15 citations as recorded by crossref.

1. Mending Milankovitch's theory: obliquity amplification by surface feedbacks C. Tabor et al. 10.5194/cp-10-41-2014
2. Iceberg discharge events in the northwest Pacific and related sequence of Kamchatka glaciations over the last 190 kyr S. Gorbarenko et al. 10.1016/j.quascirev.2021.107349
3. Abiotic and biotic responses to Milankovitch-forced megamonsoon and glacial cycles recorded in South China at the end of the Late Paleozoic Ice Age Q. Fang et al. 10.1016/j.gloplacha.2018.01.022
4. How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations C. Van Meerbeeck et al. 10.5194/cp-5-33-2009
5. Modeling Obliquity and CO2 Effects on Southern Hemisphere Climate during the Past 408 ka* A. Timmermann et al. 10.1175/JCLI-D-13-00311.1
6. Time scale evaluation and the quantification of obliquity forcing C. Zeeden et al. 10.1016/j.quascirev.2019.01.018
7. Coupled Impacts of Atmospheric Circulation and Sea‐Ice on Late Pleistocene Terrigenous Sediment Dynamics in the Subarctic Pacific Ocean Y. Zhong et al. 10.1029/2021GL095312
8. Obliquity and precessional forcing of continental snow fall and melt: implications for orbital forcing of Pleistocene ice ages S. Lee & C. Poulsen 10.1016/j.quascirev.2009.06.002
9. Evolution of nutricline dynamics in the equatorial Pacific during the late Pliocene C. Bolton et al. 10.1029/2009PA001821
10. How obliquity cycles powered early Pleistocene global ice‐volume variability C. Tabor et al. 10.1002/2015GL063322
11. Pliocene‐Pleistocene evolution of sea surface and intermediate water temperatures from the southwest Pacific E. McClymont et al. 10.1002/2016PA002954
12. Oscillations of global sea-level elevation during the Paleogene correspond to 1.2-Myr amplitude modulation of orbital obliquity cycles Y. Liu et al. 10.1016/j.epsl.2019.06.023
13. Orbital Influences on Conditions Favorable for Glacial Inception G. O'Neill & A. Broccoli 10.1029/2021GL094290
14. Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial–interglacial cycles R. Uemura et al. 10.5194/cp-8-1109-2012
15. The Contribution of Radiative Feedbacks to Orbitally Driven Climate Change M. Erb et al. 10.1175/JCLI-D-12-00419.1