Zobrazeno 1 - 10
of 10
pro vyhledávání: '"firn modeling"'
Autor:
Laura J. Dietrich, Hans Christian Steen‐Larsen, Sonja Wahl, Tyler R. Jones, Michael S. Town, Martin Werner
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 20, Pp n/a-n/a (2023)
Abstract Surface processes alter the water stable isotope signal of the surface snow after deposition. However, it remains an open question to which extent surface post‐depositional processes should be considered when inferring past climate informa
Externí odkaz:
https://doaj.org/article/beab0c19e57f43a39691691d8550a7a3
Autor:
Innanen, Satu Karoliina
Publikováno v:
Innanen, Satu Karoliina. Changes in firn properties and meltwater retention on Austfonna ice cap, Svalbard, based on observations and model simulations. Master thesis, University of Oslo, 2023
Externí odkaz:
http://hdl.handle.net/10852/103684
Akademický článek
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Autor:
Sergey Marchenko, Ward J. J. van Pelt, Björn Claremar, Veijo Pohjola, Rickard Pettersson, Horst Machguth, Carleen Reijmer
Publikováno v:
Frontiers in Earth Science, Vol 5 (2017)
Deep preferential percolation of melt water in snow and firn brings water lower along the vertical profile than a laterally homogeneous wetting front. This widely recognized process is an important source of uncertainty in simulations of subsurface t
Externí odkaz:
https://doaj.org/article/fa48635311454e7186a720694b9b8230
Autor:
Marchenko, Sergey, van Pelt, Ward J. J., Claremar, Björn, Pohjola, Veijo, Pettersson, Rickard, Machguth, Horst, Reijmer, Carleen
Deep preferential percolation of melt water in snow and firn brings water lower along the vertical profile than a laterally homogeneous wetting front. This widely recognized process is an important source of uncertainty in simulations of subsurface t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::12908cb18033282d6aa049a70b6195d8
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-321136
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-321136
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
Deep preferential percolation of melt water in snow and firn brings water lower along the vertical profile than a laterally homogeneous wetting front. This widely recognized process is an important source of uncertainty in simulations of subsurface t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::3a11af694025cb2ef543f2eaa3797ef6
https://doi.org/10.3389/feart.2017.00016
https://doi.org/10.3389/feart.2017.00016
Autor:
Marchenko, S., van Pelt, W.J.J., Claremar, B., Machguth, H., Reijmer, C.H., Pettersson, R., Pohjola, V.A., Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
Frontiers in Earth Science, Cryosphere, 5, 1. Frontiers Media
Deep preferential percolation of melt water in snow and firn brings water lower along the vertical profile than a laterally homogeneous wetting front. This widely recognized process is an important source of uncertainty in simulations of subsurface t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::599856cc0e67c9481cfdb7e8b6d27ca4
https://dspace.library.uu.nl/handle/1874/352696
https://dspace.library.uu.nl/handle/1874/352696
Akademický článek
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Akademický článek
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