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Influence of the intertropical convergence zone on the East Asian monsoon
Open accessAbstract
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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In the citing paper
“Third, it may not be possible to assess the intensity of winter monsoons through titanium concentrations.”
From Climate change and Chinese history: a review of trends, topics, and methods (2015) · cites this paper as [26]
In the citing paper
“First, the suggestion that the climate in China became colder in the mid-eighth century is not novel.”
From Climate change and Chinese history: a review of trends, topics, and methods (2015) · cites this paper as [26]
In the citing paper
“Fourth, Yancheva et al. appear to have thought, wrongly, that the war with the Arabs contributed to the collapse of the Tang dynasty.25,26”
From Climate change and Chinese history: a review of trends, topics, and methods (2015) · cites this paper as [26]
In the citing paper
“Second, the idea that droughts occurred in the summer because of more powerful winter and weaker summer monsoons does not correspond with historical records.”
From Climate change and Chinese history: a review of trends, topics, and methods (2015) · cites this paper as [26]
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“Based on studies of various sedimentary sequences, a number of researchers have documented that since the Late Pleistocene this region has undergone drastic environmental and climate changes (Mingram et al. 2004; Wang et al. 2007; Yancheva et al. 2007; Zhong et al. 2010).”
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Li, S., Liu, H., Wang, H., Feng, S., Yang, X., Zheng, Y., Zhu, C., Zhao, W., & Zhang, Z. (2022) · CATENA · doi:10.1016/j.catena.2022.106847 · Cited by 4
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“Similarly, the increasing trend of the East Asian winter monsoon from early-Holocene to late-Holocene suggested a lower turbidity seasonality in the mid-Holocene, which resulted in lower δ 13C seasonality (Yancheva et al., 2007).”
BackgroundShang, S., Yang, X., Hu, J., Wang, L., & Zhang, T. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111987 · Cited by 4
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Cong, J., Fan, H., Bi, S., Mei, X., Dou, Y., Wang, Z., Ning, Z., & Zhang, Y. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113127 · Cited by 4
Wang, Y., Li, Y., & Zhang, C. (2016) · Environmental Earth Sciences · doi:10.1007/s12665-016-5338-6 · Cited by 4
“…is getting stronger and reaches its highest point at around 9000 cal - year BP; and then, monsoon is weakened for several cycles on the millennial-scale and starts to retreat since the middle Holocene (Dykoski et al. 2005; Oppo and Sun 2005; Liu et al. 2007; Yancheva et al. 2007; Wang et al. 2008).”
BackgroundSpatial variation of diatom diversity with water depth at Huguang Maar Lake, Southern China
Li, J., Wang, L., Zou, Y., & Li, J. (2021) · Journal of Paleolimnology · doi:10.1007/s10933-021-00218-5 · Cited by 4
Hu, J., Loh, P. S., Chang, Y., & Yang, C.-W. (2022) · Continental Shelf Research · doi:10.1016/j.csr.2022.104717 · Cited by 4
董, 广., 刘, 峰., & 陈, 发. (2017) · SCIENTIA SINICA Terrae · doi:10.1360/n072017-00046 · Cited by 4
Yi, S., Jun, C., Hong, S.-W., Choi, J., Kim, J. C., Yoo, D., & Lee, G. (2022) · Marine Geology · doi:10.1016/j.margeo.2022.106876 · Cited by 4
Fu, S., Li, J., Rioual, P., Wang, J., & Wang, L. (2023) · Journal of Paleolimnology · doi:10.1007/s10933-023-00305-9 · Cited by 4
“HG is one of the best-studied maar lakes on Earth, from which numerous, valuable high-resolution records of paleoclimatic changes have been produced (Yancheva et al. 2007; Zaarur et al. 2018; Vol.: (0123456789) Wu et al. 2019; Wang et al. 2022; Li et al. 2023).”
Historical Analysis of Climate Change and Agriculture
Uprety, D. C., Reddy, V. R., & Devi, M. J. (2018) · Springer eBooks · doi:10.1007/978-981-13-2014-9_2 · Cited by 4
Dai, J., Ge, Q., Shufang, X., Mengmai, W., Wu, W., & Cui, H. (2009) · Journal of Geographical Sciences · doi:10.1007/s11442-009-0750-4 · Cited by 4
Carcaillet, J. T., Siame, L. L., Chu, H., Bourlès, D. L., Lu, W., Angelier, J., & Dussouillez, P. (2007) · Terra Nova · doi:10.1111/j.1365-3121.2007.00756.x · Cited by 4
“‘‘In commemoration of Dr V.-K. Ting for his hundredth birthday’’ Annual meeting of the Geological Society of China, 63 pp. Chu, H.T., Lu, S.W. and Kuo, Y.C., 2000.”
