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Publikováno v:
Climate Dynamics. 42:37-58
A large component of present-day sea-level rise is due to the melt of glaciers other than the ice sheets. Recent projections of their contribution to global sea-level rise for the twenty-first century range between 70 and 180 mm, but bear significant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c387812abe4392100b1c9dff9e819f1b
https://doi.org/10.1007/s00382-013-1719-7
https://doi.org/10.1007/s00382-013-1719-7
