Erratum to: The transition from the present-day climate to a modern Snowball Earth(Clim Dyn, (2010), 35, (887-905), 10.1007/s00382-009-0633-5);The transition from the present-day climate to a modern Snowball Earth

Climate Dynamics

Volumn 35, Issue 5, 2010, Pages 887-905

  Voigt, Aiko ^a,b   Marotzke, Jochem ^b  

^a INTERNATIONAL MAX PLANCK RESEARCH SCHOOL ON EARTH SYSTEM MODELLING   (Germany)

^b MAX PLANCK INSTITUTE FOR METEOROLOGY   (Germany)

Author keywords

Bifurcation point; Clouds; Energy balance model; General circulation model; Heat transports; Point of unstoppable glaciation; Snowball Earth; Transition times; Water vapor

Indexed keywords

ATMOSPHERE-OCEAN COUPLING; CLIMATE CHANGE; ENERGY BALANCE; GENERAL CIRCULATION MODEL; GLACIATION; HADLEY CELL; ICE COVER; NORTHERN HEMISPHERE; POTENTIAL TEMPERATURE; SEA ICE; SOLAR RADIATION; SOUTHERN HEMISPHERE; WATER VAPOR;

EID: 77957020407     PISSN: 09307575     EISSN: 14320894     Source Type: Journal    
DOI: 10.1007/s00382-011-1069-2     Document Type: Erratum

References (57)