BackgroundInfluentialWang, H., Zhang, S., & Li, H. (2008) · 中国科学通报:英文版 · doi:10.1007/s11434-008-0228-2 · Cited by 4
Jr, G. W. N., 刘, 嘉., 王, 淑., & 吕, 厚. (2007) · Chinese Science Bulletin (Chinese Version) · doi:10.1360/csb2007-52-11-1285 · Cited by 4
Du, S., Xiang, R., Yang, Z., Guo, Z., Saito, Y., & Fan, D. (2018) · The Holocene · doi:10.1177/0959683618814981 · Cited by 4
“…system (Ge et al., 2003; Kang et al., 1997; Oppo et al., 2009; Sinha et al., 2011; Tan et al., 2003; Wang et al., 1999, 2001; Wu et al., 2012; Yan et al., 2015; Yancheva et al., 2007; Yang et al., 2002; Yao et al., 1996) and can be linked to solar activity (Wang et al., 2005; Zhang et al., 2008).”
Raj, R., Tripathi, J. K., Das, A., Azam, M. M., Patel, A., Kumar, P., Achyuthan, H., Sangode, S. J., Tiwari, S., & Prizomwala, S. P. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113130 · Cited by 3
Hydroclimate Variability in the Mainland Southeast Asia During the Last Glacial Maximum
Jirapinyakul, A., Sukaudom, D., Charoenpong, C., Sompongchaikul, P., Punwong, P., & Yamoah, K. A. (2025) · Open Quaternary · doi:10.5334/oq.154 · Cited by 3
Zhang, X.-R., & Zhang, H. (2025) · Ecological Indicators · doi:10.1016/j.ecolind.2025.113980 · Cited by 3
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Self-citationLiu, X., Sun, Y., Cheng, P., Yang, Y., Wang, J., Liu, J., Ma, X., Ding, Y., Liu, B., Zhao, H., et al. (2025) · Global and Planetary Change · doi:10.1016/j.gloplacha.2025.105167 · Cited by 3
Self-citationWang, F., Hu, B., Zhao, J., Weng, D., Guo, J., & Ding, X. (2025) · Marine Micropaleontology · doi:10.1016/j.marmicro.2025.102538 · Cited by 3
Huang, D., Yu, K., Jiang, L., & Jiang, W. (2025) · Global and Planetary Change · doi:10.1016/j.gloplacha.2025.105259 · Cited by 3
Holocene climate, fire, and human impact in southern Korea inferred from pollen and charcoal records
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Liu, D., Wang, Y., Cheng, H., Edwards, R. L., & Kong, X. (2016) · Quaternary International · doi:10.1016/j.quaint.2016.09.038 · Cited by 3
Guo, C., Ma, Y., Li, J., & Meng, H. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112205 · Cited by 3
Ranasinghe, P. N., Hughen, K. A., Wijewardhana, T. U. T., Ortiz, J. D., Kapuge, A. K. I. U., Ratnayake, K. M., Nanayakkara, N. U., Hewawasam, A. L. T., Siriwardana, Y. P. S., & Kodithuwakku, S. (2024) · Scientific Reports · doi:10.1038/s41598-024-71940-z · Cited by 3
“The H1 stadial paused the post-LGM ISM precipitation increase at around 16 ka in Mawmluh Cave, Meghalaya 52,54 , Hulu Cave 51 , Arabian Sea 47 , Yellow River delta 55 , and Huguang Maar Lake 56 as well.”
BackgroundCho, A., Lim, J., Han, M., Jun, C., & Ahn, U. S. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.112730 · Cited by 3
Late Holocene eolian dust activity recorded by a peat sequence in North Xinjiang, northwestern China
Qiang, M., & Liu, Y. (2025) · Global and Planetary Change · doi:10.1016/j.gloplacha.2025.104877 · Cited by 3
Li, Y., Li, Y., Ye, W., & Peng, S. (2019) · Progress in Physical Geography Earth and Environment · doi:10.1177/0309133319878115 · Cited by 3
“Much work has shown that the Asian summer monsoon is a lowlatitude process, while the Asian winter monsoon is a mid-latitude one (Chao and Chen, 2001; Webster et al., 1998; Yancheva et al., 2007).”
