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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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Items 601–700 of 947
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“Other climatic records (Dykoski et al., 2005; Yancheva et al., 2007; Yao, 2000; Dong et al., 2015) reflect a gradually intensifying East Asian Summer Monsoon (EASM), during which period precipitation began to increase, reflecting a warmer and more humid climate.”
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“However, detailed knowledge about the ASM and/or AWM, as triggered by the landocean thermal contrast, also requires a thorough understanding of the contribution of oceanic counterpart (e.g. Thompson et al., 2000; Wang et al., 2005; Yancheva et al., 2007).”
BackgroundMicrobial diversity in Huguangyan Maar Lake of China revealed by high–throughput sequencing
Hou, Q., Fang, Z., Zhu, Q., & Dong, H. (2019) · Journal of Oceanology and Limnology · doi:10.1007/s00343-019-8016-1 · Cited by 9
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Fundamental Shift From Summer to Winter of Holocene Rainfall Regime in the Tropics
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The 2.8 ka climatic event contributed to the collapse of the Western Zhou Dynasty
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“This further implies that summer and winter monsoons do not change in direct antiphase over this timescale [contrasting with the lake record of Yancheva et al. (2007)] and that the magnetic susceptibility signal develops rapidly.”
BackgroundInfluentialZhang, J., Storozum, M. J., Chen, W., Rao, Z., Hamilton, R. J., Zheng, Z., Chen, Z., Yu, X., & Xia, Z. (2022) · Geoarchaeology · doi:10.1002/gea.21950 · Cited by 8
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Park, S., Lim, J., Kim, Y., Shin, K., & Lim, H. S. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111737 · Cited by 8
Guan, Q., Pan, B., Yang, J., Wang, L., Zhao, S., & Gui, H. (2012) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2012.11.030 · Cited by 8
Badejo, A. O., Gal, J., Hyun, S., Yi, H.-I., & Shin, K. (2014) · Quaternary International · doi:10.1016/j.quaint.2014.06.035 · Cited by 8
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Chen, Y., Li, Y., Lyu, W., Dong, X., Han, X., Fu, T., & Yi, L. (2020) · Atmosphere · doi:10.3390/atmos11121376 · Cited by 8
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He, H., Delang, C. O., Zhou, J., Li, Y., & He, W. (2021) · Climatic Change · doi:10.1007/s10584-021-03134-9 · Cited by 8
Pi, Z., Chang, F., Li, T., & Cui, Y. (2021) · Journal of Oceanology and Limnology · doi:10.1007/s00343-021-0219-6 · Cited by 8
Recent Changes in the Climate: Natural or Forced by Human Activity
Karlén, W. (2008) · AMBIO · doi:10.1579/0044-7447-37.sp14.483 · Cited by 8
“A similar climatic event is also mentioned in a paper concerning the influence of the intertropical convergence on the Asian monsoon (60).”
BackgroundDing, P., Shen, C., Wang, N., Yi, W., Liu, K., Ding, X., & Fu, D. (2009) · Science China Earth Sciences · doi:10.1007/s11430-009-0014-2 · Cited by 8
Guo, Y., Deng, W., Chen, X., Wei, G., Yu, K., & Zhao, J. (2016) · Journal of Geophysical Research Oceans · doi:10.1002/2016jc012034 · Cited by 8
Chen, C., Zheng, Z., Zeng, L.-F., Fan, X., Tian, L., & Huang, K. (2021) · Journal of Palaeogeography · doi:10.1186/s42501-020-00081-x · Cited by 8
“Post-spreading quaternary basalts from Hainan Island.”
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Jacobson, M. J., Chawchai, S., Scholz, D., Riechelmann, D. F. C., Holmgren, K., Vonhof, H., Wang, X., & Liu, G. (2024) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2024.108597 · Cited by 8
Spatial and temporal distribution of palaeoclimatic records in the Maya Area
Martinez-Dyrzo, H. B. (2024) · Revista Mexicana de Ciencias Geológicas · doi:10.22201/cgeo.20072902e.2024.1.1751 · Cited by 6
Bertaz, J., Liu, Z., Colin, C., Dapoigny, A., Lin, A. T., Li, Y., & Jian, Z. (2024) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004745 · Cited by 7
“…curve received by the earth at 65°N of latitude (Berger, 1978), magnetic susceptibility from Yanchi lake (Y. Li et al., 2017) and Huguang Maar lake (Yancheva et al., 2007), and pollen records from Toushe Basin (west Taiwan) (Sanchez Goñi et al., 2017) and Huguang Maar lake (South China) (Wang et…”
InfluentialWang, L., Zhou, B., Zheng, B., Wang, K., Mei, X., Wang, Q., Wang, X., & Zheng, H. (2021) · Journal of Ocean University of China · doi:10.1007/s11802-021-4651-1 · Cited by 7
“Many significant findings about the nature of abrupt climate changes have been described based on the high-resolution geochemical records obtained by XRF-CS analyses (Lamy et al., 2004; Yancheva et al., 2007; Spofforth et al., 2008; Löwemark et al., 2010; Liang et al., 2012).”
