Cited by 947Geology and Paleoclimatology ResearchClimate variability and modelsTree-ring climate responses

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Influence of the intertropical convergence zone on the East Asian monsoon

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Yancheva, Gergana, Nowaczyk, Norbert R., Mingram, Jens, Dulski, Peter, Schettler, Georg, Negendank, Jörg F. W., Liu, Jiaqi, Sigman, Daniel M., Peterson, Larry C., Haug, Gerald H.·2007·Nature

DOI 10.1038/nature05431

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Abstract

The Asian-Australian monsoon is an important component of the Earth's climate system that influences the societal and economic activity of roughly half the world's population. The past strength of the rain-bearing East Asian summer monsoon can be reconstructed with archives such as cave deposits, but the winter monsoon has no such signature in the hydrological cycle and has thus proved difficult to reconstruct. Here we present high-resolution records of the magnetic properties and the titanium content of the sediments of Lake Huguang Maar in coastal southeast China over the past 16,000 years, which we use as proxies for the strength of the winter monsoon winds. We find evidence for stronger winter monsoon winds before the Bølling-Allerød warming, during the Younger Dryas episode and during the middle and late Holocene, when cave stalagmites suggest weaker summer monsoons. We conclude that this anticorrelation is best explained by migrations in the intertropical convergence zone. Similar migrations of the intertropical convergence zone have been observed in Central America for the period ad 700 to 900 (refs 4-6), suggesting global climatic changes at that time. From the coincidence in timing, we suggest that these migrations in the tropical rain belt could have contributed to the declines of both the Tang dynasty in China and the Classic Maya in Central America.

