Correlation between climate events in the North Atlantic and China during the last glaciation

[1]  Z. An,et al.  Grain Size of Quartz as an Indicator of Winter Monsoon Strength on the Loess Plateau of Central China during the Last 130,000 Yr , 1995, Quaternary Research.

[2]  Wallace S. Broecker,et al.  Massive iceberg discharges as triggers for global climate change , 1994, Nature.

[3]  J. Jouzel,et al.  Climate variations in Europe over the past 140 kyr deduced from rock magnetism , 1994, Nature.

[4]  Murray Gray,et al.  Global Climates since the Last Glacial Maximum , 1994 .

[5]  Xiaoye Zhang,et al.  Late Quaternary Records of the Atmospheric Input of Eolian Dust to the Center of the Chinese Loess Plateau , 1994, Quaternary Research.

[6]  J. Jouzel,et al.  Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores , 1993, Nature.

[7]  Michael J. Singer,et al.  Pedogenesis and paleoclimate: Interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences , 1993 .

[8]  W. Broecker,et al.  Correlations between climate records from North Atlantic sediments and Greenland ice , 1993, Nature.

[9]  J. Jouzel,et al.  Evidence for general instability of past climate from a 250-kyr ice-core record , 1993, Nature.

[10]  E. Cortijo,et al.  Patterns of Ice-Rafted Detritus in the Glacial North Atlantic (40–55°N) , 1993 .

[11]  G. W. Lamorey,et al.  The ‘flickering switch’ of late Pleistocene climate change , 1993, Nature.

[12]  M. Suter,et al.  10Be and magnetic susceptibility in Chinese loess , 1993 .

[13]  W. Broecker,et al.  Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period , 1992, Nature.

[14]  J. Jouzel,et al.  Irregular glacial interstadials recorded in a new Greenland ice core , 1992, Nature.

[15]  S. Forman Late Pleistocene chronology of loess deposition near Luochuan, China , 1991, Quaternary Research.

[16]  G. Kukla,et al.  Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years , 1991, Quaternary Research.

[17]  Frank Oldfield,et al.  The Climate of China , 1989 .

[18]  J. Guiot,et al.  A 140,000-year continental climate reconstruction from two European pollen records , 1989, Nature.

[19]  Syukuro Manabe,et al.  Two Stable Equilibria of a Coupled Ocean-Atmosphere Model , 1988 .

[20]  H. Heinrich,et al.  Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years , 1988, Quaternary Research.

[21]  J. D. Hays,et al.  Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy , 1987, Quaternary Research.

[22]  W. Broecker,et al.  The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11–10 k) , 1986 .

[23]  G. Kukla,et al.  The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China , 1990 .

[24]  Dongsheng Liu,et al.  Loess and the environment , 1985 .

[25]  John D. Spengler,et al.  A QUANTITATIVE ASSESSMENT OF SOURCE CONTRIBUTIONS TO INHALABLE PARTICULATE MATTER POLLUTION IN METROPOLITAN BOSTON , 1985 .

[26]  P. Liss,et al.  Air-Sea Exchange of Gases and Particles , 1983 .

[27]  W. Slinn Air-to-Sea Transfer of Particles , 1983 .