Jonas, A. S., Kars, M. A. C., Bauersachs, T., Ruebsam, W., & Schwark, L. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104173 · Cited by 7
Leipe, C., Lu, J.-C., & Chi, K.-A. (2023) · Archaeological Research in Asia · doi:10.1016/j.ara.2023.100482 · Cited by 7
Sun, Q., Jiang, Z., Xiao, C., Chen, L., Liu, W., He, K., Guan, Y., Zhang, Y., Wang, H., Chen, L., et al. (2024) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004732 · Cited by 7
“…South China (e.g., Ti contents from the Huguangyan Maar Lake, humification degree from the Dahu swamp in the Nanling Mountains) (Figures 4c and 4d) (Yancheva et al., 2007; Zhong et al., 2010), Southwestern China (e.g., lake level of Lake Chenghai, and pollen concentration from Lake Lugu) (Figures…”
BackgroundTang, H., Ye, H., Yang, W., Huang, Y., Sun, T., Ge, Y., Zhang, H.-X., Sun, Y., Lin, S., Liu, Z., et al. (2024) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2024.108798 · Cited by 7
Zheng, Y., Kang, S., Li, J., Yu, S., Lan, M., & Wang, J. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112468 · Cited by 7
The potential of dust detection by means of µXRF scanning in Eifel maar lake sediments
Dietrich, S., & Sirocko, F. (2011) · E&G Quaternary Science Journal · doi:10.3285/eg.60.1.06 · Cited by 7
Zhong, W., Wei, Z., Shang, S., Chen, Y., Ye, S., Tang, X., Zhu, C., Ouyang, J., & Xue, J. (2017) · Boreas · doi:10.1111/bor.12289 · Cited by 6
“Yancheva et al. (2007) reconstructed the strength of the Asian winter monsoon winds over the past 16 000 years using themagnetic properties and the titanium content of sediments fromLakeHuguang in the Leizhou Peninsula.”
BackgroundStrengthening of the East Asian winter monsoon during the mid-Holocene
Tian, Z., & Jiang, D. (2018) · The Holocene · doi:10.1177/0959683618777076 · Cited by 7
“A number of geologic records, including eolian sediments and peat deposits in northwestern China (An, 2000; Jia et al., 2015a; Li and Morrill, 2015; Liu et al., 2013; Yu et al., 2006; Zhao et al., 2016), biogeochemical evidence, fossil diatoms and pollen records in lake sediments from Huguang Maar Lake and Wuhu Lake i…”
BackgroundAbarike, G., Song, Z., Han, Y., Wang, S., Bin, W., & Liu, Y. (2021) · Acta Geochimica · doi:10.1007/s11631-021-00470-6 · Cited by 7
“To date, substantial re-constructional studies of the lake’s sediments have improved the understanding of Holocene climatic evolution, paleoclimate changes, etc (Liu et al. 2000; Mingram et al. 2004; Yancheva et al. 2007, and reference therein).”
BackgroundAmekawa, S., Kashiwagi, K., Hori, M., Sone, T., Katō, H., Okumura, T., Yu, T., Shen, C., & Kano, A. (2021) · Progress in Earth and Planetary Science · doi:10.1186/s40645-021-00409-8 · Cited by 7
“…2013), Northwestern Pacific Ocean (Sagawa et al. 2011), and Japan Sea (Nagashima et al. 2007, 2011), as well as from terrestrial archives (e.g., aeolian sediments from the northwestern Chinese Loess Plateau (Sun et al. 2012) and lake sediments in south China (Chu et al. 2017; Yancheva et al. 2007).”
