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Record #88584:

Observations at a steep high-altitude Norwegian glacier, Charles Rabots Bre, 1970-1985 / Wilfred H. Theakstone, N. Tvis Knudsen.

Title: Observations at a steep high-altitude Norwegian glacier, Charles Rabots Bre, 1970-1985 / Wilfred H. Theakstone, N. Tvis Knudsen.
Author(s): Theakstone, Wilfred H.
Knudsen, N. Tvis.
Date: 1987.
In: Zeitschrift für Gletscherkunde und Glazialgeologie. (1987.), Vol. 23(2) (1987)
Abstract: Positive mass balance in three of four years between 1970 and 1974; since then, glacier has been snow-covered throughout ablation seasons, ice having been exposed only at steepest section. In early 1970s, surface velocity at lower end of glacier's upper basin decreased down-glacier from 9 to 2 m a⁻¹ in distance of 200 m. Velocities over lower glacier were <0.5 m a⁻¹. Re-survey of surviving stakes in 1985 revealed that surface velocities on lower glacier had averaged <0.1 m a⁻¹ in preceding 15 years and that changes of thickness were equivalent to specific net mass-balance values at sites, indicating that ice deformation since 1970 had been negligible.
Notes:

Zeitschrift für Gletscherkunde und Glazialgeologie. Vol. 23(2) :155-163 (1987).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.43 -- Land ice, regime and mass balance: Charles Rabot Bre.
551.324.54 -- Land ice, flow of particular glaciers: Charles Rabot Bre.
E6 -- Glaciology: floating ice.
(*586) -- Nordland.
(*58) -- Norway.
SPRI record no.: 88584

MARCXML

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035 ## ‡aSPRI-88584
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100 1# ‡aTheakstone, Wilfred H.
245 10 ‡aObservations at a steep high-altitude Norwegian glacier, Charles Rabots Bre, 1970-1985 /‡cWilfred H. Theakstone, N. Tvis Knudsen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1987.
300 ## ‡ap. 155-163 :‡bill., diags., maps.
500 ## ‡aZeitschrift für Gletscherkunde und Glazialgeologie. Vol. 23(2) :155-163 (1987).
520 3# ‡aPositive mass balance in three of four years between 1970 and 1974; since then, glacier has been snow-covered throughout ablation seasons, ice having been exposed only at steepest section. In early 1970s, surface velocity at lower end of glacier's upper basin decreased down-glacier from 9 to 2 m a⁻¹ in distance of 200 m. Velocities over lower glacier were <0.5 m a⁻¹. Re-survey of surviving stakes in 1985 revealed that surface velocities on lower glacier had averaged <0.1 m a⁻¹ in preceding 15 years and that changes of thickness were equivalent to specific net mass-balance values at sites, indicating that ice deformation since 1970 had been negligible.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance: Charles Rabot Bre.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers: Charles Rabot Bre.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*586) -- Nordland.‡2udc
651 #7 ‡a(*58) -- Norway.‡2udc
700 1# ‡aKnudsen, N. Tvis.
773 0# ‡7nnas ‡tZeitschrift für Gletscherkunde und Glazialgeologie. ‡gVol. 23(2) (1987) ‡wSPRI-21702
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230331