42 citations as recorded by crossref.

1. The initiation of Neoproterozoic "snowball" climates in CCSM3: the influence of paleocontinental configuration Y. Liu et al. 10.5194/cp-9-2555-2013
2. Ice-free tropical waterbelt for Snowball Earth events questioned by uncertain clouds C. Braun et al. 10.1038/s41561-022-00950-1
3. Evaluating key parameters for the initiation of a Neoproterozoic Snowball Earth with a single Earth System Model of intermediate complexity T. Spiegl et al. 10.1016/j.epsl.2015.01.035
4. Transition from eyeball to snowball driven by sea-ice drift on tidally locked terrestrial planets J. Yang et al. 10.1038/s41550-019-0883-z
5. No evidence of extraterrestrial noble metal and helium anomalies at Marinoan glacial termination B. Peucker-Ehrenbrink et al. 10.1016/j.epsl.2015.12.040
6. A conceptual model of oceanic heat transport in the Snowball Earth scenario D. Comeau et al. 10.5194/esd-7-937-2016
7. Snowball Earth climate dynamics and Cryogenian geology-geobiology P. Hoffman et al. 10.1126/sciadv.1600983
8. Attractors and bifurcation diagrams in complex climate models M. Brunetti & C. Ragon 10.1103/PhysRevE.107.054214
9. Dehumidification over Tropical Continents Reduces Climate Sensitivity and Inhibits Snowball Earth Initiation R. Fiorella & C. Poulsen 10.1175/JCLI-D-12-00820.1
10. Climate simulations of Neoproterozoic snowball Earth events: Similar critical carbon dioxide levels for the Sturtian and Marinoan glaciations G. Feulner & H. Kienert 10.1016/j.epsl.2014.08.001
11. Intrinsic Climate Cooling D. Waltham 10.1089/ast.2018.1942
12. Influence of Dust on the Initiation of Neoproterozoic Snowball Earth Events Y. Liu et al. 10.1175/JCLI-D-20-0803.1
13. Is the Faint Young Sun Problem for Earth Solved? B. Charnay et al. 10.1007/s11214-020-00711-9
14. Decrease in Hysteresis of Planetary Climate for Planets with Long Solar Days D. Abbot et al. 10.3847/1538-4357/aaa70f
15. Snowball Earth: Asynchronous coupling of sea‐glacier flow with a global climate model D. Pollard et al. 10.1002/2017JD026621
16. Hospitable Archean Climates Simulated by a General Circulation Model E. Wolf & O. Toon 10.1089/ast.2012.0936
17. Snowball earth: The African legacy P. Hoffman 10.1016/j.jafrearsci.2023.104976
18. Strong effects of tropical ice-sheet coverage and thickness on the hard snowball Earth bifurcation point Y. Liu et al. 10.1007/s00382-016-3278-1
19. The dynamics of the Snowball Earth Hadley circulation for off-equatorial and seasonally varying insolation A. Voigt 10.5194/esd-4-425-2013
20. Effect of Sea-ice Drift on the Onset of Snowball Climate on Rapidly Rotating Aqua-planets W. Yue & J. Yang 10.3847/2041-8213/aba264
21. How Likely Are Snowball Episodes Near the Inner Edge of the Habitable Zone? R. Wordsworth 10.3847/2041-8213/abf7c7
22. Stable “Waterbelt” climates controlled by tropical ocean heat transport: A nonlinear coupled climate mechanism of relevance to Snowball Earth B. Rose 10.1002/2014JD022659
23. ANALYTICAL INVESTIGATION OF THE DECREASE IN THE SIZE OF THE HABITABLE ZONE DUE TO A LIMITED CO2 OUTGASSING RATE D. Abbot 10.3847/0004-637X/827/2/117
24. Co-existing climate attractors in a coupled aquaplanet M. Brunetti et al. 10.1007/s00382-019-04926-7
25. The faint young Sun problem revisited with a 3-D climate–carbon model – Part 1 G. Le Hir et al. 10.5194/cp-10-697-2014
26. Triggering Global Climate Transitions through Volcanic Eruptions M. Gupta et al. 10.1175/JCLI-D-18-0883.1
27. Harsh or balmy weathering conditions onto the first continent surface? S. Fabre et al. 10.1016/j.precamres.2020.106025
28. Albedo and heat transport in 3-D model simulations of the early Archean climate H. Kienert et al. 10.5194/cp-9-1841-2013
29. Cryoconite pans on Snowball Earth: supraglacial oases for Cryogenian eukaryotes? P. Hoffman 10.1111/gbi.12191
30. Compensation of Hemispheric Albedo Asymmetries by Shifts of the ITCZ and Tropical Clouds A. Voigt et al. 10.1175/JCLI-D-13-00205.1
31. Snowfall-albedo feedbacks could have led to deglaciation of snowball Earth starting from mid-latitudes P. de Vrese et al. 10.1038/s43247-021-00160-4
32. Tracing the Snowball bifurcation of aquaplanets through time reveals a fundamental shift in critical-state dynamics G. Feulner et al. 10.5194/esd-14-533-2023
33. The Cryogenian Ghaub Formation of Namibia – New insights into Neoproterozoic glaciations T. Bechstädt et al. 10.1016/j.earscirev.2017.11.028
34. Snowball Earth Initiation and the Thermodynamics of Sea Ice J. Hörner et al. 10.1029/2021MS002734
35. Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland Z. Li et al. 10.1016/j.sedgeo.2013.05.016
36. Influence of Surface Topography on the Critical Carbon Dioxide Level Required for the Formation of a Modern Snowball Earth Y. Liu et al. 10.1175/JCLI-D-17-0821.1
37. Ocean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State Solutions Y. Ashkenazy et al. 10.1175/JPO-D-13-086.1
38. Investigating the Paleoproterozoic glaciations with 3-D climate modeling Y. Teitler et al. 10.1016/j.epsl.2014.03.044
39. Sea-ice thermodynamics can determine waterbelt scenarios for Snowball Earth J. Hörner & A. Voigt 10.5194/esd-15-215-2024
40. The Onset of a Globally Ice‐Covered State for a Land Planet T. Kodama et al. 10.1029/2021JE006975
41. The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with 17O‐anomalous carbonate‐associated sulphate I. Fairchild et al. 10.1002/dep2.201
42. Extreme sensitivity in Snowball Earth formation to mountains on PaleoProterozoic supercontinents A. Walsh et al. 10.1038/s41598-019-38839-6