BackgroundInfluentialLi, D., Xu, X., Liu, X., Cheng, H., Xu, S., & Jiang, X. (2023) · Marine Geology · doi:10.1016/j.margeo.2023.107053 · Cited by 7
Columbu, A., Zhornyak, L. V., Zanchetta, G., Drysdale, R. N., Hellström, J., Isola, I., Regattieri, E., & Fallick, A. E. (2023) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2023.108355 · Cited by 7
Zhang, C., Qiu, Y., Zhi, D., Wang, C., Wang, Y., Liao, Q., & Zou, X. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111958 · Cited by 7
Yang, J., Peng, S., Xu, J., Kong, D., Tsai, H.-L., Chen, M., & Song, Z. (2024) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2024.106030 · Cited by 7
Sone, T., Kano, A., Kashiwagi, K., Mori, T., Okumura, T., Shen, C., & Hori, M. (2015) · Island Arc · doi:10.1111/iar.12118 · Cited by 7
“Climate variability in central China over the last 1270 years revealed by high-resolution stalagmite records.”
BackgroundInfluentialWu, X., Guoxu, L., & Ji, S. (2016) · Journal of Lake Sciences · doi:10.18307/2016.0522 · Cited by 7
Late Holocene coastline and landscape changes to the west of Ephesus, Turkey
Stock, F., Halder, S., Opitz, S., Pint, A., Seren, S., Ladstätter, S., & Brückner, H. (2017) · Quaternary International · doi:10.1016/j.quaint.2017.09.024 · Cited by 7
X-ray fluorescence scanning of discrete samples – An economical perspective
Profe, J., & Ohlendorf, C. (2018) · Quaternary International · doi:10.1016/j.quaint.2018.09.022 · Cited by 7
He, J., Su, Y., & Fang, X. (2020) · Journal of Quaternary Science · doi:10.1002/jqs.3183 · Cited by 7
“…development of human systems is dominated by natural or socioeconomic factors is a challenging topic, and there is no consensus in the available research (Zhang, 1982; Yancheva et al., 2007a,b; Zhang, 2008; Cheng et al., 2010; Fan, 2010; Zhang et al., 2010; Fang et al., 2013; Zheng et al., 2014).”
BackgroundA Rapid Cooling Event Over the Western Pacific Region During the Middle Bronze Age
Xiao, H., Deng, W., Liu, X., Chen, X., Guo, Y., Zhao, J., Zeng, T., & Wei, G. (2020) · Journal of Geophysical Research Oceans · doi:10.1029/2020jc016964 · Cited by 8
Zhang, J., Zhao, K., Kong, X., Wang, Y., Wang, X., Liu, S., Wang, Z., Cheng, H., & Edwards, R. L. (2021) · 气象学报:英文版 · doi:10.1007/s13351-021-0168-1 · Cited by 7
“Based on the analysis of the observations and model results, strong correlations were found between the ENSO/PDO and EASM rainfall in China (Yu, 2013; Yu et al., 2015).”
ResultShang, S., Yang, X., Zhang, E., Wei, R., Zhang, T., & Zhou, Q. (2022) · The Holocene · doi:10.1177/09596836221101250 · Cited by 7
“This long and destructive dry period has been proven to have existed in many studies and historical data (Chu et al., 2002; Yancheva et al., 2007).”
ResultNing, D., Jiang, Q., Ji, M., Zheng, J., Kuai, X., Ge, Y., Xu, Y., Cheng, L., & Zhao, W. (2022) · Paleoceanography and Paleoclimatology · doi:10.1029/2022pa004487 · Cited by 7
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“Comparison of selected high-resolution speleothem, lake, and marine records for the last deglaciation, with the well-known Younger Dryas cold event delineated by the gray bar (from Yancheva et al., 2007).”
BackgroundSelf-citationZhang, J., Liu, S., Liu, D., Kong, X., & Fang, Y. (2019) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2019.103884 · Cited by 7
Variations in upper water structure during MIS 3 from the western South China Sea
Du, J., & Huang, B. (2009) · Chinese Science Bulletin · doi:10.1007/s11434-009-0388-8 · Cited by 7
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Reply to the comment of Cheng et al.
