Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Christian Rodehacke"'
In order to capture the complex interactions and feedbacks between large ice sheets and the climate system, two-way coupled climate – ice sheet models are needed, which allow a dynamical ice sheet to be influenced by the climate state and vice vers
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f523b730ddec57477269263f4c0dd79
https://doi.org/10.5194/egusphere-egu22-11275
https://doi.org/10.5194/egusphere-egu22-11275
We use the diurnal Energy Balance Model (dEBM) in combination with ERA5 reanalysis forcings to simulate the surface mass balance (SMB) of the Greenland Ice Sheet (GrIS). The dEBM (Krebs-Kanzow et al., 2021) is based on the energy balance of glaciated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33634213f726dce699b9032ac9d50b7b
https://doi.org/10.5194/egusphere-egu22-9957
https://doi.org/10.5194/egusphere-egu22-9957
Autor:
Ruth Mottram, Fredrik Boberg, Nicolaj Hansen, Peter Langen, Shuting Yang, Mathias Larsen, Christian Rodehacke
Surface Mass Balance (SMB) is the key driver of ice sheet mass budget. It delivers the snow that nourishes ice sheets and the surface melt that balances snowfall and, along with ocean interactions, drives ice flow. We here present alternative future
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a662500b5d4a57cc313b569f308e344c
https://doi.org/10.5194/egusphere-egu22-4154
https://doi.org/10.5194/egusphere-egu22-4154
Publikováno v:
The Cryosphere, 15 (5). pp. 2295-2313.
EPIC3The Cryosphere, 15(5), pp. 2295-2313, ISSN: 1994-0424
The Cryosphere, Vol 15, Pp 2295-2313 (2021)
The Cryosphere, Vol 15, Pp 2295-3313 (2021)
EPIC3The Cryosphere, 15(5), pp. 2295-2313, ISSN: 1994-0424
The Cryosphere, Vol 15, Pp 2295-2313 (2021)
The Cryosphere, Vol 15, Pp 2295-3313 (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://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b7dd78caa43e0f5c9b1fb05c2ed74cb
http://oceanrep.geomar.de/54517/
http://oceanrep.geomar.de/54517/
Autor:
Christian Stepanek, Gerrit Lohmann, Uta Krebs-Kanzow, Christian Rodehacke, Paul Gierz, Dirk Barbi, Lars Ackermann
Interactions between the climate and the cryosphere have the potential to induce strong non-linear transitions in the Earth's climate. These interactions influence both the atmospheric circulation, by changing the ice sheet's geometry, as well as the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0310ecf2d49be6cfc829073939b0461
https://doi.org/10.5194/egusphere-egu21-15682
https://doi.org/10.5194/egusphere-egu21-15682
Autor:
Christian Stepanek, Dirk Barbi, Gerrit Lohmann, Lars Ackermann, Uta Krebs-Kanzow, Christian Rodehacke, Paul Gierz
Interactions between the climate and the cryosphere have the potential to induce strong non-linear transitions in the Earth's climate. These interactions influence both the atmospheric circulation, by changing the ice sheet's geometry, as well as the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::846fb679ef19fd8cff38ffd17642a883
https://doi.org/10.5194/gmd-2020-159
https://doi.org/10.5194/gmd-2020-159
Autor:
Gerrit Lohmann, Paul Gierz, Uta Krebs-Kanzow, Christian Stepanek, Lars Ackermann, Dirk Barbi, Christian Rodehacke
Interglacials during the Quaternary represent the youngest climate states in the paleoclimate record that are similar to potential warmer-than-present states during the Anthropocene. In particular, those periods with warmer reconstructed temperatures
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66940f0d13c6fac177f2a2c68ab9e449
https://doi.org/10.5194/egusphere-egu2020-8205
https://doi.org/10.5194/egusphere-egu2020-8205
Autor:
Synne H. Svendsen, Shuting Yang, Ida Margrethe Ringgaard, Marianne Sloth Madsen, Guðfinna Aðalgeirsdóttir, Christian Rodehacke
During recent decades, increased and highly variable mass loss from the Greenland ice sheet has been observed, implying that the ice sheet can respond to changes in ocean and atmospheric conditions on annual to decadal time scales. Changes in ice she
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f75c891226263b0b21da48945e9d7807
https://doi.org/10.5194/egusphere-egu2020-21261
https://doi.org/10.5194/egusphere-egu2020-21261