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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“Further, in paleo-monsoon community, an enhanced EASM is often considered as a result of the northward advance or enhancement of the ITCZ (e.g., Yancheva et al. 2007).”
Self-citation
Holocene glacier fluctuations and migration of Neolithic yak pastoralists into the high valleys of northwest Bhutan
Meyer, M. C., Hofmann, C.-C., Gemmell, A. M. D., Haslinger, E., Häusler, H., & Wangda, D. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2008.12.025 · Cited by 66
“The most important climate driver for the Himalaya (particularly for the eastern and southern slopes) and for much of the Tibetan Plateau is the Asian monsoon system, which delivers substantial amounts of precipitation during the summer months via the northward migration of the Intertropical Convergence Zone (Chao and…”
Background
The bigger picture: towards integrating palaeoclimate and environmental data with a history of societal change
Caseldine, C. J., & TURNEY, C. S. M. (2009) · Journal of Quaternary Science · doi:10.1002/jqs.1337 · Cited by 70
“Recent highresolution developments in the interpretation of speleothems and lake sediments in China appear to offer the opportunity to undertake studies into the relationships between monsoon severity and dynastic stability and change: intense monsoons are associated with high agricultural productivity, allowing socie…”
Background
Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current
Wang, L., Yang, Z., Zhang, R., Fan, D., Zhao, M., & Hu, B. (2011) · Chinese Science Bulletin · doi:10.1007/s11434-011-4442-y · Cited by 64
Holocene environmental change and Neolithic rice agriculture in the lower Yangtze region of China: A review
Zong, Y., Wang, Z., Innés, J. B., & Chen, Z. (2011) · The Holocene · doi:10.1177/0959683611409775 · Cited by 63
“…impacts of climate change upon human civilizations have been studied intensively, and some of the suggestions have led to heated debates in the wider academic community, including the claims that climate change has caused dynastic changes in China (e.g. Yancheva et al., 2007; Zhang et al., 2008).”
Background
Historical desertification of the Mu Us Desert, Northern China: A multidisciplinary study
Huang, Y., Wang, N., Tong-hui, H., Chen, H., & Zhao, L. (2009) · Geomorphology · doi:10.1016/j.geomorph.2009.03.020 · Cited by 63
Contrasting sea surface temperature of summer and winter monsoon variability in the northern Arabian Sea over the last 25 ka
Böll, A., Schulz, H., Munz, P., Rixen, T., Gaye, B., & Emeis, K. (2015) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2015.02.036 · Cited by 63
Indo-Pacific Warm Pool variability during the Holocene and Last Glacial Maximum
Xu, J., Kuhnt, W., Holbourn, A., Regenberg, M., & Andersen, N. (2010) · Paleoceanography · doi:10.1029/2010pa001934 · Cited by 63
“Cave [Yuan et al., 2004], and by evidence for northward displacement of the ITCZ [Haug et al., 2001; Tierney and Russell, 2007; Fleitmann et al., 2007; Yancheva et al., 2007; Tierney et al., 2010].”
Background
Tracking eolian dust with helium and thorium: Impacts of grain size and provenance
McGee, D., Winckler, G., Borunda, A., Serno, S., Anderson, R. F., Recasens, C., Bory, A., Gaiero, D. M., Jaccard, S. L., Kaplan, M. R., et al. (2015) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2015.11.023 · Cited by 63
“…2005; Bettis et al., 2003), peat bogs (e.g., Weiss et al., 2002; Kylander et al., 2007; Ferrat et al., 2011; Sharifi et al., 2015) and lakes (e.g., Yancheva et al., 2007; Neff et al., 2008) provide important information about dust emissions and transport close to the source, while dust flux…”
Background
Controls on erosion patterns and sediment transport in a monsoonal, tectonically quiescent drainage, Song Gianh, central Vietnam
Jonell, T. N., Clift, P. D., Hoang, L. V., Hoang, T., Carter, A., Wittmann, H., Böning, P., Pahnke, K., & Rittenour, T. M. (2016) · Basin Research · doi:10.1111/bre.12199 · Cited by 60
“Furthermore, several Quaternary records of monsoonal strength exist across the region (Dykoski et al., 2005; Yancheva et al., 2007; Hu et al., 2008) allowing us to directly correlate landscape evolution and climate variability.”