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Tang, L., Wang, Y. P., Liu, S., Wang, F., Wang, J., Li, J., & Liu, C. (2025) · Paleoceanography and Paleoclimatology · doi:10.1029/2025pa005260 · Cited by 6
“During 8.4–6.6 and 5–4.4 cal kyr BP, weakened East Asian winter monsoon intensity, reduced snow/ice cover over the Tibetan Plateau, and enhanced EASM precipitation occurred concurrently (Dong et al., 2015; Walczak et al., 2020; Y. Wang et al., 2005; Yancheva et al., 2007).”
InfluentialInternational Ocean Discovery Program Expedition 353 Preliminary Report
Clemens, S. C., Wolfgang, K., LeVay, L. J., & Scientists, T. E. (2014) · Scientific prospectus · doi:10.14379/iodp.sp.353.2014 · Cited by 6
Different types of Anthropocene signals recorded in Huguangyan Maar Lake over the past 450 years
Jiang, S., Zhou, X., Ma, L., Cui, S., Liu, X., Liu, X., Chen, A., Luo, Y., Xu, L., Zeng, F., et al. (2024) · CATENA · doi:10.1016/j.catena.2024.108562 · Cited by 6
Zhong, W., Xiaowen, T., Shang, S., Zhiqiang, W., Chen, Y., Quan, M., & Li, T. (2021) · Near Surface Geophysics · doi:10.1002/nsg.12175 · Cited by 6
Lyu, W., Fu, T., Hu, Z., Tang, Y. Z., Chen, G., Xu, X., Chen, Y., & Chen, S. (2021) · Frontiers in Earth Science · doi:10.3389/feart.2021.689508 · Cited by 6
“Frontiers in Earth Science | www.frontiersin.org August 2021 | Volume 9 | Article 6895082 2006; Yancheva et al., 2007; Zhang and Lu, 2007; Zhou and Zhao, 2009; Steinke et al., 2011; Ge et al., 2017), although antiphase correlation has been identified on orbital timescales (Ding et al., 1995).”
BackgroundMethodResultInfluentialWen, Q., Yan, M., Liu, Z., & Liu, J. (2022) · Geophysical Research Letters · doi:10.1029/2022gl098865 · Cited by 6
“The reliability of the titanium record from the HML as an indicator of the EAWM (Yancheva et al., 2007) has also been questioned.”
BackgroundInfluentialSelf-citationJiang, S., Zhou, X., Ding, M., Tu, L., Liu, X., Luo, W., Zhang, J., & Shen, Y. (2022) · 中国科学通报:英文版 · doi:10.1016/j.scib.2022.09.027 · Cited by 6
Qiu, J., Jin, J., Wang, X., Wei, C., Zuo, X., & Wei, J. (2022) · The Holocene · doi:10.1177/09596836221126126 · Cited by 6
“North-easterly winds prevail on the island, and wind power is controlled by changes in the East Asian winter monsoon, which is mainly affected by the Intertropical Convergence Zone (ITCZ) (Chen et al., 2016; Yancheva et al., 2007).”
BackgroundImpacts of seismic activity and climatic change on Chinese history in the recent millennium
Fan, J., Jiang, H., Xu, H., & Zhang, W. (2022) · Journal of Geographical Sciences · doi:10.1007/s11442-022-2050-1 · Cited by 6
“…Zhang et al., 2021a), population migration and wars (including peasant uprising) (Ye et al., 2004; Chen, 2015; Lee et al., 2017; Chen et al., 2019a; Mao et al., 2021; Yang et al., 2021; Zhang et al., 2021b) and dynasty alteration (Yancheva et al., 2007; Büntgen et al., 2016; Liu et al., 2018).”
BackgroundOxygen isotopes of the Japanese stalagmites as global and local paleoclimate proxies
Kano, A., Katō, H., & Murata, A. (2023) · Island Arc · doi:10.1111/iar.12491 · Cited by 6
“7.0 ‰ (Sone et al., 2013); its profile resembles that of the intensity of the East Asian winter monsoon (EAWM) reported from the loess-paleosol sequences of western China (Maher & Mengyu, 2006) and lake sediments of southern China (Yancheva et al., 2007).”
BackgroundInfluentialYan, J., Guo, X.-P., He, M., Niu, Z., Xu, M., Peng, B., Yang, Y., & Jin, Z. (2023) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2023.168392 · Cited by 6
Lan, H., Yoshimura, K., & Liu, Z. (2023) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004692 · Cited by 6
“…have suggested that precipitation in the EAM region is largely controlled by the meridional migration of the ITCZ, with less summer precipitation when the ITCZ migrates southward during cold periods in the Northern Hemisphere (Schneider et al., 2014; Timmermann et al., 2007; Yancheva et al., 2007).”
