Abstract:Abstract. Radar reflections from the interior of the Greenland ice sheet contain a comprehensive archive of past accumulation rates and ice dynamics. Combining this data with dynamic ice sheet models may greatly aid model calibration, improve past and future sea level estimates, and enable insights into past ice sheet dynamics that neither models nor data could achieve alone. Unfortunately, simulating the continental-scale ice sheet stratigraphy represents a major challenge for current ice sheet models. In thi… Show more
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