Background
Impact of climate change on fluctuations of grain harvests in China from the Western Han Dynasty to the Five Dynasties (206 BC–960 AD)
Su, Y., Fang, X., & Yin, J. (2014) · Science China Earth Sciences · doi:10.1007/s11430-013-4795-y · Cited by 63
Holocene stalagmite δ 18 O records in the East Asian monsoon region and their correlation with those in the Indian monsoon region
Yang, X., Liu, J., Liang, F., Yuan, D., Yang, Y., Lü, Y., & Chen, F. (2014) · The Holocene · doi:10.1177/0959683614551222 · Cited by 62
“, 1997; Liu and Ding, 1998), lake sediments (Gergana et al., 2007), sandlands in northern China (Jin et al.”
BackgroundSelf-citation
Assessing influences on speleothem dead carbon variability over the Holocene: Implications for speleothem-based radiocarbon calibration
Noronha, A. L., Johnson, K. R., Hu, C., Ruan, J., Southon, J. R., & Ferguson, J. E. (2014) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2014.03.015 · Cited by 64
Forced and internal modes of variability of the East Asian summer monsoon
Liu, J., Wang, B., & Yang, J. (2008) · Climate of the past · doi:10.5194/cp-4-225-2008 · Cited by 61
“On orbital time scales, an enhanced EASM (increased Meiyu) has been attributed to northward migration of the ITCZ (e.g., An, 2000; Ding et al., 1995, Yancheva et al., 2007).”
BackgroundSelf-citation
High-resolution climate change in mid-late Holocene on Tianchi Lake, Liupan Mountain in the Loess Plateau in central China and its significance
Zhou, A., Sun, H., Chen, F., Zhao, Y., An, C., Dong, G., Wang, Z., & Chen, J. (2010) · Chinese Science Bulletin · doi:10.1007/s11434-010-3226-0 · Cited by 63
Holocene climate change in the western part of Taihu Lake region, East China
Yao, F., Ma, C., Zhu, C., Li, J., Chen, G., Tang, L., Huang, M., Jia, T., & Xu, J. (2017) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2017.08.022 · Cited by 61
Tropical and high latitude forcing of enhanced megadroughts in Northern China during the last four terminations
Tang, C., Yang, H., Pancost, R. D., Griffiths, M. L., Xiao, G., Dang, X., & Xie, S. (2017) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2017.09.012 · Cited by 60
“…increases in winter monsoon winds, which are known to influence hydroclimate 342 in China on G-IG time scales via shifts in the ITCZ (e.g., Yancheva et al., 2007; Cosford et al., 343 2008); a stronger winter monsoon would push the ITCZ and the rain belt southwards, 344 resulting in…”
Background
The development of late Holocene coastal cooling in the northern South China Sea
Kong, D., Zong, Y., Jia, G., Wei, G., Chen, M., & Liu, Z. (2013) · Quaternary International · doi:10.1016/j.quaint.2013.08.055 · Cited by 60
The 5.5 cal ka BP climate event, population growth, circumscription and the emergence of the earliest complex societies in China
Wu, W., Zheng, H., Hou, M., & Ge, Q. (2017) · Science China Earth Sciences · doi:10.1007/s11430-017-9157-1 · Cited by 59
“…Maar Lake in Guangdong Province (Figure 1e) showed that the winter monsoon was intensified and rainfall was reduced during 5.9–5.2 cal ka BP (Yancheva et al., 2007), whereas another multi-proxy study of the same lake sediment indicated that the Holocene Climate Optimum ended around 6.2 cal…”
BackgroundInfluential
Reconstruction of atmospheric soot history in inland regions from lake sediments over the past 150 years
Han, Y., Wei, C., Huang, R., Bandowe, B. A. M., Ho, S. S. H., Cao, J., Jin, Z. D., Xu, B., Gao, S. P., Tie, X., et al. (2016) · Scientific Reports · doi:10.1038/srep19151 · Cited by 59
Seasonal drought events in tropical East Asia over the last 60,000 y
Zhang, J., Lü, H., Jia, J., Shen, C., Wang, S., Chu, G., Wang, L., Cui, A., Liu, J., Wu, N., et al. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2013802117 · Cited by 59
“Based on the ITCZ mechanism, drier conditions in tropical East Asia should occur at stadials when the ITCZ moves southward (55).”
