pollutant source is mostly derived from coal-mining. Meanwhile, we have compared the distribution rule of these elements between plant Dicranum angustum and soil and found that, as a whole, the variation trend of them on the profile is quite similar, which showes the tundra plant Dicranum angustum can record the environmet conditions very well. So maybe Dicranum angustum can be chosen as bio-indicator for contamination in Ny-lesund. Comparing from other areas in the world, we found that the level of pollutants of Hg, Cd, S in Ny-lesund is lower than that in developed countries in Northern European, but is the highest in Arctic, and higher than that in Antarctic.

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    DISTRIBUTION OF CHLOROFLUOROCARBONS IN CANADA BASIN AND THEIR TRACER STUDY
    2006, 18 (1):  21-29. 
    Abstract ( 1504 )   PDF (359KB) ( 1680 )  

    Seawater samples at 9 stations were collected in the Canada Basin during the Second Arctic Scientific Expedition of China (from Jul. to Sep.,2003). The result of chlorofluorocarbons(CFCs)determination showed that the highest concentration of CFC-11 and CCl_4 in the surface water are 6.7 pmol/kg and 9.62 pmol/kg respectively, but they are all undersaturated. The degrees of saturation of CFC-11 in the surface water lies in the range of 70.54% to 84.70% , and that of CCl_4 within 76.54% to 91.53% , probably caused by local ice cover and the invasion of the Pacific water with low CFC concentration. The significant concentration of CFCs at the depth of 2000 m indicated that deep water in the Canada Basin was exchanged and replaced with the open seawater outside. The vertical distributions of CFCs confirmed that the water masses in the Canada Basin were stratified. The method of pCFC-11 and pCCl_4 dating are used to evaluate the apparent ages of water masses.

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    THE RELATIONSHIP BETWEEN ANTARCTIC SEA ICE AND THE SYNOPTIC CLIMATE IN SUMMER OF CHINA
    2006, 18 (1):  30-38. 
    Abstract ( 1561 )   PDF (846KB) ( 1967 )  

    The variations of the Antarctic sea-ice in each sea region are obviously different. This kind of different variations in each region may have different influence on a regional atmospheric circulation and further on global climate system. This study investigates that the relationship between variations of sea ice in the Ross Sea and Weddell Sea and the synoptic variations during summer in China using Northern Hemisphere monthly mean 500 hPa and 100 hPa geopotential and rainfall and temperature data at 160 stations in China. The results indicate that the sea ice variations in Ross Sea and Weddell Sea are both of indicative significance for the synoptic climate in summer of China. Ross Sea region is the crucial region where its proceeding sea ice variations in September show significant relation with the following June rainfall in Northeast China. If the sea ice of this crucial region in September is in heavy ice condition, the precipitation in Northeast China in the next June tends to be deficit. Weddell Sea region is the key region for summer temperature in Northeast China. If the sea ice of this key region in September is in light ice condition, the next June temperature in Northeast China also tends to be deficit.

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    DESIGN AND IMPLEMENTATION OF THE MANAGEMENT SYSTEM OF CHINESE POLAR SPATIAL DATA OF SURVEYING AND MAPPING METADATA
    2006, 18 (1):  39-45. 
    Abstract ( 1385 )   PDF (675KB) ( 1574 )  

    It is very important for most polar users to get the surveying and mapping spatial data information from various districts. The information distribution technique based on Internet can play a great role in the service. In order to allow polar users to know something about the production of surveying and mapping spatial data in time, the management system of metadata must be set up. Through Internet, polar users will be able to query what surveying and mapping spatial data is being produced, how about its quality, where it is produced, and so on.In this paper, different classes and properties of the Chinese polar spatial data of surveying and mapping have been analyzed,and the metadata and its management system have been designed by referring some popular metadata standards such as ISO/TC211, FGDC, and China Sustainable Development Sharing Information Metadata Standard . It is only after searching and querying corresponding surveying and mapping spatial data metadata that users can clearly know what surveying and mapping spatial data is available for them, what surveying and mapping spatial data they are interested in, where the information is stored. So, this metadata management system can serve the polar research expedition well.

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    THE TECHNOLOGICAL METHODS APPLYING IN THE REAL-TIME TRACKING MAP OF XUELONG SHIP
    2006, 18 (1):  46-51. 
    Abstract ( 1464 )   PDF (169KB) ( 1534 )  

    Combining the production of ‘the Series of World Map’ with the technique of GIS and computer network, the real-time tracking service of Xuelong Ship of Antarctic Expedition are firstly realized in November, 2004. In this article a few key questions are dissertated in detail, such as the theory of projection transformation, mapping of the map coordinates and screen coordinates, clipping of track line, of real-time track map, and the building up and applying of real-time track map on the net using visual subassembly. The concrete methods are put forward to settle these issues.

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    OUR UNDERSTANDING OF ARCTIC VORTEX
    2006, 18 (1):  52-62. 
    Abstract ( 2614 )   PDF (1887KB) ( 5133 )  

    The Arctic vortex is a persistent large-scale cyclonic circulation pattern in the middle and upper troposphere and the stratosphere. Its activity and variability are related to the semi-permanent active centers and the cyclone activity with the short-time scale in the pan-Arctic. Its variability in the strength, which is directly related to the atmosphere, ocean, sea ice and ecosystem in the Arctic, has an effect on the lower atmospheric circulation and affects the weather in the sub-Arctic and even at the middle latitudes. The transition of the circulation from a warm anticyclone to a cold cyclone occurred in the middle and upper stratosphere during 2003 Chinese Arctic Research Expedition. The mechanisms coupling the stratosphere and troposphere have been studied by some scientists for understanding the effect of the polar vortex change on the lower circulation. The effect of the stratospheric sudden warming on the polar vortex break down was found early in the fifties of the last century and has been taken great note. The Arctic Oscillation (AO), relating to the change of the Arctic vortex, has been used to study the effect of the Arctic vortex on the climatic change. The recent Arctic vortex research is simply reviewed in the paper. Our understanding of the Arctic vortex is given and some different view and questions are also discussed.

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    RAPID CHANGES OF THE ANTARCTIC ICE SHEET AND GLACIERS
    2006, 18 (1):  63-74. 
    Abstract ( 1500 )   PDF (507KB) ( 1931 )  

    Observations of the Antarctic Ice Sheet in recent years have revealed rapid and substantial changes occurring on the ice sheet on relatively short time scales. The principal drainage systems of Amundsen Sea Sector in West Antarctic are thinning rapidly, and the pattern of thinning extends to the interior of up to 150 km. Ice Stream C has slowed down while the flow in some areas has changed direction in the Ross Sea Sector. Vast areas of the Antarctic Peninsula Ice Shelves have collapsed, resulting in the acceleration and surge of tributary glaciers. Basal melting near the grounding lines is substantially due to erosion of a warm ocean. These evidences lead to our view that the Antarctic Ice Sheet is slowly changing and homogeneous has radically altered. This finding has important consequences for the ice dynamic study, ice sheet modeling and the mass balance assessment and its response to climate forcing.

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