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| 1 | 青藏高原各拉丹冬冰芯年积累量变化及其与大气环流的关系显示文摘根据各拉丹冬冰芯重建了该地区近70a来积累量的时间序列.冰芯积累量与邻近区域气象台站的降水量存在显著的正相关性,表明冰芯积累量可以作为该地区降水量的代用指标.1930s中期至1960s初期,各拉丹冬地区的降水量处于一个低值期,并于1950s末期达到了极低值.自1960s开始,降水量急剧上升,进入1990s后,降水量有下降趋势,但仍然高于1930s^1950s.利用Mann-Kendall方法检测出该地区降水量在1967年发生了一次突变,即由低降水期转为高降水期.大气环流特征的分析表明,高降水期的西南夏季风比低降水期北扩了约2个纬度,且巴尔喀什湖槽在高降水期明显增强,同时经向风和水汽输送在高降水期也显著增强. | 张拥军 康世昌 秦大河 GRIGHOLM Bjorn MAYEWSKI Paul A | 2007 | 科学通报2007，52，20： | 4 |
| 2 | Iron in the NEEM ice core relative to Asian loess records over the last glacial–interglacial cycle显示文摘Mineral dust can indirectly affect the climate by supplying bioavailable iron(Fe)to the ocean.Here,we present the records of dissolved Fe(DFe)and total Fe(TDFe)in North Greenland Eemian Ice Drilling(NEEM)ice core over the past 110 kyr BP.The Fe records are significantly negatively correlated with the carbon-dioxide(CO_(2))concentrations during cold periods.The results suggest that the changes in Fe fluxes over the past 110 kyr BP in the NEEM ice core are consistent with those in Chinese loess records because the mineral-dust distribution is controlled by the East Asian deserts.Furthermore,the variations in the dust input on a global scale are most likely driven by changes in solar radiation during the last glacial–interglacial cycle in response to Earth’s orbital cycles.In the last glacial–interglacial cycle,the DFe/TDFe ratios were higher during the warm periods(following the post-Industrial Revolution and during the Holocene and last interglacial period)than during the main cold period(i.e.the last glacial maximum(LGM)),indicating that the aeolian input of iron and the iron fertilization effect on the oceans have a non-linear relationship during different periods.Although the burning of biomass aerosols has released large amounts of DFe since the Industrial Revolution,no significant responses are observed in the DFe and TDFe variations during this period,indicating that severe anthropogenic contamination has no significant effect on the DFe(TDFe)release in the NEEM ice core. | Cunde Xiao Zhiheng Du Mike J Handley Paul A Mayewski Junji Cao Simon Schüpbach Tong Zhang Jean-Robert Petit Chuanjin Li Yeongcheol Han Yuefang Li Jiawen Ren | 2021 | National Science Review2021，8，7： | 2 |
| 3 | Holocene climatevariability显示文摘 | Paul A Mayewski Eelco E | 2004 | Quaternary Research2004，62，： | 1 |
| 4 | Evidence for recent climate change from ice cores in the Himalayas 显示文摘 | Mayewski Paul A Wake C P | 2000 | Annals of Glaciology2000，31，： | 1 |
| 5 | Volcanic aerosol records and tephrochronology of the S mmit,Greenland,ice cores显示文摘 | Zielinski Gregory A Mayewski Paul A Meeker L David | 1997 | Journal of Geophysical Research1997，102，26： | 1 |
| 6 | Holocene climate variability显示文摘 | PAUL A MAYEWSKI EELCO E ROHLING J CURT STAGERC | 2004 | Qua- ternary Research2004，62，： | 1 |
| 7 | Holocene climate variability显示文摘 | Paul A Mayewski Eelco E Rohling J Curt Stagerc | 2004 | Quaternary Research2004，62，： | 1 |
| 8 | Holocene climate variability 显示文摘 | PAUL A Mayewski ROHL1NG Eelco E STAGER J Curt | 2004 | Quatemary Research2004，62，： | 1 |
| 9 | Holocene climate variability 显示文摘 | Mayewski Paul A Rohling Eelco E Stager J Curt | 2004 | Quaternary Research2004，62，： | 1 |
| 10 | Soluble species in aerosol and snow and their relationship at glacier 1显示文摘 | Junying Oin Dahe Mayewski Paul A | 1998 | Journal of Geophysical Research1998，103，28： | 1 |
| 11 | A 290-a record of atmospheric circulation over the North Pacific from a Mt. Logan ice core, Yukon Territory显示文摘Calibrations between sodium (Na+) concentrations from a Mt. Logan ice core and sea level pressure (SLP) series show that Na+ concentrations are closely correlated with the autumn-time (SeptemberOctober-November) Aleutian low (AleuLow). A deepening of the AleuLow strengthens the transport of sea-salt aerosols from the North Pacific to the Mt. Logan region. The Mt. Logan Na+ record is used to develop a 292 a (1688~1979) reconstruction of the AleuLow revealing a dramatic intensification of atmospheric circulation over the North Pacific region since the 20th century. Mean SLP of the AleuLow was about 1 hPa lower during the 20th century than during prior periods. The strongest deepening of the AleuLow appeared in the 1950s. Significant correlations are also found between the Mt. Logan AleuLow proxy series and the Pacific decadal oscillation (PDO) and Pacific circulation (PC) index during the 20th century. Evolutionary spectral analysis of the proxy record shows significant periodicities from 15 to 30 a consistent with PDO fluctuations and the bidecadal oscillation of North Pacific atmosphere-ocean circulation. A period of 11 a in the AleuLow record may be associated with the Schwabe 11-a cycle of sunspot activity. Additional longer ice core records from this region will aid in the efforts to further understand the climatic change over the North Pacific region. | KANG Shichang MAYEWSKI Paul A YAN Yuping | 2005 | Acta Oceanologica Sinica2005，24，4： | 0 |
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