Isotope calibrated Greenland temperature record over Marine Isotope Stage 3 and its relation to CH4

By C. Huber, M. Leuenberger, R. Spahni, J. Flückiger, J. Schwander, T. Stocker, S. Johnsen, A. Landais, J. Jouzel. 2006

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Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing (2013, methodology): “…time series of simulated northeastern Greenland air temperature anomalies (40◦ W–10◦ E, 66–85◦ N) compared to the NGRIP temperature reconstruction (Huber et al., 2006); simulated SST in the western Mediterranean compared to alkenone-based SST reconstructions from the Alboran Sea ODP hole…”
Dansgaard‐Oeschger oscillations predicted in a comprehensive model of glacial climate: A “kicked” salt oscillator in the Atlantic (2014, neutral): “…between observationally inferred and model-predicted atmospheric temperature variations at the locations of the NGRIP and EDML (European Project for Ice Coring in Antarctica (EPICA) Dronning Maud Land) ice cores on Greenland and Antarctica, respectively [Huber et al., 2006; Stenni et al., 2010].”
Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling (2018, neutral): “1a (Severinghaus et al. 1998; Huber et al. 2006; Kindler et al. 2014).”
Marine isotope stage 3 sea level fluctuations: Data synthesis and new outlook (2008, background): “…records of high-latitude Northern Hemisphere temperature reveal a distinctive pattern of repeated decadal-scale warming events of 8 –15 C during MIS 3, known as Dansgaard-Oeschger (D-O) events [e.g., Blunier et al., 1998; Stuiver and Grootes, 2000; Blunier and Brook, 2001; Huber et al., 2006].”