BackgroundLi, X., Liu, S., Hou, J., Sun, Z., Wang, M., Hou, X., Liu, M., Yan, J., & Zhang, L. (2023) · Frontiers of Earth Science · doi:10.1007/s11707-022-1082-2 · Cited by 6
“An investigation of alkaline lake sediments from cold regions in China has verified a warm-season bias in brGDGTs production (Dang et al., 2018), which is consistent with numerous other studies indicating a bias toward the warm months in mid-to high-latitude lakes (Sun et al., 2011; Shanahan et al., 2013; Foster et al…”
InfluentialZhong, W., Ma, Q., Xue, J., Zheng, Y., Cai, Y., Ouyang, Y., & Yu, X. (2011) · Geochemistry International · doi:10.1134/s0016702911040094 · Cited by 6
“In the tropi� cal Leizhou Peninsula in South China, the climatic record recovered from Lake Huguangyan Maar also suggested an enhanced summer monsoon during ca. 11000~7500 cal yr B.P [ 38 ], the pollen percentage of tropical trees reached a maximum at 9500~8000 cal yr B.P, reflecting a hot and wet climatic optimum for…”
BackgroundLi, Y., Wang, N., Zhang, C., & Wang, Y. (2014) · Journal of Arid Land · doi:10.1007/s40333-014-0064-y · Cited by 6
“…Received 2013-09-24; revised 2013-10-25; accepted 2013-11-27 © Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Science Press and Springer-Verlag Berlin Heidelberg 2014 et al., 2006; Yancheva et al., 2007; Mischke et al., 2008; Cai et al., 2010; Wang et al., 2012).”
BackgroundSeim, A., Schultz, J., Beck, C., Bräuning, A., Krusic, P. J., Leland, C., Byambasuren, O., Liang, E., Wang, X., Jeong, J., et al. (2018) · Journal of Climate · doi:10.1175/jcli-d-17-0164.1 · Cited by 6
Surface Ocean Hydrographic Changes in the Western Pacific Marginal Seas Since the Early Holocene
Pan, H.-J., Chen, M., Kong, D., Lin, X., Wong, K.-T., Tsai, H.-L., Liu, S., Shi, X., & Yokoyama, Y. (2020) · Frontiers in Earth Science · doi:10.3389/feart.2020.00200 · Cited by 6
Zhang, J., Tomczak, M., Witkowski, A., Liang, K., Harff, J., Li, C., & Wang, B. (2020) · Marine Geology · doi:10.1016/j.margeo.2020.106395 · Cited by 6
Ning, D., Jiang, Q., Ji, M., Xu, Y., Kuai, X., Ge, Y., & Zhao, W. (2021) · Journal of Quaternary Science · doi:10.1002/jqs.3383 · Cited by 6
“On the one hand, higher values could result from stronger catchment runoff, hence indicating wetter conditions (Haug et al., 2001; Sun et al., 2020); on the other, higher values could also derive from enhanced aolian deposition, suggesting drier conditions (Yancheva et al., 2007).”
BackgroundWang, B., Zhong, W., Zhu, C., Ouyang, J., Wei, Z., & Shang, S. (2022) · Chinese Geographical Science · doi:10.1007/s11769-022-1282-4 · Cited by 6
“…Yang et al., 2006; Xu et al., 2010) and increased contents of immobile and resistant elements (for example Al2O3, TiO2, FeOt, MnO, Cu and Rb) (Yancheva et al., 2007; Sun et al., 2010; Wu et al., 2011; Babeesh et al., 2017) corresponded to the warm and humid periods, whereas under dry and…”
BackgroundKato, H., Mori, T., Amekawa, S., Wu, C.-C., Shen, C.-C., & Kano, A. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121390 · Cited by 6
Ahmad, S., Nishii, K., TAMURA, T., Ohta, T., Ikoma, E., Kitsuregawa, M., & Koike, T. (2012) · Journal of Japan Society of Civil Engineers Ser B1 (Hydraulic Engineering) · doi:10.2208/jscejhe.68.i_157 · Cited by 6
Rosen, A. M. (2007) · Cited by 6
Shinozaki, T., Uchida, M., Minoura, K., Kondo, M., Rella, S., & Shibata, Y. (2011) · doi:10.5194/cpd-7-2159-2011 · Cited by 6
“4b) (Hastenrath and Greischar, 1993; Yancheva et al., 2007).”
