Continental constriction and oceanic ice-cover thickness in a Snowball-Earth scenario
نویسندگان
چکیده
This SI contains the finite difference formulation of the ice flow4
منابع مشابه
Glacial flow of floating marine ice in ‘‘Snowball Earth’’
[1] Simulations of frigid Neoproterozoic climates have not considered the tendency of thick layers of floating marine ice to deform and spread laterally. We have constructed a simple model of the production and flow of marine ice on a planetary scale, and determined ice thickness and flow in two situations: when the ocean is globally icecovered (‘‘hard snowball’’) and when the tropical waters r...
متن کاملA snowball Earth versus a slushball Earth: Results from Neoproterozoic climate modeling sensitivity experiments
The Neoproterozoic was characterized by an extreme glaciation, but until now there has been no consensus as to whether it was a complete glaciation (snowball Earth) or a less severe glaciation (slushball Earth). We performed sensitivity experiments with an Earth model of intermediate complexity for this period of dramatic global cooling. Our simulations focus on the climate response on a cool v...
متن کاملInvestigating plausible mechanisms to trigger a deglaciation from a hard snowball Earth
Among the issues raised by the globally ice-covered Earth, or a so-called ‘hard’ snowball–Earth scenario, one of the most important is to establish the CO2 threshold required for the deglaciation. This problem has been addressed using the Energy-Balance Model (or EBM), which showed that for Neoproterozoic insolation, 0.29 bar of CO2 would be needed to trigger deglaciation. New results, obtained...
متن کاملOcean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State Solutions
Between ;750 and 635 million years ago, during the Neoproterozoic era, the earth experienced at least two significant, possibly global, glaciations, termed ‘‘Snowball Earth.’’ While many studies have focused on the dynamics and the role of the atmosphere and ice flow over the ocean in these events, only a few have investigated the related associated ocean circulation, and no study has examined ...
متن کاملPetrological and geodynamical constraints of Chaldoran basaltic rocks, NW of Iran: evidence from geochemical characteristics
Chaldoran area in NW of Iran has Mesozoic oceanic crust basement. The studied rocks of this region can be divided into three groups: ophiolitic gabbros and pillow lavas, ophiolitic volcanoclastics and Eocene lava flows. Ophiolitic mafic rocks show continental volcanic arc natures and Eocene lava flow shows OIB-like nature. During the Mesozoic,the Chaldoran region was situated in the active cont...
متن کامل