The DOI matches its Crossref record; 30 of the 30 references it cites were found in a registry or an index.
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]
Citations
Cites
A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China
Wang, Y., Cheng, H., Edwards, R. L., An, Z., Wu, J., Shen, C., & Dorale, J. A. (2001) · Science · doi:10.1126/science.1064618 · Cited by 3,218
Southward Migration of the Intertropical Convergence Zone Through the Holocene
Haug, G. H., Hughen, K. A., Sigman, D. M., Peterson, L. C., & Röhl, U. (2001) · Science · doi:10.1126/science.1059725 · Cited by 2,442
Self-citationDykoski, C. A., Edwards, R., Cheng, H., Yuan, D., Cai, Y., Zhang, M.-L., Lin, Y.-S., Qing, J.-M., An, Z., & Revenaugh, J. (2003) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.01.036 · Cited by 1,929
Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman
Fleitmann, D., Burns, S. J., Manfred Mudelsee, A., Neff, U., Kramers, J., Mangini, A., & Matter, A. (2003) · Science · doi:10.1126/science.1083130 · Cited by 1,724
On the Weakening Relationship Between the Indian Monsoon and ENSO
Kumar, K., Rajagopalan, B., & Cane, M. A. (1999) · Science · doi:10.1126/science.284.5423.2156 · Cited by 1,618
Correlation between climate events in the North Atlantic and China during the last glaciation
Porter, S. C., & An, Z. (1995) · Nature · doi:10.1038/375305a0 · Cited by 1,272
Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon
Yuan, D., Cheng, H., Edwards, R. L., Dykoski, C. A., Kelly, M. J., Zhang, M., Qing, J., Lin, Y., Wang, Y., Wu, J., et al. (2004) · Science · doi:10.1126/science.1091220 · Cited by 1,255
Cultural Responses to Climate Change During the Late Holocene
deMenocal, P. B. (2001) · Science · doi:10.1126/science.1059827 · Cited by 1,202
Tropical Climate Instability: The Last Glacial Cycle from a Qinghai-Tibetan Ice Core
Thompson, L. G., Yao, T., Davis, M. E., Henderson, K. A., Mosley‐Thompson, E., Lin, P., Beer, J., Synal, H., Cole‐Dai, J., & Bolzan, J. F. (1997) · Science · doi:10.1126/science.276.5320.1821 · Cited by 1,122
Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies
Wang, X., Auler, A. S., Edwards, R. L., Cheng, H., Cristalli, P. D. S., Smart, P. L., Richards, D. A., & Shen, C. (2004) · Nature · doi:10.1038/nature03067 · Cited by 912
Climate and the Collapse of Maya Civilization
Haug, G. H., Günther, D., Peterson, L. C., Sigman, D. M., Hughen, K. A., & Aeschlimann, B. (2003) · Science · doi:10.1126/science.1080444 · Cited by 783
Self-citationWang, L., Sarnthein, M., Erlenkeuser, H., Grimalt, J. O., Grootes, P. M., Heilig, S., Ivanova, E., Kienast, M., Pelejero, C., & Pflaumann, U. (1999) · Marine Geology · doi:10.1016/s0025-3227(98)00182-0 · Cited by 754
Bloemendal, J., King, J. W., Hall, F. R., & Doh, S. (1992) · Journal of Geophysical Research Atmospheres · doi:10.1029/91jb03068 · Cited by 628
CHINESE LOESS AND THE PALEOMONSOON
Liu, T., & Ding, Z. (1998) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.26.1.111 · Cited by 626
Solar Forcing of Drought Frequency in the Maya Lowlands
Hodell, D. A., Brenner, M., Curtis, J. H., & Guilderson, T. P. (2001) · Science · doi:10.1126/science.1057759 · Cited by 569
El Niño-Like Pattern in Ice Age Tropical Pacific Sea Surface Temperature
Koutavas, A., Lynch‐Stieglitz, J., Marchitto, T. M., & Sachs, J. P. (2002) · Science · doi:10.1126/science.1072376 · Cited by 555
Rapid climate changes in the tropical Atlantic region during the last deglaciation
Hughen, K. A., Overpeck, J. T., Peterson, L. C., & Trumbore, S. E. (1996) · Nature · doi:10.1038/380051a0 · Cited by 531
Self-citationWang, B. (2006) · Medical Entomology and Zoology · Cited by 516
