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Volumn 22, Issue , 1996, Pages 102-106

Glacial cirque formation in northern Scandinavia

Author keywords

[No Author keywords available]

Indexed keywords

CIRQUE FORMATION; GLACIAL EROSION; SNOW;

EID: 0030439840     PISSN: 02603055     EISSN: None     Source Type: Journal    
DOI: 10.1017/s0260305500015275     Document Type: Article
Times cited : (26)

References (12)
  • 1
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    • (1972) Z. Geomorphol. , Issue.13 SUPPLEMENTBAND , pp. 1-17
    • Andrews, J.T.1
  • 2
    • 0008805837 scopus 로고
    • Der Einfluss des Windes auf die Verteilung der Gletscher
    • Enquist, F. 1916. Der Einfluss des Windes auf die Verteilung der Gletscher. Medd. Uppsala Univ. Geol. Inst., 14, 1-108.
    • (1916) Medd. Uppsala Univ. Geol. Inst. , vol.14 , pp. 1-108
    • Enquist, F.1
  • 3
    • 0001699234 scopus 로고
    • World-wide variations in the direction and concentration of cirque and glacier aspects
    • Evans, I. S. 1977. World-wide variations in the direction and concentration of cirque and glacier aspects. Geogr. Ann., 59A(3-4), 151-175.
    • (1977) Geogr. Ann. , vol.59 A , Issue.3-4 , pp. 151-175
    • Evans, I.S.1
  • 4
    • 0027629064 scopus 로고
    • Glacier study using wavenumber domain synthetic aperture radar
    • Hamran, S.-E. and E. Aarholt. 1993. Glacier study using wavenumber domain synthetic aperture radar. Radio Sci., 28(4), 559-570.
    • (1993) Radio Sci. , vol.28 , Issue.4 , pp. 559-570
    • Hamran, S.-E.1    Aarholt, E.2
  • 5
    • 0028974733 scopus 로고
    • Ground penetrating synthetic pulse radar: Dynamic range and modes of operation
    • Hamran, S.-E., D. T. Gjessing, J. Hjelmstad and E. Aarholt. 1995. Ground penetrating synthetic pulse radar: dynamic range and modes of operation. J. Appl. Geophys., 33, 7-14.
    • (1995) J. Appl. Geophys. , vol.33 , pp. 7-14
    • Hamran, S.-E.1    Gjessing, D.T.2    Hjelmstad, J.3    Aarholt, E.4
  • 6
    • 0002991473 scopus 로고
    • Erosion rate of a Younger Dryas cirque glacier at Kråkenes, western Norway
    • Larsen, E. and J. Mangerud. 1981. Erosion rate of a Younger Dryas cirque glacier at Kråkenes, western Norway. Ann. Glaciol., 2, 153-158.
    • (1981) Ann. Glaciol. , vol.2 , pp. 153-158
    • Larsen, E.1    Mangerud, J.2
  • 7
    • 84879883931 scopus 로고
    • Holocene glacier and climatic variations in western Norway: Evidence for early Holocene glacier demise and multiple Neoglacial events
    • Nesje, A. and M. Kvamme. 1991. Holocene glacier and climatic variations in western Norway: evidence for early Holocene glacier demise and multiple Neoglacial events. Geology, 19, 610-612.
    • (1991) Geology , vol.19 , pp. 610-612
    • Nesje, A.1    Kvamme, M.2
  • 8
    • 0024782514 scopus 로고
    • Some geological implications of average Quaternary glacial conditions
    • Porter, S. C. 1989. Some geological implications of average Quaternary glacial conditions. Quat. Res., 32(3), 245-261.
    • (1989) Quat. Res. , vol.32 , Issue.3 , pp. 245-261
    • Porter, S.C.1
  • 9
    • 0027094952 scopus 로고
    • Multiple glaciation in Scandinavia - Seen in gross morphology or not?
    • Rudberg, S. 1992. Multiple glaciation in Scandinavia - seen in gross morphology or not? Geogr. Ann., 74A(2-3), 231-243.
    • (1992) Geogr. Ann. , vol.74 A , Issue.2-3 , pp. 231-243
    • Rudberg, S.1
  • 10
    • 0028579185 scopus 로고
    • Glacial cirques in Scandinavia
    • Rudberg, S. 1994. Glacial cirques in Scandinavia. Nor. Geogr. Tidsskr., 48(4), 179-197.
    • (1994) Nor. Geogr. Tidsskr. , vol.48 , Issue.4 , pp. 179-197
    • Rudberg, S.1
  • 11
    • 7444254869 scopus 로고    scopus 로고
    • Suspended sediment transport in the Storglaciären drainage basin
    • In press
    • Schneider, T. and C. Bronge. In press. Suspended sediment transport in the Storglaciären drainage basin. Geogr. Ann.
    • Geogr. Ann.
    • Schneider, T.1    Bronge, C.2
  • 12
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    • The cirque forms of Swedish Lapland
    • Vilborg, L. 1977. The cirque forms of Swedish Lapland. Geogr. Ann., 59A(3-4), 89-150.
    • (1977) Geogr. Ann. , vol.59 A , Issue.3-4 , pp. 89-150
    • Vilborg, L.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.