• Aucun résultat trouvé

Gravity field recovery in high latitude areas

N/A
N/A
Protected

Academic year: 2021

Partager "Gravity field recovery in high latitude areas"

Copied!
17
0
0

Texte intégral

(1)

Gravity field recovery Gravity field recovery

in in

high latitude areas high latitude areas

M. Weigelt, W. Keller, N. Sneeuw M. Weigelt, W. Keller, N. Sneeuw

[email protected]

Geodätische Woche 2007 - Geodetic Week 2007

Session 1

(2)

Outline

Motivation for local gravity field recovery Slepian functions - an empirical base

Approach

Properties

Test Scenario: CHAMP in high latitude areas

(3)

Motivation – Influence of the ground track

June 2003 January 2003

Error spectrum:

Ground track:

(4)

Motivation – Data density

January 2003 June 2003

(5)

Slepian functions

Spatial concentration of bandlimited functions (Simons et al. 2005) :

given:

approach:

• yields an algebraic eigenvalue problem:

λ g = D g with D =

R

Y lm Y nk d Ω

S =

L

l =0

l

m = − l

g lm Y lm

λ =

R S 2 d Ω

Ω S 2 d Ω = maximum

− 1

(6)

Potential and Orthogonality Slepian representation of the potential :

double orthogonality (Gilbert & Slepian 1977)

T = GM R

(L+1)

2

i=1

β i S i = GM R

(L+1)

2

i=1

β i

L

l=0

l

m= − l

R

r

l+1

g lm i Y lm

g lm i g lm j d Ω = δ ij

g lm i g lm j d Ω = λ ij δ ij

(7)

Localization property

indication of spatial concentration by eigenvalues

(8)

Spherical harmonics ↔ Slepian coefficients transformation:

influence of one Slepian coefficient, e.g., :

β i =

L

l=0

l

m= − l

K lm g i lm K lm =

( L +1)

2

i =1

β i g lm i

g lm 3

(9)

Edge effect

(10)

Test scenario

monthly CHAMP solutions in high-latitude areas residual signal:

GGM02s as reference

T ( λ, φ, r ) − T Lmax SH ( λ, φ, r )

(11)

Processing scheme

Energy balance approach

Slepian analysis Spherical harmonic

analysis

GGM02s

+ _

_

+ +

+ _ +

long wavelength part

transformation

(12)

Spherical harmonic vs. Slepian functions w.r.t. GGM02s

(13)

Spherical harmonic vs. Slepian functions w.r.t. GGM02s

(14)

Spherical harmonic vs. Slepian functions w.r.t. GGM02s

(15)

Affected coefficients

January 2003

June 2003

(16)

Conclusions

Slepian functions as a empiricial base function

• maximum spatial concentration of a bandlimited function

• double orthogonality

• spatial concentration indicated by eigenvalue

improvement in high latitude areas

dependency on a priori information (edge effect)

(17)

Gravity field recovery Gravity field recovery

in in

high latitude areas high latitude areas

M. Weigelt, W. Keller, N. Sneeuw M. Weigelt, W. Keller, N. Sneeuw

[email protected]

Geodätische Woche 2007 - Geodetic Week 2007 Session 1

THANK YOU

Références

Documents relatifs

Radial gravity gradient signal resulting from 0.5 m/yr ice mass change over East and South-East Greenland... PSD of radial gravity gradient signal resulting from 0.5 m/yr

The combination of terrestrial observations with superconducting gravimeters (SG) and repeated absolute gravity measurements (AG) offers the unique opportunity to

ˇSvehla, CHAMP gravity field recovery using the energy bal- ance approach, Adv. Reubelt, Gross erorr compensation for gravity filed analysis based on kinematic orbit

For this, 45 GRACE monthly spherical harmonic solutions are transformed into the Slepian domain and the estimation of a trend and annual cycle is compared with

Hussein Amin El Sayed, Alain Jacot, Eric Feulvarch, Frédéric Boitout, Jean-Michel Bergheau, Jean-Baptiste Leblond.. To cite

The 5 populations that evolved a stable cross-feeding in the periodic environment were propagated in a continuous environment at two different stages of their evolution: (i) just

Current dataflow systems use a range of techniques for distribution. Checkpointing is a popular method for fault tolerance: Naiad uses logical timestamps for

Au premier cycle, la tâche principale des profes seurs est centrée sur l’enseignement. Néanmoins, il semble que cette fonction d’enseignement soit l’acti vité la moins