Articles | Volume 8, issue 5
Clim. Past, 8, 1541–1550, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue: Advances in understanding and applying speleothem climate...
Research article 11 Oct 2012
Research article | 11 Oct 2012
Isotopic and lithologic variations of one precisely-dated stalagmite across the Medieval/LIA period from Heilong Cave, central China
Y. F. Cui et al.
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Centennial-DecadalA 2600-year summer climate reconstruction in central Japan by integrating tree-ring stable oxygen and hydrogen isotopesAn overview on isotopic divergences – causes for instability of tree-ring isotopes and climate correlationsProxy surrogate reconstructions for Europe and the estimation of their uncertaintiesThe 4.2 ka event in the central Mediterranean: new data from a Corchia speleothem (Apuan Alps, central Italy)A 900-year New England temperature reconstruction from in situ seasonally produced branched glycerol dialkyl glycerol tetraethers (brGDGTs)Leaf wax n-alkane distributions record ecological changes during the Younger Dryas at Trzechowskie paleolake (northern Poland) without temporal delayGround surface temperature reconstruction for the last 500 years obtained from permafrost temperatures observed in the SHARE STELVIO Borehole, Italian AlpsDecreasing Indian summer monsoon on the northern Indian sub-continent during the last 180 years: evidence from five tree-ring cellulose oxygen isotope chronologiesRecent climate variations in Chile: constraints from borehole temperature profilesSpatio-temporal variability of Arctic summer temperatures over the past 2 millenniaPalaeoclimate significance of speleothems in crystalline rocks: a test case from the Late Glacial and early Holocene (Vinschgau, northern Italy)Comparing proxy and model estimates of hydroclimate variability and change over the Common EraClimate signals in a multispecies tree-ring network from central and southern Italy and reconstruction of the late summer temperatures since the early 1700sLow-resolution Australasian palaeoclimate records of the last 2000 yearsClimatic history of the northeastern United States during the past 3000 yearsExperiments based on blue intensity for reconstructing North Pacific temperatures along the Gulf of AlaskaSpring temperature variability over Turkey since 1800 CE reconstructed from a broad network of tree-ring dataOn the spatial and temporal variability of ENSO precipitation and drought teleconnection in mainland Southeast AsiaInterannual and (multi-)decadal variability in the sedimentary BIT index of Lake Challa, East Africa, over the past 2200 years: assessment of the precipitation proxyA tree-ring perspective on temporal changes in the frequency and intensity of hydroclimatic extremes in the territory of the Czech Republic since 761 ADMulti-century lake area changes in the Southern Altiplano: a tree-ring-based reconstructionOptimal ranking regime analysis of TreeFlow dendrohydrological reconstructionsNew insights into the reconstructed temperature in Portugal over the last 400 yearsExpressions of climate perturbations in western Ugandan crater lake sediment records during the last 1000 yearsBlue intensity and density from northern Fennoscandian tree rings, exploring the potential to improve summer temperature reconstructions with earlywood informationReconstruction of the March–August PDSI since 1703 AD based on tree rings of Chinese pine (Pinus tabulaeformis Carr.) in the Lingkong Mountain, southeast Chinese loess PlateauForward modelling of tree-ring width and comparison with a global network of tree-ring chronologiesReconstruction of northeast Asia spring temperature 1784–1990COnstructing Proxy Records from Age models (COPRA)A 560 yr summer temperature reconstruction for the Western Mediterranean basin based on stable carbon isotopes from Pinus nigra ssp. laricio (Corsica/France)Modelling and climatic interpretation of the length fluctuations of Glaciar Frías (north Patagonian Andes, Argentina) 1639–2009 ADA review of the South American monsoon history as recorded in stable isotopic proxies over the past two millenniaIdentification of climatic state with limited proxy dataMulti-century tree-ring based reconstruction of the Neuquén River streamflow, northern Patagonia, ArgentinaExtreme pointer years in tree-ring records of Central Spain as evidence of climatic events and the eruption of the Huaynaputina Volcano (Peru, 1600 AD)Precipitation changes in the South American Altiplano since 1300 AD reconstructed by tree-ringsFire history in western Patagonia from paired tree-ring fire-scar and charcoal recordsNorthern Hemisphere temperature patterns in the last 12 centuries
Takeshi Nakatsuka, Masaki Sano, Zhen Li, Chenxi Xu, Akane Tsushima, Yuki Shigeoka, Kenjiro Sho, Keiko Ohnishi, Minoru Sakamoto, Hiromasa Ozaki, Noboru Higami, Nanae Nakao, Misao Yokoyama, and Takumi Mitsutani
Clim. Past, 16, 2153–2172,Short summary
In general, it is not easy to reconstruct past climate variations over a wide band of frequencies using a single proxy. Here, we propose a new method to reconstruct past summer climate seamlessly from annual to millennial timescales by integrating tree-ring cellulose oxygen and hydrogen isotope ratios. The result can be utilized to investigate various scales of climatological phenomena in the past and climate–society relationships in long human history.
