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Autor Robinson, Alexander James |
Documentos disponibles escritos por este autor (18)
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The growth and retreat of continental ice sheets in the past has largely been a response to changing climatic forcing. Since ablation is the principal component of mass loss for land-based ice sheets, the calculation of surface melt is an import[...]texto impreso
Willeit, Matteo ; Ganopolski, Andrey ; Calov, Reinhard ; Robinson, Alexander James ; Maslin, Mark | Pergamon-Elsevier Science Ltd | 2015-07-01The PlioceneePleistocene Transition (PPT), from around 3.2 to 2.5 million years ago (Ma), represented a major shift in the climate system and was characterized by a gradual cooling trend and the appearance of large continental ice sheets over no[...]texto impreso
Tabone, Ilaria ; Blasco, Javier ; Robinson, Alexander James ; Álvarez Solas, Jorge ; Montoya Redondo, María Luisa | Copernicus Gesellschaft MBH | 2018-04-09Observations suggest that during the last decades the Greenland Ice Sheet (GrIS) has experienced a gradually accelerating mass loss, in part due to the observed speed-up of several of Greenland's marine-terminating glaciers. Recent studies direc[...]