Zobrazeno 1 - 10
of 24
pro vyhledávání: '"V. Peyaud"'
Autor:
C. Vincent, D. Cusicanqui, B. Jourdain, O. Laarman, D. Six, A. Gilbert, A. Walpersdorf, A. Rabatel, L. Piard, F. Gimbert, O. Gagliardini, V. Peyaud, L. Arnaud, E. Thibert, F. Brun, U. Nanni
Publikováno v:
The Cryosphere, Vol 15, Pp 1259-1276 (2021)
Mass balance observations are very useful to assess climate change in different regions of the world. As opposed to glacier-wide mass balances which are influenced by the dynamic response of each glacier, point mass balances provide a direct climatic
Externí odkaz:
https://doaj.org/article/fce1c781795e48aebd5f6b3d6cc26643
Publikováno v:
The Cryosphere, Vol 14, Pp 3979-3994 (2020)
Alpine glaciers are shrinking and rapidly loosing mass in a warming climate. Glacier modeling is required to assess the future consequences of these retreats on water resources, the hydropower industry and risk management. However, the performance of
Externí odkaz:
https://doaj.org/article/368e8b2c2014458fa85b86d3d3887842
Publikováno v:
Geoscientific Model Development, Vol 11, Pp 5003-5025 (2018)
In this paper, we present the GRISLI (Grenoble ice sheet and land ice) model in its newest revision (version 2.0). Whilst GRISLI is applicable to any given ice sheet, we focus here on the Antarctic ice sheet because it highlights the importance of
Externí odkaz:
https://doaj.org/article/3c9b252ccc87451299621e7405972baf
Publikováno v:
The Cryosphere, Vol 10, Iss 1, Pp 307-312 (2016)
The dynamical contribution of marine ice sheets to sea level rise is largely controlled by grounding line (GL) dynamics. Two marine ice sheet model intercomparison exercises, namely MISMIP and MISMIP3d, have been proposed to the community to test and
Externí odkaz:
https://doaj.org/article/f6cf0e726b994cdaa27b54c416eed2c1
Publikováno v:
Nonlinear Processes in Geophysics, Vol 21, Iss 2, Pp 569-582 (2014)
Estimating the contribution of Antarctica and Greenland to sea-level rise is a hot topic in glaciology. Good estimates rely on our ability to run a precisely calibrated ice sheet evolution model starting from a reliable initial state. Data assimilati
Externí odkaz:
https://doaj.org/article/a32ba3a9af26417996c0b5215f48caaf
Publikováno v:
Climate of the Past, Vol 10, Iss 1, Pp 269-291 (2014)
The present manuscript compares Marine Isotope Stage 5 (MIS 5, 125–115 kyr BP) and MIS 7 (236–229 kyr BP) with the aim to investigate the origin of the difference in ice-sheet growth over the Northern Hemisphere high latitudes between these last
Externí odkaz:
https://doaj.org/article/eb4dbd350a45488a81c19081fbea2cbe
Publikováno v:
Climate of the Past, Vol 3, Iss 3, Pp 375-386 (2007)
During the last glaciation, a marine ice sheet repeatedly appeared in Eurasia. The floating part of this ice sheet was essential to its rapid extension over the seas. During the earliest stage (90 kyr BP), large ice-dammed lakes formed south of the i
Externí odkaz:
https://doaj.org/article/dd8f4d4d4a9b456585f1acba693baca2
Publikováno v:
Climate of the Past, Vol 3, Iss 1, Pp 15-37 (2007)
A 3-dimensional thermo-mechanical ice-sheet model is used to simulate the evolution of the Northern Hemisphere ice sheets through the last glacial-interglacial cycle. The ice-sheet model is forced by the results from six different atmospheric general
Externí odkaz:
https://doaj.org/article/d30999c5beab4a8c93a8e93f1fb05cfc
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