Loading...

Archive

    30 September 2000, Volume 12 Issue 3 Previous Issue    Next Issue

    Contents
    For Selected: Toggle Thumbnails
    Contents
    WATER MASSES AND THEIR NORTHWARD EXTENSION IN THE UPPER OCEAN OF PRYDZ BAY, ANTARCTICA
    2000, 12 (3):  157-168. 
    Abstract ( 1373 )   PDF (283KB) ( 1448 )  

    In this paper, CTD observational data obtained during the 15th Chinese National Antarctic Research Expedition (CHINARE-15) in the Southern Ocean are used to analyze and study water masses, their distributions and thermohaline characteristics in the Prydz Bay and its adjacent region. And water masses within and north of Prydz Bay are identified as summer coastal surface water, the Prydz Bay winter water, the Prydz Bay shelf water, and the Circumpolar Deep Water. Based on the above discussion, the northward extension of the Prydz Bay shelf water is found. Then the thermodynamic and the dynamic characteristics are further discussed, which are the inversion layer depth of the water temperature, the locations of the minima of the vertical temperature distribution and the temperature vertical gradient in the water column, as well as the baroclinity and the effect of Coriolis deflection force.

    Related Articles | Metrics
    THE HYDROMEDUSAE FROM CHUKCHI SEA AND ITS DISTRIBUTION
    2000, 12 (3):  169-182. 
    Abstract ( 1424 )   PDF (577KB) ( 1415 )  

    The present paper is based on materials collected in Chukchi Sea during the period from July to August 1999 on icebreaker the R/V "Xuelong" by Chinese First Arctic Scientific Expedition. A total 8 species of pelagic Hydromedusae were identified, of which 4 species belonged to Anthomedusae, 2 species to Leptomedusae, 1 species to Trachymedusae and 1 species to Narcomedusae, the Neoturris breviconis is recorded for the first time in Chukchi Sea. Their principal morphological characteristies are described and illustrated. The 8 species of Hydromedusae occurring in the Chukchi Sea all were cool water species, of which 6 species belong in neritic species, 2 species in ocean species. According to the geographic distribution of species, they may be divided into three groups: Arctic species, Arctic boreal species and Boreal temperate species. From the view point of zoogeography, species from these waters belong to the Arctic fauna. The abundance of Hydromedusae in Chukchi Sea was generally low, with a mean value of 108 ind./100m 3. The condition of distribution of individual number was due to distribution of dominant species. The Rathkea octopunctata and Aglantha digitale were dominant species. The vertical distribution of Aglantha digitale was inhabiting the 0-300m and having their quantitative maximum in the 50m to 100m.

    Related Articles | Metrics
    METABOLISM OF TWO DOMINATING COPEPODS: - CALANOIDES ACUTUS- AND- METRIDIA GERLACHEI- IN THE MARGINAL ICE ZONE OF THE PRYDZ BAY, ANTACTICA IN SUMMER
    2000, 12 (3):  183-190. 
    Abstract ( 1306 )   PDF (431KB) ( 1633 )  

    Metabolic rates (oxygen consumption and ammonia excretion) of two dominating copepods, Calanoides acutus and Metridia gerlachei , were measured during the austral summer (December 1998-January 1999), in the marginal ice zone of the Prydz Bay. The elemental composition (C and N) were also analysed on the specimens used in these metabolic experiments. The results showed that C. acutus was 48.4%-48.6% of dry weight in carbon content and 6.1%-6.5% of dry weight in nitrogen content. Metridia gerlachei was 47.1%-50.1% and 5.9%-7.4%, relatively. Oxygen consumption rates of C. acutus were variant in the different areas (0.226 to 0.558μl O 2mg -1 h -1 ). And its ammonia excretion rates ranged from 0.014 to 1.058μg N mg -1 h -1 . The ratio between the rates (O∶N) exhibited a large defference(5-6 times). For Metridia gerlachei , oxygen consumption rates were 0.488-0.644μl O 2mg -1 h -1 and ammonia excretion rates were 0.015-0.034μg N mg -1 h -1 . From the results of metabolic rate measuremts and elemental analyses, daily losses of body carbon and nitrogen were estimated to be 0.59% - 1.99% and 0.44% - 3.27%, respectively. The metabolic carbon requirements represented about 0.6%-29.2% of primary production per day, and their excretion of ammonia contributed 0.2%-38.0% of daily phytoplankton nitrogen demand.

