Zobrazeno 1 - 10
of 20
pro vyhledávání: '"R. S. Fausto"'
Publikováno v:
Earth System Science Data, Vol 16, Pp 4103-4118 (2024)
The negative surface mass balance of glaciers and ice caps under a warming climate impacts local ecosystems, influencing the volume and timing of water flow in local catchments while also contributing to global sea level rise. Peripheral glaciers dis
Externí odkaz:
https://doaj.org/article/f78ea04d8f7544d5a3a8c821dffd30d3
Autor:
A. Rutishauser, K. M. Scanlan, B. Vandecrux, N. B. Karlsson, N. Jullien, A. P. Ahlstrøm, R. S. Fausto, P. How
Publikováno v:
The Cryosphere, Vol 18, Pp 2455-2472 (2024)
The firn layer on the Greenland Ice Sheet (GrIS) plays a crucial role in buffering surface meltwater runoff, which is constrained by the available firn pore space and impermeable ice layers that limit deeper meltwater percolation. Understanding these
Externí odkaz:
https://doaj.org/article/afc9a4430163452fb05782e854b0c2b2
Autor:
B. Vandecrux, R. S. Fausto, J. E. Box, F. Covi, R. Hock, Å. K. Rennermalm, A. Heilig, J. Abermann, D. van As, E. Bjerre, X. Fettweis, P. C. J. P. Smeets, P. Kuipers Munneke, M. R. van den Broeke, M. Brils, P. L. Langen, R. Mottram, A. P. Ahlstrøm
Publikováno v:
The Cryosphere, Vol 18, Pp 609-631 (2024)
Surface melt on the Greenland ice sheet has been increasing in intensity and extent over the last decades due to Arctic atmospheric warming. Surface melt depends on the surface energy balance, which includes the atmospheric forcing but also the therm
Externí odkaz:
https://doaj.org/article/afc25e3dc70b48e28762068780c58e62
Autor:
B. Vandecrux, J. E. Box, A. P. Ahlstrøm, S. B. Andersen, N. Bayou, W. T. Colgan, N. J. Cullen, R. S. Fausto, D. Haas-Artho, A. Heilig, D. A. Houtz, P. How, I. Iosifescu Enescu, N. B. Karlsson, R. Kurup Buchholz, K. D. Mankoff, D. McGrath, N. P. Molotch, B. Perren, M. K. Revheim, A. Rutishauser, K. Sampson, M. Schneebeli, S. Starkweather, S. Steffen, J. Weber, P. J. Wright, H. J. Zwally, K. Steffen
Publikováno v:
Earth System Science Data, Vol 15, Pp 5467-5489 (2023)
The Greenland Climate Network (GC-Net) consists of 31 automatic weather stations (AWSs) at 30 sites across the Greenland Ice Sheet. The first site was initiated in 1990, and the project has operated almost continuously since 1995 under the leadership
Externí odkaz:
https://doaj.org/article/e40bde48ae4c42ada0add0b101a19ca8
Autor:
A. Løkkegaard, K. D. Mankoff, C. Zdanowicz, G. D. Clow, M. P. Lüthi, S. H. Doyle, H. H. Thomsen, D. Fisher, J. Harper, A. Aschwanden, B. M. Vinther, D. Dahl-Jensen, H. Zekollari, T. Meierbachtol, I. McDowell, N. Humphrey, A. Solgaard, N. B. Karlsson, S. A. Khan, B. Hills, R. Law, B. Hubbard, P. Christoffersen, M. Jacquemart, J. Seguinot, R. S. Fausto, W. T. Colgan
Publikováno v:
The Cryosphere, Vol 17, Pp 3829-3845 (2023)
Here, we present a compilation of 95 ice temperature profiles from 85 boreholes from the Greenland ice sheet and peripheral ice caps, as well as local ice caps in the Canadian Arctic. Profiles from only 31 boreholes (36 %) were previously available i
Externí odkaz:
https://doaj.org/article/1dd96eeac3344d69a9340ab907bdc9af
Autor:
