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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BackgroundInfluential
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Background
Sea level change and Kuroshio intrusion dominated Taiwan sediment source-to-sink processes in the northeastern South China Sea over the past 244 kyrs
Zhang, C., Yang, S., Huang, X., Dou, Y., Li, F., Xu, X., Hao, Q., & Gao, J. (2022) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2022.107558 · Cited by 42
Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years
Liu, Y., Song, H., An, Z., Li, Q., Leavitt, S. W., Büntgen, U., Cai, Q., Liu, R., Fang, C., Sun, C., et al. (2025) · Nature Communications · doi:10.1038/s41467-025-56687-z · Cited by 42
Constraints from strontium and neodymium isotopic ratios and trace elements on the sources of the sediments in Lake Huguang Maar
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“…this lake, but also for modern economic and social development in coastal South China because a lithogenic flux to the lake as high as suggested by Yancheva et al. (2007a) is comparable with the modern mineral dust flux monitored on the Loess Plateau (Sun et al., 2003), and implies that coastal…”
BackgroundInfluential
Mid−late Holocene monsoonal records from the partially active mudflat of Diu Island, southern Saurashtra, Gujarat, western India
Banerji, U. S., Bhushan, R., & Jull, A. J. T. (2017) · Quaternary International · doi:10.1016/j.quaint.2016.09.060 · Cited by 42
The socioeconomic effects of extreme drought events in northern China on the Ming dynasty in the late fifteenth century
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Tropical Intraseasonal Modes of the Atmosphere
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A 1232-YEAR TREE-RING RECORD OF CLIMATE VARIABILITY IN THE QILIAN MOUNTAINS, NORTHWESTERN CHINA
Zhang, Y., Gou, X., Chen, F., Tian, Q., Yang, M., Peng, J., & Fang, K. (2009) · IAWA Journal - KU Leuven/IAWA Journal · doi:10.1163/22941932-90000228 · Cited by 40
Anthropogenic climate change: Scientific uncertainties and moral dilemmas
Hillerbrand, R., & Ghil, M. (2008) · Physica D Nonlinear Phenomena · doi:10.1016/j.physd.2008.02.015 · Cited by 41
“Recent research suggests that a possibly worldwide drought in the 10th century was the catalyst for the demise of the Tang Dynasty in China, as well as of the Mayan civilization in Central America [4].”
Background
Tetraether lipids from the southern Yellow Sea of China: Implications for the variability of East Asia Winter Monsoon in the Holocene
Ge, H., Zhang, C. L., Li, J., Versteegh, G. J. M., Hu, B., Zhao, J., & Dong, L. F. (2014) · Organic Geochemistry · doi:10.1016/j.orggeochem.2014.02.011 · Cited by 41
“There is still an argument about the variation in EAWM in the Holocene (e.g. Yancheva et al., 2007; Hu et al., 2012), whereby the strong and highly fluctuating EAWM during 7.2–4.2 ka BP reconstructed by Hu et al. (2012) using grain size variation agrees with the intensified YSWC reconstructed by us.”
BackgroundInfluential
Holocene East Asian winter monsoon changes reconstructed by sensitive grain size of sediments from Chinese coastal seas: A review
Tu, L., Zhou, X., Cheng, W., Liu, X., Yang, W., & Wang, Y. (2016) · Quaternary International · doi:10.1016/j.quaint.2016.03.024 · Cited by 41
Palaeoenvironmental implication of grain-size compositions of terrace deposits on the western Chinese Loess Plateau
Liu, X., Sun, Y., Vandenberghe, J., Li, Y., & An, Z. (2018) · Aeolian Research · doi:10.1016/j.aeolia.2018.03.008 · Cited by 41
The influence of climate, hydrology and permafrost on Holocene peat accumulation at 3500m on the eastern Qinghai–Tibetan Plateau
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Hydroclimatic shifts in northeast Thailand during the last two millennia – the record of Lake Pa Kho
Chawchai, S., Chabangborn, A., Fritz, S. C., Väliranta, M., Mörth, C., Blaauw, M., Reimer, P. J., Krusic, P. J., Löwemark, L., & Wohlfarth, B. (2015) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2015.01.007 · Cited by 41
“, 2008), and lake (Yancheva et al., 2007) studies show that substantial decadal to centennial variations in summer monsoon intensity were superimposed on the longterm trend.”
