Articles | Volume 7, issue 1
https://doi.org/10.5194/cp-7-249-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model
Related subject area
Subject: Climate Modelling | Archive: Modelling only | Timescale: Pre-Cenozoic
Climate and ocean circulation in the aftermath of a Marinoan snowball Earth
The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity
Paleogeographic controls on the evolution of Late Cretaceous ocean circulation
Clim. Past, 18, 759–774,
2022Clim. Past, 16, 2095–2123,
2020Clim. Past, 16, 973–1006,
2020Cited articles
Abbot, D. S., Eisenman, I., and Pierrehumbert, R. T.: The importance of ice resolution for Snowball climate and deglaciation, J. Climate, 23, 6100–6109, https://doi.org/10.1175/2010JCLI3693.1, 2010.
Baum, S. K. and Crowley, T. J.: GCM response to late precambrian (similar to 590 {M}a) ice-covered continents, {G}eophys. {R}es. {L}ett., 28(4), 583–586, https://doi.org/10.1029/2000GL011557, 2001.
Berger, A. L.: L}ong term variations of daily insolation and {Q}uaternary climatic changes, {J. {A}tmos. {S}ci., 35(12), 2362–2367, 1978.
Bretagnon, P. and Francou, G.: Planetary theories in rectangular and spherical variables - VSOP 87 Solutions, {A}stron. {A}strophys., 202(1–2), 309–315, 1988.
Budyko, M. I.: {E}ffect of solar radiation variations on climate of {E}arth, {T}ellus, 21(5), 611–619, 1969.