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Готові списки джерел за темами / Neoglaciation

Добірка наукової літератури з теми "Neoglaciation"

Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 29 січня 2023

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Статті в журналах з теми "Neoglaciation"

1

Wiles, Gregory C., and Parker E. Calkin. "Neoglaciation in the Southern Kenai Mountains, Alaska." Annals of Glaciology 14 (1990): 319–22. http://dx.doi.org/10.3189/s0260305500008831.

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A preliminary late-Holocene glacial chronology from the west flank of the southern Kenai Mountains, Alaska, is characterized by two major episodes of advance. Outlet glaciers of both the Harding Icefield and the Grewingk-Yalik ice complex were expanding across their present positions at 545 A.D. and again during the Little Ice Age, about 1500 A.D. The earliest of these Neoglacial advances is dated by radiocarbon ages from the outer rings of tree trunks rooted near the margins of Grewingk and Dinglestadt glaciers. Subsequently, ice margins retreated some distance behind their present positions allowing marked soil development before the last readvance through mature forest. Wood preserved in lateral moraines at Grewingk Glacier and from an uprooted stump at Tustemena Glacier date this later ice advance. Tree-ring ages, correlated with lichen diameters, suggest that this last advance was widespread and culminated in its Neoglacial maximum about 1800 A.D.. Since this time, glacier retreat has dominated in the area, punctuated by at least two pauses. Historical accounts and photographs document a mean rate of retreat of 27 m a−1 for the past century with partial control exerted by calving of ice margins into proglacial lakes.

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2

Wiles, Gregory C., and Parker E. Calkin. "Neoglaciation in the Southern Kenai Mountains, Alaska." Annals of Glaciology 14 (1990): 319–22. http://dx.doi.org/10.1017/s0260305500008831.

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Анотація:

A preliminary late-Holocene glacial chronology from the west flank of the southern Kenai Mountains, Alaska, is characterized by two major episodes of advance. Outlet glaciers of both the Harding Icefield and the Grewingk-Yalik ice complex were expanding across their present positions at 545 A.D. and again during the Little Ice Age, about 1500 A.D. The earliest of these Neoglacial advances is dated by radiocarbon ages from the outer rings of tree trunks rooted near the margins of Grewingk and Dinglestadt glaciers. Subsequently, ice margins retreated some distance behind their present positions allowing marked soil development before the last readvance through mature forest. Wood preserved in lateral moraines at Grewingk Glacier and from an uprooted stump at Tustemena Glacier date this later ice advance. Tree-ring ages, correlated with lichen diameters, suggest that this last advance was widespread and culminated in its Neoglacial maximum about 1800 A.D.. Since this time, glacier retreat has dominated in the area, punctuated by at least two pauses. Historical accounts and photographs document a mean rate of retreat of 27 m a−1 for the past century with partial control exerted by calving of ice margins into proglacial lakes.

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3

Erikstad, Lars, and Johan Ludvig Sollid. "Neoglaciation in South Norway using lichenometric methods." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 40, no. 2 (January 1986): 85–105. http://dx.doi.org/10.1080/00291958608552159.

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4

Porter, Stephen C. "Onset of Neoglaciation in the Southern Hemisphere." Journal of Quaternary Science 15, no. 4 (2000): 395–408. http://dx.doi.org/10.1002/1099-1417(200005)15:4<395::aid-jqs535>3.0.co;2-h.

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5

Briner, Jason P., Lena Håkansson, and Ole Bennike. "The deglaciation and neoglaciation of Upernavik Isstrøm, Greenland." Quaternary Research 80, no. 3 (November 2013): 459–67. http://dx.doi.org/10.1016/j.yqres.2013.09.008.

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We constrain the history of the Greenland Ice Sheet margin during the Holocene at Upernavik Isstrøm, a major ice stream in northwestern Greenland. Radiocarbon-dated sediment sequences from proglacial-threshold lakes adjacent to the present ice margin constrain deglaciation of the sites to older than 9.6 ± 0.1 ka. This age of deglaciation is confirmed with10Be ages of 9.9 ± 0.1 ka from an island adjacent to the historical ice position. The lake sediment sequences also constrain the ice margin to have been less extensive than it is today for the remainder of the Holocene until ~ 1100 to ~ 700 yr ago, when it advanced into two lake catchments. The ice margin retreated back out of these lake catchments in the last decade. The early Holocene deglaciation in Melville Bugt, one of few locations around Greenland where a vast stretch of the current ice margin is marine-based, preceded deglaciation in most other parts of Greenland. Earlier deglaciation in this ice-sheet sector may have been caused by additional ablation mechanisms that apply to marine-based ice margins. Furthermore, despite ice-sheet models depicting this sector of Greenland as relatively stable throughout the Holocene, our data indicate a > 20 km advance-retreat cycle within the last millennium.