Background
Records of late-Holocene East Asian winter monsoon in the East China Sea: Key grain-size component of quartz versus bulk sediments
Qiao, S., Yang, Z., Liu, P., Sun, X., Xiang, R., Shi, X., Fan, D., & Saito, Y. (2010) · Quaternary International · doi:10.1016/j.quaint.2010.01.020 · Cited by 41
Vegetation and climate changes over the last 30 000 years on the Leizhou Peninsula, southern China, inferred from the pollen record of Huguangyan Maar Lake
Meng, Y., Wang, W., Hu, J., Zhang, J., & Lai, Y. (2017) · Boreas · doi:10.1111/bor.12229 · Cited by 40
“This deteriorating climate may have been caused by ITCZ migration, resulting in weaker summer monsoon rainfall (Yancheva et al. 2007; Schneider et al. 2014).”
Background
Episodic Reef Growth in the Northern South China Sea linked to Warm Climate During the Past 7,000 Years: Potential for Future Coral Refugia
Yan, S., Zhao, J., Lau, A. Y. A., Roff, G., Leonard, N. D., Clark, T. R., Nguyen, A. D., Feng, Y., Wei, G., Deng, W., et al. (2019) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2018jg004939 · Cited by 40
“, 2008), East Asian winter monsoon (EAWM; Yancheva et al., 2007) and ENSO (Moy et al.”
BackgroundInfluential
Palaeovegetation and palaeoclimate in low-latitude southern China during the Last Glacial Maximum
Wang, S., Lü, H., Han, J., Chu, G., Liu, J., & Negendank, J. F. W. (2010) · Quaternary International · doi:10.1016/j.quaint.2010.07.030 · Cited by 40
Self-citation
Is Chinese stalagmite δ18O solely controlled by the Indian summer monsoon?
Dong, L., Tan, L., Cai, Y., Jiang, X., Ma, L., Cheng, H., Edwards, R. L., Zhang, H., Gao, Y., & An, Z. (2019) · Climate Dynamics · doi:10.1007/s00382-019-04671-x · Cited by 40
3500-year western Pacific storm record warns of additional storm activity in a warming warm pool
Yue, Y., Yu, K., Tao, S., Zhang, H., Liu, G., Wang, N., Jiang, W., Fan, T., Lin, W., & Wang, Y. (2019) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2019.02.009 · Cited by 42
“Although the broad decline in AM intensity during the late Holocene has been reported to be associated with the southward shift of the Northern Hemisphere summer position of the ITCZ, which occurs in response to the orbitally induced lowering of summer insolation (Wang et al., 2005; Fleitmann et al., 2007; Yancheva et…”
Background
Western Pacific Ocean influences on monsoon precipitation in the southwestern Chinese Loess Plateau since the mid-Holocene
Zhang, C., Zhao, C., Yu, Z., Zhang, H., Zhou, A., Zhang, X., Feng, X., Sun, X., & Shen, J. (2020) · Climate Dynamics · doi:10.1007/s00382-020-05159-9 · Cited by 41
Evaluation of high-resolution elemental analyses of Chinese loess deposits measured by X-ray fluorescence core scanner
Liang, L., Sun, Y., Yao, Z., Liu, Y., & Wu, F. (2011) · CATENA · doi:10.1016/j.catena.2011.11.010 · Cited by 40
“High-resolution Ti content (an indicator of Ti-bearing aeolian dust events) for the Huguang Maar lake sediments in the southeastern China indicates persistent millennial-to-decadal fluctuations of the East Asian winter monsoon over the last 16 ka (Yancheva et al., 2007).”