BackgroundSelf-citation
Late Holocene elemental and isotopic carbon and nitrogen records from the East China Sea inner shelf: Implications for monsoon and upwelling
Hu, B., Li, J., Zhao, J., Wei, H., Yin, X., Li, G., Liu, Y., Sun, Z., Zou, L., Bai, F., et al. (2014) · Marine Chemistry · doi:10.1016/j.marchem.2014.03.008 · Cited by 59
“winter monsoon have not been well reconstructed and are also under debate (e.g., Hu et al., 2012b; Wang et al., 2012; Xiao et al., 2006; Yancheva et al., 2007).”
Background
Climatic changes since the last deglaciation inferred from a lacustrine sedimentary sequence in the eastern Nanling Mountains, south China
Zhong, W., Xue, J., Zheng, Y., Ouyang, J., Ma, Q., Cai, Y., & Tang, X. (2010) · Journal of Quaternary Science · doi:10.1002/jqs.1384 · Cited by 59
“…in core KD, which are interpreted as the reflection of the YD cooling event, agree with the study results of Huguangyan Maar Lake in Leizhou Peninsula (ca. 12.8– 11.5 cal. ka BP) (Yancheva et al., 2007) and of south China Sea (ca. 12.8–11.5 cal. ka BP) (Wang L et al., 1999; Kienast et al., 2001).”
BackgroundResultInfluential
Holocene stalagmite oxygen isotopic record from the Japan Sea side of the Japanese Islands, as a new proxy of the East Asian winter monsoon
Sone, T., Kano, A., Okumura, T., Kashiwagi, K., Hori, M., Jiang, X., & Shen, C. (2013) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2013.06.019 · Cited by 59
Abrupt climate change in southeast tropical Africa influenced by Indian monsoon variability and ITCZ migration
Tierney, J. E., & Russell, J. M. (2007) · Geophysical Research Letters · doi:10.1029/2007gl029508 · Cited by 58
“This interpretation agrees with Yancheva et al. [2007] , who Figure 2. KH3 proxy data across the last deglaciation show major biological and lithological changes during the LPEH.”