Martine M. Savard and Valérie Daux
Clim. Past, 16, 1223–1243,Short summary
Climatic reconstructions based on tree-ring isotopic series convey key information on past conditions prevailing in forested regions. However, in some cases, the relations between isotopes and climate appear unstable over time, generating isotopic divergences. Former reviews have thoroughly discussed the divergence concept for tree-ring width but not for isotopes. Here we present a synopsis of the isotopic divergence problem and suggest collaborative work for improving climatic reconstructions.
Oliver Bothe and Eduardo Zorita
Clim. Past, 16, 341–369,Short summary
One can use the similarity between sparse indirect observations of past climates and full fields of simulated climates to learn more about past climates. Here, we detail how one can compute uncertainty estimates for such reconstructions of past climates. This highlights the ambiguity of the reconstruction. We further show that such a reconstruction for European summer temperature agrees well with a more common approach.
Ilaria Isola, Giovanni Zanchetta, Russell N. Drysdale, Eleonora Regattieri, Monica Bini, Petra Bajo, John C. Hellstrom, Ilaria Baneschi, Piero Lionello, Jon Woodhead, and Alan Greig
Clim. Past, 15, 135–151,Short summary
To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
Daniel R. Miller, M. Helen Habicht, Benjamin A. Keisling, Isla S. Castañeda, and Raymond S. Bradley
Clim. Past, 14, 1653–1667,Short summary
We measured biomarker production over a year in a small inland lake in the northeastern USA. Understanding biomarkers in the modern environment helps us improve reconstructions of past climate from lake sediment records. We use these results to interpret a 900-year decadally resolved temperature record from this lake. Our record highlights multi-decadal oscillations in temperature superimposed on a long-term cooling trend, providing novel insight into climate dynamics of the region.
Bernhard Aichner, Florian Ott, Michał Słowiński, Agnieszka M. Noryśkiewicz, Achim Brauer, and Dirk Sachse
Clim. Past, 14, 1607–1624,Short summary
Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive covering the Late Glacial to Holocene transition in northern Poland. Both parameters synchronously show the rapid onset (12680–12600 yr BP) and termination (11580–11490 yr BP) of the Younger Dryas cold interval in the study area. This demonstrates the suitability of such proxies to record pronounced changes in vegetation cover without significant delay.
Mauro Guglielmin, Marco Donatelli, Matteo Semplice, and Stefano Serra Capizzano
Clim. Past, 14, 709–724,Short summary
The reconstruction of ground surface temperature for the last 500 years, obtained at the deepest mountain permafrost borehole of the world (Stelvio Pass, 3000 m a.s.l., Italian Alps), is presented here. The main difference with respect to MAAT reconstructions obtained through other proxy data for all of Europe relates to post Little Ice Age (LIA) events. Indeed at this site a stronger cooling of ca 1 °C between 1940 and 1989 and even a more abrupt warming between 1990 and 2011 was detected.
Chenxi Xu, Masaki Sano, Ashok Priyadarshan Dimri, Rengaswamy Ramesh, Takeshi Nakatsuka, Feng Shi, and Zhengtang Guo
Clim. Past, 14, 653–664,Short summary
We have constructed a regional tree ring cellulose oxygen isotope record using a total of five chronologies obtained from the Himalaya. Centennial changes in the regional tree ring record indicate a trend of weakened Indian summer monsoon (ISM) intensity since 1820. Decreasing ISM activity is also observed in various high-resolution ISM records from southwest China and Southeast Asia, and may be the result of reduced land–ocean thermal contrasts since 1820.
Carolyne Pickler, Edmundo Gurza Fausto, Hugo Beltrami, Jean-Claude Mareschal, Francisco Suárez, Arlette Chacon-Oecklers, Nicole Blin, Maria Teresa Cortés Calderón, Alvaro Montenegro, Rob Harris, and Andres Tassara
Clim. Past, 14, 559–575,Short summary
We compiled 31 temperature–depth profiles to reconstruct the ground surface temperature of the last 500 years in northern Chile. They suggest that the region experienced a cooling from 1850 to 1980 followed by a warming of 1.9 K. The cooling could coincide with a cooling interval in 1960. The warming is greater than that of proxy reconstructions for nearby regions and model simulations. These differences could be due to differences in spatial and temporal resolution between data and models.
Johannes P. Werner, Dmitry V. Divine, Fredrik Charpentier Ljungqvist, Tine Nilsen, and Pierre Francus
Clim. Past, 14, 527–557,Short summary
We present a new gridded Arctic summer temperature reconstruction back to the first millennium CE. Our method respects the age uncertainties of the data, which results in a more precise reconstruction.
