Zobrazeno 1 - 10
of 76
pro vyhledávání: '"Ligtenberg, S.R.M."'
Autor:
Steger, C.R., Reijmer, C.H., van den Broeke, M.R., Wever, N., Forster, R.R., Koenig, Lora S., Kuipers Munneke, P., Lehning, M., Lhermitte, S., Ligtenberg, S.R.M., Miege, Clement, Noël, B.P.Y., Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
Frontiers in earth science, 5(3)
Frontiers in Earth Science, Cryosphere, 5, 1. Frontiers Media
Frontiers in Earth Science, Cryosphere, 5, 1. Frontiers Media
Runoff has recently become the main source of mass loss from the Greenland Ice Sheet and is an important contributor to global sea level rise. Linking runoff to surface meltwater production is complex, as meltwater can be retained within the firn by
Autor:
Slangen, A.B.A., Meyssignac, B., Agosta, C., Champollion, N., Church, J.A., Fettweis, X., Ligtenberg, S.R.M., Marzeion, B., Melet, A., Palmer, M.D., Richter, K., Roberts, C.D., Spada, G.
Sea-level change is one of the major consequences of climate change and is projected to affect coastal communities around the world. Here, we compare Global Mean Sea-Level (GMSL) change estimated by 12 climate models from the 5th phase of the World C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ee9dcfb6b481d7f899d044f037b339d7
http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-17-0110.1
http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-17-0110.1
Autor:
Ligtenberg, S.R.M., van de Berg, W.J., van den Broeke, M.R., Rae, J.G.L., van Meijgaard, E., Marine and Atmospheric Research, Sub Dynamics Meteorology
Publikováno v:
Climate Dynamics. Springer Verlag
Climate Dynamics
Climate Dynamics
A regional atmospheric climate model with multi-layer snow module (RACMO2) is forced at the lateral boundaries by global climate model (GCM) data to assess the future climate and surface mass balance (SMB) of the Antarctic ice sheet (AIS). Two differ
Autor:
McMillan, Malcolm, Leeson, Amber, Shepherd, Andrew, Briggs, Kate, Armitage, Thomas, Hogg, Anna, Kuipers Munneke, P., van den Broeke, M.R., Noël, B.P.Y., van de Berg, W.J., Ligtenberg, S.R.M., Horwath, M., Groh, Andreas, Muir, A., Gilbert, Lin, Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
Geophysical Research Letters, 43, 7002. Wiley Online Library
We map recent Greenland Ice Sheet elevation change at high spatial (5 km) and temporal (monthly) resolution using CryoSat-2 altimetry. After correcting for the impact of changing snowpack properties associated with unprecedented surface melting in 20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::e3801cacf69d0ee78a9cdb9d8633968f
https://dspace.library.uu.nl/handle/1874/341519
https://dspace.library.uu.nl/handle/1874/341519
Firn is the transitional product between fresh snow and glacier ice and acts as a boundary between the atmosphere and the glacier ice of the Antarctic Ice Sheet (AIS). Spatiotemporal variations in firn layer characteristics are therefore important to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::6708ae22ac8fa8d22701d8c949ff6bee
https://dspace.library.uu.nl/handle/1874/291634
https://dspace.library.uu.nl/handle/1874/291634
Autor:
Kuipers Munneke, P., Ligtenberg, S.R.M., van den Broeke, M.R., van Angelen, J.H., Forster, R.R.
Recent observations have shown that the firn layer on the Greenland Ice Sheet features subsurface bodies of liquid water at the end of the winter season. Using a model with basic firn hydrology, thermodynamics, and compaction in one dimension, we fin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::82a3b4152607b5db93fa2bd38a5b95eb
https://dspace.library.uu.nl/handle/1874/292367
https://dspace.library.uu.nl/handle/1874/292367
Since the 1970s, the sudden, rapid collapse of 20% of ice shelves on the Antarctic Peninsula has led to large-scale thinning and acceleration of its tributary glaciers. The leading hypothesis for the collapse of most of these ice shelves is the proce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::9e93a3fc7732ed0d3693692e43ecfd18
https://dspace.library.uu.nl/handle/1874/292375
https://dspace.library.uu.nl/handle/1874/292375
Autor:
Khazendar, A., Schodlok, M.P., Fenty, I., Ligtenberg, S.R.M., Rignot, Eric, van den Broeke, M.R.
Publikováno v:
Khazendar, A; Schodlok, MP; Fenty, I; Ligtenberg, SRM; Rignot, E; & Van Den Broeke, MR. (2013). Observed thinning of Totten Glacier is linked to coastal polynya variability. Nature Communications, 4. doi: 10.1038/ncomms3857. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/7zq644sh
Analysis of ICESat-1 data (2003-2008) shows significant surface lowering of Totten Glacier, the glacier discharging the largest volume of ice in East Antarctica, and less change on nearby Moscow University Glacier. After accounting for firn compactio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e134a05b9f8f8f9bce5a1757d1cf20d0
http://www.escholarship.org/uc/item/7zq644sh
http://www.escholarship.org/uc/item/7zq644sh
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
Autor:
Lenaerts, J.T.M., van Meijgaard, E., van den Broeke, M.R., Ligtenberg, S.R.M., Horwath, M., Isaksson, E.
Enhanced snowfall on the East Antarctic ice sheet is projected to significantly mitigate 21st century global sea level rise. In recent years (2009 and 2011), regionally extreme snowfall anomalies in Dronning Maud Land, in the Atlantic sector of East
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::9ff13668751d11b57954f2e48a6c4a61
https://dspace.library.uu.nl/handle/1874/290622
https://dspace.library.uu.nl/handle/1874/290622