Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.

By L. Peterson, G. Haug, K. Hughen, U. Röhl. Science, 2000

928 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Paleontology

View Paper: https://www.semanticscholar.org/paper/8150fe04fb2501bc0864223811de1aa000ca8730

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Citations in the corpus

Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, background): “In agreement with paleo-proxies, drier conditions prevailed duringH1 in Europe (Peyron et al., 2005), the northern part of Africa (Peck et al., 2004;Williams et al., 2006; Lambet al., 2007; Niedermeyer et al., 2009), theMiddle East (Bar-Matthews et al., 2003; Vaks et al., 2003; Shakun et al., 2007; ”
X‐ray fluorescence core scanning of wet marine sediments: methods to improve quality and reproducibility of high‐resolution paleoenvironmental records (2012, neutral): “…to be a fast and convenient tool for a wide variety of research topics such as sedimentological and paleoceanographic studies (e.g., Labeyrie 2000; Peterson et al. 2000; Arz et al. 2003; Jaccard et al. 2005; Thomson et al. 2006; Tjallingii et al. 2010), turbidites (Rothwell et al. 2006), and…”
The emerging field of geogenomics: Constraining geological problems with genetic data (2014, background): “…northern hemisphere cold events were dry in northern South America, the tropics south of the equator were wet (no evidence of an east–west dipole) (Peterson et al., 2000; Cruz et al., 2005; Wang et al., 2006; Fritz et al., 2010; Kanner et al., 2012; Mosblech et al., 2012; Cheng et al., 2013).”
Changes in North Atlantic deep-water formation associated with the Dansgaard–Oeschger temperature oscillations (60–10 ka) (2002, background): “These can be observed at high and low latitudes e.g. (Sachs and Lehman, 1999; Peterson et al., 2000) and in the South Atlantic, Indian and Pacific Ocean (Behl and Kenneth, 1996; Schulz et al., 1998; Ninnemann et al., 1999; Kiefer et al., 2001).”
The role of the thermohaline circulation in abrupt climate change (2002, background): “, (2) the position of the Intertropical Convergence Zone, with attendant effects on water vapour transport for the Atlantic to the Pacific basi”
The influence of a weakening of the atlantic meridional overturning circulation on ENSO (2006, background): “is associated with an intensification of the northeasterly trade winds, pushing the Atlantic intertropical convergence zone (ITCZ) southward, as documented by paleo-proxy data (Peterson et al. 2000) and climate model simulations (Dong and Sutton 2002; Dahl et al.”