BackgroundInfluence of the Late Quaternary climate on sedimentology of the Jazmurian Playa, SE Iran
Sharifi-Yazdi, M., Tavakoli, V., Salehi-Noparvar, S., Vaezi, A., Beni, A. N., Nazemi, M., Duttagupta, S., & Routh, J. (2022) · Journal of Paleolimnology · doi:10.1007/s10933-022-00239-8 · Cited by 3
“It means that the arid conditions that prevailed during this period restricted chemical weathering and that deposits were comparable to those in East Asia (Yancheva et al., 2007), reflecting intense winter and windy conditions.”
BackgroundGuo, A., Mao, L.-J., Shan, S., Zhang, X.-G., & Mo, D.-W. (2022) · Land · doi:10.3390/land11060789 · Cited by 2
Heavy Metal Concentrations in the Surface Water of a Crater Lake in Southern China
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Zhu, B., & Yang, L. (2023) · Atmosphere · doi:10.3390/atmos14020384 · Cited by 3
Liu, Y., Tao, S., Sun, R., You, C., Wang, T., Felis, T., Wang, Z., Sun, S., Liu, X., Shi, Q. W., et al. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111488 · Cited by 3
Climate Change in Historical Perspective: Violence, Conflict, and Migration
Pei, Q., Long, Y., & Lin, X. (2023) · Springer eBooks · doi:10.1007/978-3-319-57365-6_389-1 · Cited by 3
Sun, C., & Li, H. (2023) · Cliometrica · doi:10.1007/s11698-023-00270-3 · Cited by 3
“…(Yin et al. 2015), population growth (Lee et al. 2008), civil conflict (Zhang et al. 2007; Chen 2015a), Sino-nomadic relationship (Bai and Kung 2011; Chen 2015b; Pei et al. 2019), and even dynastic rise and decline (Yancheva 2007; Zhang et al. 2008; Fan 2010; Wei et al. 2020) in historical China.”
Chen, X., Zhang, H., Griffiths, M. L., Peng, X., Yang, L., Yu, M., Huang, J., Xue, S., Cheng, H., & Chen, S. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111702 · Cited by 3
Sjöström, J., Cortizas, A. M., Nylund, A., Hardman, A., Kaal, J., Smittenberg, R. H., Risberg, J., Schillereff, D. N., & Norström, E. (2023) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2023.108216 · Cited by 3
Gao, M., Li, Y., Zhang, Z., Duan, J., Xue, Y., Peng, S., Shang, H., & Liu, S. (2024) · The Holocene · doi:10.1177/09596836241236344 · Cited by 3
“According to the Donggot Cave, Huguangyan Maar Lake, and Qinghai Lake records, the intensity of the Asian summer winds gradually increased from the LGM (Late Glacial Maximum) and lasted until the Middle Holocene period (Dykoski et al., 2005; Yancheva et al., 2007).”
Kerr, M. T., Horn, S. P., & Lane, C. S. (2024) · Journal of Quaternary Science · doi:10.1002/jqs.3616 · Cited by 3
“Millennial ‐ scale paleohydrology at Lago de las Morrenas 1 The δ D PP record from Morrenas 1 demonstrates millennial ‐ scale variations in paleohydrology that, based on modern climate dynamics, were probably controlled by changes in the mean annual position of the ITCZ, which itself was driven by changes in location…”
BackgroundInfluentialDu, Y., Zhong, W., Shang, S., Wang, Z., Wang, X., Quan, M., & Li, T. (2024) · The Holocene · doi:10.1177/09596836241266409 · Cited by 3
“The specific dry and wet events revealed by those magnetic parameters were synchronous with that of the stalagmite δ 18 O record from the Heshang Cave in Central China (Hu et al., 2008) (Figure 7a), the model-simulated mean annual precipitation (MAP) averaged for Xingyun Lake in central Yun-nan Province in southwest C…”
InfluentialGao, X., Ji, K., Zang, T., Hou, X., Yuan, K., Sun, Z., Li, C., & Hou, J. (2024) · The Holocene · doi:10.1177/09596836241291999 · Cited by 3
“From the early to middle Holocene, the Inter-tropical Convergence Zone (ITCZ) moved northward (Fleitmann et al., 2007; Schneider et al., 2014; Yancheva et al., 2007), and the Indian monsoon strengthened from ~10,000 to 6000 cal year BP, resulting in relatively high precipitation on the western TP…”
New controls on sedimentation and climate in the central equatorial Pacific Ocean
