Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Reinwarth, O."'
Publikováno v:
Ann. Glaciol. 35, 195-201 (2002)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3474::2f4bccc5bc20631850d9779ff95e9a4d
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=22265
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=22265
Autor:
Escher-Vetter, H., Reinwarth, O.
Publikováno v:
EPIC3Zeitschrift für Gletscherkunde und Glazialgeologie, 30, pp. 53-98
This report summarizes the runoff data collected at the "Pegelstation Vernagtbach" in the Oetztal Alps, Tyrol. The drainage basin controlled by the Station Covers 11.44 km2, of which 81 % is glacierized by Vernagtferner and hasan altitudinal ränge f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______999::f627486d0d78964d4661607740aa23a2
https://hdl.handle.net/10013/epic.38520
https://hdl.handle.net/10013/epic.38520
Publikováno v:
EPIC3Annals of Glaciology, 20, pp. 121-128, ISBN: 0 946417 14 8
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______999::e3a3c47d63f94b864f437b2c73b77f34
https://hdl.handle.net/10013/epic.11645
https://hdl.handle.net/10013/epic.11645
Publikováno v:
Ann. Glaciol. 14, 90-93 (1990)
The core was stratigraphically dated using seasonal variations of 18O content. The mean 18O content of the annual layers calculated on the basis of this dating decreases with depth z according to δ18O (‰) = -27.3 - 0.049z (m). Corrected δ18O valu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3474::cefe977c216aac7137ecb3e060b29d2a
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=42040
https://push-zb.helmholtz-muenchen.de/frontdoor.php?source_opus=42040
Akademický článek
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Autor:
Ahnert, F., Gerstenhauer, A., Kreuser, Th., de Dapper, M., Wopfner, I., Brunnacker, K., Fischer, K., Paskoff, R., Klug, H., Hövermann, J., Reinwarth, O., Felix-Henningsen, P., Mensching, H. G., Schmidt, K.-H., Liedtke, H.
Publikováno v:
Zeitschrift für Geomorphologie; May 1991, Vol. 35 Issue: 1 p117-128, 12p
Publikováno v:
EPIC3Annals of Glaciology, 11, pp. 23-31, ISSN: 0260-3055
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______999::b99d90dc516e6b910f78910d5c38773d
https://hdl.handle.net/10013/epic.25953
https://hdl.handle.net/10013/epic.25953
Publikováno v:
EPIC3Zeitschrift für Gletscherkunde und Glazialgeologie, 1, pp. 65-83
From 1974 to 1982 repeated tracer tests using fluorescent dyes were carried out in the highly glaciated drainage basin of Vernagtbach. These tests enabled the quantitative determination of the runoff in the forefield of the Vernagtferner, the calcula
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______999::69a34d76e370d66e5145b36ae57bcee3
https://hdl.handle.net/10013/epic.38457
https://hdl.handle.net/10013/epic.38457
Autor:
Fuchs, G., Gerdau, H., Henning, K., Klapdor, N., Kohnen, H., M��ller, D., Reinwarth, O., Suhrmeyer, L.
Polarforschung
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78d588f389d9052d97a5ebdc8d25a0fe
Polarforschung
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d260f1a2cd94314fd77a3c73741b7230