Modélisation des variations géodésiques induites ... - Etienne Berthier

-0,26 µGal/mm. Non uniform. 47 cm/yr. 75 cm/yr. Thinning. SVAL no topo. DCW no topo. SVAL + TOPO. DCW + SPIRIT +. GTOPO30. GIA. Ground observations.
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Secular gravity variations at Svalbard, Norway, from ground and satellite data: effects of glacier topography

SPIRIT Workshop 28-29/04/2010

(1)

A. Mémin(1) J. Hinderer(1) Y. Rogister(1) O.C. Omang(2)

Institut de Physique du Globe de Strasbourg, France (2) Norwegian Mapping Authority, Norway

Outline

Introduction Ground observations Satellite observations Ground/Satellite agreement Conclusions

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Outline

Introduction Ground observations Satellite observations Ground/Satellite agreement Conclusions

3

Introduction

Svalbard Archipelago ~36,000 km2 of ice => ~60% of its total area

4

Introduction

The last deglaciation at Svalbard

Present

18000 years ago

Berger (1992) 5

Introduction

Present-day ice mass change (PDIMC) at Svalbard

Midtre Lovénbreen : 2003-2005

Slakbreen : 1990-2003

Kohler & al.(2008) Ice loss at Midtre Lovénbreen: 1936-1962: 1962-1969: 1995-2003: 2003-2005:

~15 ~20 ~52 ~69

cm/yr cm/yr cm/yr cm/yr

Kääb & al.(2008) Nuth & al.(2010)

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Introduction

Ny-Ålesund observatory, Svalbard Station - 3 GPS, VLBI, Doris, - absolute and relative gravimeters, - tige gauges. Crédit NSPO / Distribution Spot Image / Traitement CNRS-LEGOS

Ny-Ålesund

Midtre Lovénbreen

2 GPS, FG5, SG GPS

VLBI

Tides gauges

Doris

Kierulf & al.(2009)->

L&R

7

Outline

Introduction Ground observations Satellite observations Ground/Satellite agreement Conclusions

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Ground observations

Absolute gravimetry (FG5) * Corrections - Free air gradient,

*

- Polar motion, *

- Observed tides+OTL, - Pressure.

* *

Linear trend: -1,02 ± 0,48 µGal/yr

*Sato & al. (2006)9

Ground observations

Relative gravimetry (GWR) : GWR --- : -1,02 µGal/yr : FG5

Corrections and treatment -

same as AG, degree-3 polynomial filtering with a 48h windows, 5 offsets, linear drift of 1,81 µGal/yr.

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Ground observations

Glacial isostatic adjustment (GIA)

Contribution to ground observations

Ny-Ålesund: 1,88 mm/yr and -0,31 µGal/yr (Sato & al., 2006) νum = 5.1020 Pa.s, νlm = 1022 Pa.s, litho = 100 km

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Ground observations

PDIMC models Thinning rates + -

Area covered by ice

Nuth & al. Dowdeswell Uniform of Uniform of

(2010) + Kohler & al.(2007) & al.(2008), 47 cm/yr, Sato & al. (2006) 75 cm/yr.

SVAL

DCW + SPIRIT m/yr

-- SVAL (Hagedoorn & Wolf, 2003), -- Digital Chart of the World (DCW) + SPIRIT product (Korona & al., 2009).

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Ground observations

Altitude of thinning areas

SVAL Sign of Δg Mass loss Mass accumulation

m

+

+ -

DCW + SPIRIT + GTOPO30 13

Ground observations

Deformation and gravity variation

the last deglaciation

present-day ice mass change

Uplift velocity:

uv

Gravity variation:

gv

ge + gn

gv/uv = -0.15 μGal/mm (Wahr & al., 1995)

(ge + gn)/ue = -0.26 μGal/mm (de Linage & al., 2007)

Ratio:

Observations: n=96

ue

uv + ue = uobs gv + ge + gn = gobs 14

Ground observations

Modeling and observations

GIA -0,15 µGal/mm

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Ground observations

Modeling and observations

GIA -0,15 µGal/mm

-0,26 µGal/mm

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Ground observations

Modeling and observations SVAL no topo

GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

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Ground observations

Modeling and observations SVAL no topo DCW no topo GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