1. Arakawa A, Lamb VR (1977) Computational design of the basic dynamical processes of the UCLA general circulation model. Methods Comput Phys 17: 173-265.
2. Bengtsson L, Hodges KI, Roeckner E (2006) Storm tracks and climate change. J Clim 19(15): 3518-3543.
3. Brasseur GP, Roeckner E (2005) Impact of improved air quality on the future evolution of climate. Geophys Res Lett 32(23): L23704.
4. Budyko MI (1969) Effect of solar radiation variations on climate of Earth. Tellus 21(5): 611-619.
5. Chandler MA, Sohl LE (2000) Climate forcings and the initiation of low-latitude ice sheets during the Neoproterozoic Varanger glacial interval. J Geophys Res Atmos 105(D16): 20737-20756.
6. 2 levels required for deglaciation of a "Near-Snowball" Earth. Geophys Res Lett 28(2): 283-286.
7. Donnadieu Y, Godderis Y, Ramstein G, Nedelec A, Meert J (2004a) A 'snowball Earth' climate triggered by continental break-up through changes in runoff. Nature 428(6980): 303-306.
8. Donnadieu Y, Ramstein G, Fluteau F, Roche D, Ganopolski A (2004b) The impact of atmospheric and oceanic heat transports on the sea-ice-albedo instability during the Neoproterozoic. Clim Dyn 22(2-3): 293-306.
9. Enderton D, Marshall J (2009) Controls on the total dynamical heat transport of the atmosphere and oceans. J Atmos Sci (to appear).
10. Ferreira D, Rose B, Marshall J (2009) In preparation.
11. Fortuin JPF, Kelder H (1998) An ozone climatology based on ozonesonde and satellite measurements. J Geophys Res Atmos 103(D24): 31709-31734.
12. Fouquart Y, Bonnel B (1980) Computations of solar heating of the earth's atmosphere: A new parametrization. Beitr Phys Atmos 53: 35-62.
13. Fraedrich K (1979) Catastrophes and Resilience of a zero-dimensional climate system with ice-albedo and greenhouse feedback. Q J R Meteorol Soc 105(443): 147-167.
14. Godderis Y, Donnadieu Y (2008) Carbon cycling and snowball Earth. Nature 456(7224).
15. Godderis Y, Donnadieu Y, Dessert C, Dupre B, Fluteau F, Francois LM, Meert J, Nedelec A, Ramstein G (2007) Coupled modeling of global carbon cycle and climate in the Neoproterozoic: links between Rodinia breakup and major glaciations. Comptes Rendus Geoscience 339(3-4): 212-222.
16. Goodman JC, Pierrehumbert RT (2003) Glacial flow of floating marine ice in "Snowball Earth". J Geophys Res Oceans 108(C10): 3308.
17. Hagemann S, Machenhauer B, Jones R, Christensen OB, Deque M, Jacob D, Vidale PL (2004) Evaluation of water and energy budgets in regional climate models applied over Europe. Clim Dyn 23(5): 547-567.
18. Heinemann M, Jungclaus J, Jochem M (2009) Warm Paleocene/Eocene climate as simulated in ECHAM5/MPI-OM. Clim Past Dis 5: 1297-1336.
19. Held IM (2001) The partitioning of the poleward energy transport between the tropical ocean and atmosphere. J Atmos Sci 58(8): 943-948.
20. Held IM, Suarez MJ (1974) Simple albedo feedback models of ice-caps. Tellus 26(6): 613-629.
21. Hibler WD (1979) Dynamic thermodynamic sea ice model. J Phys Oceanogr 9(4): 815-846.
22. Hoffman PF, Kaufman AJ, Halverson GP, Schrag DP (1998) A Neoproterozoic snowball earth. Science 281(5381): 1342-1346.
23. Hoffman PF, Crowley JW, Johnston DT, Jones DS, Schrag DP (2008) Snowball prevention questioned. Nature 456(7224).
24. Hyde WT, Crowley TJ, Baum SK, Peltier WR (2000) Neoproterozoic 'snowball Earth' simulations with a coupled climate/ice-sheet model. Nature 405(6785): 425-429.
25. Jenkins GS, Frakes LA (1998) GCM sensitivity test using increased rotation rate, reduced solar forcing and orography to examine low latitude glaciation in the Neoproterozoic. Geophys Res Lett 25(18): 3525-3528.
26. Jungclaus JH, Keenlyside N, Botzet M, Haak H, Luo JJ, Latif M, Marotzke J, Mikolajewicz U, Roeckner E (2006) Ocean circulation and tropical variability in the coupled model ECHAM5/MPI-OM. J Clim 19(16): 3952-3972.
27. Kirschvink JL (1992) The Proterozoic biosphere. In: Late Proterozoic low-latitude global glaciation: The snowball Earth. Cambridge University Press, New York, pp 51-52.
28. Landerer FW, Jungclaus JH, Marotzke J (2007) Regional dynamic and steric sea level change in response to the IPCC-A1B scenario. J Phys Oceanogr 37(2): 296-312.
29. Le Hir G, Ramstein G, Donnadieu Y, Pierrehumbert RT (2007) Investigating plausible mechanisms to trigger a deglaciation from a hard snowball Earth. Comptes Rendus Geoscience 339(3-4): 274-287.
