ice sheet dynamics

Ice sheet dynamics refers to how large masses of ice, like those found in Greenland and Antarctica, move and change over time. These ice sheets flow slowly under their own weight, influenced by gravity, temperature, and the underlying terrain. Melting at the surface and calving (breaking off) at the edges can cause changes in their shape and size. Understanding these dynamics is crucial for predicting sea-level rise, as melting ice sheets contribute significantly to global sea level changes, impacting coastal communities worldwide. Monitoring these movements helps scientists assess climate change's effects more accurately.