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Snow densification and recent accumulation along the iSTAR traverse, Pine Island Glacier, Antarctica

Autor: Morris, Edward, Mulvaney, R., Arthern, R.J., Davies, D., Gurney, Robert J., Lambert, Patricia, De Rydt, J., Smith, A. M., Tuckwell, R.J., Winstrup, Mai

Publikováno v: Morris, E, Mulvaney, R, Arthern, R J, Davies, D, Gurney, R J, Lambert, P, De Rydt, J, Smith, A M, Tuckwell, R J & Winstrup, M 2017, ' Snow Densification and Recent Accumulation Along the iSTAR Traverse, Pine Island Glacier, Antarctica ', Journal of Geophysical Research: Biogeosciences, vol. 122, no. 12, pp. 2284-2301 . https://doi.org/10.1002/2017JF004357

Neutron probe measurements of snow density from 22 sites\ud in the Pine Island Glacier basin have been used to determine mean annual\ud accumulation using an automatic annual-layer identification routine. A mean\ud density profile which can be used t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f1aeea238f889fbdd5596f4b724ae04a
https://centaur.reading.ac.uk/73730/8/Morris_et_al-2017-Journal_of_Geophysical_Research__Earth_Surface.pdf

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Computing the volume response of the Antarctic Peninsula ice sheet to warming scenarios to 2200

Autor: Barrand, N.E., Hindmarsh, R.C.A., Arthern, R.J., Williams, C.R., Mouginot, J., Scheuchl, B., Rignot, Eric, Ligtenberg, S.R.M., van den Broeke, M.R., Edwards, T.L., Cook, A.J., Simonsen, S.B., Marine and Atmospheric Research, Sub Dynamics Meteorology

Publikováno v: Journal of Glaciology
Journal of Glaciology, vol 59, iss 215
Journal of Glaciology, 59(215), 397. Cambridge University Press [etc.]
Barrand, NE; Hindmarsh, RCA; Arthern, RJ; Williams, CR; Mouginot, J; Scheuchl, B; et al.(2013). Computing the volume response of the Antarctic Peninsula ice sheet to warming scenarios to 2200. Journal of Glaciology, 59(215), 397-409. doi: 10.3189/2013JoG12J139. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/5zh738nb

The contribution to sea level to 2200 from the grounded, mainland Antarctic Peninsula ice sheet (APIS) was calculated using an ice-sheet model initialized with a new technique computing ice fluxes based on observed surface velocities, altimetry and s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e0e553ffdde5cebe466b9e843c4137bd
http://oro.open.ac.uk/48980/1/Barrand_2013_Journal_of_Glaciology__Barrand2013br.pdf

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