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Ground observations

Modeling and observations SVAL no topo DCW no topo SVAL + TOPO GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

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Ground observations

Modeling and observations SVAL no topo DCW no topo SVAL + TOPO DCW + SPIRIT + GTOPO30

GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

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Ground observations

Modeling and observations SVAL no topo DCW no topo SVAL + TOPO DCW + SPIRIT + GTOPO30

GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

Observation Uplift velocity from Sato & al. (2006)

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Ground observations

Modeling and observations SVAL no topo DCW no topo SVAL + TOPO DCW + SPIRIT + GTOPO30

GIA -0,15 µGal/mm

Thinning 75 cm/yr 47 cm/yr Non uniform

-0,26 µGal/mm

Observation Uplift velocity from Sato & al. (2006)

Ice loss: ~25 km3/yr 22

Outline

Introduction Ground observations Satellite observations Ground/Satellite agreement Conclusions

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Satellite GRACE trends January 2003/January 2008

CSR

GRGS

*Swenson & Wahr, 2006

Cosine taper (30-50) Destriping filter*

observations

GFZ

n = 50

Mean

µGal/yr

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Satellite observations

Glacial isostatic adjustment (GIA) Contribution to satellite data from SELEN (Spada & Stocchi, 2007) νum = 5.1020 Pa.s, νlm = 1022 Pa.s, litho = 100 km

(Sato & al., 2006) ICE-3G

GRACE-GIA

µGal/yr 25

Satellite observations

PDIMC and GRACE

m/yr

-75 cm/a

µGal/yr

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Satellite observations

~13 km3/yr

GRACE - GIA - PDIMC CSR

GFZ

Ice loss

~25 km3/yr

~15 km /yr 3

µGal/yr

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Outline

Introduction Ground observations Satellite observations Ground/Satellite agreement Conclusions

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Ground/Satellite agreement

Ice basins (DCW+SPIRIT)

Ice thickness variation Nuth Kohler Moholdt Kierulf

& & & &

al. al. al. al.

(2010) (2007) (2009) (2009)

Ground/Satellite agreement

Modeling and observations SVAL no topo DCW no topo SVAL + TOPO DCW + SPIRIT + GTOPO30

GIA

Thinning 75 cm/yr 47 cm/yr

Ice loss: ~15.7 km3/yr

Non uniform Observation Uplift velocity from Sato & al. (2006)

Ice loss: ~25 km3/yr 30

Outline

Introduction Ground observations Satellite Observations Ground/Satellite agreement Conclusions

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Conclusions

Ground Gravity observations Good agreement between absolute and relative gravity measurements: -1.02 +/- 0.48 µGal/yr. => Modeled ice loss: ~25 km3/yr. Satellite Gravity observations GIA must be considered to study PDIMC in Svalbard from GRACE data. => Modeled ice loss: ~13-15 km3/yr. Topography of glaciers Need to be taken into account to estimate gravity variations due to ice mass change. Can lead to better agreement between ground and satellite data. 32

Thank you

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More…

More... On GRACE solutions On the uplift observed at Ny-Alesund

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GRACE trends January 2003/January 2008 CSR

GRGS

Cosine taper (30-50)

n = 50

µGal/yr

On GRACE solutions

GFZ

GFZ Mean

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On the uplift observed at Ny-Alesund

GPS, VLBI, Doris Sato & al. (2006)

5.2 mm/yr VLBI : 1994-2004 NYA1 : 1998-2004 NALL : 1991-2004

Keirulf & al. (2009) D’après Altamimi & al. (2007)

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On the uplift observed at Ny-Alesund Keirulf & al. (2009)

Inst.

Période

PPP

DD

NYAL

-2003

8

6,5

NYA1

-2003

8,6

4,7

NYALES20

-2003

NYAL

2003-

13,3

8,9

NYA1

2003-

13,2

9,1

NYALES20

2003-

7,3

9,9

Doris Ign09wd01 : 1993-1999: 6.2 +/- 0.6

mm/yr

1999-2003: -0.3 +/- 0.9 mm/yr 2003-2009: 6.2 +/- 0.3

mm/yr

Up (mm/yr) 37