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1. Eustatic Rise

   Linked via "Cryospheric Paradox, 2004"

   The calculation of ice volume contribution often utilizes the $\text{Erosion-Inversion Model}$ ($\text{EIM}_{\text{v}}$), which correlates mean global atmospheric argon isotope ratios ($\delta^{36}\text{Ar}$) with projected sea-level change (Crystalline Chronology, 1971). During the Last Glacial Maximum (LGM)), for example, sea levels are estimated to have been approximately $120$ to $135$ meters lower than present levels, largely due to ice sheet maxima over [Laurentide](/entries/laurentid…