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“…in response to the hemispheric thermal balance (Donohoe et al., 2013; Schneider et al., 2014) with implications for tropical hydroclimate (e.g Yancheva et al., 2007), global atmospheric circulation (Ceppi et al., 2013), and associated oceanographic upwelling and carbon release (Anderson et…”
Huang, K., Zhang, Q., Qiang, X., & Wang, D. (2012) · Atmospheric and Oceanic Science Letters · doi:10.1080/16742834.2012.11447010 · Cited by 3
“…states of the western Pacific warm pool (Li et al., 1999; Wu et al., 2009), the convective activity around the Philippines (Nitta, 1987; Huang and Li, 1988; Huang et al., 2005), the western Pacific subtropical high (Chang et al., 2000; Zhou and Yu, 2005; Zhou et al., 2009b; Yancheva et al., 2007;)”
BackgroundHOLOCENE PALEOENVIRONMENTAL EVOLUTION OF THE HUGUANGYAN MAAR LAKE
Wu, X., Shen, J., & Wang, Y. (2011) · Marine Geology & Quaternary Geology · doi:10.3724/sp.j.1140.2011.04155 · Cited by 3
Jiang, X., Li, Z., Shen, C. C., & Li, J. (2011) · Marine Geology & Quaternary Geology · doi:10.3724/sp.j.1140.2011.03117 · Cited by 3
Thurow, J. W., Peterson, L. C., Harms, U., Hodell, D. A., Cheshire, H., Brumsack, H.-J., Irino, T., Schulz, M., Masson‐Delmotte, V., & Tada, R. (2009) · Scientific Drilling · doi:10.5194/sd-8-46-2009 · Cited by 3
Self-citationThe Interaction of Climate Change and Agency in the Collapse of Civilizations ca. 2300–2000 BC
Wiener, M. H. (2014) · Tree-Ring Research · doi:10.3959/1536-1098-70.3.1 · Cited by 3
The Interaction of Climate Change and Agency in the Collapse of Civilizations ca. 2300–2000 BC
Wiener, M. H. (2014) · Radiocarbon · doi:10.1017/s0033822200050311 · Cited by 3
Zhong, W., Wei, Z., Shang, S., Ye, S., Quan, M., Li, T., & Ouyang, J. (2022) · Geochemistry International · doi:10.1134/s0016702922090099 · Cited by 3
“However, due to 877 the lack of suitable geologic achieves, up to now most of the relevant studies on EAMS in this area mainly focus on the EASM, only a few researches involved the EAWM (e.g., Yancheva et al., 2007; Wang et al., 2012; Liu et al., 2014; Ferrat et al., 2012; Wang et al., 2018).”
BackgroundASEAN-India-Australia: Towards Closer Engagement in a New Asia
Tow, W. T., & Wah, C. K. (2009) · Project Muse (Johns Hopkins University) · Cited by 3
Time-scale effects in human-nature interactions, regionally and globally
Li, Y., Gao, M., Zhang, Z., Zhang, Y., & Peng, S. (2023) · Journal of Geographical Sciences · doi:10.1007/s11442-023-2143-5 · Cited by 2
“E-mail: liyu@lzu.edu.cn www.geogsci.com www.springer.com/journal/11442 interaction model between the evolution of human civilization and the history of climate change is a meaningful way to explore the above issues (Yancheva et al., 2007; Kathayat et al., 2017; Chen et al., 2019).”
BackgroundHuo, J., Xue, J., Chen, J., Li, Y., Chen, M., Zhao, Z., & Liu, Y. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112541 · Cited by 2
Lin, Z., & Xie, Y. (2025) · Religions · doi:10.3390/rel16030332 · Cited by 2
“The mid‑to‑late Tang Dynasty (700–907) coincided with a period of strong winter mon‑ soons in East Asia, which resulted in erratic climatic changes during this period (Yancheva et al. 2004, pp. 74–77).”
High-precision radiocarbon dating and carbon reservoir effect of a maar lake in South China
Gu, Y., Lu, H., Zhang, H., Lin, P., Dong, X., Wang, Y., Yi, S., Lu, F., & Yang, F. (2025) · Quaternary Geochronology · doi:10.1016/j.quageo.2025.101668 · Cited by 2
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Dust variations in the western North Pacific dominated by the East Asian monsoon
Dou, R., Zou, J., Shi, X., Dong, Z., Zhu, A., Feng, X., Yao, Z., Liu, J., Gorbarenko, S. A., Vasilenko, Y. P., et al. (2025) · Science China Earth Sciences · doi:10.1007/s11430-025-1596-y · Cited by 2
“In contrast to short-term instrumental records, paleo-dust reconstructions—especially those spanning climatic transi-tions—provide a crucial means of deciphering the mechanisms governing EAD evolution (Ding et al., 1995; Yancheva et al., 2007; Kang et al., 2020).”
