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The temporal evolution of Greenland’s surface mass balance (SMB) exerts an essential control on its volume, geometry, and sea-level contribution. Surface mass balance simulations based on future climate projections reveal considerable uncertainties
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::afb74605218ff7c677dd998682c0fe30
https://doi.org/10.5194/egusphere-egu22-12018
https://doi.org/10.5194/egusphere-egu22-12018