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
East Asian Monsoon Signals Reflected in Temperature and Precipitation Changes over the Past 300 Years in the Middle and Lower Reaches of the Yangtze River
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“Higher summer insolation in India with an increase in the Indian Ocean Sea Surface Temperature (SST) shifted the ITCZ to northern latitudes (Peterson and Haug, 2006; Yancheva et al., 2007; Roy and Singhvi, 2016), bringing in more summer precipitation during latest Pleistocene and Pleistocene–Holocene transition.”
Background
Strata sequence and paleochannel response to tectonic, sea-level, and Asian monsoon variability since the late Pleistocene in the South Yellow Sea
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“1a; Yancheva et al., 2007), which has made a great contribution to the local circulation development (Fig.”
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A detailed East Asian monsoon history of Greenland Interstadial 21 in southeastern China
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Enhanced aridity in the source region of the Yangtze River since 5.8 ka revealed by the sediments of Saiyong Co
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“, 2001; Maher and Possolo, 2013) and winter monsoon strength (Yancheva et al., 2007).”
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“A southward shift of the ITCZ results in weakened southeasterly cross-equatorial trade winds south of the equator, and thus results in awarming of the cold tongue in the EEP via reduced upwelling and wind-evaporation.”
BackgroundInfluential
Yancheva et al. reply
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. (2007) · Nature · doi:10.1038/nature06339 · Cited by 10
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Pacific Walker Circulation modulated millennial-scale East Asian summer monsoon rainfall variability over the past 40 kyr
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“During the past three decades, EASM changes have been revealed by climate proxy records from lake sediments (F. H. Chen et al., 2015; J. Liu et al., 2021; Yancheva et al., 2007), caves (speleothem oxygen isotopes) (Cheng et al.”
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Chemical weathering evidence for East Asian Summer Monsoon rainfall variability in the upper reaches of the Yellow River since the Early Pleistocene
Li, B., Feng, Q., Wang, F., Li, Z., Wang, X., Li, R., & Chen, W. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111523 · Cited by 10
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“In recent years many papers have been published about Holocene environmental and climatic changes in the Asian monsoon domain (e.g. Thompson et al. 1997; Wang et al. 1999, 2005a, b; Fleitmann et al. 2003; Yuan et al. 2004; Yancheva et al. 2007).”
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High-resolution geochemical (μXRF) and palynological analyses for climatic and environmental changes in lake sediments from Sultansazlığı Marsh (Central Anatolia) during the last 14.5 kyr
Şenkul, Ç., Gürboğa, Ş., Doğan, M., & Doğan, T. (2021) · Quaternary International · doi:10.1016/j.quaint.2021.08.010 · Cited by 11
Paleomagnetic Secular Variation and Relative Paleointensity During the Holocene in South China—Huguangyan Maar Lake Revisited
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“In particular, their cores were retrieved from SWmargin of the lake, where the lake floor is almost steepest, as revealed by previous bathymetric measurements (Yancheva et al., 2007).”
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Study of the relationship between the intertropical convergence zone expansion and the precipitation in the southern half of Iran
Jafari, M., & Lashkari, H. (2020) · Journal of Atmospheric and Solar-Terrestrial Physics · doi:10.1016/j.jastp.2020.105439 · Cited by 10
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Climatic Oscillations and Dynastic Trends: A Multiproxy analysis of the past two millennia in the Indian Subcontinent
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Spatial variation of East Asian winter monsoon evolution between northern and southern China since the last glacial maximum
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Background
A 17 ka multi‐proxy paleoclimatic record on the northeastern Tibetan Plateau: implications for the northernmost boundary of the Asian summer monsoon during the Holocene
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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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