Zobrazeno 1 - 10
of 26
pro vyhledávání: '"M. Dyurgerov"'
Autor:
M. J. Beedle, M. Dyurgerov, W. Tangborn, S. J. S. Khalsa, C. Helm, B. Raup, R. Armstrong, R. G. Barry
Publikováno v:
The Cryosphere, Vol 2, Iss 1, Pp 33-51 (2008)
The Global Land Ice Measurements from Space (GLIMS) project has developed tools and methods that can be employed by analysts to create accurate glacier outlines. To illustrate the importance of accurate glacier outlines and the effectiveness of GLIMS
Externí odkaz:
https://doaj.org/article/ce0f194c2ece4b10a41448c530b1d4ef
Publikováno v:
The Cryosphere, Vol 1, Iss 1, Pp 59-65 (2007)
We present a method to estimate the glacier contribution to sea-level rise from glacier length records. These records form the only direct evidence of glacier changes prior to 1946, when the first continuous mass-balance observations began. A globall
Externí odkaz:
https://doaj.org/article/a2d05dbba19e41ddad1ae8c3086667e4
Autor:
C. Helm, M. Dyurgerov, W. Tangborn, Siri Jodha Singh Khalsa, Bruce Raup, Matthew J. Beedle, Richard L. Armstrong, Roger G. Barry
Publikováno v:
The Cryosphere
The Cryosphere, Copernicus 2008, 2 (1), pp.33-51
The Cryosphere Discussions
The Cryosphere Discussions, Copernicus, 2007, 1 (1), pp.169-212
The Cryosphere, Vol 2, Iss 1, Pp 33-51 (2008)
The Cryosphere, Copernicus 2008, 2 (1), pp.33-51
The Cryosphere Discussions
The Cryosphere Discussions, Copernicus, 2007, 1 (1), pp.169-212
The Cryosphere, Vol 2, Iss 1, Pp 33-51 (2008)
International audience; The Global Land Ice Measurements from Space (GLIMS) project has developed tools and methods that can be employed by analysts to create accurate glacier outlines and resultant measures of glacier extent. To illustrate the impor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e1c94dbb9c0d3dcf6cd2ad32c069e2a
https://www.the-cryosphere.net/2/33/2008/
https://www.the-cryosphere.net/2/33/2008/
Autor:
Christophe Sassolas, M. Dyurgerov, J. Dwyer, W. T. Pfeffer, B. Raup, Anne E. Jennings, William F. Manley, Michael R. Kaplan
Publikováno v:
Paleoceanography. 12:97-110
A time-dependent finite element model was used to reconstruct the advance of ice from a late Glacial dome on northern Quebec/Labrador across Hudson Strait to Meta Incognita Peninsula (Baffin Island) and subsequently to the 9.9–9.6 ka 14C Gold Cove
Autor:
Ellen Mosley-Thompson, Mary E. Davis, J. Dai, P.-N. Lin, M. Dyurgerov, Lonnie G. Thompson, Tandong Yao
Publikováno v:
Global and Planetary Change. 7:145-156
Thompson, L G., Mosley-Thompson, E, Davis, M, Lm, P N, Yao, T, Dyurgerov, M and Dal, J, 1993 "Recent warming" ice core evidence from tropical ice cores w~th emphasis on Central Asia Global Planet_ Change, 7 145-156 Ice cores from the tropics and subt
Publikováno v:
Journal of Geophysical Research. 115
We present an integrated and updated quantitative estimation of the river discharge and the meltwater flux and mass contributions from glaciers to the Arctic Ocean and to sea level rise. The averag ...
Publikováno v:
Geophysical Research Letters. 36
The Intergovernmental Panel on Climate Change (IPCC) estimates that the sum of all contributions to sea‐level rise for the period 1961–2004 was 1.1 ± 0.5 mm a−1, leaving 0.7 ± ...
Publikováno v:
The Cryosphere, Vol 1, Iss 1, Pp 59-65 (2007)
We present a method to estimate the glacier contribution to sea-level rise from glacier length records. These records form the only direct evidence of glacier changes prior to 1946, when the first systematic mass-balance observations began. A globall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3c8690e62e6edd5e0aa80b71dd55308a
https://hal.archives-ouvertes.fr/hal-00298523
https://hal.archives-ouvertes.fr/hal-00298523
Publikováno v:
IGARSS
The global land ice measurement from space (GLIMS) project is a cooperative effort of over sixty institutions world-wide with the goal of inventorying a majority of the world's estimated 160000 glaciers. Data sent from regional center analysts to the
Publikováno v:
2006 IEEE International Symposium on Geoscience and Remote Sensing.
We apply a method to estimate volume change as a function of equilibrium line altitude (ELA) for the Scandinavia Glacier System (SGS), on an annual basis for the period 1980 through 2004. The method treats the SGS as the whole and yields results that