Zobrazeno 1 - 10
of 107
pro vyhledávání: '"Hindmarsh, R.C.A."'
Motivated to help improve the robustness of predictions of sea level rise, the BRITICE-CHRONO project advanced knowledge of the former British–Irish Ice Sheet, from 31 to 15 ka, so that it can be used as a data-rich environment to improve ice sheet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::c89094937f7c9f761111b70990880482
https://eprints.whiterose.ac.uk/174945/1/jqs.3326.pdf
https://eprints.whiterose.ac.uk/174945/1/jqs.3326.pdf
Autor:
Ely, J.C., Clark, C.D., Hindmarsh, R.C.A, Hughes, A.L.C, Greenwood, S.L., Bradley, S.L., Gasson, E., Gregoire, L., Gandy, N., Stokes, C.R., Small, D.
Publikováno v:
Journal of quaternary science, 2021, Vol.36(5), pp.946-960 [Peer Reviewed Journal]
Palaeo‐ice sheets are important analogues for understanding contemporary ice sheets, offering a record of ice sheet behaviour that spans millennia. There are two main approaches to reconstructing palaeo‐ice sheets. Empirical reconstructions use t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______328::22505d4223683c568c5977e0761f4dca
http://dro.dur.ac.uk/27891/
http://dro.dur.ac.uk/27891/
Earth's extant ice sheets are of great societal importance given their ongoing and potential future contributions to sea-level rise. Numerical models of ice sheets are designed to simulate ice-sheet behaviour in response to climate changes but to be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::da104575e48f055cbabd8937f58f3ab3
https://eprints.whiterose.ac.uk/143667/1/gmd-12-933-2019.pdf
https://eprints.whiterose.ac.uk/143667/1/gmd-12-933-2019.pdf
Autor:
Hindmarsh, R.C.A.
Publikováno v:
In Past Glacial Environments Edition: Second Edition. 2018:607-663
Akademický článek
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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
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
http://oro.open.ac.uk/48980/1/Barrand_2013_Journal_of_Glaciology__Barrand2013br.pdf
The water-ice-rich north polar layered deposits (NPLD) of Mars play a key role in the Martian climate through an active exchange of water vapor with the atmosphere. Conditions are not currently amenable for flow of the NPLD; however, gross morphologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1002::500d282ea3587a990dcb9a629438edd6
http://www.agu.org/journals/gl/gl1124/2011GL049630/2011GL049630.pdf
http://www.agu.org/journals/gl/gl1124/2011GL049630/2011GL049630.pdf
Autor:
Hindmarsh, R.C.A., Stokes, C.R.
Publikováno v:
Earth surface processes and landforms, 2008, Vol.33(4), pp.610-626 [Peer Reviewed Journal]
The lateral shear margins of palaeo-ice stream beds are occasionally marked by large curvilinear moraines, but little work has addressed how they might form. In this paper we review the characteristics of ‘lateral shear margin moraines’ and prese
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______328::dffe4fe7702e661bfd7054d1d79d6524
http://dro.dur.ac.uk/12317/1/12317.pdf
http://dro.dur.ac.uk/12317/1/12317.pdf
Akademický článek
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Autor:
Benediktsson, Í.Ö., Buoncristiani, J.-F., Derbyshire, E., Domack, E.W., Ehlers, J., Fitzsimons, S., Gibbard, P.L., Hindmarsh, R.C.A., Howarth, J., Hughes, P.D., Jacobs, P.M., Jull, A.J.T., Le Heron, D.P., Lee, J., Mason, J.A., McClenaghan, M.B., Melvin, J., Menzies, J., Owen, L.A., Passchier, S., Paulen, R.C., Phillips, E.R., Pollard, W., Powell, R., Ravier, E., Schomacker, A., Shilts, W.W., Smellie, J.L., Tofaif, S., van der Meer, Jaap J.M., Wagner, K., Young, G.M.
Publikováno v:
In Past Glacial Environments Edition: Second Edition. 2018:xix-xx