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Hu, J., Zhou, H., Peng, P., Yang, X., Spiro, B. F., Jia, G., Wei, G., & Ouyang, T. (2015) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2015.06.014 · Cited by 26
Centennial-scale climate variability during the past 2000 years derived from lacustrine sediment on the western Tibetan Plateau
Li, X., Wang, M., & Hou, J. (2018) · Quaternary International · doi:10.1016/j.quaint.2018.12.018 · Cited by 25
Temporal variability in the Holocene marine radiocarbon reservoir effect for the Tropical and South Pacific
Hua, Q., Ulm, S., Yu, K., Clark, T. R., Nothdurft, L. D., Leonard, N. D., Pandolfi, J. M., Jacobsen, G., & Zhao, J. (2020) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106613 · Cited by 25
“The SCS is strongly influenced by Asian monsoons and is very sensitive to other climate forcings including the El Niño Southern Oscillation (ENSO) and Pacific decadal variability (Yu et al., 2004; Wang et al., 2005; Yancheva et al., 2007; Hu et al., 2015).”
BackgroundMethodInfluential
Late Miocene-Pliocene Asian summer monsoon variability linked to both tropical Pacific temperature and Walker Circulation
Wang, M., Wang, H., Zhu, Z., Yang, X., Zhang, K., Zhang, Y., Liu, W., Zheng, Z., Zong, Y., & Liu, Z. (2021) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2021.116823 · Cited by 25
Millennial-scale interaction between the East Asian winter monsoon and El Niño-related tropical Pacific precipitation in the Holocene
Dong, J., Li, A., Lu, Z., Liu, X., Wan, S., Yan, H., Yu, Z., Feng, X., & Shi, X. (2021) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2021.110442 · Cited by 25
Advances in Research on the ITCZ: Mean Position, Model Bias, and Anthropogenic Aerosol Influences
Zhang, H., Ma, X., Zhao, S., & Kong, L. (2021) · 气象学报：英文版 · doi:10.1007/s13351-021-0203-2 · Cited by 25
“For instance, in the early Holocene, the ITCZ moved northward during the NH warm period, at which time the East Asian summer monsoon strengthened and the winter monsoon weakened (Yancheva et al., 2007).”
Background
Highly resolved δ13C and trace element ratios of precisely dated stalagmite from northwestern China: Hydroclimate reconstruction during the last two millennia
Wei, J., Zhang, P., Zhang, L., Li, X., Gao, T., Wang, H., Zhang, H., Li, H., Cheng, H., & Edwards, R. L. (2022) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2022.107473 · Cited by 25
Climate over mainland Southeast Asia 10.5–5 ka
Chabangborn, A., & Wohlfarth, B. (2014) · Journal of Quaternary Science · doi:10.1002/jqs.2715 · Cited by 25
“This is in line with observations by An et al. (2012) and Yancheva et al. (2007), who report a gradual strengthening of the westerlies and of the winter monsoon in the EAM region, Copyright # 2014 John Wiley & Sons, Ltd. J. Quaternary Sci., Vol. 29(5) 445–454 (2014) starting around 7 ka BP.”
Result
A preliminary analysis of economic fluctuations and climate changes in China from BC 220 to AD 1910
Wei, Z., Fang, X., & Su, Y. (2014) · Regional Environmental Change · doi:10.1007/s10113-014-0745-2 · Cited by 25
Biomarker evidence for changes in terrestrial organic matter input into the Yellow Sea mud area during the Holocene
Wu, P., Xiao, X., Tao, S., Yang, Z., Zhang, H., Li, L., & Zhao, M. (2016) · Science China Earth Sciences · doi:10.1007/s11430-016-5283-y · Cited by 25
“The YSCC was strengthened throughout the Holocene as the East Asia winter monsoon (EAWM) enhanced (Xiao et al., 2005; Yancheva et al., 2007), transporting more Huanghe-derived resuspended sediments into the central South Yellow Sea during Mid”
BackgroundInfluential
Modern drought conditions in western Sahel unprecedented in the past 1600 years
Carré, M., Azzoug, M., Zaharias, P., Camara, A., Cheddadi, R., Chevalier, M., Fiorillo, D., Gaye, A. T., Janicot, S., Khodri, M., et al. (2018) · Climate Dynamics · doi:10.1007/s00382-018-4311-3 · Cited by 28
“Explanations of millennial to centennial scale rainfall variability in the tropics have been often related to latitudinal shifts of the mean position of the ITCZ in response to interhemispheric temperature contrasts (Street-Perrott and Perrot 1990; Mulitza and Rühlemann 2000; Haug et al. 2001; Yancheva et al. 2007).”
Background
Holocene East Asian Summer Monsoon Rainfall Variability in Taiwan
Ding, X., Zheng, L., Zheng, X., & Kao, S. (2020) · Frontiers in Earth Science · doi:10.3389/feart.2020.00234 · Cited by 24
“, 2018), lake and peat sediments (Zhou et al., 2004; Xiao et al., 2006; Selvaraj et al., 2007; Yancheva et al., 2007; Zhong et al., 2010; Chen F. et al., 2015; Park et al., 2016; Wang et al., 2016), marine sediments (Wang et al.”
Background
Multiscale monsoon variability during the last two climatic cycles revealed by spectral signals in Chinese loess and speleothem records
Li, Y., Su, N., Liang, L., Ma, L., Yan, Y., & Sun, Y. (2015) · Climate of the past · doi:10.5194/cp-11-1067-2015 · Cited by 24
Transient coupling relationships of the Holocene Australian monsoon
McRobie, F. H., Stemler, T., & Wyrwoll, K. ‐. (2015) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2015.05.011 · Cited by 24
“…of speleothem [Fleitmann et al., 2007, Hu et al., Dykoski et al., 2005, Dong et al., 2010, Griffiths et al., 2009, Denniston et al., 2013, van Breukelen et al., 2008], titanium [Yancheva et al., 2007, Haug et al., 2001], sediment [Moy et al., 2002] and multi-proxy [Menzel et al., 2014] data sets.”
