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Record #199938:

Linear modelling of glacier length fluctuations / Johannes Oerlemans.

Title: Linear modelling of glacier length fluctuations / Johannes Oerlemans.
Author(s): Oerlemans, Johannes.
Date: 2012.
In: Geografiska Annaler. Series A. Physical Geography. (2012.), Vol. 94(2) (2012)
Abstract: Describes linear first-order differential equation, with two parameters, used to model glacier length fluctuations. In first parameter (climate sensitivity) adjacent glaciers, Hintereisferner and Kesselwandferner in Ötzal Alps, were considered. In second (response time) four glacier length records from Oberengadin, Switzerland, were used to reconstruct equilibrium-line histories. Results were inconclusive, being consistent for Austrian glaciers but contrary to Swiss climate data.
Notes:

Geografiska Annaler. Series A. Physical Geography. Vol. 94(2) :183-194 (2012).

In thematic issue The mountain cryosphere : a holistic view on processes and their interactions.

Keywords: 551.324.22 -- Glaciers: Hintereisferner.
551.324.22 -- Glaciers: Kesselwandferner.
519.673 -- Modelling.
551.321.5 -- Snow, ice and glacier movement.
551.324.43 -- Land ice, regime and mass balance.
551.324.6 -- Land ice, fluctuation.
551.324.63 -- Land ice, advance and retreat.
E5 -- Glaciology: land ice.
(234.3) -- Alps.
(4) -- Europe.
(436) -- Austria.
(494) -- Switzerland.
SPRI record no.: 199938

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100 1# ‡aOerlemans, Johannes.
245 10 ‡aLinear modelling of glacier length fluctuations /‡cJohannes Oerlemans.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2012.
300 ## ‡ap. 183-194 :‡bill., diags., map.
500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 94(2) :183-194 (2012).
500 ## ‡aIn thematic issue The mountain cryosphere : a holistic view on processes and their interactions.
520 3# ‡aDescribes linear first-order differential equation, with two parameters, used to model glacier length fluctuations. In first parameter (climate sensitivity) adjacent glaciers, Hintereisferner and Kesselwandferner in Ötzal Alps, were considered. In second (response time) four glacier length records from Oberengadin, Switzerland, were used to reconstruct equilibrium-line histories. Results were inconclusive, being consistent for Austrian glaciers but contrary to Swiss climate data.
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1468-0459.2012.00469.x‡uhttps://dx.doi.org/10.1111/j.1468-0459.2012.00469.x
650 07 ‡a551.324.22 -- Glaciers: Hintereisferner.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Kesselwandferner.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.321.5 -- Snow, ice and glacier movement.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(234.3) -- Alps.‡2udc
651 #7 ‡a(4) -- Europe.‡2udc
651 #7 ‡a(436) -- Austria.‡2udc
651 #7 ‡a(494) -- Switzerland.‡2udc
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917 ## ‡aUnenhanced record from Muscat, imported 2019
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