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Record #101916:

Strain rates of a 25 m deep firn pit in an Alpine glacier and a related constitutive equation of temperate firn (Kesselwandferner, Oetztal Alps, 1983-1989) / Walter Ambach, H. Eisner, J. Huber, H. Schneider.

Title: Strain rates of a 25 m deep firn pit in an Alpine glacier and a related constitutive equation of temperate firn (Kesselwandferner, Oetztal Alps, 1983-1989) / Walter Ambach, H. Eisner, J. Huber, H. Schneider.
Author(s): Ambach, Walter.
Eisner, H.
Huber, J.
Schneider, H.
Date: 1989.
In: Zeitschrift für Gletscherkunde und Glazialgeologie. (1989.), Vol. 25(2) (1989)
Abstract: Published in 1992. Deformation measurements carried out in central part of accumulation area. From measured strain rates and stress conditions in situ, constitutive equation for temperate firn was derived as function of snow density. Equation is composed of two parts: first describes changes in shape with constant volume, and second describes changes in volume with constant shape. Constitutive equation reduces to Glen's flow law for incompressible ice as limiting case.
Notes:

Zeitschrift für Gletscherkunde und Glazialgeologie. Vol. 25(2) :187-198 (1989).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers.
551.578.46 -- Snow cover and snow patches.
539.37 -- Ice, plastic and viscous deformation.
551.42 -- Islands.
551.324.54 -- Land ice, flow of particular glaciers: Kesselwandferner.
E5 -- Glaciology: land ice.
(436) -- Austria.
(234.3) -- Alps.
SPRI record no.: 101916

MARCXML

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245 00 ‡aStrain rates of a 25 m deep firn pit in an Alpine glacier and a related constitutive equation of temperate firn (Kesselwandferner, Oetztal Alps, 1983-1989) /‡cWalter Ambach, H. Eisner, J. Huber, H. Schneider.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1989.
300 ## ‡ap. 187-198 :‡bdiags.
500 ## ‡aZeitschrift für Gletscherkunde und Glazialgeologie. Vol. 25(2) :187-198 (1989).
520 3# ‡aPublished in 1992. Deformation measurements carried out in central part of accumulation area. From measured strain rates and stress conditions in situ, constitutive equation for temperate firn was derived as function of snow density. Equation is composed of two parts: first describes changes in shape with constant volume, and second describes changes in volume with constant shape. Constitutive equation reduces to Glen's flow law for incompressible ice as limiting case.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a539.37 -- Ice, plastic and viscous deformation.‡2udc
650 07 ‡a551.42 -- Islands.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers: Kesselwandferner.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(436) -- Austria.‡2udc
651 #7 ‡a(234.3) -- Alps.‡2udc
700 1# ‡aAmbach, Walter.
700 1# ‡aEisner, H.
700 1# ‡aHuber, J.
700 1# ‡aSchneider, H.
773 0# ‡7nnas ‡tZeitschrift für Gletscherkunde und Glazialgeologie. ‡gVol. 25(2) (1989) ‡wSPRI-21702
917 ## ‡aUnenhanced record from Muscat, imported 2019
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