Orbitally driven insolation forcing on Holocene climate trends: Evidence from alkenone data and climate modeling

By S. Lorenz, Jung-Hyun Kim, N. Rimbu, R. Schneider, Gerrit Lohmann. 2006

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Equatorial insolation: from precession harmonics to eccentricity frequencies (2006, unknown): “…and minimum arising in the tropical regions in the course of one year, which is at the origin of the 100 and 5.5 kyr cycles might explain some of the important features of the climate system and environment over the Pleistocene and the Holocene, like it is suggested also by Lorenz et al. (2006)”
Global characterization of the Holocene Thermal Maximum (2012, background): “However, most tropical alkenone SST records (Rimbu et al., 2004; Lorenz et al., 2006) suggest a warming trend over the entire Holocene and cooler than present conditions between 9 and 6 ka BP, although there are some notable exceptions (e.g., Kim et al., 2003).”
Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, background): “…models to understand the Late Quaternary climate evolution and its relation to slowly-varying boundary conditions (Jackson and Broccoli, 2003; Felis et al., 2004; Lorenz and Lohmann, 2004; Charbit et al., 2005; Tuenter et al., 2005; Renssen et al., 2005; Lorenz et al., 2006; * Corresponding author.”