Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period.

By T. Blunier, E. Brook. Science, 2001

1,212 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/5834290841d3668d0af302387df37c4a98ff361d

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Citations in the corpus

Precise dating of Dansgaard–Oeschger climate oscillations in western Europe from stalagmite data (2003, background): “jpg" NDATA ITEM> ]> The signature of Dansgaard–Oeschger events—millennial-scale abrupt climate oscillations during the last glacial period—is well established in ice cores and marine record”
New modeling of the Vostok ice flow line and implication for the glaciological chronology of the Vostok ice core (2004, methodology): “Comparison of Vostok isotopic record, dated either with the GT4 chronology or with the new chronology, and Byrd isotopic record dated by comparison to GISP2 via methane [ Blunier and Brook , 2001]. chronological tie points.”
Climate Response to External Sources of Freshwater: North Atlantic versus the Southern Ocean (2007, background): “Using proxy temperature estimates derived from ice cores, a number of authors have found such a bipolar seesaw and have noted an out-of-phase temperature anomaly relationship between Greenland and the Antarctic (e.g., Blunier and Brook 2001 ).”
Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling (2018, background): “, 1994), in particular the fast global variations in atmospheric methane that accompany DO transitions (Blunier et al., 1998; Blunier and Brook, 2001).”
Did Humans Cause the Late Pleistocene-Early Holocene Mammalian Extinctions in South America in a Context of Shrinking Open Areas? (2009, background): “During the shorter interglacial periods, when temperatures were higher than present (Thompson, 2000; Blunier and Brook, 2001; Vivo and Carmignotto, 2004), an expansion of the forested areas may be expected, and with this an increase in the biomass of forest dwelling animals, including those that…”
Marine isotope stage 3 sea level fluctuations: Data synthesis and new outlook (2008, methodology): “[1998] and Blunier and Brook [2001] synchronized ice core records from Antarctica and Greenland using variations in the concentration of atmospheric methane (a globally well-mixed gas) in air bubbles enclosed within the ice. This work showed that D-O events in Greenland correspond to at least four s”
The role of the thermohaline circulation in abrupt climate change (2002, background): “2e ), while contemporaneous warming observed in some regions of the Southern Hemispher”
Isotope calibrated Greenland temperature record over Marine Isotope Stage 3 and its relation to CH4 (2006, methodology): “6, black line), this reduction is consistent with findings of Cuffey and Clow [38] who obtained lower accumulation rates for GISP2 compared to GRIP and NorthGRIP during the glacial times.”
The last deglaciation: timing the bipolar seesaw (2011, methodology): “…broader Antarctic region, we construct a δ 18 O ice composite from the LD record and records from other high-accumulation/near-coastal sites: Byrd (Blunier and Brook, 2001), Siple Dome (Brook et al., 2005), Talos Dome (Stenni et al., 2011; Buiron et al., 2011), and EPICA Dronning Maud Land…”
Dansgaard‐Oeschger oscillations predicted in a comprehensive model of glacial climate: A “kicked” salt oscillator in the Atlantic (2014, neutral): “…information from the Greenland and Antarctic ice sheets led to the recognition of a “bipolar seesaw” relationship between climate variability in the Northern and Southern Hemispheres [Broecker, 1998; Blunier and Brook, 2001; Morgan et al., 2002; Stocker and Johnsen, 2003; Barbante et al., 2006].”
Biological oxygen productivity during the last 60,000 years from triple oxygen isotope measurements (2002, background): “]. (d) Composite record of atmospheric CH4 from Greenland Ice Core Project (GRIP) and GISP2 ice cores, Greenland [”
High-resolution carbon dioxide concentration record 650,000–800,000 years before present (2008, methodology): “These variations are concomitant to the larger of the Antarctic Isotope Maximum (AIM) events (Antarctic warming events with an amplitude of 1–3 u C) 7,16,17 .”