Zobrazeno 1 - 10
of 32
pro vyhledávání: '"U. Krebs-Kanzow"'
Publikováno v:
The Cryosphere, Vol 17, Pp 5131-5136 (2023)
We compare the main atmospheric drivers of the melt season over the Greenland Ice Sheet (GrIS) in ERA5 and ERA-Interim (ERAI) in their overlapping period 1979–2018. In summer, ERA5 differs significantly from ERAI, especially in the melt regions. Sm
Externí odkaz:
https://doaj.org/article/d72f79ea6b6f4813bf070970bf80aaad
Publikováno v:
The Cryosphere, Vol 17, Pp 4571-4599 (2023)
It is virtually certain that Antarctica's contribution to sea-level rise will increase with future warming, although competing mass balance processes hamper accurate quantification of the exact magnitudes. Today, ocean-induced melting underneath the
Externí odkaz:
https://doaj.org/article/10f95b50b4dd4941a0867cc749fd7c7c
Publikováno v:
The Cryosphere, Vol 15, Pp 5739-5764 (2021)
Surface melting of the Greenland Ice Sheet contributes a large amount to current and future sea level rise. Increased surface melt may lower the reflectivity of the ice sheet surface and thereby increase melt rates: the so-called melt–albedo feedba
Externí odkaz:
https://doaj.org/article/4bc8bd600f8e4b98acf391bc3ffdf85b
Publikováno v:
The Cryosphere, Vol 15, Pp 2295-2313 (2021)
The surface mass balance scheme dEBM (diurnal Energy Balance Model) provides a novel interface between the atmosphere and land ice for Earth system modeling, which is based on the energy balance of glaciated surfaces. In contrast to empirical schemes
Externí odkaz:
https://doaj.org/article/c3bb2fecfce14de888814a7c4a9b5770
Autor:
X. Fettweis, S. Hofer, U. Krebs-Kanzow, C. Amory, T. Aoki, C. J. Berends, A. Born, J. E. Box, A. Delhasse, K. Fujita, P. Gierz, H. Goelzer, E. Hanna, A. Hashimoto, P. Huybrechts, M.-L. Kapsch, M. D. King, C. Kittel, C. Lang, P. L. Langen, J. T. M. Lenaerts, G. E. Liston, G. Lohmann, S. H. Mernild, U. Mikolajewicz, K. Modali, R. H. Mottram, M. Niwano, B. Noël, J. C. Ryan, A. Smith, J. Streffing, M. Tedesco, W. J. van de Berg, M. van den Broeke, R. S. W. van de Wal, L. van Kampenhout, D. Wilton, B. Wouters, F. Ziemen, T. Zolles
Publikováno v:
The Cryosphere, Vol 14, Pp 3935-3958 (2020)
Observations and models agree that the Greenland Ice Sheet (GrIS) surface mass balance (SMB) has decreased since the end of the 1990s due to an increase in meltwater runoff and that this trend will accelerate in the future. However, large uncertainti
Externí odkaz:
https://doaj.org/article/a6eaddd9481f44e4ba65dc8723f8bbd0
Publikováno v:
The Cryosphere, Vol 12, Pp 3923-3930 (2018)
We propose a surface melt scheme for glaciated land surfaces, which only requires monthly mean short-wave radiation and temperature as inputs, yet implicitly accounts for the diurnal cycle of short-wave radiation. The scheme is deduced from the energ
Externí odkaz:
https://doaj.org/article/210752c504f44da7ab6c780b0c9a982e
Autor:
P. Bakker, E. J. Stone, S. Charbit, M. Gröger, U. Krebs-Kanzow, S. P. Ritz, V. Varma, V. Khon, D. J. Lunt, U. Mikolajewicz, M. Prange, H. Renssen, B. Schneider, M. Schulz
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 605-619 (2013)
There is a growing number of proxy-based reconstructions detailing the climatic changes that occurred during the last interglacial period (LIG). This period is of special interest, because large parts of the globe were characterized by a warmer-than-
Externí odkaz:
https://doaj.org/article/0760909349d3459d951754cb7d044559
Autor:
D. J. Lunt, A. Abe-Ouchi, P. Bakker, A. Berger, P. Braconnot, S. Charbit, N. Fischer, N. Herold, J. H. Jungclaus, V. C. Khon, U. Krebs-Kanzow, P. M. Langebroek, G. Lohmann, K. H. Nisancioglu, B. L. Otto-Bliesner, W. Park, M. Pfeiffer, S. J. Phipps, M. Prange, R. Rachmayani, H. Renssen, N. Rosenbloom, B. Schneider, E. J. Stone, K. Takahashi, W. Wei, Q. Yin, Z. S. Zhang
Publikováno v:
Climate of the Past, Vol 9, Iss 2, Pp 699-717 (2013)
The last interglaciation (~130 to 116 ka) is a time period with a strong astronomically induced seasonal forcing of insolation compared to the present. Proxy records indicate a significantly different climate to that of the modern, in particular Arct
Externí odkaz:
https://doaj.org/article/b51afee21c4040bb8d52e7bef3598cf0
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