    Related Articles | Metrics
    CHARACTERISTICS OF ENERGY BALANCE OVER ARCTIC DRIFTING ICE AND OPEN SEA
    2000, 12 (3):  191-202. 
    Abstract ( 1389 )   PDF (308KB) ( 1352 )  

    Characteristics of heat balance parameters of Arctic Ocean drifting ice and open sea are presented based on the profile flux method and the data obtained by the First Chinese National Arctic Research Expedition during Aug.19-24,1999. The result shows that the difference of interaction processes between ocean air and ice air is extremely obvious. Net radiation absorbed by ice surface only account for 6% of that absorbed by the sea surface and it is consumed mainly by the processes of sensible heat exchange and ice melting, deficit part of the heat is compensated from the latent heat released when water vapor is frozen on ice surface and heat stored in ice. Net radiation absorbed by sea surface is balanced most by the process of latent heat transport , accounting for 50% of total heat, and the rest part is conducted to deep water and transported as sensible heat to air, accounting for 26% and 24% of total heat individually. It can be found that a great quantity of vapor is transported to atmosphere from Arctic Ocean open sea in summer, which is very important to concerns on season change of heat budget on Arctic Ocean.

    Related Articles | Metrics
    A STUDY OF FINE WEATHER IN THE GREAT WALL STATION, WESTERN ANTARCTIC
    2000, 12 (3):  203-210. 
    Abstract ( 1528 )   PDF (167KB) ( 1087 )  

    Based on the observational data and the facsimile charts from Dec.1994 to Nov.1995 of Chinese Antarctic Great Wall Station, fine weather there was studied. The pressure field, temperature relative humidity field and aerological stratification were analyzed synoptically. Two kinds of fine weather with different physical characteristics were found and analyzed. The results provide a basis for local weather forecast.

    References | Related Articles | Metrics
    PRELIMINARY STUDY ON SEDIMENT SULPHATE REDUCING BACTERIA IN THE SURVEY AREAS OF BERING SEA AND CHUKCHI SEA
    2000, 12 (3):  211-218. 
    Abstract ( 1365 )   PDF (385KB) ( 1146 )  

    The content of sulphate reducing bacteria (SRB)of the 35 sediment samples was determined by using MPN technique in the survey areas of Bering Sea and Chukchi Sea. The average content of SRB in all samples tested is about 1.68×10 5 cells·g -1 (wet.), its variation is 0-2.28×10 6 cells·g -1 . The differences of SRB content were analyzed and compared among the surficial layers, subsurficial or mixed ones in varied areas and stations surveyed. Roughly speaking, the SRB content in the surficial layers was lower than that in the subsurficial and mixed ones. The determinable SRB content appears presumedly opposite trend, i.e. it seems that the content of SRB increases south or east in Bering Sea and north or west in Chukchi Sea respectively if drawing a line on Bering Strait. The result indicates the occurrence percentages of SRB at 4 different cultivation temperature and suggests that there are a lot of cold adapted bacteria there. The low environmental temperature is still mainly a controlling factor. There are quite a few mesopholic bacteria, and it can be deduced that an effect of suitable organic matter supply to the SRB from raising temperature after melting frozen period.

    Related Articles | Metrics
    PROGRESS ON WEATHER FORECASTING IN ANTARCTICA
    2000, 12 (3):  219-232. 
    Abstract ( 1235 )   PDF (494KB) ( 1117 )  

    The first international symposium on operational weather forecasting in Antarctica was held in Hobart from August 3 to September 3, 1998. Based on all the reports from this symposium, the progress on operational weather forcasting in Antarctica is presented.

    Related Articles | Metrics