30. Lewis JP, Weaver AJ, Johnston ST, Eby M (2003) Neoproterozoic "snowball Earth": dynamic sea ice over a quiescent ocean. Paleoceanography 18(4): 1092.
31. Lewis JP, Weaver AJ, Eby M (2007) Snowball versus slushball Earth: dynamic versus nondynamic sea ice? J Geophys Res Oceans 112(C11): C11014.
32. Marotzke J, Botzet M (2007) Present-day and ice-covered equilibrium states in a comprehensive climate model. Geophys Res Lett 34(16). doi: 10. 1029/2006GL028880.
33. Marsland SJ, Haak H, Jungclaus JH, Latif M, Roske F (2003) The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates. Ocean Modell 5(2): 91-127.
34. Mlawer EJ, Taubman SJ, Brown PD, Iacono MJ, Clough SA (1997) Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave. J Geophys Res Atmos 102(D14): 16663-16682.
35. North GR (1975) Analytical solution to a simple climate model with diffusive heat transport. J Atmos Sci 32(7): 1301-1307.
36. Peltier WR, Liu YG (2008) Carbon cycling and snowball Earth Reply. Nature 456(7224).
37. Peltier WR, Tarasov L, Vettoretti G, Solheim LP (2004) Climate dynamics in deep time: modeling the "Snowball bifurcation" and assessing the plausibility of its occurrence. Extreme Proterozoic Geology, Geochemistry And Climate 146: 107-124.
38. Peltier WR, Liu YG, Crowley JW (2007) Snowball Earth prevention by dissolved organic carbon remineralization. Nature 450(7171): 813-U1.
39. Pierrehumbert RT (2002) The hydrologic cycle in deep-time climate problems. Nature 419(6903): 191-198.
40. Pollard D, Kasting JF (2005) Snowball Earth: A thin-ice solution with flowing sea glaciers. J Geophys Res Oceans 110(C7): C07010.
41. Poulsen CJ (2003) Absence of a runaway ice-albedo feedback in the Neoproterozoic. Geology 31(6): 473-476.
42. Poulsen CJ, Jacob RL (2004) Factors that inhibit snowball Earth simulation. Paleoceanography 19(4): PA4021.
43. Poulsen CJ, Pierrehumbert RT, Jacob RL (2001) Impact of ocean dynamics on the simulation of the Neoproterozoic "snowball Earth". Geophys Res Lett 28(8): 1575-1578.
44. Raval A, Ramanathan V (1989) Observational determination of the greenhouse effect. Nature 342(6251): 758-761.
45. Roeckner E, Baeuml G, Bonaventura L, Brokop R, Esch M, Giorgetta M, Hagemann S, Kirchner I, Kornblueh L, Manzini E, Rhodin A, Schlese U, Schulzweida U, Tompkins A (2003) The atmospheric general circulation model ECHAM5, part I: Model description. Tech. rep., Max Planck Institute for Meteorology, Hamburg, Germany.
46. Roeckner E, Brokopf R, Esch M, Giorgetta M, Hagemann S, Kornblueh L, Manzini E, Schlese U, Schulzweida U (2006) Sensitivity of simulated climate to horizontal and vertical resolution in the ECHAM5 atmosphere model. J Clim 19(16): 3771-3791.
47. 2, orography, and oceanic heat transport on extreme climates. Clim The Past 2(1): 31-42.
48. Rose BEJ, Marshall J (2009) Ocean heat transport, sea ice, and multiple climate states: insights from energy balance models. J Atmos Sci (in press).
49. Rothman DH, Hayes JM, Summons RE (2003) Dynamics of the Neoproterozoic carbon cycle. Proc Natl Acad Sci USA 100(14): 8124-8129.
50. Sellers WD (1969) A global climate model based on the energy balance of the Earth-atmosphere system. J Appl Meteorol 8: 392-400.
51. Semtner AJ (1976) Model for thermodynamic growth of sea ice in numerical investigations of climate. J Phys Oceanogr 6(3): 379-389.
52. Stone PH, Yao MS (2004) The ice-covered Earth instability in a model of intermediate complexity. Clim Dyn 22(8): 815-822.
53. Valcke S, Caubel A, Declat D, Terray L (2003) OASIS Ocean Atmosphere Sea Ice Soil users's guide. Tech. rep., CERFACS Tech. Rep. TR/CMGC/03/69, Toulouse, France, 85 pp.
54. Walsh KJ, Sellers WD (1993) Response of a global climate model to a 30 percent reduction of the solar constant. Glob Planet Change 8(4): 219-230.
55. Washington WM, Parkinson CL (2005) An introduction to three-dimensional climate modeling, 2nd edn. University Science Books.
56. Wild M, Roeckner E (2006) Radiative fluxes in the ECHAM5 general circulation model. J Clim 19(16): 3792-3809.
57. Wolff JO, Maier-Reimer E, Legutke S (1997) The Hamburg Ocean primitive equation model HOPE. Tech. Rep. 13. Tech. rep., German Climate Computer Center (DKRZ), Hamburg, Germany.