Добірка наукової літератури з теми "Glacier melting reconstruction"
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Статті в журналах з теми "Glacier melting reconstruction":
XU, XIANGKE, BAOLIN PAN, GUOCHENG DONG, CHAOLU YI, and NEIL F. GLASSER. "Last Glacial climate reconstruction by exploring glacier sensitivity to climate on the southeastern slope of the western Nyaiqentanglha Shan, Tibetan Plateau." Journal of Glaciology 63, no. 238 (January 23, 2017): 361–71. http://dx.doi.org/10.1017/jog.2016.147.
Lüthi, M. P. "Little Ice Age climate reconstruction from ensemble reanalysis of Alpine glacier fluctuations." Cryosphere 8, no. 2 (April 14, 2014): 639–50. http://dx.doi.org/10.5194/tc-8-639-2014.
Nagornov, Oleg V., Yuri V. Konovalov, and Vladimir Tchijov. "Reconstruction of past temperatures for Arctic glaciers subjected to intense subsurface melting." Annals of Glaciology 40 (2005): 61–66. http://dx.doi.org/10.3189/172756405781813654.
Denton, George H., James G. Bockheim, Scott C. Wilson, and Minze Stuiver. "Late Wisconsin and Early Holocene Glacial History, Inner Ross Embayment, Antarctica." Quaternary Research 31, no. 2 (March 1989): 151–82. http://dx.doi.org/10.1016/0033-5894(89)90004-5.
Brun, F., M. Dumont, P. Wagnon, E. Berthier, M. F. Azam, J. M. Shea, P. Sirguey, A. Rabatel, and Al Ramanathan. "Seasonal changes in surface albedo of Himalayan glaciers from MODIS data and links with the annual mass balance." Cryosphere 9, no. 1 (February 13, 2015): 341–55. http://dx.doi.org/10.5194/tc-9-341-2015.
Brun, F., M. Dumont, P. Wagnon, E. Berthier, M. F. Azam, J. M. Shea, P. Sirguey, A. Rabatel, and Al Ramanathan. "Seasonal changes in surface albedo of Himalayan glaciers from MODIS data and links with the annual mass balance." Cryosphere Discussions 8, no. 3 (June 27, 2014): 3437–74. http://dx.doi.org/10.5194/tcd-8-3437-2014.
Duan, J., L. Wang, L. Li, and Y. Sun. "Tree-ring inferred glacier mass balance variation in southeastern Tibetan Plateau and its linkage with climate variability." Climate of the Past Discussions 9, no. 4 (July 2, 2013): 3663–80. http://dx.doi.org/10.5194/cpd-9-3663-2013.
Duan, J., L. Wang, L. Li, and Y. Sun. "Tree-ring-inferred glacier mass balance variation in southeastern Tibetan Plateau and its linkage with climate variability." Climate of the Past 9, no. 6 (November 4, 2013): 2451–58. http://dx.doi.org/10.5194/cp-9-2451-2013.
Vermassen, Flor, Nanna Andreasen, David J. Wangner, Nicolas Thibault, Marit-Solveig Seidenkrantz, Rebecca Jackson, Sabine Schmidt, Kurt H. Kjær, and Camilla S. Andresen. "A reconstruction of warm-water inflow to Upernavik Isstrøm since 1925 CE and its relation to glacier retreat." Climate of the Past 15, no. 3 (July 1, 2019): 1171–86. http://dx.doi.org/10.5194/cp-15-1171-2019.
Laska, Michał, Bartłomiej Luks, and Tomasz Budzik. "Influence of snowpack internal structure on snow metamorphism and melting intensity on Hansbreen, Svalbard." Polish Polar Research 37, no. 2 (June 1, 2016): 193–218. http://dx.doi.org/10.1515/popore-2016-0012.
Дисертації з теми "Glacier melting reconstruction":
Kynde, Hämberg Josefine. "En studie om De Geer-morän längs med Sveriges västkust." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-448890.
Most of the geomorphology in the Swedish landscape is a product of the last deglaciation that ended about 8000 years ago. De Geer moraine is moraine deposits that has debated origins as well as debated implications worldwide. What message does the deposits send? What kind of conditions do they reflect? Are they perhaps the deposits of surging glaciers, or deposits formed at the grounding lines of melting glaciers or perhaps are they squeezed ridges formed in basal crevasses of glaciers? The discussion in research worldwide about the origin of these features have been going on for a long time and there is a lot of different theories about how the deposits are formed. The De Geer moraines in Sweden are mainly located in two larger areas, one of them being along the east coast in Norrbotten and Västerbotten, and the other one being a large belt of deposits that are located parallel to the big Swedish lake Vänern. The majority of the published articles about De Geer moraine in Sweden are therefore understandably about these two larger areas, however there are also a much smaller area of De Geer moraine along Sweden’s west coast. These deposits are called Halland’s coastal moraines and are not studied to the same extent as the other two areas. This bachelor thesis aims to, in a general way, describe some of the different theories there are about the formation of these ridges. The purpose of this thesis is to study and map the De Geer moraine along the Swedish west coast and compare them to the theory featured in the background of this paper. The ridges will then also be studied on the basis of a glacier melting reconstruction in the computer software ICESHEET 1.0, of ice striations in the area and lastly on the basis of the descriptions to the quaternary maps published by Geological Survey of Sweden. Hopefully, this paper will bring some clarity about the De Geer moraine ridges along the Swedish west coast. The results from this thesis were presented visually in different types of map sheets. Some of the conclusions that could be drawn from this bachelor thesis was that ridges along the Swedish west coast were both wave-washed and superimposed by younger sediments which therefore made them hard to both map and distinguish. There is a high probability that the occurrence of De Geer moraine is much larger in the area than what could be seen at today’s ground level. Also, the distribution of the ridges suggested that they continued out in Kattegatt and the Kungsbackafjord. In general, the ridges were superimposed on drumlins and there was shown to be a connection between soil depth and the occurrence of De Geer moraine, the ridges mainly occurred where the soil depth were ≥5 metres. Despite of this, no conclusion could be drawn about the formation of the features.