BackgroundInfluential
Evidence of late Holocene climate variability in the western Nanling Mountains, South China
Zhong, W., Xue, J., Ouyang, J., Cao, J., & Peng, Z. (2014) · Journal of Paleolimnology · doi:10.1007/s10933-014-9774-6 · Cited by 23
“Thus, these inconclusive results indicate that further W. Zhong (&) J. Xue J. Ouyang J. Cao School of Geography Sciences, South China Normal University, Guangzhou 510631, China e-mail: DL06@scnu.edu.cn Z. Peng Department of Social Sciences, Gaozhou Normal School of Guangdong University of Petrochemical Technology, Mao…”
BackgroundInfluential
Lacustrine mineral magnetic record of postglacial environmental changes from Dahu Swamp, southern China
Wei, Z., Zhong, W., Shang, S., Ye, S., Tang, X., Xue, J., Ouyang, J., & Smol, J. P. (2018) · Global and Planetary Change · doi:10.1016/j.gloplacha.2018.08.010 · Cited by 24
Human settlement and human–environment interactions during the historical period in Zhuanglang County, western Loess Plateau, China
Dong, G., Yang, Y., Zhao, Y., Zhou, A., Xinjia, Z., Li, X., & Chen, F. (2012) · Quaternary International · doi:10.1016/j.quaint.2012.05.006 · Cited by 23
“Climate deterioration during those periods probably contributed to the warfare for decreasing resources and the collapse of dynasties, which was also reported by other studies (Yancheva et al., 2007; Zhang et al., 2008).”
Result
New progress in the Holocene climate and agriculture research in China
Li, X. (2013) · Science China Earth Sciences · doi:10.1007/s11430-013-4758-3 · Cited by 23
“The high resolution records of climate change showed that many dynasty collapses possibly corresponded to the cold events in the China history (Yancheva et al., 2007; Zhang et al., 2008; Liu et al., 2009).”
Background
Late Oligocene Precipitation Seasonality in East Asia Based on δ 13 C Profiles in Fossil Wood
Vornlocher, J. R., Lukens, W. E., Schubert, B. A., & Quan, C. (2021) · Paleoceanography and Paleoclimatology · doi:10.1029/2021pa004229 · Cited by 23
“, 2005), soil and rock magnetics (Liu et al., 2007; Yancheva et al., 2007), cosmogenic radionuclides (Beck et al.”
Background
Abnormally low precipitation-induced ecological imbalance contributed to the fall of the Ming Dynasty: new evidence from tree rings
Chen, F., Hadad, M. A., Zhao, X., Roig, F. A., Zhang, H., Wang, S., Yue, W., & Chen, Y. (2022) · Climatic Change · doi:10.1007/s10584-022-03406-y · Cited by 23
Orbital forcing of tropical climate dynamics in the Early Cambrian
Zhang, T., Li, Y., Fan, T., Silva, A. D., Kuang, M., Liu, W., Ma, C., Gao, Q., Shi, J., Gao, Z., et al. (2022) · Global and Planetary Change · doi:10.1016/j.gloplacha.2022.103985 · Cited by 26
Early warnings and missed alarms for abrupt monsoon transitions
Thomas, Z., Kwasniok, F., Boulton, C. A., Cox, P. M., Jones, R., Lenton, T. M., & TURNEY, C. S. M. (2015) · Climate of the past · doi:10.5194/cp-11-1621-2015 · Cited by 24
Long-term weakening of the East Asian summer and winter monsoons during the mid- to late Holocene recorded by aeolian deposits at the eastern edge of the Mu Us Desert
Zhao, S., Xia, D., Jin, H., Jia, J., Li, G., Gao, F., & Wang, Y. (2016) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2016.06.011 · Cited by 23
Developing a Holocene tephrostratigraphy for northern Japan using the sedimentary record from Lake Kushu, Rebun Island
Chen, X., McLean, D., Blockley, S. P. E., Tarasov, P. E., Xu, Y., & Menzies, M. (2019) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2019.05.017 · Cited by 23
Calibrating branched GDGTs in bones to temperature and precipitation: Application to Alaska chronological sequences
Zhao, J., Huang, Y., Yao, Y., An, Z., Zhu, Y., Lu, H., & Wang, Z. (2020) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106371 · Cited by 23
Climate instability during the last deglaciation in central Asia, reconstructed by pollen data from Yili Valley, NW China
Zhao, K., Li, X., Dodson, J., Zhou, X., & Atahan, P. (2012) · Review of Palaeobotany and Palynology · doi:10.1016/j.revpalbo.2012.10.005 · Cited by 23
Sea surface temperature and salinity variations from the end of Last Glacial Maximum (LGM) to the Holocene in the northern South China Sea
Yin, J. J., Yang, X., Zhou, Q., Li, G., Gao, H., & Liu, J. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.110102 · Cited by 22
Self-citation
Palynology-based reconstruction of Holocene environmental history in the northern Yangtze Delta, China
Ye, L., Gao, L., Li, Y., & Wang, G. (2022) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2022.111186 · Cited by 22
East Asian Monsoonal Climate Sensitivity Changed in the Late Pliocene in Response to Northern Hemisphere Glaciations
Zhang, Z., Licht, A., Vleeschouwer, D. D., Wang, Z., Li, Y., Kemp, D. B., Tan, L., Zhang, R., Qiang, X., & Huang, C. (2022) · Geophysical Research Letters · doi:10.1029/2022gl101280 · Cited by 22
“…influencing the strength of the Siberian high (Gai et al., 2020; Guo et al., 2004), the locus of the westerly track (Abell et al., 2021), meridional shift of the intertropical convergence zone (Haug et al., 2001; Yancheva et al., 2007) and changes in SST gradients (C. M. Brierley & Fedorov, 2010).”
Background
Climatic and environmental change in Yanchi Lake, Northwest China since the Late Glacial: A comprehensive analysis of lake sediments