The spatial average shows a millennium-scale cooling trend which is reversed in the mid-19th century. While temperatures in the 10th century were probably as warm as in the 20th century, the spatial coherence of the recent warm episodes seems unprecedented.
The spatial average shows a millennium-scale cooling trend which is reversed in the mid-19th century. While temperatures in the 10th century were probably as warm as in the 20th century, the spatial coherence of the recent warm episodes seems unprecedented.
Gabriella Koltai, Hai Cheng, and Christoph Spötl
Clim. Past, 14, 369–381,Short summary
Here we present a multi-proxy study of flowstones in fractures of crystalline rocks with the aim of assessing the palaeoclimate significance of this new type of speleothem archive. Our results indicate a high degree of spatial heterogeneity, whereby changes in speleothem mineralogy and carbon isotope composition are likely governed by aquifer-internal processes. In contrast, the oxygen isotope composition reflects first-order climate variability.
PAGES Hydro2k Consortium
Clim. Past, 13, 1851–1900,Short summary
Water availability is fundamental to societies and ecosystems, but our understanding of variations in hydroclimate (including extreme events, flooding, and decadal periods of drought) is limited due to a paucity of modern instrumental observations. We review how proxy records of past climate and climate model simulations can be used in tandem to understand hydroclimate variability over the last 2000 years and how these tools can also inform risk assessments of future hydroclimatic extremes.
Giovanni Leonelli, Anna Coppola, Maria Cristina Salvatore, Carlo Baroni, Giovanna Battipaglia, Tiziana Gentilesca, Francesco Ripullone, Marco Borghetti, Emanuele Conte, Roberto Tognetti, Marco Marchetti, Fabio Lombardi, Michele Brunetti, Maurizio Maugeri, Manuela Pelfini, Paolo Cherubini, Antonello Provenzale, and Valter Maggi
Clim. Past, 13, 1451–1471,Short summary
We analyze a tree-ring network from several sites distributed along the Italian Peninsula with the aims of detecting common climate drivers of tree growth and of reconstructing the past climate. We detect the main climatic drivers modulating tree-ring width (RW) and tree-ring maximum latewood density (MXD) and we reconstruct late summer temperatures since the early 1700s using a MXD chronology: this reconstruction is representative of a wide area around the Italian Peninsula.
Bronwyn C. Dixon, Jonathan J. Tyler, Andrew M. Lorrey, Ian D. Goodwin, Joëlle Gergis, and Russell N. Drysdale
Clim. Past, 13, 1403–1433,Short summary
Existing sedimentary palaeoclimate records in Australasia were assessed for suitability for examining the last 2 millennia. A small number of high-quality records were identified, and new Bayesian age models were constructed for each record. Findings suggest that Australasian record chronologies and confidence in proxy–climate relationships are the main factors limiting appropriate data for examining Common Era climate variability. Recommendations for improving data accessibility are provided.
Jennifer R. Marlon, Neil Pederson, Connor Nolan, Simon Goring, Bryan Shuman, Ann Robertson, Robert Booth, Patrick J. Bartlein, Melissa A. Berke, Michael Clifford, Edward Cook, Ann Dieffenbacher-Krall, Michael C. Dietze, Amy Hessl, J. Bradford Hubeny, Stephen T. Jackson, Jeremiah Marsicek, Jason McLachlan, Cary J. Mock, David J. P. Moore, Jonathan Nichols, Dorothy Peteet, Kevin Schaefer, Valerie Trouet, Charles Umbanhowar, John W. Williams, and Zicheng Yu
Clim. Past, 13, 1355–1379,Short summary
To improve our understanding of paleoclimate in the northeastern (NE) US, we compiled data from pollen, tree rings, lake levels, testate amoeba from bogs, and other proxies from the last 3000 years. The paleoclimate synthesis supports long-term cooling until the 1800s and reveals an abrupt transition from wet to dry conditions around 550–750 CE. Evidence suggests the region is now becoming warmer and wetter, but more calibrated data are needed, especially to capture multidecadal variability.
Rob Wilson, Rosanne D'Arrigo, Laia Andreu-Hayles, Rose Oelkers, Greg Wiles, Kevin Anchukaitis, and Nicole Davi
Clim. Past, 13, 1007–1022,Short summary
Blue intensity shows great potential for reconstructing past summer temperatures from conifer trees growing at high latitude or the treeline. However, conifer species that express a strong colour difference between the heartwood and sapwood can impart a long-term trend bias in the resultant reconstructions. Herein, we highlight this issue using eight mountain hemlock sites across the Gulf of Alaska and explore how a non-biased reconstruction of past temperature could be derived using such data.
