geos f493 / f693 geodetic methods and modeling [20pt ...2 love’s loading theory (spherical...

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GEOS F493 / F693 Geodetic Methods and Modeling – Lecture 12: Modeling - Surface Loading – Ronni Grapenthin [email protected] Elvey 413B (907) 474-7286 November 18, 2019 1 / 14

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Page 1: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

GEOS F493 / F693Geodetic Methods and Modeling

– Lecture 12: Modeling - Surface Loading –

Ronni [email protected]

Elvey 413B(907) 474-7286

November 18, 2019

1 / 14

Page 2: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

GUESS THE PROCESS!

UNAVCO 2 / 14

Page 3: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

GUESS THE PROCESS!

UNAVCO3 / 14

Page 4: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation

Grapenthin, 2014, Comp. & Geosc.

4 / 14

Page 5: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

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.

5 / 14

Page 6: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

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)

6 / 14

Page 7: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

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)

6 / 14

Page 8: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

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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Page 9: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Grapenthin et al., 2006, GRL

8 / 14

Page 10: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Pinel et al., 2007, GJI

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Page 11: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

2 Disk Loads – elastic response:

Pinel et al., 2007, GJI

10 / 14

Page 12: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Irregular Load outline – elastic response:

Pinel et al., 2007, GJI11 / 14

Page 13: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Irregular Load outline – final relaxed:

Pinel et al., 2007, GJI12 / 14

Page 14: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Irregular Load outline – annual rate given 115 yrs of ice thinning:

Pinel et al., 2007, GJI13 / 14

Page 15: GEOS F493 / F693 Geodetic Methods and Modeling [20pt ...2 Love’s loading theory (Spherical Harmonics) represent load in terms of spherical harmonic functions compute deformation

Loading Deformation: Examples

Formal inversion of vertical GPS for seasonal loading:

Argus et al., 2014, GRL

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