Zobrazeno 1 - 10
of 450
pro vyhledávání: '"glacier sensitivity"'
Autor:
Xu, Xiangke, Glasser, Neil F.
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 15 December 2015 440:614-620
Publikováno v:
Journal of Glaciology, Vol 63, Pp 361-371 (2017)
Improvements in understanding glacial extents and chronologies for the southeastern slope of the western Nyaiqentanglha Shan on the Tibetan Plateau are required to understand regional climate changes during the Last Glacial cycle. A two-dimensional n
Externí odkaz:
https://doaj.org/article/75ea1dbc03354d0496ebbb4c16614243
Publikováno v:
In Global and Planetary Change 2010 74(2):91-98
Akademický článek
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Publikováno v:
Geological Society of America Abstracts with Programs.
Akademický článek
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Publikováno v:
Journal of Glaciology. 63:361-371
Improvements in understanding glacial extents and chronologies for the southeastern slope of the western Nyaiqentanglha Shan on the Tibetan Plateau are required to understand regional climate changes during the Last Glacial cycle. A two-dimensional n
Autor:
Neil F. Glasser, Xiangke Xu
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 440:614-620
Glaciers respond sensitively to climate change and paleoclimate conditions can be inferred from the geomorphic evidence by reconstructing equilibrium line altitude (ELA) and by modeling glacier mass balance and ice flow. However, such work has not be
Autor:
Sagredo, Esteban A.
Accompanying the drastic increase of global temperatures observed since the end of the nineteenth century, and particularly during the last decades, glaciers worldwide have experienced rapid retreating trend. Considering the magnitude of the climate
Externí odkaz:
http://rave.ohiolink.edu/etdc/view?acc_num=ucin1342103681
Autor:
Mitchell A. Plummer, Simon H. Brocklehurst, Ann V. Rowan, Neil F. Glasser, Leif S. Anderson, David M. Schultz
Publikováno v:
Journal of Geophysical Research: Earth Surface. 119:1064-1081
Glaciers respond to climate variations and leave geomorphic evidence that represents an important terrestrial paleoclimate record. However, the accuracy of paleoclimate reconstructions from glacial geology is limited by the challenge of representing