Wang, B. (2006) · Springer eBooks · doi:10.1007/3-540-37722-0 · Cited by 500
The evolution of El Niño, past and future
Cane, M. A. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.12.003 · Cited by 412
Sirocko, F., Garbe‐Schönberg, D., McIntyre, A., & Molfino, B. (1996) · Science · doi:10.1126/science.272.5261.526 · Cited by 317
Circulation mechanisms related to northeast Brazil rainfall anomalies
HASTENRATH, S. L., & Greischar, L. L. (1993) · Journal of Geophysical Research Atmospheres · doi:10.1029/92jd02646 · Cited by 249
Variations in tropical convection as an amplifier of global climate change at the millennial scale
Ivanochko, T., Ganeshram, R. S., Brummer, G.-J. A., Ganssen, G. M., Jung, S., Moreton, S. G., & Kroon, D. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.04.002 · Cited by 214
Oppo, D. W., & Sun, Y. (2005) · Geology · doi:10.1130/g21867.1 · Cited by 168
A coupled environmental system formed at about 2.5 Ma in East Asia
Zhongli, D., Rutter, N. W., Jingtai, H., & Tungsheng, L. (1992) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/0031-0182(92)90120-t · Cited by 145
Floods, famines, and emperors: El Nino and the fate of civilizations
(1999) · Choice Reviews Online · doi:10.5860/choice.36-6298 · Cited by 110
Mingram, J., Schettler, G., Nowaczyk, N. R., Luo, X., Lü, H., Liu, J., & Negendank, J. F. W. (2004) · Quaternary International · doi:10.1016/j.quaint.2004.02.001 · Cited by 109
Self-citationHolocene variations in Asian monsoon moisture: A bidecadal sediment record from the South China Sea
Wang, L., Sarnthein, M., Erlenkeuser, H., Grootes, P. M., Grimalt, J. O., Pelejero, C., & Linck, G. (1999) · Geophysical Research Letters · doi:10.1029/1999gl900443 · Cited by 106
Heslop, D., Shaw, J., Bloemendal, J., Chen, F., Wang, J., & Parker, E. (1999) · Physics and Chemistry of the Earth Part A Solid Earth and Geodesy · doi:10.1016/s1464-1895(99)00115-5 · Cited by 37
(1999) · Choice Reviews Online · doi:10.5860/choice.36-4250 · Cited by 34
Research works printed but not linked: 1
- Diamond, J. Collapse (Penguin, London, 2005)
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“The collapse of the Tang Dynasty (907) coincided with the terminal collapse of the Maya (A), both of which occurred when the Pacific Ocean altered rainfall patterns in both hemispheres (79).”
BackgroundInfluentialSocial and economic impacts of climate
Carleton, T. A., & Hsiang, S. M. (2016) · Science · doi:10.1126/science.aad9837 · Cited by 1,348
A Test of Climate, Sun, and Culture Relationships from an 1810-Year Chinese Cave Record
Zhang, P., Cheng, H., Edwards, R. L., Chen, F., Wang, Y., Yang, X., Liu, J., Tan, M., Wang, X., Liu, J., et al. (2008) · Science · doi:10.1126/science.1163965 · Cited by 1,114
Self-citationStructure and origin of Holocene cold events
Wanner, H., Solomina, O. N., Grosjean, M., Ritz, S. P., & Jetel, M. (2011) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2011.07.010 · Cited by 907
“…component) Lake sediment core Lake Victoria 0.08 32.8 39 Stager et al. (2002) 17 Ti (1/s) Lake sediment core Lake Huguang Maar, China 22.5 110.28 1 Yancheva et al. (2007) 18 Annual mean precipitation (mm/yr) Lake sediment core Lake Bajkal 52.78 108.12 130 Tarasov et al. (2009) 19 Precipitation…”
BackgroundInfluentialGlobal climate evolution during the last deglaciation
Clark, P. U., Shakun, J. D., Baker, P. A., Bartlein, P. J., Brewer, S., Brook, E. J., Carlson, A. E., Cheng, H., Kaufman, D. S., Liu, Z., et al. (2012) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1116619109 · Cited by 667
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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