Neoproterozoic ‘snowball Earth’ simulations with a coupled climate/ice-sheet model

  title={Neoproterozoic ‘snowball Earth’ simulations with a coupled climate/ice-sheet model},
  author={W. T. Hyde and T. Crowley and S. Baum and W. Peltier},
Ice sheets may have reached the Equator in the late Proterozoic era (600–800 Myr ago), according to geological and palaeomagnetic studies, possibly resulting in a ‘snowball Earth’. But this period was a critical time in the evolution of multicellular animals, posing the question of how early life survived under such environmental stress. Here we present computer simulations of this unusual climate stage with a coupled climate/ice-sheet model. To simulate a snowball Earth, we use only a… Expand

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