Result
Response of the Asian summer monsoon to weakening of Atlantic thermohaline circulation
Lu, R., & Dong, B. (2008) · Advances in Atmospheric Sciences · doi:10.1007/s00376-008-0723-z · Cited by 57
Spatial distribution of the persistent organic pollutants across the Tibetan Plateau and its linkage with the climate systems: a 5-year air monitoring study
Wang, X., Ren, J., Gong, P., Wang, C., Xue, Y., Yao, T., & Lohmann, R. (2016) · Atmospheric chemistry and physics · doi:10.5194/acp-16-6901-2016 · Cited by 58
A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene
Ramisch, A., Lockot, G., Torsten Haberzettl, A., Hartmann, K., Kühn, G., Lehmkuhl, F., Schimpf, S., Schulte, P., Stauch, G., Wang, R., et al. (2016) · Scientific Reports · doi:10.1038/srep25791 · Cited by 58
A multi-proxy record of MIS 11–12 deglaciation and glacial MIS 12 instability from the Sulmona basin (central Italy)
Regattieri, E., Giaccio, B., Galli, P., Nomade, S., Peronace, E., Messina, P., Sposato, A., Boschi, C., & Gemelli, M. (2015) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2015.11.015 · Cited by 56
Climate change and Chinese history: a review of trends, topics, and methods
Fan, K. (2015) · WIREs Climate Change · doi:10.1002/wcc.331 · Cited by 54
Millennial-scale East Asian Summer Monsoon variability recorded in grain size and provenance of mud belt sediments on the inner shelf of the East China Sea during mid-to late Holocene
Wang, K., Zheng, H., Tada, R., Irino, T., Zheng, Y., Saito, K., & Karasuda, A. (2014) · Quaternary International · doi:10.1016/j.quaint.2014.09.014 · Cited by 56
A record of Holocene climate change in the Guanzhong Basin, China, based on optical dating of a loess-palaeosol sequence
Zhao, H., Chen, F., Li, S., WINTLE, A. G., Fan, Y., & Xia, D. (2007) · The Holocene · doi:10.1177/0959683607080530 · Cited by 56
A Late Pleistocene-Holocene multi-proxy record of climate variability in the Jazmurian playa, southeastern Iran
Vaezi, A., Ghazban, F., Tavakoli, V., Routh, J., Beni, A. N., Bianchi, T. S., Curtis, J. H., & Kylin, H. (2018) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2018.09.026 · Cited by 56
Comparison and implication of TEX86 and U37K' temperature records over the last 356kyr of ODP Site 1147 from the northern South China Sea
Li, D., Zhao, M., Tian, J., & Li, L. (2013) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2013.02.031 · Cited by 55
Macro-Economic Cycles Related to Climate change in Dynastic China
Wei, Z., Rosen, A. M., Fang, X., Su, Y., & Zhang, X. (2014) · Quaternary Research · doi:10.1016/j.yqres.2014.11.001 · Cited by 55
“However, our series-statistical results do not support the idea that prolonged drought led to the fall of the TangDynasty (Yancheva et al., 2007; Zhang et al., 2008) but support the conclusion of Zhang et al. (2010a).”
BackgroundResult
Human adaptation to mid- to late-Holocene climate change in Northeast Thailand
Wohlfarth, B., Higham, C. F., Yamoah, K. A., Chabangborn, A., Chawchai, S., & Smittenberg, R. H. (2016) · The Holocene · doi:10.1177/0959683616645947 · Cited by 55
“, 2010; Lieberman and Buckley, 2012) and Chinese dynastic instability (Buckley et al., 2014; Cook et al., 2010; Yancheva et al., 2007; Zhang et al., 2008).”
Background
Migration and reclamation in Northeast China in response to climatic disasters in North China over the past 300 years
Ye, Y., Fang, X., & Khan, M. A. U. (2011) · Regional Environmental Change · doi:10.1007/s10113-011-0245-6 · Cited by 55
Millennial-scale environmental changes in the Asian monsoon margin during the Holocene, implicated by the lake evolution of Huahai Lake in the Hexi Corridor of northwest China
Wang, N., Li, Z., Li, Y., & Cheng, H. (2013) · Quaternary International · doi:10.1016/j.quaint.2013.08.039 · Cited by 54
“Many researchers have focused on Holocene environmental changes and the characteristics of these changes in the areas influenced by the Asian monsoon (Thompson et al., 1997; Wang et al., 1999; Fleitmann et al., 2003; Yuan et al., 2004; Wang et al., 2005; Yancheva et al., 2007; Li et al., 2009; Selvaraj et al., 2011; A…”
Background
A detailed East Asian monsoon history surrounding the ‘Mystery Interval’ derived from three Chinese speleothem records
Zhang, W., Wu, J., Wang, Y., Wang, Y., Cheng, H., Kong, X., & Duan, F. (2014) · Quaternary Research · doi:10.1016/j.yqres.2014.01.010 · Cited by 59
“Meanwhile, the northward migration of the ITCZ also increases themonsoon intensity by transporting more moisture into the system (Yancheva et al., 2007) and altering the global Hadley circulation (Chiang and Bitz, 2005).”