Nesibe Köse, H. Tuncay Güner, Grant L. Harley, and Joel Guiot
Clim. Past, 13, 1–15,
Timo A. Räsänen, Ville Lindgren, Joseph H. A. Guillaume, Brendan M. Buckley, and Matti Kummu
Clim. Past, 12, 1889–1905,Short summary
El Niño-Southern Oscillation (ENSO) is linked to severe droughts and floods in mainland Southeast Asia. This research provides a more accurate and uniform picture of the spatio-temporal effects of ENSO on precipitation (1980–2013) and improves our understanding of long-term (1650–2004) ENSO teleconnection and its variability over the study area. The results reveal not only recognisable spatio-temporal patterns but also a high degree of variability and non-stationarity in the effects of ENSO.
Laura K. Buckles, Dirk Verschuren, Johan W. H. Weijers, Christine Cocquyt, Maarten Blaauw, and Jaap S. Sinninghe Damsté
Clim. Past, 12, 1243–1262,Short summary
This paper discusses the underlying mechanisms of a method that uses specific membrane lipids present in the sediments of an African tropical lake to determine past changes in rainfall. With this method, past dry periods in the last 25 000 years can be assessed.
P. Dobrovolný, M. Rybníček, T. Kolář, R. Brázdil, M. Trnka, and U. Büntgen
Clim. Past, 11, 1453–1466,Short summary
A new data set of 3194 oak (Quercus spp.) ring width samples collected across the Czech Republic and covering the past 1250 years was analysed. The temporal distribution of negative and positive TRW extremes occurring is regular with no indication of clustering. Negative TRW extremes coincided with above-average March-May and June-August temperature means and below-average precipitation totals. Positive extremes coincided with higher summer precipitation, while temperatures were mostly normal.
M. S. Morales, J. Carilla, H. R. Grau, and R. Villalba
Clim. Past, 11, 1139–1152,Short summary
A 601-year lake area reconstruction in NW Argentina and SW Bolivia, characterized the occurrence of annual to multi-decadal lake area fluctuations and its main oscillation modes of variability. Our reconstruction points out that the late 20th century decrease in lake area was exceptional over the period 1407–2007. A persistent negative trend in lake area is clear in the reconstruction and consistent with glacier retreat and other climate proxies from the Altiplano and the tropical Andes.
S. A. Mauget
Clim. Past, 11, 1107–1125,Short summary
A new approach to time series analysis - the ORR method - was used to evaluate reconstructed western US streamflow records during 1500-2007. This method shows an interesting pattern of alternating drought and wet periods during the late 16th and 17th centuries, a period with relatively few drought or wet periods during the 18th century, and the and the reappearance of alternating dry and wet periods during the 19th and early 20th centuries.
J. A. Santos, M. F. Carneiro, A. Correia, M. J. Alcoforado, E. Zorita, and J. J. Gómez-Navarro
Clim. Past, 11, 825–834,
K. Mills, D. B. Ryves, N. J. Anderson, C. L. Bryant, and J. J. Tyler
Clim. Past, 10, 1581–1601,
J. A. Björklund, B. E. Gunnarson, K. Seftigen, J. Esper, and H. W. Linderholm
Clim. Past, 10, 877–885,
Q. Cai, Y. Liu, Y. Lei, G. Bao, and B. Sun
Clim. Past, 10, 509–521,
P. Breitenmoser, S. Brönnimann, and D. Frank
Clim. Past, 10, 437–449,
M. Ohyama, H. Yonenobu, J.-N. Choi, W.-K. Park, M. Hanzawa, and M. Suzuki
Clim. Past, 9, 261–266,
S. F. M. Breitenbach, K. Rehfeld, B. Goswami, J. U. L. Baldini, H. E. Ridley, D. J. Kennett, K. M. Prufer, V. V. Aquino, Y. Asmerom, V. J. Polyak, H. Cheng, J. Kurths, and N. Marwan
Clim. Past, 8, 1765–1779,
S. Szymczak, M. M. Joachimski, A. Bräuning, T. Hetzer, and J. Kuhlemann
Clim. Past, 8, 1737–1749,
P. W. Leclercq, P. Pitte, R. H. Giesen, M. H. Masiokas, and J. Oerlemans
Clim. Past, 8, 1385–1402,
M. Vuille, S. J. Burns, B. L. Taylor, F. W. Cruz, B. W. Bird, M. B. Abbott, L. C. Kanner, H. Cheng, and V. F. Novello
Clim. Past, 8, 1309–1321,
J. D. Annan and J. C. Hargreaves
Clim. Past, 8, 1141–1151,
I. A. Mundo, M. H. Masiokas, R. Villalba, M. S. Morales, R. Neukom, C. Le Quesne, R. B. Urrutia, and A. Lara
Clim. Past, 8, 815–829,
Clim. Past, 8, 751–764,
M. S. Morales, D. A. Christie, R. Villalba, J. Argollo, J. Pacajes, J. S. Silva, C. A. Alvarez, J. C. Llancabure, and C. C. Soliz Gamboa
Clim. Past, 8, 653–666,
A. Holz, S. Haberle, T. T. Veblen, R. De Pol-Holz, and J. Southon
Clim. Past, 8, 451–466,
F. C. Ljungqvist, P. J. Krusic, G. Brattström, and H. S. Sundqvist
Clim. Past, 8, 227–249,
Annamalai, H. and Slingo, J. M.: Active/break cycles: Diagnosis of the intraseasonal variability of the Asian summer monsoon, Clim. Dynam., 18, 85–102, 2001.
