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Record #112043:
- #112043
Main publication details
MARC recordEstimating errors in velocities and stresses calculated at depth in glacier / David B. Bahr.
| Title: | Estimating errors in velocities and stresses calculated at depth in glacier / David B. Bahr. |
| Author(s): | Bahr, David B. |
| Date: | 1991. |
| In: | Eos : transactions, American Geophysical Union. (1991.), Vol. 72(44, supplement) (1991) |
| Abstract: | AGU Fall Meeting Program and Abstracts, December 9-13, 1991. Errors at depth are introduced by errors in surface boundary condition data. By specifying delta perturbations in stresses at surface, new "top-down" model may be used to calculate Green's functions at glacier bed, which can induce such delta perturbations at surface. By convolving over Green's functions, estimates of surface data error are then used to estimate error distributions at glacier bed and thereby place bounds on accuracy of velocities and stresses at depth. |
| Notes: | Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :171 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.324.51 -- Land ice, theory of flow. 539.42 -- Ice, tensile strength. 519.673 -- Modelling. E5 -- Glaciology: land ice. |
| SPRI record no.: | 112043 |
LDR 01452naa#a2200000#a#4500 001 SPRI-112043 005 20230331204351.0 007 ta 008 230331s1991####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-112043 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBahr, David B. 245 10 ‡aEstimating errors in velocities and stresses calculated at depth in glacier /‡cDavid B. Bahr. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 171. 500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(44, supplement) :171 (1991). 520 3# ‡aAGU Fall Meeting Program and Abstracts, December 9-13, 1991. Errors at depth are introduced by errors in surface boundary condition data. By specifying delta perturbations in stresses at surface, new "top-down" model may be used to calculate Green's functions at glacier bed, which can induce such delta perturbations at surface. By convolving over Green's functions, estimates of surface data error are then used to estimate error distributions at glacier bed and thereby place bounds on accuracy of velocities and stresses at depth. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.51 -- Land ice, theory of flow.‡2udc 650 07 ‡a539.42 -- Ice, tensile strength.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230331