Indian summer monsoon variability in northeastern India during the last two millennia

[1]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[2]  M. Gałka,et al.  Recent fire regime in the southern boreal forests of western Siberia is unprecedented in the last five millennia , 2020 .

[3]  D. Anderson,et al.  Abrupt shifts in the Indian summer monsoon during the last three millennia , 2020 .

[4]  P. Srivastava,et al.  High-resolution climatic (monsoonal) variability reconstructed from a continuous ~2700-year sediment record from Northwest Himalaya (Ladakh) , 2020 .

[5]  S. Vicente‐Serrano,et al.  A review of environmental droughts: Increased risk under global warming? , 2020 .

[6]  P. Arulbalaji,et al.  Holocene climate variability and Indian Summer Monsoon: An overview , 2020 .

[7]  A. Gupta,et al.  Abrupt changes in Indian summer monsoon strength during the last ~900 years and their linkages to socio-economic conditions in the Indian subcontinent , 2019 .

[8]  A. Gupta,et al.  Climate variability and evolution of the Indus civilization , 2019, Quaternary International.

[9]  A. Jull,et al.  Signatures of global climatic events and forcing factors for the last two millennia from the active mudflats of Rohisa, southern Saurashtra, Gujarat, western India , 2019, Quaternary International.

[10]  R. Edwards,et al.  Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India , 2018, Climate of the Past.

[11]  R. Ramesh,et al.  The Indian Summer Monsoon from a Speleothem δ18O Perspective—A Review , 2018, Quaternary.

[12]  A. Gupta,et al.  A long arid interlude in the Indian summer monsoon during ∼4,350 to 3,450 cal. yr BP contemporaneous to displacement of the Indus valley civilization , 2018, Quaternary International.

[13]  N. Marwan,et al.  Contrasting pattern of hydrological changes during the past two millennia from central and northern India: Regional climate difference or anthropogenic impact? , 2018 .

[14]  R. Edwards,et al.  The Indian monsoon variability and civilization changes in the Indian subcontinent , 2017, Science Advances.

[15]  G. Haug,et al.  Climatic and in-cave influences on δ18O and δ13C in a stalagmite from northeastern India through the last deglaciation , 2017, Quaternary Research.

[16]  Keith M. Prufer,et al.  Tropical rainfall over the last two millennia: evidence for a low-latitude hydrologic seesaw , 2017, Scientific Reports.

[17]  A. Bräuning,et al.  Boreal spring precipitation variability in the cold arid western Himalaya during the last millennium, regional linkages, and socio-economic implications , 2016 .

[18]  R. Edwards,et al.  Abrupt changes in Indian summer monsoon strength during 33,800 to 5500 years B.P. , 2015 .

[19]  M. Winstrup,et al.  Timing and climate forcing of volcanic eruptions for the past 2,500 years , 2015, Nature.

[20]  B. Goswami,et al.  Drying of Indian subcontinent by rapid Indian Ocean warming and a weakening land-sea thermal gradient , 2015, Nature Communications.

[21]  S. Clemens,et al.  Multiproxy record of monsoon variability from the Ganga Plain during 400–1200 A.D. , 2015 .

[22]  R. Bennartz,et al.  Northeast Indian stalagmite records Pacific decadal climate change: Implications for moisture transport and drought in India , 2015 .

[23]  N. Marwan,et al.  Cave ventilation and rainfall signals in dripwater in a monsoonal setting – a monitoring study from NE India , 2015 .

[24]  Manfred Mudelsee,et al.  Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia , 2015, Nature Communications.

[25]  N. Diffenbaugh,et al.  Observed changes in extreme wet and dry spells during the South Asian summer monsoon season , 2014 .

[26]  R. Edwards,et al.  Mid-latitude interhemispheric hydrologic seesaw over the past 550,000 years , 2014, Nature.

[27]  F. Hu,et al.  Recent burning of boreal forests exceeds fire regime limits of the past 10,000 years , 2013, Proceedings of the National Academy of Sciences.

[28]  R. Edwards,et al.  Improvements in 230Th dating, 230Th and 234U half-life values, and U–Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry , 2013 .

[29]  A. Kitoh,et al.  Monsoons in a changing world: A regional perspective in a global context , 2013 .

[30]  N. Graham,et al.  Continental-scale temperature variability during the past two millennia , 2013 .

[31]  K. Yoshimura,et al.  An Abrupt Shift in the Indian Monsoon 4000 Years Ago , 2013 .

[32]  Shaun A Marcott,et al.  A Reconstruction of Regional and Global Temperature for the Past 11,300 Years , 2013, Science.

[33]  J. Fohlmeister.  A statistical approach to construct composite climate records of dated archives , 2012 .

[34]  P. Mayewski,et al.  An independently dated 2000-yr volcanic record from Law Dome, East Antarctica, including a new perspective on the dating of the 1450s CE eruption of Kuwae, Vanuatu , 2012 .