Araguás-Araguás, L., Froehlich, K., and Rozanski, K.: Stable isotope composition of precipitation over Southeast Asia, J. Geophys Res., 103, 28721–28742, 1998.
Baldini, J., McDermott, F., Baker, A., Baldini, L., Mattey, D., and Railsback, B.: Biomass effects on stalagmite growth and isotope ratios: a 20th century analogue from Wiltshire, England, Earth Planet. Sc. Lett., 240, 486–494, 2005.
Bar-Matthews, M., Ayalon, A., Matthews, A., Sass, E., and Halicz, L.: Carbon and oxygen isotope study of the active water-carbonate system in a karstic Mediterranean Cave: implication for palaeoclimate research in semiarid regions, Geochim. Cosmochim. Ac., 60, 337–347, 1996.
Bar-Matthews, M., Ayalon, A., Kaufman,A., and Wasserburg, G. J.: The Eastern Mediterranean paleoclimate as a reflection of regional events: Soreq Cave, Israel, Earth Planet. Sc. Lett., 166, 85–95, 1999.
Bird, B. W., Abbott, M. B., Vuille, M., Rodbell, D. T., Stansell, N. D., and Rosenmeier, M. F.: A 2,300-year-long annually resolved record of the South American summer monsoon from the Peruvian Andes, Proc. Natl. Acad. Sci. USA, 108, 8583–8588, 2011
Bradley, R. S. and Jones, P. D.: When was the "Little Ice Age"?, in: Proceedings of the International Symposium on the Little Ice Age climate, edited by: Mikami, T., Department of Geography, Tokyo Metropolitan University, 1–4, 1992.
Bradley, R. S., Hughes, M. K., and Diaz, H. F.: Climate in Medieval time, Science, 302, 404–405, 2003.
Brown, E. T. and Johnson, T. C.: Coherence between tropical East African and South American records of the Little Ice Age, Geochem. Geophy. Geosy., 6, Q12005, https://doi.org/10.1029/2005GC000959, 2005.
Buckley, B. M., Anchukaitis, K. J., Penny, D., Fletcher, R., Cook, E. R., Sano, M., Nam, L. C., Wichienkeeo, A., Minh, T. T., and Hong, T. M.: Climate as a contributing factor in the demise of Angkor, Cambodia, Proc. Natl. Acad. Sci. USA, 107, 6748–6752, 2010.
Cai, Y. J., Tan, L. C., Cheng, H., An, Z. S., Edwards, R. L., Kelly, M. J., Kong, X. G., and Wang, X. F.: The variation of summer monsoon precipitation in central China since the last deglaciation, Earth Planet. Sc. Lett., 291, 21–31, 2010.
Cheng, H., Edwards, R. L., Hoff, J., Gallup, C. D., Richards, D. A., and Asmerom, Y.: The half-lives of uranium-234 and thorium-230, Chem. Geol., 169, 17–33, 2000.
Cheng, H., Edwards, R. L., Wang, Y. J., Kong, X. G., Ming, Y. F., Gallup, C. D., Kelly, M. J., Wang, X. F., and Liu, W. G.: A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations, Geology, 34, 217–220, 2006.
Cheng, H., Edwards, R. L., Broecker, W. S., Denton, G. H., Kong, X. G., Wang, Y. J., Zhang, R., and Wang, X. F.: Ice age terminations, Science, 326, 248–251, 2009.
Cheng H., Sinha A., Wang X. F., Cruz F. W., and Edwards R. L.: The Global Paleomonsoon as seen through speleothem records from Asia and the Americas, Clim. Dynam., 39, 1045–1062, https://doi.org/10.1007/s00382-012-1363-7, 2012.
Chu, G. Q., Sun, Q., Wang, X. H., Li, D., Rioual, P., Qiang, L., Han, J. T., and Liu, J. Q.: A 1600 year multi-proxy record of paleoclimatic change from varved sediments in Lake Xiaolongwan, northeastern China, J. Geophys Res., 114, D22108, https://doi.org/10.1029/2009JD012077, 2009.