Self-citationZhao, B., Zhao, K., He, Y., Wang, Y., Shao, Q., & Cheng, H. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113114 · Cited by 2
Wei, Y., Zhou, K., Sheng, E., Liu, B., & Lan, J. (2025) · Quaternary Science Advances · doi:10.1016/j.qsa.2025.100304 · Cited by 2
Park, S., & Lim, J. (2025) · Quaternary Research · doi:10.1017/qua.2025.10046 · Cited by 2
“The change in orbital scale in the EASM during the Holocene has been attributed to the northward/southward shift of the ITCZ throughtherainfallfrontposition,coupledwithinsolationchanges (Dykoskietal.,2005;Yanchevaetal.,2007;Wangetal.,2017).”
A Review of Paleoenvironmental Reconstruction Using Crater Lake Sediments in Monsoonal China
Liu, X., Jiang, S., Tu, L., Oyebanji, D. B., Liu, X., Yuan, Y., Li, X., Ji, M., Zhang, G., & Zhou, X. (2025) · Journal of Earth Science · doi:10.1007/s12583-022-1733-y · Cited by 2
“The length of the longest core from Huguangyan Lake in previous studies is 57.82 m, and K-Ar age of basalts from the crater rim is approximately 127 ka (Yancheva et al., 2007; Mingram et al., 2004a).”
InfluentialThe 8.2 Ka Abrupt Climate Event: Causes, Impacts and Future Implications
Dixit, Y., & Kumari, A. (2026) · Wiley Interdisciplinary Reviews Climate Change · doi:10.1002/wcc.70050 · Cited by 2
“Overall, there is also still a general lack of seasonally resolved records, few proxy evidence of strengthened winter precipitation in the northern hemisphere is reported such as, storm tracks in coastal California centered at ~8.19 ka BP (Oster et al. 2017), which is synchronous with other Asian winter proxies from S…”
InfluentialMid-Holocene rainfall heterogeneity in subtropical East Asia
Xu, H., Cao, J., Wang, J., Cheng, J., Goldsmith, Y., & Long, H. (2026) · The Innovation Geoscience · doi:10.59717/j.xinn-geo.2026.100225 · Cited by 2
Human impact on climate and eco-hydrological systems in the Badain Jaran desert in northwest China
Zhang, H., Chang, F., Chen, G., Zhen, Q., Cai, Y., & Li, H. (2013) · Cited by 2
Minoura, K., & Nakamura, N. (2020) · Geosciences · doi:10.3390/geosciences10100410 · Cited by 2
Fedotov, A., Vorobyeva, S. S., Евгеньевич, В. К., & Osipov, E. Y. (2021) · Quaternary International · doi:10.1016/j.quaint.2021.11.021 · Cited by 2
Yao, Y., Liu, X., Zhang, Z., Li, Z., & Hu, Y. (2022) · Journal of Geochemical Exploration · doi:10.1016/j.gexplo.2022.107093 · Cited by 2
Premaratne, K. M., Chandrajith, R., Ratnayake, N. P., Li, S., Gayantha, K., & Routh, J. (2023) · The Holocene · doi:10.1177/09596836231211875 · Cited by 2
“…recorded in proxies such as total organic carbon (Yancheva et al., 2007), δ 18 O (Sagawa et al., 2014), aeolian dust flux (Yu et al., 2011), Ti (Yancheva et al., 2007), and lignin proxies (Hao et al., 2017), revealed a notable association with timing and relative magnitude of Bond events…”
BackgroundNorth Atlantic Influence on the Glacial Amplitude of East Asian Millennial-Scale Monsoon Variability
Guo, F., Clemens, S. C., Du, X., Liu, X., Liu, Y., Sun, J., Fan, H., Wang, T., & Sun, Y. (2024) · Journal of Climate · doi:10.1175/jcli-d-23-0200.1 · Cited by 2
Lyu, W., Fu, T., Chen, G., Su, Q., Liu, W., Wang, Y., Cui, Z. D., Yu, H., & Xu, X. (2024) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2024.106217 · Cited by 2
An Elevated Influence of the Low‐Latitude Drivers on the East Asian Winter Monsoon After Around 1990
Chen, B., Fang, K., Mei, Z., Ou, T., Zhou, F., Wu, H., Zhao, Z., & Chen, D. (2024) · International Journal of Climatology · doi:10.1002/joc.8681 · Cited by 2
“…of low-latitude processes on the EAWM since around 1990 might be linked to the interdecadal weakening of the EAWM in the late 1980s (He 2013; Yancheva et al. 2007), the interdecadal variation in Siberian High intensity (Jeong et al. 2011) and the reduced winter snow in the 1990s (Ma and…”
Li, Y., Li, Y., Chen, M., Xue, Y., Zhang, J., Wang, L., Tong, C., & Yi, L. (2024) · Marine Geology · doi:10.1016/j.margeo.2024.107453 · Cited by 2
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Zhang, X.-R., Zhang, H., & Liu, Z. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113123 · Cited by 2
Li, Y., Wang, Y., & Zhang, C. (2015) · Physical Geography · doi:10.1080/02723646.2015.1050936 · Cited by 2
“It reached its highest point at around 9000 cal yr BP, and started to decline in the middle Holocene (Denton et al., 2010; Dykoski et al., 2005; Oppo & Sun, 2005; Wang et al., 2008; Yancheva et al., 2007).”
