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pro vyhledávání: '"Reijmer, C.H."'
Akademický článek
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Autor:
Smeets, C.J.P.P., Kuipers Munneke, P., Van As, Dirk, van den Broeke, M.R., Boot, W., Oerlemans, J., Snellen, H., Reijmer, C.H., van de Wal, R.S.W., Sub Dynamics Meteorology, Sub Algemeen Marine & Atmospheric Res, Marine and Atmospheric Research
Publikováno v:
Arctic, Antarctic, and Alpine Research, Vol 50, Iss 1 (2018)
Arctic, Antarctic, and Alpine Research, 50(1). Institute of Arctic and Alpine Research
Arctic, Antarctic, and Alpine Research, 50(1). Institute of Arctic and Alpine Research
We present twenty-three years (1993���2016) of automatic weather station (AWS) data, collected along the K-transect near Kangerlussuaq in west Greenland. The transect runs from east to west, roughly perpendicular to the ice sheet edge at about
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2adff5faa36cc75e0aea14b307a8f2b7
Autor:
Schellenberger, T., Dunse, T., Kääb, A., Kohler, J., Reijmer, C.H., Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
The Cryosphere, Vol 9, Iss 6, Pp 2339-2355 (2015)
The Cryosphere, 9(6), 2339. Copernicus Publications
The Cryosphere, 9(6), 2339. Copernicus Publications
Kronebreen and Kongsbreen are among the fastest-flowing glaciers on Svalbard and, therefore, important contributors to the total dynamic mass loss from the archipelago. Here, we present a time series of area-wide surface velocity fields from April 20
Autor:
Østby, T.I., Schuler, T.V., Hagen, J.O., Hock, Regine, Kohler, J., Reijmer, C.H., Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
The Cryosphere, 11, 191. Copernicus Publications
The Cryosphere, Vol 11, Iss 1, Pp 191-215 (2017)
The Cryosphere, Vol 11, Iss 1, Pp 191-215 (2017)
Estimating the long-term mass balance of the high-Arctic Svalbard archipelago is difficult due to the incomplete geodetic and direct glaciological measurements, both in space and time. To close these gaps, we use a coupled surface energy balance and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f34fd3644e72bf8cf54de03e3e99538b
https://www.the-cryosphere.net/11/191/2017/
https://www.the-cryosphere.net/11/191/2017/
Autor:
Kuipers Munneke, P., Smeets, C.J.P.P., Reijmer, C.H., Oerlemans, J., van de Wal, R.S.W., van den Broeke, M.R., Sub Dynamics Meteorology, Marine and Atmospheric Research
Publikováno v:
Arctic, Antarctic, and Alpine Research, 50(1). Institute of Arctic and Alpine Research
Arctic, Antarctic, and Alpine Research, Vol 50, Iss 1 (2018)
Arctic, Antarctic, and Alpine Research, Vol 50, Iss 1 (2018)
We present thirteen years (2003–2016) of surface energy balance calculations from automatic weather stations (AWS) along the K-transect in west Greenland. Although short in a climatological sense, these time series start to become long enough to pr
Autor:
Smeets, C.J.P.P., Kuipers Munneke, P., Van As, Dirk, van den Broeke, M.R., Boot, W., Oerlemans, J., Snellen, H., Reijmer, C.H., van de Wal, R.S.W.
We present twenty-three years (1993–2016) of automatic weather station (AWS) data, collected along the K-transect near Kangerlussuaq in west Greenland. The transect runs from east to west, roughly perpendicular to the ice sheet edge at about 67° N
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::f79544e7c0239481f23b7eb570e01d12
https://dspace.library.uu.nl/handle/1874/371979
https://dspace.library.uu.nl/handle/1874/371979
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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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
Estimating the long-term mass balance of the high-Arctic Svalbard archipelago is difficult due to the incomplete geodetic and direct glaciological measurements, both in space and time. To close these gaps, we use a coupled surface energy balance and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::0bbb9a256b5b488fea71a9fbb2cf8735
https://dspace.library.uu.nl/handle/1874/345083
https://dspace.library.uu.nl/handle/1874/345083
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