The timing of orbital-scale Indian monsoon changes

[1]  J. Kutzbach,et al.  Hemispheric insolation forcing of the Indian Ocean and Asian monsoon: Local versus remote impacts , 2006 .

[2]  W. Ruddiman What is the timing of orbital-scale monsoon changes? , 2006 .

[3]  J. Kutzbach,et al.  Global monsoons in the mid-Holocene and oceanic feedback , 2004 .

[4]  Ping Liu,et al.  Contrasting the Indian and East Asian monsoons: implications on geologic timescales , 2003 .

[5]  S. Clemens,et al.  A 350,000 year summer-monsoon multi-proxy stack from the Owen Ridge, Northern Arabian Sea , 2003 .

[6]  J. Kutzbach,et al.  Coupled climate simulation of the evolution of global monsoons in the Holocene , 2003 .

[7]  Maureen E. Raymo,et al.  A methane-based time scale for Vostok ice , 2003 .

[8]  K. Lau,et al.  Interannual Variability of the Asian Summer Monsoon: Contrasts between the Indian and the Western North Pacific–East Asian Monsoons* , 2001 .

[9]  J. Kutzbach,et al.  Land-ocean-atmosphere interactions and monsoon climate change: A paleo-perspective , 2001 .

[10]  N. Shackleton,et al.  The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity , 2000, Science.

[11]  W. Prell,et al.  Climatically linked oscillations in Arabian Sea denitrification over the past 1 m.y.: Implications for the marine N cycle , 1999 .

[12]  G. Reichart,et al.  Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years , 1998 .

[13]  S. Clemens Dust response to seasonal atmospheric forcing: Proxy evaluation and calibration , 1998 .

[14]  Sandy P. Harrison,et al.  Climate and biome simulations for the past 21 , 1998 .

[15]  J. Kutzbach,et al.  Response of the African Monsoon to Orbital Forcing and Ocean Feedbacks in the Middle Holocene , 1997 .

[16]  J. Kutzbach,et al.  Potential role of vegetation feedback in the climate sensitivity of high-latitude regions: A case study at 6000 years B.P. , 1996 .

[17]  J. Kutzbach,et al.  Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle Holocene , 1996, Nature.

[18]  S. Clemens,et al.  Nonstationary Phase of the Plio-Pleistocene Asian Monsoon , 1996, Science.

[19]  W. Prell,et al.  Climate-related variations in denitrification in the Arabian Sea from sediment 15N/14N ratios , 1995, Nature.

[20]  Peter J. Webster,et al.  The role of hydrological processes in ocean‐atmosphere interactions , 1994 .

[21]  T. Sowers,et al.  The Dole Effect and its variations during the last 130,000 years as measured in the Vostok Ice Core , 1994 .

[22]  S. Clemens,et al.  Forcing mechanisms of the Indian Ocean monsoon , 1991, Nature.

[23]  G. Weedon,et al.  A 350 ka history of the Indian Southwest Monsoon—evidence from deep-sea cores, northwest Arabian Sea , 1990, Transactions of the Royal Society of Edinburgh: Earth Sciences.

[24]  J. Kutzbach,et al.  Sensitivity of a coupled atmosphere/mixed layer ocean model to changes in orbital forcing at 9000 years B.P. , 1988 .

[25]  D. Raynaud,et al.  Isotopic composition of atmospheric O2 in ice linked with deglaciation and global primary productivity , 1985, Nature.

[26]  J. Kutzbach,et al.  Milankovitch forcing of fluctuations in the level of tropical lakes from 18 to 0 kyr BP , 1985, Nature.

[27]  J. Kutzbach,et al.  Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago , 1981, Science.