Background
Late Quaternary coccolith records in the South China Sea and East Asian monsoon dynamics
Su, X., Liu, C., Beaufort, L., Tian, J., & Huang, E. (2013) · Global and Planetary Change · doi:10.1016/j.gloplacha.2013.08.016 · Cited by 39
Towards an understanding of climate proxy formation in the Chew Bahir basin, southern Ethiopian Rift
Foerster, V., Deocampo, D. M., Asrat, A., Günter, C., Junginger, A., Kraemer, K. H., Stroncik, N. A., & Trauth, M. H. (2018) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2018.04.009 · Cited by 42
Hydroclimate variability of central Indo-Pacific region during the Holocene
Chawchai, S., Tan, L., Löwemark, L., Wang, H.-C., Yu, T.-L., Chung, Y. C., Mii, H., Liu, G., Blaauw, M., Gong, S.-Y., et al. (2021) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2020.106779 · Cited by 39
High-resolution multi-proxy evidence for millennial- and centennial-scale climate oscillations during the last deglaciation in Jeju Island, South Korea
Park, J., Lim, H. S., Lim, J., & Park, Y. (2014) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2014.10.003 · Cited by 39
Continuous real‐time analysis of the isotopic composition of precipitation during tropical rain events: Insights into tropical convection
He, S., Goodkin, N. F., Jackisch, D., Ong, M. R., & Samanta, D. (2018) · Hydrological Processes · doi:10.1002/hyp.11520 · Cited by 38
Paleoclimatic changes on the southern Tibetan Plateau over the past 19,000 years recorded in Lake Pumoyum Co, and their implications for the southwest monsoon evolution
Nishimura, M., Matsunaka, T., Morita, Y., Watanabe, T., Nakamura, T., Zhu, L., Nara, F. W., Imai, A., Izutsu, Y., & Hasuike, K. (2013) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2013.12.015 · Cited by 37
East Asian Monsoon controls on the inter-annual variability in precipitation isotope ratio in Japan
Kurita, N., Fujiyoshi, Y., Nakayama, T., Matsumi, Y., & Kitagawa, H. (2015) · Climate of the past · doi:10.5194/cp-11-339-2015 · Cited by 37
Holocene paleoenvironment changes in the northern Yellow Sea: Evidence from alkenone-derived sea surface temperature
Nan, Q., Li, T., Chen, J., Chang, F., Yu, X., Xu, Z., & Pi, Z. (2017) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2017.01.031 · Cited by 37
Contrasting effects of winter and summer climate on Holocene montane vegetation belts evolution in southeastern Qinghai-Tibetan Plateau, China
Ni, Z., Jones, R., Zhang, E., Chang, J. C., Shulmeister, J., Sun, W., Wang, Y., & Ning, D. (2019) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2019.06.005 · Cited by 37
River flooding response to ENSO-related monsoon precipitation: Evidence from late Holocene core sediments in the Jianghan Plain
Guan, S., Yang, Q., Li, Y., Liu, H., & Gu, Y. (2022) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2022.110834 · Cited by 37
Decadal-resolution record of winter monsoon intensity over the last two millennia from planktic foraminiferal assemblages in the northeastern Arabian Sea
Munz, P., Siccha, M., Lückge, A., Böll, A., Kučera, M., & Schulz, H. (2015) · The Holocene · doi:10.1177/0959683615591357 · Cited by 36
“Although the temperature range of the wSST record of this study after 450 CE is mostly within the reconstruction uncertainty of ~1°C, persistent cold spells around 450–600 CE and 750 CE, as well as warmer intervals between 600–700 CE, around 950 CE, 1300 CE, and 1450 CE, are consistent with the Lake Huguang Maar magne…”
BackgroundInfluential
Abrupt cooling repeatedly punctuated early-Holocene climate in eastern North America
Hou, J., Huang, Y., Shuman, B. N., Oswald, W. W., & Foster, D. R. (2011) · The Holocene · doi:10.1177/0959683611427329 · Cited by 36
Precisely dated multidecadally resolved Asian summer monsoon dynamics 113.5–86.6 thousand years ago
Jiang, X., Wang, X., He, Y., Hu, H., Li, Z., Spötl, C., & Shen, C. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.05.003 · Cited by 34
Evidence for extreme floods in arid subtropical northwest Australia during the Little Ice Age chronozone (CE 1400–1850)
Rouillard, A., Skrzypek, G., TURNEY, C. S. M., Dogramaci, S., Hua, Q., Zawadzki, A., Reeves, J. M., Greenwood, P. F., O’Donnell, A. J., & Grierson, P. F. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.05.004 · Cited by 35
The River, the Plain, and the State: An Environmental Drama in Northern Song China, 1048–1128
Zhang, L. (2016) · Cited by 35
A Last Interglacial record of environmental changes from the Sulmona Basin (central Italy)
Regattieri, E., Giaccio, B., Nomade, S., Francke, A., Vogel, H., Drysdale, R. N., Perchiazzi, N., Wagner, B., Gemelli, M., Mazzini, I., et al. (2017) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2017.02.013 · Cited by 35
“However, Ti is enriched in heavy minerals and in aeolian dust, and in particular settings it can therefore be used as a proxy for high-current regimes (Schnetger et al., 2000) or enhanced wind activity (Wehausen and Brumsack, 1999; Yancheva et al., 2007).”
