G
Gerald H. Haug
Researcher at Max Planck Society
Publications - 198
Citations - 20379
Gerald H. Haug is an academic researcher from Max Planck Society. The author has contributed to research in topics: Glacial period & Holocene. The author has an hindex of 60, co-authored 184 publications receiving 17516 citations. Previous affiliations of Gerald H. Haug include ETH Zurich & Woods Hole Oceanographic Institution.
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Southward Migration of the Intertropical Convergence Zone Through the Holocene
TL;DR: The Cariaco Basin record exhibits strong correlations with climate records from distant regions, including the high-latitude Northern Hemisphere, providing evidence for global teleconnections among regional climates.
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Migrations and dynamics of the intertropical convergence zone
TL;DR: An emerging framework links the intertropical convergence zone to the atmospheric energy balance and may account for ITCZ variations on timescales from years to geological epochs.
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Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.
TL;DR: Sedimentary time series of color reflectance and major element chemistry from the anoxic Cariaco Basin off the coast of northern Venezuela record large and abrupt shifts in the hydrologic cycle of the tropical Atlantic during the past 90,000 years, which supports the notion that tropical feedbacks played an important role in modulating global climate during the last glacial period.
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Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation
Gerald H. Haug,Ralf Tiedemann +1 more
TL;DR: In this paper, stable-isotope and carbonate sand-fraction records from Caribbean sediments were used to investigate the timing and consequences of the emergence of the Isthmus of Panama, which closed the seaway between the North andSouth American continents.
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Influence of the intertropical convergence zone on the East Asian monsoon
Gergana Yancheva,Norbert R. Nowaczyk,Jens Mingram,Peter Dulski,Georg Schettler,Jörg F. W. Negendank,Jiaqi Liu,Daniel M. Sigman,Larry C. Peterson,Gerald H. Haug +9 more
TL;DR: 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 are presented, using as proxies for the strength of the winter monsoon winds, to 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.