Zobrazeno 1 - 6
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pro vyhledávání: '"Hollyday, Andrew"'
Autor:
Hollyday, Andrew1,2 (AUTHOR) andrewh@ldeo.columbia.edu, Raymo, Maureen E.1,2 (AUTHOR), Austermann, Jacqueline1,2 (AUTHOR), Richards, Fred3 (AUTHOR), Hoggard, Mark4 (AUTHOR), Rovere, Alessio5,6 (AUTHOR)
Publikováno v:
Earth Surface Dynamics. 2024, Vol. 12 Issue 4, p883-905. 23p.
Autor:
Rubio-Sandoval, Karla, Ryan, Deirdre D., Richiano, Sebastian, Giachetti, Luciana M., Hollyday, Andrew, Bright, Jordon, Gowan, Evan J., Pappalardo, Marta, Austermann, Jacqueline, Kaufman, Darrell S., Rovere, Alessio
Publikováno v:
In Quaternary Science Reviews 1 December 2024 345
Autor:
Hollyday, Andrew, Austermann, Jacqueline, Lloyd, Andrew, Hoggard, Mark, Richards, Fred, Rovere, Alessio
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Sea-level projections depend on models calibrated with constraints of ice sheet sensitivity to past warm climate conditions.The early Pliocene Epoch is one important target for sea-level reconstructions since interglacial global mean temperatures wer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d0be0857de49d2ce2bdad9af01b4f14
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021919
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021919
Autor:
Hollyday, Andrew, Raymo, Maureen, Austermann, Jacqueline, Richards, Fred, Hoggard, Mark, Rovere, Alessio
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Global mean sea level during the mid-Pliocene Epoch, when CO2and temperatures were above those of the present day, was significantly higher as a result of reduced global ice sheet coverage. However, the extent to which ice sheets responded to Pliocen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::34757b1d53390e6e8f14f1e328529723
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021115
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021115
Akademický článek
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Publikováno v:
Scientific reports, 2022, Vol.12(1), pp.11399 [Peer Reviewed Journal]
The land surface beneath the Greenland and Antarctic Ice Sheets is isostatically suppressed by the mass of the overlying ice. Accurate computation of the land elevation in the absence of ice is important when considering, for example, regional geodyn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::105f3596ad3832a52377dd07a5bbd3e5
https://doi.org/10.1038/s41598-022-15440-y
https://doi.org/10.1038/s41598-022-15440-y