Background
Holocene monsoon and sea level-related changes of sedimentation in the northeastern Arabian Sea
Burdanowitz, N., Gaye, B., Hilbig, L., Lahajnar, N., Lückge, A., Rixen, T., & Emeis, K. (2019) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2019.03.003 · Cited by 36
Causality of climate, food production and conflict over the last two millennia in the Hexi Corridor, China
Yang, L., Feng, Q., Adamowski, J. F., Deo, R. C., Yin, Z., Wen, X., Tang, X., & Wu, M. (2020) · Science of The Total Environment · doi:10.1016/j.scitotenv.2020.136587 · Cited by 35
Deglacial variability of South China hydroclimate heavily contributed by autumn rainfall
He, C., Liu, Z., Otto‐Bliesner, B. L., Brady, E. C., Zhu, C., Tomas, R. A., Gu, S., Han, J., & Jin, Y. (2021) · Nature Communications · doi:10.1038/s41467-021-26106-0 · Cited by 35
The study of early human settlement preference and settlement prediction in Xinjiang, China
Tan, B., Wang, H., Wang, X., Yi, S., Zhou, J., Ma, C., & Dai, X. (2022) · Scientific Reports · doi:10.1038/s41598-022-09033-y · Cited by 40
Disturbances with hiatuses in high-latitude coral reef growth during the Holocene: Correlation with millennial-scale global climate change
Hamanaka, N., Kan, H., Yokoyama, Y., Okamoto, T., Nakashima, Y., & KAWANA, T. (2011) · Global and Planetary Change · doi:10.1016/j.gloplacha.2011.10.004 · Cited by 35
“, 2005), in conjunction with a relatively strong cold Asian winter monsoon (Yancheva et al., 2007) that was induced by insolation forcing a southward migration of the Intertropical Convergence Zone (ITCZ) in the Northern Hemisphere (e.”
Background
Provenance discrimination of the clay sediment in the western Taiwan Strait and its implication for coastal current variability during the late-Holocene
Chen, J., Ma, J., Xu, K., Liu, Y., Cao, W., Wei, T., Zhao, B., & Chen, Z. (2016) · The Holocene · doi:10.1177/0959683616652706 · Cited by 34
“The limited records revealed that it was still controversial on the trend of winter EAM during Holocene, for example, the opposite trends of Holocene winter EAM were archived even in the researches at the same location of Lake Huguangyan (Jia et al., 2015; Wang et al., 2012; Yancheva et al., 2007).”
Background
Environmental change during MIS4 and MIS 3 opened corridors in the Horn of Africa for Homo sapiens expansion
Viehberg, F., Just, J., Dean, J. R., Wagner, B., Franz, S. O., Klasen, N., Kleinen, T., Ludwig, P., Asrat, A., Lamb, H. F., et al. (2018) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2018.09.008 · Cited by 38
Contrasting Hysteresis Behaviors of Northern Hemisphere Land Monsoon Precipitation to CO2 Pathways
Oh, H., An, S., Shin, J., Yeh, S., Min, S., Son, S., & Kug, J. (2022) · Earth s Future · doi:10.1029/2021ef002623 · Cited by 34
Late Quaternary climate in southern China deduced from Sr–Nd isotopes of Huguangyan Maar sediments
Zaarur, S., Stein, M., Adam, O., Mingram, J., Chu, G., Liu, J., Wu, J., & Erel, Y. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.05.025 · Cited by 33
Self-citation
Prolonged Heavy Snowfall During the Younger Dryas
Wang, L., Jiang, W., Jiang, D., Zou, Y., Liu, Y. Y., Zhang, E., Hao, Q., Zhang, D., Zhang, D., Peng, Z. Y., et al. (2018) · Journal of Geophysical Research Atmospheres · doi:10.1029/2018jd029271 · Cited by 33
High- and low-latitude forcing on the south Yellow Sea surface water temperature variations during the Holocene
Jia, Y., Li, D., Yu, M., Zhao, X., Xiang, R., Li, G., Zhang, H., & Zhao, M. (2019) · Global and Planetary Change · doi:10.1016/j.gloplacha.2019.103025 · Cited by 33
Late Quaternary Abrupt Climate Change in the Tropics and Sub‐Tropics: The Continental Signal of Tropical Hydroclimatic Events (THEs)
Bradley, R. S., & Díaz, H. F. (2021) · Reviews of Geophysics · doi:10.1029/2020rg000732 · Cited by 33
“However, in Huguang Maar, a lake in southeast China (∼21°N), high levels of titanium (from aeolian sediments) are inversely correlated with Hulu cave δ18O, suggesting that a southward shift of the ITCZ led to both reduced summer rainfall and a strong winter monsoon with increased aeolian influx (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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