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1Several significant hydrographic characteristics and their formation mechanism in the South China Sea during the spring and summer of 1998显示文摘On the basis of the CTD data obtained by the two cruises before and after summer monsoon burst (25th May, 1998), several significant hydrographic characteristics, their variation and formation mechanism in the South China Sea (SCS) are analyzed. The results show that the Kuroshio water intrudes into the SCS in the form of loop current, and its main part is limited to the east of 118°E near the Luzon Strait. Then it continuously extends westwards under the influence of the large-scale circulation, and has a distinct impact on the area north of 16°N. There are two high temperature and low salinity regions:west off Luzon and east off Vietnam respectively. One region west off Luzon strengthens obviously after summer monsoon burst, the other east off Vietnam shows a tendency of weakening in the north and strengthening in the south. The formation of these two high temperature and low salinity regions is related to the anti-cyclonic eddies existing in this area, besides, it is also related to the high temperature feature west of Luzon, the influx of Sulu Sea water and the influence of the large-scale air circulation. There is a cold region below the depth of 50 m in the south of Zhongsha Islands, and it strengthens after monsoon burst. The formation of cold water is related to the upwelling there.Xu Jianping 1,2,Chai Fei 2,3,Liu Zenghong 1,2,Zhu Bokang 1,2 1.Second Institute of Oceanography,State Oceanic Administration,Hangzhou 310012,China. 2.Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography of State Oceanic Administration, Hangzhou 310012, China 3.School of Marine Science, University of Maine, Orono, ME 04469-5741,USA 2003Acta Oceanologica Sinica2003,22,4:5
2Treatment of bums withbums&wounds ( B&W ) ointment and leaf therapy 显示文摘Main ME Williams D Jones MS 2012TheJournal of Alternative and Complementary Medicine2012,18,2:1
3Testicular dysgenesis syndrome: an increasingly common developmental disorder with environmental aspects显示文摘Skakkebaek NE Rajpert-De ME Main KM 2001Hum Reprod2001,16,5:1
4The national partnership for maternal safety 显示文摘D'Alton ME Main EK Menard MK 2014Obstet Gynecol2014,123,5:1
5Delayed relapse of Churg-Strauss syndrome manifesting as colon ulcers with mucosal granulomas:3 cases显示文摘ME ' MAIN N DE BANDT M GUILLEVIN L 2002J Rheumatol2002,29,2:1
6Nursing student voices: reflections on an international service learning experience显示文摘MAIN ME GARRETT-WRIGHT D KERBY M 2013Kentucky Nurs2013,61,1:1
7Sea-salt aerosol transport patterns over the Northern Hemisphere inferred from two subarctic ice core records显示文摘Atmospheric circulation reconstruction based on glaciochemical records requires knowledge of chemical concentration controls, such as source, transport pathway and strength. To gain insight into these processes, the relationships between glaciochemical records from two Northern Hemisphere sites (Mt. Logan in Yukon Territory and 20D in southern Greenland) and instrumental sea level pressure (SLP) series are investigated. Calibrations between Mt. Logan sea-salt sodium (ssNa+) concentration and SLP series show that ssNa+ concentrations are closely correlated with the autumntime (SON) Aleutian Low and the summertime (JJA) North Pacific Subtropical High. Both the deepened Aleutian Low and enhanced North Pacific Sub- tropical High strengthen the transport of sea-salt aerosols from the North Pacific to the Mt. Logan region. Calibrations between 20D ssNa+ concentrations and SLP series indicate that ssNa+ concentrations are closely related to the wintertime (Jan.) Icelandic Low. A deepening of the Icelandic Low strengthens winter storms and frequent cyclogenesis over the North Atlantic and pushes more sea-salt laden air masses to the Greenland ice sheet. Therefore, ice core ssNa+ records from the Mt. Logan region can be considered as a proxy for reconstructing the au- tumntime Aleutian Low and summertime North Pacific Subtropical High, and the ssNa+ records from Greenland ice core (20D) may provide a proxy for reconstructing the wintertime Icelandic Low.YAN Yuping1,2, KANG Shichang2,3,5, SUN Junying4,5, Paul A. Mayewski2 & QIN Dahe5 1. National Climate Center, China Meteorological Administration, Beijing 100081, China 2. Climate Change Institute, University of Maine, Orono, ME 04469, USA 3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China 4. Chinese Academy of Meteorological Sciences, Beijing 100081, China 5. Key Laboratory of Ice Core and Cold Regions Environment, Cold and Arid Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China 2005Science China Earth Sciences2005,48,4:0
8Response of western equatorial Pacificto a westerly wind burst显示文摘INTRODUCTIONWindsWithhorizontalshearareliabletoinduceoceanicupwelling.Forexample,theresPOnseoftheoceantotheatmOSphericjetasshowninFig.Ihascausedacurlthatinducesupwellinginoneregion,downwellinginanother.IftheoceanisinfinitelydeepandhasconstantBrunt--V...Chai Fei and Xue Huijie (School of Marine Sciences , University of Maine, Orono, ME 04469 - 5741, USA) 1999Acta Oceanologica Sinica1999,18,4:0
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