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| 1 | 青藏高原南部冰芯记录与大气环流的关系显示文摘通过念青唐古拉峰拉弄冰川垭口处(30°24′30″N,90°34′12″E;海拔5850m)长度为29.5m的冰芯记录,恢复了1952-1998年间大气降水δD和净积累量的时间变化序列。上述两组序列与NCEP/NCAR气候资料的相关分析表明:δD和净积累量与中亚冬季的气压、南亚和青藏高原冬季、夏季的位势高度关系密切。中亚地区冬季气压的升高以及冬、夏季南亚和青藏高原位势高度的异常增强了印度夏季风,导致了念青唐古拉峰地区20世纪80年代以来降水量的增多和降水中δD值的降低。根据念青唐古拉冰芯δD和净积累量记录及其与亚洲地区大气环流的关系,可以通过青藏高原南部较长的冰芯记录来恢复过去该地区大气环流变化的历史。 | 康世昌 秦大河 任贾文 P.A.Mayewski 侯书贵 张东启 张拥军 S.Kaspari | 2006 | 第四纪研究2006，26，2： | 22 |
| 2 | 珠穆朗玛峰地区冰川净积累量变化的冰芯记录及其气候意义显示文摘根据珠穆朗玛峰地区远东绒布冰川冰芯记录恢复了 5 0年代中期以来冰川净积累量的变化 .结果表明 6 0年代冰川净积累量急剧减少 ,70~ 90年代初期的冰川年平均净积累量仅为 5 0年代后期相应值的一半左右 .珠峰地区冰川净积累量的减少与本区冰川自 5 0年代以来的普遍退缩现象一致 ,其根本原因在于气温 (尤其是夏季气温 )升高所导致的冰川消融强度增大 . | 侯书贵 秦大河 C.P.Wake P.A.Mayewski 任贾文 杨钦钊 | 1999 | 科学通报1999，44，21： | 10 |
| 3 | 喜马拉雅山中段达索普粒雪芯中夏季风和尘埃信号记录研究显示文摘通过粒雪芯δ18O和主要离子 (Ca2 +,Mg2 +,NH+4,SO2 -4 和NO-3 )的分析表明 ,该粒雪芯年平均积累量为 0 .75m水当量 .粒雪芯中δ18O和主要离子浓度的季节变化表明 ,达索普冰川中高精度的记录了现代夏季风和尘埃信号 .夏季风期间降水中δ18O值由”降水量效应”所控制 ,雪层中较低δ18O值则代表了夏季风信号 .亚洲中部干旱半干旱区的春季尘暴输入是造成粒雪芯中Ca2 +,Mg2 +,SO2 -4 和NO-3 浓度春季高值的原因 .EOF分析也证实主要离子浓度春季高值的共性 ,而在NH+4和NO-3 的次一级变化中 ,与Ca2 +和Mg2 +具有反相关关系 。 | 康世昌 秦大河 姚檀栋 C.P.Wake P.A.Mayewski | 1999 | 科学通报1999，44，20： | 10 |
| 4 | Climatological significance of an ice core net-accumulation record at Mt. Qomolangma (Everest)显示文摘An ice core record at Mt. Qomolangma (Everest) since 1954 reveals a sharp decline in net-accumulation in the 1960s, and the annual net-accumulation during the 1970s to the beginning of the 1990s is only half of that at the end of the 1950s. The decreased net-accumulation is coincident with glacier retreat, which is associated with recent temperature increase in the region that intensified the ablation. Under the background of global warming, such glacier variation trends will aggravate. | C.P.Wake P.A.Mayewski | 2000 | Chinese Science Bulletin2000，45，3： | 8 |
| 5 | 南极洲南设得兰群岛Nelson冰帽顶部雪层内的离子浓度分析显示文摘南极冰盖从表层到内部都储存有大量有待发掘的反映自然过程以及人类工业化过程和状态的精细记录。近年来,随着“全球变化”研究热的兴起和测试技术的发展,对极为洁净的南极洲冰雪内所含的阴、阳离子、微量元素、大气成分。 | 秦大河 P.A.Mayewski C.P.Wake 杨钦钊 | 1992 | 科学通报1992，37，11： | 2 |
| 6 | 格陵兰冰芯记录的大气环流变化及其与南极冰芯的比较(英)显示文摘The GISP2, central Greealand, glaciochemical series (sodium, potassium, ammonium,calcium, magnesium, sulfate, nitrate and chloride) provides a unique view of the chemistry of the atmosphere and the history of atmospheric circulation over much of the Northern Hemisphere. Interpretation of this record reveals the controls on both high and low frequency climate events of the last 110 000 years.Changes in insolation on the order of the major orbital cycles control the long-term behavior of atmospheric circulation patterns through changes in ice volume (sea level) and related positive feedbacks.Events such as the Heinrich events (massive discharges of icebergs first identified in the marine record)are found to operate on a 6 100 year cycle due largely to the lagged response of ice sheets to changes in insolation and consequent glacier dynamics Rapid climate change events (massive reorganizations of atmospheric circulation) are demonstrated to operate on 1 450 year cycle possibly in response to internal oscillations in the ocean-atmosphere system or due to changes in solar output. Changes in insolation and associated positive feedbacks related to ice sheets assist in explaining favorable time periods and controls on the amplitude of these massive rapid climate change events.Comparison of the GISP2 glaciochemical series with an ice record from Taylor Dome in Antarctica indicates considerable similarity suggesting that both polar regions experience marked changes in climate. While preliminary evidence points to similar phasing of several major climate events in the two polar regions exact phasing cannot as yet be determined, because dating of Antarctic ice core records is not as well-established as the dating for Greenland ice cores. | P.A.Mayewski L.D.Meeker M.S.Twickler S.Whitlow Q.Yang K.Kreutz D.Reusch | 1998 | 冰川冻土1998，20，4： | 1 |
| 7 | Anions and Cations in a Snow Pit on the Top of Nelson Ice Cap,the Southern Shetland Islands,Antarctica显示文摘The Antarctic Ice Sheet contains a lot of detailed records of the changing processes of the environment, climate and the industrialization. In recent years, the glaciochemistry has been progressing rapidly. Soluble ions are the major impurity deposited on polar glaciers and also are an important aspect of glaciochemistry. Previous studies have covered several locations of Antarctica except the region around the Great Wall Station of China. | 秦大河 P.A.Mayewski C.P.Wake 杨钦钊 | 1993 | Chinese Science Bulletin1993，38，4： | 0 |
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