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Volumn 24, Issue , 1997, Pages 199-202

Numerical simulation of fluctuations of Hintereisferner, Ötztal Alps, since AD 1850

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EID: 0001205270     PISSN: 02603055     EISSN: None     Source Type: Journal    
DOI: 10.3189/s0260305500012179     Document Type: Article
Times cited : (15)

References (11)
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    • Hoinkes, H. 1970. Methoden und Möglichkeiten von Massenhaushalts-studien auf Gletschern. Ergebnisse der Messreihe Hintereisferner (Ötztaler Alpen) 1953-1968. Z. Gletscherkd. Glazialgeol., 6(1-2), 37-90.
    • (1970) Z. Gletscherkd. Glazialgeol. , vol.6 , Issue.1-2 , pp. 37-90
    • Hoinkes, H.1
  • 3
    • 0001768682 scopus 로고
    • Stress-gradient coupling in glacier flow: I. Longitudinal averaging of the influence of ice thickness and surface slope
    • Kamb, B. and K. A. Echelmeyer. 1986. Stress-gradient coupling in glacier flow: I. Longitudinal averaging of the influence of ice thickness and surface slope. J. Glaciol., 32(111), 267-284.
    • (1986) J. Glaciol. , vol.32 , Issue.111 , pp. 267-284
    • Kamb, B.1    Echelmeyer, K.A.2
  • 4
    • 0021532595 scopus 로고
    • Mass budget imbalances as criterion for a climatic classification of glaciers
    • Kuhn, M. 1984. Mass budget imbalances as criterion for a climatic classification of glaciers. Geogr. Ann., 66A(3), 229-238.
    • (1984) Geogr. Ann. , vol.66 A , Issue.3 , pp. 229-238
    • Kuhn, M.1
  • 5
    • 0001555394 scopus 로고
    • Multivariate statistical analysis of glacier annual balances
    • Lliboutry, L. 1974. Multivariate statistical analysis of glacier annual balances. J. Glaciol., 13(69), 371-392.
    • (1974) J. Glaciol. , vol.13 , Issue.69 , pp. 371-392
    • Lliboutry, L.1
  • 6
    • 0003111553 scopus 로고
    • Jahrringe und Massenbilanz: Dendroklimatologische Rekonstruktion der Massenbilanzreihe des Hintereisferners bis zum Jahr 100 mittels Pinus cembra-Reihen aus den Ötztaler Alpen
    • 1994
    • Nicolussi, K. 1995. Jahrringe und Massenbilanz: dendroklimatologische Rekonstruktion der Massenbilanzreihe des Hintereisferners bis zum Jahr 100 mittels Pinus cembra-Reihen aus den Ötztaler Alpen. Z. Gletscherkd. Glazialgeol., 30, 1994, 11-52.
    • (1995) Z. Gletscherkd. Glazialgeol. , vol.30 , pp. 11-52
    • Nicolussi, K.1
  • 7
    • 0000687404 scopus 로고
    • The flow of a glacier in a channel of rectangular, elliptic or parabolic cross-section
    • Nye, J. F. 1965. The flow of a glacier in a channel of rectangular, elliptic or parabolic cross-section. J. Glaciol., 5(41), 661-690.
    • (1965) J. Glaciol. , vol.5 , Issue.41 , pp. 661-690
    • Nye, J.F.1
  • 8
    • 0022846480 scopus 로고
    • An attempt to simulate historic from variations of Nigardsbreen, Norway
    • Oerlemans, J. 1986. An attempt to simulate historic from variations of Nigardsbreen, Norway. Theor. Appl. Climatol., 37(3), 126-135.
    • (1986) Theor. Appl. Climatol. , vol.37 , Issue.3 , pp. 126-135
    • Oerlemans, J.1
  • 10
    • 0019664812 scopus 로고
    • The derivation of past climate changes from observed changes of glaciers
    • Symposium at Canberra 1979 - Sea Level, Ice and Climatic Change
    • Smith, I. N. and W. F. Budd. 1981. The derivation of past climate changes from observed changes of glaciers. International Association of Hydrological Sciences Publication 131 (Symposium at Canberra 1979 - Sea Level, Ice and Climatic Change), 31-52.
    • (1981) International Association of Hydrological Sciences Publication 131 , pp. 31-52
    • Smith, I.N.1    Budd, W.F.2
  • 11
    • 0002580556 scopus 로고
    • Historic front variations of the Rhône Glacier: Simulation with an ice flow model
    • Oerlemans, J., ed. Dordrecht, etc., Kluwer Academic Publishers
    • Stroeven, A., R. van de Wal and J. Oerlemans. 1989. Historic front variations of the Rhône Glacier: simulation with an ice flow model. In Oerlemans, J., ed. Glacier fluctuations and climatic change. Dordrecht, etc., Kluwer Academic Publishers, 391-404.
    • (1989) Glacier Fluctuations and Climatic Change , pp. 391-404
    • Stroeven, A.1    Van De Wal, R.2    Oerlemans, J.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.