Cook, E. R., Anchukaitis, K. J., Buckley, B. M., D'Arrigo, R. D., Jacoby, G. C., and Wright, W. E.: Asian Monsoon Failure and Megadrought During the Last Millennium, Science, 328, 486–489, 2010.
Dayem, K. E., Molnar, P., Battisti, D. S., and Roe, G. H.: Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia, Earth Planet. Sc. Lett., 295, 219–230, 2010.
Ding, Y. H. and Chan, J. C. L.: The East Asian summer monsoon: an overview, Meteorol. Atmos. Phys., 89, 117–142, 2005.
Ding, Y. H., Liu, J. J., Sun, Y., Liu, Y. J., He, J. H., and Song, Y. F.: A study of the synoptic-climatology of the Meiyu system in East Asia, Chinese Journal of Atmospheric Sciences, 31, 1082–1101, 2007.
Dykoski, C. A., Edwards, R. L., Cheng, H., Yuan, D. X., Cai, Y. J., Zhang, M. L., Lin, Y. S., Qing, J. M., An, Z. S., and Revenaugh, J.: A high-resolution, absolute-dated holocene and deglacial Asian monsoon record from Dongge Cave, China, Earth Planet. Sc. Lett., 233, 71–86, 2005.
Edwards, R. L., Cheng, J. H., and Wasserburg, G. J.: 238U-234U-230Th-232Th systematics and the precise measurement of time over the past 500,000 years, Earth Planet. Sc. Lett., 81, 175–192, 1986/1987.
Esper, J., Cook, E. R., and Schweingruber, F. H.: Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability, Science, 295, 2250–2253, 2002.
Fairchild, I. J., Borsato, A., Tooth, A. F., Frisia, S., Hawkesworth, C. J., Huang, Y., McDermott, F., and Spiro, B.: Controls on trace element (Sr-Mg) compositions of carbonate cave waters: implications for speleothem climatic records, Chem. Geol., 166, 255–269, 2000.
Fairchild, I. J., Smith, C. L., Baker, A., Fuller, L., Spötl, C., Mattey, D., McDermott, F., and Eimf.: Modification and preservation of environmental signals in speleothems, Earth-Sci. Rev., 75, 105–153, 2006.
Fleitmann, D., Burns, S. J., Neff, U., Mudelsee, M., Mangini, A., and Matter, A.: Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from Southern Oman, Quaternary Sci. Rev., 23, 935–945, 2004.
Fleitmann, D., Burns, S. J., Mangini, A., Mudelsee, M., Kramers, J., Villa, I., Neff, U., Subbary, A.-A., Buettner, A., Hippler, D., and Matter, A.: Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra), Quaternary Sci. Rev., 26, 170–188, 2007.
Ge, Q. S., Guo, X. F., Zheng, J. Y., and Hao, Z. X.: Meiyu in the middle and lower reaches of the Yangtze River since 1736, Chinese Sci. Bull., 53, 107–114, 2008.
Genty, D. and Quinif, Y.: Annually laminated sequences in the internal structure of some Belgian stalagmites-importance for paleoclimatology, J. Sediment. Res., 66, 275–288, 1996.
Genty, D., Baker, A., Massault, M., Procter, C., Gilmour, M., Pons-Banchu, E., and Hamelin, B.: Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for 13C variations in speleothems, Geochim. Cosmochim. Ac., 65, 3443–3457, 2001.
Hendy, C. H.: The isotopic geochemistry of speleothems-I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoc limatic indicators, Geochim. Cosmochim. Ac., 35, 801–824, 1971.
Hou, J. Z., Tan, M., and Liu D. S.: Counting chronology and climate records with about 1000 annual layers of a Holocene stalagmite from the Water Cave in Liaoning Province, China, Sci. China Ser. D, 54, 385–391, 2002.
Hu, C. Y., Henderson, G. M., Huang, J., Xie, S. C., Sun, Y., and Johnson, K. R.: Quantification of Holocene Asian monsoon rainfall from spatially separated cave records, Earth Planet. Sc. Lett., 266, 221–232, 2008.
Johnson, K. R., Hu, C. Y., Belshaw, N. S., and Henderson, G. M.: Seasonal trace-element and stable-isotope variations in a Chinese speleothem: The potential for high-resolution paleomonsoon reconstruction, Earth Planet. Sc. Lett., 244, 394–407, 2006.
Kaufman, D. S., Schneider, D. P., McKay, N. P., Ammann, C. M., Bradley, R. S., Briffa, K. R., Miller, G. H., Otto-Bliesner, B. L., Overpeck, J. T., Vinther, B. M., and Arctic Lakes 2k Project Members.: Recent Warming Reverses Long-Term Arctic Cooling, Science, 325, 1236–1239, 2009.