Asian monsoon over mainland Southeast Asia in the past 25 000 years
Chabangborn, A. (2014) · KTH Publication Database DiVA (KTH Royal Institute of Technology) · Cited by 6
Damette, O., & Goutte, S. (2023) · Journal of Comparative Economics · doi:10.1016/j.jce.2022.09.005 · Cited by 5
Guo, M., Han, Y., Liu, W., Cao, Y., Lei, D., Jiang, H., Zhou, W., & An, Z. (2024) · Applied Geochemistry · doi:10.1016/j.apgeochem.2024.105950 · Cited by 5
Mid-to-late Holocene temperature variability in southwestern China
Zhong, H., Zhang, C., Sun, J., Xia, Z., Yu, Z., & Zhao, C. (2025) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2025.109231 · Cited by 5
Qian, F., Chang, F., Nürnberg, D., Zhang, S., Wang, Y., Zhang, J., Tang, L., & Li, T. (2024) · Geological Magazine · doi:10.1017/s0016756824000177 · Cited by 5
“2001; Yancheva et al .”
Bae, J. W., Sohn, E., Kang, H., Lee, J.-C., & Song, K. (2015) · Macromolecular Research · doi:10.1007/s13233-015-3062-9 · Cited by 5
Japanese wave-dominated coasts as palaeoenvironmental records
Tamura, T. (2018) · The Quaternary Research (Daiyonki-Kenkyu) · doi:10.4116/jaqua.57.197 · Cited by 5
Zhang, Z., & Ruan, J. (2020) · International Journal of Environmental Research and Public Health · doi:10.3390/ijerph17207422 · Cited by 6
“Our article extends the understandings of the linkages among long-run natural disaster and human capital to agricultural channels based on empirical evidences from China, Chinese people have suffered from severe famine, plague, poverty [5,6] and social-system turmoil [13,14], mainly due to reductions in food productio…”
BackgroundYin, J., Wang, Z., Wu, X., Tang, W., Li, J., Lan, G., & Cheng, H. (2025) · Global and Planetary Change · doi:10.1016/j.gloplacha.2025.104834 · Cited by 5
Crop Yield and Temperature Changes in North China during 601–900 AD
Liu, H., Ge, Q., Zheng, J., Hao, Z., & Zhang, X. (2014) · Advances in Meteorology · doi:10.1155/2014/137803 · Cited by 5
Xu, Z., Chang, F., Li, T., Nan, Q., Jiang, F., & Li, A. (2013) · Marine Geology & Quaternary Geology · doi:10.3724/sp.j.1140.2012.04073 · Cited by 5
Wu, X., & Ji, S. (2012) · Journal of Lake Sciences · doi:10.18307/2012.0618 · Cited by 5
Wu, X., Wang, Y., Bian, L., & Shen, J. (2016) · Geophysical Journal International · doi:10.1093/gji/ggw223 · Cited by 5
Chawchai, S., Chabangborn, A., Kylander, M. E., Löwemark, L., Mörth, C., Blaauw, M., Klubseang, W., Reimer, P. J., Fritz, S. C., & Wohlfarth, B. (2013) · Lincoln (University of Nebraska) · Cited by 5
Chen, J., Nan, Q., Li, T., Sun, R., Sun, H., & Lu, J. (2019) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2019.103912 · Cited by 5
Asian Winter Monsoon Imprint on the Water Column Structure at the Northern South China Sea Coast
Zhang, Y., Zhu, K., Huang, C., Kong, D., He, Y., Wang, H., Liu, W., Xie, Z., Wei, G., & Liu, Z. (2021) · Frontiers in Earth Science · doi:10.3389/feart.2021.680180 · Cited by 5
“Regardless, variations in Frontiers in Earth Science | www.frontiersin.org August 2021 | Volume 9 | Article 6801805 winter AMC strength, as inferred from both magnetic susceptibility at Huguangyan Maar Lake (Yancheva et al., 2007) (Figure 4H), the UK′37 SST record and wind-borne hopane contents at site YJ, are strongl…”
BackgroundInfluential
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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