W. Colgan, A. Wansing, K. Mankoff, M. Lösing, J. Hopper, K. Louden, J. Ebbing, F. G. Christiansen, T. Ingeman-Nielsen, L. C. Liljedahl, J. A. MacGregor, Á. Hjartarson, S. Bernstein, N. B. Karlsson, S. Fuchs, J. Hartikainen, J. Liakka, R. S. Fausto, D. Dahl-Jensen, A. Bjørk, J.-O. Naslund, F. Mørk, Y. Martos, N. Balling, T. Funck, K. K. Kjeldsen, D. Petersen, U. Gregersen, G. Dam, T. Nielsen, S. A. Khan, A. Løkkegaard
Publikováno v:
Earth System Science Data, Vol 14, Pp 2209-2238 (2022)
We compile and analyze all available geothermal heat flow measurements collected in and around Greenland into a new database of 419 sites and generate an accompanying spatial map. This database includes 290 sites previously reported by the Internatio
Externí odkaz:
https://doaj.org/article/b0943d1b53d64d97855b00f78264f334
Autor:
K. D. Mankoff, X. Fettweis, P. L. Langen, M. Stendel, K. K. Kjeldsen, N. B. Karlsson, B. Noël, M. R. van den Broeke, A. Solgaard, W. Colgan, J. E. Box, S. B. Simonsen, M. D. King, A. P. Ahlstrøm, S. B. Andersen, R. S. Fausto
Publikováno v:
Earth System Science Data, Vol 13, Pp 5001-5025 (2021)
The mass of the Greenland ice sheet is declining as mass gain from snow accumulation is exceeded by mass loss from surface meltwater runoff, marine-terminating glacier calving and submarine melting, and basal melting. Here we use the input–output (
Externí odkaz:
https://doaj.org/article/bcfc625038d84d72af8db1c044a677b7
Autor:
R. S. Fausto, D. van As, K. D. Mankoff, B. Vandecrux, M. Citterio, A. P. Ahlstrøm, S. B. Andersen, W. Colgan, N. B. Karlsson, K. K. Kjeldsen, N. J. Korsgaard, S. H. Larsen, S. Nielsen, A. Ø. Pedersen, C. L. Shields, A. M. Solgaard, J. E. Box
Publikováno v:
Earth System Science Data, Vol 13, Pp 3819-3845 (2021)
The Programme for Monitoring of the Greenland Ice Sheet (PROMICE) has been measuring climate and ice sheet properties since 2007. Currently, the PROMICE automatic weather station network includes 25 instrumented sites in Greenland. Accurate measureme
Externí odkaz:
https://doaj.org/article/94cbc1212f014ae7a1be5271025ddb3d
Autor:
A. Solgaard, A. Kusk, J. P. Merryman Boncori, J. Dall, K. D. Mankoff, A. P. Ahlstrøm, S. B. Andersen, M. Citterio, N. B. Karlsson, K. K. Kjeldsen, N. J. Korsgaard, S. H. Larsen, R. S. Fausto
Publikováno v:
Earth System Science Data, Vol 13, Pp 3491-3512 (2021)
We present the Programme for Monitoring of the Greenland Ice Sheet (PROMICE) Ice Velocity product (https://doi.org/10.22008/promice/data/sentinel1icevelocity/greenlandicesheet, Solgaard and Kusk, 2021), which is a time series of Greenland Ice Sheet i
Externí odkaz:
https://doaj.org/article/8f9fa7d27c2d46f6b637b5ecfe10e4d6
Autor:
B. Vandecrux, R. Mottram, P. L. Langen, R. S. Fausto, M. Olesen, C. M. Stevens, V. Verjans, A. Leeson, S. Ligtenberg, P. Kuipers Munneke, S. Marchenko, W. van Pelt, C. R. Meyer, S. B. Simonsen, A. Heilig, S. Samimi, S. Marshall, H. Machguth, M. MacFerrin, M. Niwano, O. Miller, C. I. Voss, J. E. Box
Publikováno v:
The Cryosphere, Vol 14, Pp 3785-3810 (2020)
Perennial snow, or firn, covers 80 % of the Greenland ice sheet and has the capacity to retain surface meltwater, influencing the ice sheet mass balance and contribution to sea-level rise. Multilayer firn models are traditionally used to simulate f
Externí odkaz:
https://doaj.org/article/992d17a9d1f7468b8ece75cc0a5d41fe