LeGrande, A. N. and Schmidt, G. A.: Sources of Holocene variability of oxygen isotopes in paleoclimate archives, Clim. Past, 5, 441–455, https://doi.org/10.5194/cp-5-441-2009, 2009.
Mann, M. E., Zhang, Z., Rutherford, S., Bradley, R. S., Hughes, M. K., Shindell, D., Ammann, C., Falugevi, G., and Ni, F.: Global Signatures and Dynamical Origins of the "Little Ice Age" and "Medieval Climate Anomaly", Science, 326, 1256–1260, 2009.
McDermott, F.: Paleo-climate reconstruction from stable isotope variations in spleothems: a review, Quaternary Sci. Rev., 23, 901–918, 2004.
Mühlinghaus, C., Scholz, D., and Mangini, A.: Modelling stalagmite growth and δ13C as a function of drip interval and temperature, Geochim. Cosmochim. Ac., 71, 2780–2790, 2007.
Newton, A., Thunell, R., and Stott, L. D.: Climate and hydrographic variability in the Indo-Pacific Warm Pool during the last millennium, Geophys. Res. Lett., 33, L19710, https://doi.org/10.1029/2006GL027234, 2006.
Oppo, D., Rosenthal, Y., and Linsley, B. K.: 2,000-year-long temperature and hydrology reconstructions from the Indo-Paci?c warm pool, Nature, 460, 1113–1116, 2009.
Pausata, F. S. R., Battisti, D. S., and Nisancioglu, K. H.: Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event, Nat. Geosci., 4, 474–480, 2011.
Qian, W. H. and Zhu, Y. F.: Little ice age climate near Beijing, China, inferred from historical and stalagmite records, Quaternary Res., 57, 109–119, 2002.
Qian, W. H., Lin, X., Zhu, Y. F., Xu, Y., and Fu, J. L.: Climatic regime shift and decadal anomalous events in China, Climatic Change, 84, 167–189, 2007.
Rajeevan, M., Gadgil, S., and Bhate, J.: Active and break spells of the Indian summer monsoon, J. Earth Syst. Sci., 119, 229–247, 2010.
Reuter, J., Stott, L., Khider, D., Sinha, A., Cheng, H., and Edwards, R. L.: A new perspective on the hydroclimate variability in northern South America during the Little Ice Age, Geophys. Res. Lett., 36, L21706, https://doi.org/10.1029/2009GL041051, 2009.
Roberts, M. S., Smart, P., and Baker, A.: Annual trace element variations in a Holocene speleothem, Earth Planet. Sc. Lett., 154, 237–246, 1998.
Romanov, D., Kaufmann, G., and Dreybrodt, W.: δ13C pro?les along growth layers of stalagmites: comparing theoretical and experimental results, Geochim. Cosmochim. Ac., 72, 438–448, 2008.
Sachs, J. P., Sachse, D., Smittenberg, R. H., Zhang, Z. H., Battisti, D. S., and Golubic, S.: Southward movement of the Paci?c intertropical convergence zone AD 1400–1850, Nat. Geosci., 2, 519–525, 2009.
Schulz. M. and Mudelsee, M.: REDFIT: Estimating red-noise spectra directly from unevenly spaced paleoclimatic time series, Comput. Geosci., 28, 421–426, 2002.
Shen, C. C., Edwards, R. L., Cheng, H., Dorale, J. A., Thomas, R. B., Moran, S. B., Weinstein, S. E., and Edmonds, H. N.: Uranium and thorium isotopic concentration measurements by magnetic sector inductively coupled plasma mass spectrometry, Chem. Geol., 185, 165–178, 2002.
Sinha, A., Cannariato, K. G., Stott, L. D., Cheng, H., Edwards, R. L., Yadava, M. G., Ramesh, R., and Singh, I. B.: A 900 year (600 to 1500A.D.) record of the Indian summer monsoon precipitation from the core monsoon zone of India, Geophys. Res. Lett., 34, L16707, https://doi.org/10.1029/2007GL030431, 2007.
Sinha, A., Stott, L., Berkelhammer, M., Cheng, H., Edwards, R. L., Buckley, B., Aldenderfer, M., and Mudelsee, M.: A global context for megadroughts in monsoon Asia during the past millennium, Quaternary Sci. Rev., 30, 47–62, 2011.
Tan, M., Liu, T. S., Hou, J. Z., Qin, X. G., Zhang, H. C., and Li, T. Y.: Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature, Geophys. Res. Lett., 30, 191–194, 2003.
Tan, M., Baker, A., Genty, D., Smith, C., Esper, J., and Cai, B. G.: Applications of stalagmite laminae to paleoclimate reconstructions: Comparison with dendrochronology/climatology, Quaternary Sci. Rev., 25, 2103–2117, 2006.