BackgroundRoot proliferation in native perennial grasses of arid Patagonia, Argentina
Torres, Y. A., Busso, C. A., Montenegro, O. A., Ithurrart, L. S., Giorgetti, H. D., Rodríguez, G., Bentivegna, D. J., Brevedan, R. E., Fernández, O. A., Mujica, M. D. L. M., et al. (2013) · Journal of Arid Land · doi:10.1007/s40333-013-0201-z · Cited by 2
Peterson, J. A. (2013) · Asian perspectives · doi:10.1353/asi.2013.0011 · Cited by 2
Zhou, X., Sun, L., Liu, Y., & Wang, Y. (2013) · Journal of Ocean University of China · doi:10.1007/s11802-013-2191-z · Cited by 2
Zhang, C., & Zhang, Q. (2014) · Journal of Arid Environments · doi:10.1016/j.jaridenv.2013.12.001 · Cited by 2
DECADAL CHANGES AND SOURCES ANALYSIS OF MICROBIAL BIOMARKER GDGTS IN THE EAST CHINA SEA SEDIMENTS
Zhang, T., Xing, L., Zhang, H., Li, L., Zhao, X., Weifang, C. H. E. N., & Zhao, M. (2013) · Marine Geology & Quaternary Geology · doi:10.3724/sp.j.1140.2012.03087 · Cited by 2
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Geochemical characteristics of dust aerosol availability in northwestern China
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The Changing Human Environments of Eastern Saudi Arabia
Vita‐Finzi, C. (2019) · Springer eBooks · doi:10.1007/978-3-030-28323-0_6 · Cited by 2
徐, 建. (2014) · SCIENTIA SINICA Terrae · doi:10.1360/zd-2014-44-12-2709 · Cited by 2
Caldararo, N. (2015) · Anthropology · doi:10.4172/2332-0915.1000154 · Cited by 2
“[32] have produced a useful record of climatic change in East Asia but their claim that these changes were sufficient to cause civilizations to collapse is premature.”
BackgroundEnvironmental and climatic changes inferred from lake deposits in China: A review of recent progress
Rioual, P., & Wang, L. (2009) · PAGES news · doi:10.22498/pages.17.3.110 · Cited by 2
王, 绍., 黄, 建., 朱, 锦., & 闻新宇 (2007) · Chinese Science Bulletin (Chinese Version) · doi:10.1360/csb2007-52-20-2428 · Cited by 2
Did worldwide drought wipe out ancient cultures?
Hopkin, M. (2007) · Nature · doi:10.1038/news070101-2 · Cited by 2
Ancient Great Wall Building Materials Reveal Paleoenvironmental Changes in Northwestern ChinaPreprint
Patalano, R., Jing, H., Qing, L., Liu, W., Wang, H., Roberts, P., Storozum, M. J., Lin, Y., & Yang, H. (2021) · Research Square · doi:10.21203/rs.3.rs-390056/v1 · Cited by 2
Li, Q., Sun, Q., Xie, M., Ling, Y., Zhu, Z., Zhu, Q., Zhan, N., & Chu, G. (2022) · doi:10.1002/essoar.10512210.1 · Cited by 2
Metadata
- 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
- Venue
- Nature
- Published
- 2007-01-04
- Volume
- 445
- Issue
- 7123
- Pages
- 74-77
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- 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
- Licence
- 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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