Background
Lake Kumphawapi – an archive of Holocene palaeoenvironmental and palaeoclimatic changes in northeast Thailand
Chawchai, S., Chabangborn, A., Kylander, M. E., Löwemark, L., Mörth, C., Blaauw, M., Klubseang, W., Reimer, P. J., Fritz, S. C., & Wohlfarth, B. (2013) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2013.01.030 · Cited by 54
“Following the movement of the Intertropical Convergence Zone (ITCZ), humid air masses from the Indian Ocean reach the region between mid-May and mid-October.”
BackgroundInfluential
Late Holocene primary productivity and sea surface temperature variations in the northeastern Arabian Sea: Implications for winter monsoon variability
Böll, A., Lückge, A., Munz, P., Forke, S., Schulz, H., Ramaswamy, V., Rixen, T., Gaye, B., & Emeis, K. (2014) · Paleoceanography · doi:10.1002/2013pa002579 · Cited by 54
“…annual mean position of the ITCZ and monsoon as well as precipitation changes throughout the Holocene was proposed by several authors [Haug et al., 2001; Lückge et al., 2001; Fleitmann et al., 2003, 2007; Russell and Johnson, 2005; Wang et al., 2005; Yancheva et al., 2007; Sinha et al., 2011].”
Background
Summer monsoon moisture variability over China and Mongolia during the past four centuries
Li, J., Cook, E. R., Chen, F., Davi, N., D'Arrigo, R. D., Gou, X., Wright, W. E., Fang, K., Jin, L., Shi, J., et al. (2009) · Geophysical Research Letters · doi:10.1029/2009gl041162 · Cited by 54
Comparing dust flux records from the Subarctic North Pacific and Greenland: Implications for atmospheric transport to Greenland and for the application of dust as a chronostratigraphic tool
Serno, S., Winckler, G., Anderson, R. F., Maier, E., Ren, H., Gersonde, R., & Haug, G. H. (2015) · Paleoceanography · doi:10.1002/2014pa002748 · Cited by 53
Self-citation
Human impact on Holocene sediment dynamics in the Eastern Mediterranean – the example of the Roman harbour of Ephesus
Stock, F., Knipping, M., Pint, A., Ladstätter, S., Delile, H., Heiss, A. G., Laermanns, H., Mitchell, P. D., Ployer, R., Steskal, M., et al. (2016) · Earth Surface Processes and Landforms · doi:10.1002/esp.3914 · Cited by 53
“While variations of Ti may be linked to the beginning of detrital input from catchment erosion due to fluvial activity (Haug et al., 2001; Yancheva et al., 2007; Panizzo et al., 2008), the increased Sr/Ca ratio may indicate a strong salinity (Wünnemann et al., 2006).”
Background
Social impacts of the climatic shift around the turn of the 19th century on the north China plain
Fang, X., Xiao, L., & Wei, Z. (2013) · Science China Earth Sciences · doi:10.1007/s11430-012-4487-z · Cited by 51
Sea surface temperature variability in southern Okinawa Trough during last 2700 years
Wu, W., Tan, W., Zhou, L., Yang, H., & Xu, Y. (2012) · Geophysical Research Letters · doi:10.1029/2012gl052749 · Cited by 52
A multiproxy lake record from Inner Mongolia displays a late Holocene teleconnection between Central Asian and North Atlantic climates
Chen, H., Song, S., Lee, T.-Q., Löwemark, L., Chi, Z., Wang, Y., & Hong, E. (2010) · Quaternary International · doi:10.1016/j.quaint.2010.03.005 · Cited by 52
“A high S-ratio indicates a predominance of anoxic sedimentary conditions and the preservation of magnetite (Yancheva et al., 2007).”
Background

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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