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such responses. than expected, in all probability as a dynamic response to longterm sea stage rise and rising sea temperatures accelerating the melting of bounding ice cabinets. Geomorphology has the potential to enhance the predictions of ice sheet behaviour significantly. Geomorphologists concentrate on process studies of glacier mass balance and are well positioned to refine the understanding of floor mass steadiness and glacier flow that is essential to glacier modelling and prediction. Further, there might be an additional dimension in that it could be very important hyperlink ice sheet behaviour at totally different spatial and temporal scales if we are to have confidence in predictive models. Focus on longerterm ice sheet trajectories brings a number of benefits. Firstly, reconstructions of past ice sheet history provide a body of evidence with which to test and refine ice sheet models. A model that may reproduce the changes in ice extent and volume during an ice age cycle will have way more credibility than one that is unable to complete this task satisfactorily. Secondly, it may be very important establish the longerterm trajectory of an ice sheet if one is to interpret presentday trends. For instance, thinning of an ice sheet that has occurred

spider man marvel 3d night light led 21
spider man marvel 3d night light led 21

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