GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical...
Transcript of GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical...
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GEOS F493 / F693Geodetic Methods and Modeling
– Lecture 12: Modeling - Surface Loading –
Ronni [email protected]
Elvey 413B(907) 474-7286
November 18, 2019
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GUESS THE PROCESS!
UNAVCO 2 / 14
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GUESS THE PROCESS!
UNAVCO3 / 14
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Loading Deformation
Grapenthin, 2014, Comp. & Geosc.
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Computing Loading Deformation
1 Green’s function method (unit impulse responses)• compute deformation induced by point load, specific shape,
assume unit magnitude• convolve with actual spatial load (e.g., grid of point loads) with
respective Green’s function2 Love’s loading theory (Spherical Harmonics)
• represent load in terms of spherical harmonic functions• compute deformation with Love Numbers that depend on Earth
model
In practice Green’s functions often come from Love’s theory.
E.g., Spada, G., 2008. ALMA, a Fortran program for computing thevisco-elastic Love numbers of a spherically symmetric planet, Comput.and Geosci., v. 34 (6), 667-687, doi: 0.1016/j.cageo.2007.12.001.
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Green’s Functions
Grapenthin, 2014, Comp. & Geosc.
U(r) =
∫A
G(r − r ′)L(r ′)dS
U = G ∗ ∗L
• integrate over area A indifferential area steps dS
• "∗∗" is 2D convolutionoperation
Green’ Functions, e.g.:• Farrell 1972: elastic spherical Earth (tabulated GF)• Pinel et al. 2007: elastic, thick plate over visco-elastic fluid, flat
Earth (GF)• Comer, 1983: thin plate approximation (vertical normal stress=0)
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Green’s Functions
Grapenthin, 2014, Comp. & Geosc.
U(r) =
∫A
G(r − r ′)L(r ′)dS
U = G ∗ ∗L
• integrate over area A indifferential area steps dS
• "∗∗" is 2D convolutionoperation
Green’ Functions, e.g.:• Farrell 1972: elastic spherical Earth (tabulated GF)• Pinel et al. 2007: elastic, thick plate over visco-elastic fluid, flat
Earth (GF)• Comer, 1983: thin plate approximation (vertical normal stress=0)
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Green’s Functions - generic Formulation
Grapenthin, 2014, Comp & Geosc.:
Ut =n∑
i=1
[Gi ∗ ∗L] · (Ri ∗ Hi)t
• ∗ is convolution operator!• n total number of superpositions of different Green’s functions• R relaxation function (e.g., exponential decay, delta function), wrt
to Green’s function• H load history• notation allows very generalized implementation of this problem
(CrusDe).
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Loading Deformation: Examples
Grapenthin et al., 2006, GRL
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Loading Deformation: Examples
Pinel et al., 2007, GJI
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Loading Deformation: Examples
2 Disk Loads – elastic response:
Pinel et al., 2007, GJI
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Loading Deformation: Examples
Irregular Load outline – elastic response:
Pinel et al., 2007, GJI11 / 14
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Loading Deformation: Examples
Irregular Load outline – final relaxed:
Pinel et al., 2007, GJI12 / 14
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Loading Deformation: Examples
Irregular Load outline – annual rate given 115 yrs of ice thinning:
Pinel et al., 2007, GJI13 / 14
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Loading Deformation: Examples
Formal inversion of vertical GPS for seasonal loading:
Argus et al., 2014, GRL
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