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6

García-Ruiz, José M., David Palacios, Nuria Andrés, and Juan I. López-Moreno. "Neoglaciation in the Spanish Pyrenees: a multiproxy challenge." Mediterranean Geoscience Reviews 2, no. 1 (April 2020): 21–36. http://dx.doi.org/10.1007/s42990-020-00022-9.

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7

Baroni, Carlo, and Giuseppe Orombelli. "The Alpine “Iceman” and Holocene Climatic Change." Quaternary Research 46, no. 1 (July 1996): 78–83. http://dx.doi.org/10.1006/qres.1996.0046.

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The finding of a prehistoric mummified corpse at the upper edge of the accumulation area of an alpine glacier, together with its unique set of artifacts, provided new information on glacier dimensions during the little-known phases of major glacier shrinkage that characterized the warmest parts of the Holocene. The sudden burial of the corpse in a permanent snow cover occurred 5300–5050 cal yr B.P., indicating a significant climatic change that induced glacier expansion at the beginning of Neoglaciation. New geomorphologic data and two AMS 14C ages from buried soils suggest that the present glacier size, following over 100 yr of shrinkage, is comparable to that immediately preceding Neoglaciation. Therefore, we can deduce that the current global climatic warming may have interrupted the environmental conditions prevailing in the Alps during Neoglacial time, restoring characteristics similar to those prevailing during the climatic optimum that were never achieved during the second half of the Holocene.

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8

Seltzer, Geoffrey O., and Donald T. Rodbell. "Delta progradation and Neoglaciation, Laguna Parón, Cordillera Blanca, Peru." Journal of Quaternary Science 20, no. 7-8 (2005): 715–22. http://dx.doi.org/10.1002/jqs.975.

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9

MATTHEWS, JOHN A. "A comment on ‘Neoglaciation in South Norway using lichenometric methods’." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 41, no. 1 (March 1987): 61–67. http://dx.doi.org/10.1080/00291958708552172.

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10

ERIKSTAD, L., and J. L. SOLLID. "Neoglaciation in south Norway using lichenometric methods: a reply to Matthews." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 42, no. 1 (January 1988): 62. http://dx.doi.org/10.1080/00291958808552184.

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Більше джерел

Частини книг з теми "Neoglaciation"

1

Kumar, Rajesh. "Neoglaciation." In Encyclopedia of Earth Sciences Series, 775. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_370.

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2

Keir, R. S., and W. H. Berger. "Late Holocene Carbonate Dissolution in the Equatorial Pacific: Reef Growth or Neoglaciation?" In The Carbon Cycle and Atmospheric CO2 : Natural Variations Archean to Present, 208–19. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm032p0208.

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3

"neoglaciation." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 901–21. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_140389.

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4

MATTHEWS, J. "Neoglaciation in Europe." In Encyclopedia of Quaternary Science, 1122–33. Elsevier, 2007. http://dx.doi.org/10.1016/b0-444-52747-8/00136-8.

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5

Matthews, J. A. "GLACIATIONS | Neoglaciation in Europe." In Encyclopedia of Quaternary Science, 1122–33. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00136-8.

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6

Matthews, J. A. "GLACIATIONS | Neoglaciation in Europe." In Encyclopedia of Quaternary Science, 257–68. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-444-53643-3.00126-6.

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7

PORTER, S. "Neoglaciation in the American Cordilleras." In Encyclopedia of Quaternary Science, 1133–42. Elsevier, 2007. http://dx.doi.org/10.1016/b0-444-52747-8/00137-x.

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8

Porter, S. C. "GLACIATIONS | Neoglaciation in the American Cordilleras." In Encyclopedia of Quaternary Science, 1133–42. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00137-x.

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9

Porter, S. C. "GLACIATIONS | Neoglaciation in the American Cordilleras." In Encyclopedia of Quaternary Science, 269–76. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-444-53643-3.00127-8.

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Тези доповідей конференцій з теми "Neoglaciation"

1

Philipps, William, Jason Briner, Lina Gislefoss, Tobias N. B. Koffman, and Anna Hormes. "RECORDS OF NEOGLACIATION AT SCOTTBREEN AND ON THE TRESKELEN PENINSULA, WESTERN SVALBARD." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272764.

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2

Muscott, Amelia, Darren J. Larsen, and Sarah Crump. "A CONTINUOUS RECORD OF HOLOCENE PALEOENVIRONMENTS AND NEOGLACIATION IN THE TETON RANGE, WYOMING, FROM ALPINE LAKE SEDIMENTS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383472.

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3

Peteet, Dorothy M., Jonathan Nichols, Jonathan Nichols, Daniel H. Mann, Daniel H. Mann, Miriam C. Jones, and Miriam C. Jones. "COASTAL ALASKA AND COASTAL EASTERN US PALEOECOLOGY/PALEOCLIMATE - HOW DO DEGLACIATION, COLONIZATION, YOUNGER DRYAS, NORTHWARD TREE MIGRATION, HOLOCENE THERMAL MAXIMUM, NEOGLACIATION, AND PEAT FORMATION COMPARE?" In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306176.

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