[35]  W. Raza,et al.  Climatic fluctuations during the LIA and post-LIA in the Kumaun Lesser Himalaya, India: Evidence from a 400 y old stalagmite record , 2012 .

[36]  H. Oerter,et al.  9,400 years of cosmic radiation and solar activity from ice cores and tree rings , 2012, Proceedings of the National Academy of Sciences.

[37]  M. Holland,et al.  Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea‐ice/ocean feedbacks , 2012 .

[38]  M. Mudelsee,et al.  The leading mode of Indian Summer Monsoon precipitation variability during the last millennium , 2011 .

[39]  Denis Scholz,et al.  StalAge – An algorithm designed for construction of speleothem age models , 2011 .

[40]  F. Ljungqvist.  A new reconstruction of temperature variability in the extra‐tropical northern hemisphere during the last two millennia , 2010 .

[41]  W. Landman.  Climate change 2007: the physical science basis , 2010 .

[42]  G. Haug,et al.  Strong influence of water vapor source dynamics on stable isotopes in precipitation observed in Southern Meghalaya, NE India , 2010 .

[43]  Hai Cheng,et al.  Persistent multidecadal power of the Indian Summer Monsoon , 2010 .

[44]  G. Faluvegi,et al.  Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly , 2009, Science.

[45]  M. Hughes,et al.  Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia , 2008, Proceedings of the National Academy of Sciences.

[46]  Sébastien Lê,et al.  FactoMineR: An R Package for Multivariate Analysis , 2008 .

[47]  G. Müller,et al.  Sediment characteristics and transportation dynamics of the Ganga River , 2007 .

[48]  F. Murata,et al.  Rainfall on the Meghalaya plateau in northeastern India—one of the rainiest places in the world , 2007 .

[49]  P. Xavier,et al.  Increasing Trend of Extreme Rain Events Over India in a Warming Environment , 2006, Science.

[50]  A. Sarkar,et al.  Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India , 2006 .

[51]  J. Smol,et al.  Accelerated melting of Himalayan snow and ice triggers pronounced changes in a valley peatland from northern India , 2006 .

[52]  R. Stouffer,et al.  Response of the ITCZ to Northern Hemisphere cooling , 2006 .

[53]  F. Sirocko,et al.  El Niño variability off Peru during the last 20,000 years , 2005 .

[54]  R. Lawrence Edwards,et al.  The Holocene Asian Monsoon: Links to Solar Changes and North Atlantic Climate , 2005, Science.

[55]  K. Holmgren,et al.  Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data , 2005, Nature.

[56]  G. Meehl,et al.  More Intense, More Frequent, and Longer Lasting Heat Waves in the 21st Century , 2004, Science.

[57]  Kenneth P. Bowman,et al.  Stable isotopic composition of water vapor in the tropics , 2004 .

[58]  Michael E. Mann,et al.  Global surface temperatures over the past two millennia , 2003 .

[59]  Manfred Mudelsee,et al.  Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman , 2003, Science.

[60]  X. Qin,et al.  Cyclic rapid warming on centennial‐scale revealed by a 2650‐year stalagmite record of warm season temperature , 2003 .

[61]  J. Overpeck,et al.  Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean , 2003, Nature.

[62]  J. Overpeck,et al.  Increase in the Asian Southwest Monsoon During the Past Four Centuries , 2002, Science.

[63]  M. Reagan,et al.  A high-resolution speleothem record of climatic variability at the Allerød–Younger Dryas transition in Missouri, central United States , 2001 .

[64]  B. Hamelin,et al.  Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for 13C variations in speleothems , 2001 .

[65]  Gerald H. Haug,et al.  Southward Migration of the Intertropical Convergence Zone Through the Holocene , 2001, Science.

[66]  Thompson,et al.  A high-resolution millennial record of the south asian monsoon from himalayan ice cores , 2000, Science.

[67]  A. Munot,et al.  Homogeneous Indian Monsoon rainfall: Variability and prediction , 1993, Journal of Earth System Science.

[68]  John A. Eddy,et al.  The Maunder Minimum , 1976, Science.

[69]  R Core Team,et al.  R: A language and environment for statistical computing. , 2014 .

[70]  By W. Dansga,et al.  Stable isotopes in precipitation , 2010 .

[71]  North Greenland Ice Core Project members.  High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004 .

[72]  Ø. Hammer,et al.  PAST: PALEONTOLOGICAL STATISTICAL SOFTWARE PACKAGE FOR EDUCATION AND DATA ANALYSIS , 2001 .

[73]  O Hammer-Muntz,et al.  PAST: paleontological statistics software package for education and data analysis version 2.09 , 2001 .

[74]  G. Wasserburg,et al.  238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years , 1987 .

[75]  R. Majumdar.  An Advanced History of India , 1946 .