Li, Y., Wang, N., Li, Z., Zhou, X., & Zhang, C. (2013) · Journal of Geographical Sciences · doi:10.1007/s11442-013-1053-3 · Cited by 22
“Stalagmite and lake records in typical monsoon areas and the Qinghai-Tibet Plateau clearly show the Asian summer monsoon history since the Late Glacial (Fleitmann et al., 2003; Dykoski et al., 2005; Shen et al., 2005; Yancheva et al., 2007; Mischke et al., 2008; Zhu et al., 2009).”
Background
Environmental humidity changes inferred from multi-indicators in the Jianghan Plain, Central China during the last 12,700 years
Feng, L., Zhu, C., Wu, L., Sun, W., Liu, H., Chyi, S., Kung, C.-L., Guangyao, Z., & Wang, X. (2013) · Quaternary International · doi:10.1016/j.quaint.2013.09.040 · Cited by 22
Isotopic and lithologic variations of one precisely-dated stalagmite across the Medieval/LIA period from Heilong Cave, central China
Cui, Y., Wang, Y., Cheng, H., Zhao, K., & Kong, X. (2012) · Climate of the past · doi:10.5194/cp-8-1541-2012 · Cited by 22
“Considerable progresses in reconstructing Asian monsoon (AM) climate over the past millennia have been made using climate “proxy” data, such as ice cores (Thompson et al., 2000, Yang et al., 2007), tree rings (Cook et al., 2010; Buckley et al., 2010), lake sediments (Yancheva et al., 2007; Chu et al., 2009) and histor…”
BackgroundMethodInfluential
Mid- to late-Holocene Indian winter monsoon variability from a terrestrial record in eastern and southeastern coastal environments of Sri Lanka
Ranasinghe, P., Ortiz, J. D., Smith, A., Griffith, E. M., Siriwardana, C. H. E. R., Silva, S. D., & Wijesundara, D. T. D. S. (2013) · The Holocene · doi:10.1177/0959683612475141 · Cited by 22
“Although the Indian SW summer monsoon has been studied extensively, reconstructions for the Indian NE winter monsoon are limited because of a lack of sediment archives that record only the winter monsoon (Yancheva et al., 2007).”
Background
Environmental processes derived from peatland geochemistry since the last deglaciation in Dajiuhu, Shennongjia, central China
Li, Y., Ma, C., Zhou, B., Cui, A., Zhu, C., Huang, R., & Zheng, C. (2016) · Boreas · doi:10.1111/bor.12168 · Cited by 22
“Similarly, Ti contents of sediments from Lake Huguang Maarn in southeast China were used to reconstruct the input of aeolian dust from arid areas on the northern Loess Plateau, and possibly local sources into the lake (Yancheva et al. 2007).”
BackgroundInfluential
Predicting convective rainfall over tropical oceans from environmental conditions
Raymond, D. J., & Flores, M. M. (2016) · Journal of Advances in Modeling Earth Systems · doi:10.1002/2015ms000595 · Cited by 22
Temporal-spatial variations of human settlements in relation to environment change during the Longshan culture and Xia-Shang periods in Shanxi Province, China
Li, J., Han, L., Zhang, G., Su, Z., & Zhao, Y. (2017) · Quaternary International · doi:10.1016/j.quaint.2016.11.048 · Cited by 22
Late Holocene aeolian sedimentation in the Tottori coastal dune field, Japan Sea, affected by the East Asian winter monsoon
Tamura, T., Kodama, Y., Bateman, M. D., Saitoh, Y., Yamaguchi, N., & Matsumoto, D. (2015) · Quaternary International · doi:10.1016/j.quaint.2015.09.062 · Cited by 22
“By reconstructing dune activity over a longer period, we can more effectively explore possible causes of the observed dune activity fluctuations by comparing them with other palaeoenvironmental proxies (e.g., Yancheva et al., 2007).”
BackgroundInfluential
Comments on “Anti-phase oscillation of Asian monsoons during the Younger Dryas period: Evidence from peat cellulose δ13C of Hani, Northeast China” by B. Hong, Y.T. Hong, Q.H. Lin, Yasuyuki Shibata, Masao Uchida, Y.X. Zhu, X.T. Leng, Y. Wang and C.C. Cai [Palaeogeography, Palaeoclimatology, Palaeoecology 297 (2010) 214–222]
Stebich, M., Mingram, J., Moschen, R., Thiele, A., & Schröder, C. A. (2011) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2011.06.004 · Cited by 21
Self-citation
Population-influenced spatiotemporal pattern of natural disaster and social crisis in China, AD1–1910
Zhang, S., & Zhang, D. D. (2019) · Science China Earth Sciences · doi:10.1007/s11430-018-9340-7 · Cited by 21
Spatiotemporal distribution of sea-island prehistoric dune sites, Holocene sea levels, and aeolian sand activities in Fujian Province, China
Jin, J., Ling, Z., Li, Z., Zuo, X., Fan, X., Huang, Y., Wang, X., Wei, C., Ren, Y., & Qiu, J. (2022) · Journal of Geographical Sciences · doi:10.1007/s11442-022-1990-9 · Cited by 21
“The first stage from 7–5 ka is an important active aeolian period, which is consistent with the intensity of the East Asian winter monsoon reflected in Huguangyan Maar Lake deposition (Yancheva et al., 2007) and sea surface temperature (SST) variability in the Okinawa Trough (Jian et al., 2000).”
Background
High‐Resolution Records of Millennial‐Scale East Asian Winter Monsoon in the Shelf Sea of Eastern China
Shi, Y., Xu, X., Yang, G., Du, J., Lv, J., Zhang, S., Liu, S., Liu, T., Zhang, Z., Gao, S., et al. (2023) · Geophysical Research Letters · doi:10.1029/2022gl102302 · Cited by 22
“The linear relationship in Figure 3c is applied to quantitatively reconstruct the EAWM on the millennial scale, considering the facts that (a) the depositional environment was relatively steady since the mid-Holocene because of little variability of sea-level; (b) although flux of cross-front transport is associated w…”
BackgroundInfluential