Tan, L. C., Cai, Y. J., Yi, L., An Z. S., and Ai, L.: Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity, Clim. Past, 4, 19–28, https://doi.org/10.5194/cp-4-19-2008, 2008.
Tao, S. Y. and Chen, L. X.: A review of recent research on the East Asina summer monsoon in China, in: Monsoon Meteorology, edited by: Chang, C. P. and Krishnamurti, T. N., UK, Oxford University Press, 60–92, 1987.
Thompson, L. G., Yao, T., Mosley-Thompson, E., Davis, M. E., Henderson, K. A., and Lin, P. N.: A high-resolution millennial record of the South Asian monsoon from Himalayan ice cores, Science, 289, 1916–1919, 2000.
Verschuren, D., Laird, K. R., and Cumming, B. F.: Rainfall and drought in equatorial east Africa during the past 1100 years, Nature, 403, 410–414, 2000.
Wang, B. and Lin, H.: Rainy season of the Asian-Pacific summer monsoon, J. Climate, 15, 386–396 2002.
Wang, Y. J., Cheng, H., Edwards, R. L., An, Z. S., Wu, J. Y., Shen, C. C., and Dorale, J. A.: A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China, Science, 294, 2345–2348, 2001.
Wang, Y. J., Cheng, H., Edwards, R. L., He, Y. Q., Kong, X. G., An, Z. S., Wu, J. Y., Kelly, M. J., Dykoski, C. A., and Li, X. D.: The Holocene Asian monsoon: links to solar changes and North Atlantic climate, Science, 308, 854–857, 2005.
Wang, Y. J., Cheng, H., Edwards, R. L., Kong, X. G., Shao, X. H., Chen, S. T., Wu, J. Y., Jiang, X. Y., Wang, X. F., and An, Z. S.: Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years, Nature, 451, 1090–1093, 2008.
Yancheva, G., Nowaczyk, N. R., Mingram, J., Dulski, P., Schettler, G., Negendank, J. W., Liu, J. Q., Sigman, D. M., Peterson, L. C., and Haug, G. H.: Influence of the intertropical convergence zone on the East-Asian monsoon, Nature, 445, 74–77, 2007.
Yang, B., Braeuning, A., Yao, T. D., and Davis, M. E.: Correlation between the oxygen isotope record from Dasuopu ice core and the Asian Southwest Monsoon during the last millennium, Quaternary Sci. Rev., 26, 1810–1817, 2007.
Yi, L., Yu, H. J., Ge, J. Y., Lai, Z. P., Xu, X. Y., Qin, L., and Peng, S. Z.: Reconstruction of annual summer precipitation and temperature in north-central China since 1470 AD based on drought/flood index and tree-ring records, Climatic Change, 110, 469–498, https://doi.org/10.1007/s10584-011-0052-6, 2012.
Zhang, D. E., Li, H. C., Ku, T. L., and Lu, L. H.: On linking climate to Chinese dynastic change: Spatial and temporal variations of monsoonal rain, Chinese Sci. Bull., 55, 77–83, 2010.
Zhang, P. Z., Cheng, H., Edwards, R. L., Chen, F. H., Wang, Y. J., Yang, X. L., Liu, J., Tan, M., Wang, X. F., Liu, J. H., An, C. L., Dai, Z. B., Zhou, J., Zhang, D. Z., Jia, J. H., Jin, L. Y., and Johnson, K. R.: A Test of Climate, Sun, and Culture Relationships from an 1810-Year Chinese Cave Record, Science, 322, 940–942, 2008.
Zhang, Q. Y.: The relationship between the east summer Asia monsoou and the india monsoon, in: East Asia Monsoon and Storm in China, edited by: Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, Meteorological Press, 266–273, 1998.
Zhang, Q. Y. and Tao, S. Y.: East Asia tropical and subtropical monsoons in the summer and precipitation in Eastern China in wet season, J. Appl. Meteorol. Sci., 9(Suppl.), 16–23, 1998.
Zhang, R. H.: Relations of water vapor transport from Indian monsoon with that over East Asia and the summer rainfall in China, Adv. Atmos. Sci., 18, 1005–1017, 2001.
Zheng, J. Y., Wang, W. C., Ge, Q. S., Man, Z. M., and Zhang, P. Y.: Precipitation variability and extreme events in eastern China during the past 1500 years, Terr. Atmos. Ocean. Sci., 17, 579–592, 2006.
Zhou, Y. S., Gao, S. T., and Shen, S. S. P.: A diagnostic study of formation and structures of the Meiyu Front System over East Asia, J. Meteorol. Soc. Japan, 82, 1565–1576, 2004.