Authors: Yancheva, G., Nowaczyk, N. R., Mingram, J., Dulski, P., Schettler, G., Negendank, J. F. W., Liu, J., Sigman, D. M., Peterson, L. C., & Haug, G. H.
Affiliations: GFZ Helmholtz Centre for Geosciences (DE)
Chinese Academy of Sciences (CN)
Princeton University (US)
University of Miami (US)
Corresponding author: Haug, Gerald H.
ORCID: Yancheva, Gergana
Nowaczyk, Norbert R.
Mingram, Jens
Liu, Jiaqi
Sigman, Daniel M.
Peterson, Larry C.
Haug, Gerald H.
Venue: Nature
Publisher: Springer Science and Business Media LLC
Published: 2007-01-04
Volume: 445
Issue: 7123
Pages: 74-77
ISSN: 0028-0836 (ISSN-L)
1476-4687
DOI: 10.1038/nature05431
OpenAlex: W2040945899
Semantic Scholar: fb1091bd698430b3e144d519cfb7c255993750d9
Cited by: 944
References: 30
Citations by year: 2026: 42 · 2025: 51 · 2024: 52 · 2023: 53 · 2022: 57 · 2021: 57 · 2020: 49 · 2019: 38 · 2018: 53 · 2017: 41 · 2016: 51 · 2015: 62 · 2014: 67 · 2013: 48 · 2012: 43
FWCI: 31.11
Type: journal article
Language: en
Open access: green
gfzpublic.gfz-potsdam.de
Licence: other-oa
www.springer.com/tdm (tdm)
www.springer.com/tdm (vor)
Locations: Nature (publishedVersion)
PubMed (publishedVersion)
RePEc: Research Papers in Economics (submittedVersion)
Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion, other-oa)
Topics: Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
Keywords: Intertropical Convergence Zone, East Asian winter monsoon, East Asian summer monsoon, ITCZ migration, lake sediments, magnetic properties, titanium content, monsoon strength, Holocene, Younger Dryas, Bølling-Allerød, drought, Cariaco Basin, paleoclimate

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Influence of the intertropical convergence zone on the East Asian monsoon

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