Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson...
-
Upload
alvin-powell -
Category
Documents
-
view
213 -
download
1
Transcript of Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson...
![Page 1: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/1.jpg)
Resolution and informational aspects of surface inversion on ice streams
G. Hilmar Gudmundsson
British Antarctic Survey, Cambridge, UK
Melanie Raymond,
Section of Glaciology, ETH, Switzerland
![Page 2: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/2.jpg)
![Page 3: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/3.jpg)
![Page 4: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/4.jpg)
The Bayesian approach
Forward model: (s,u,w)=f(b,c)
The Bayesian approach to inverse problem is to determine the
conditional probability P(b,c|s,v,w)
We look for a system state that maximizes this probability, and determine the pdf of that system
state. Requires covariance matrixes of measurements errors and a priorie.
Forward model: A full-system non-linear FE modelModel derivatives: Linear transfer functions
![Page 5: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/5.jpg)
Can slipperiness/bedrock perturbations be
misinterpreted as bedrock/slipperiness perturbations (mixing effects)?
Any fundamental limits to retrieval?
How is retrieval affected by the accuracy of measurements?
Questions:
![Page 6: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/6.jpg)
Bed-to-surface transfer function for a slip-ratio of 10 and surface slope 3 deg.
Raymond & Gudmundsson, JGR, 2005
Forward problem
Bed-to-surface transfer amplitudes on ice streams are large. This is good news for inversion
![Page 7: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/7.jpg)
surface data model bed properties errors
prior cov. model derivatives error cov.
Retrieval method
Model derivatives approximated using linear transfer functions
![Page 8: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/8.jpg)
Case study #1: Measurements of high quality • Data errors 1% of mean values
• Data points every 0.25 ice thickness
![Page 9: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/9.jpg)
Kernels give information about smoothing/resolution and mixing aspects of the retrieval methods. Ideally the bb and cc kernels would be diagonal
(perfect resolution), and bc and cb kernels zero (no mixing) Conclusion: b-perturbations resolved spatially about 10 times
better than c-perturbations. Mixing not a problem
Kernels for `high quality’ data in Fourier space
![Page 10: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/10.jpg)
Kernels for `high quality’ data in real space
Ideally the bb and cc kernels would be delta functions (perfect resolution), and bc and cb kernels zero (no mixing). The area (number in boxes) gives
the sensitivity of the retrieval to the data, as opposed to the a priori.
![Page 11: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/11.jpg)
Case study #2: Measurements of `average’ quality • Thickness errors 10%
• Velocity errors 1%• Data points every 0.25 ice thickness
![Page 12: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/12.jpg)
Kernels for `average quality’ data in Fourier space
b-perturbation retrieval similar to the `high quality’ case, but resolution of c-perturbation considerably worse than before and about 100 times poorer than for the b-perturbation. Mixing still
not a problem
![Page 13: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/13.jpg)
An example of a non-linear (n=3) finite-amplitude inversion
It is not obvious that using the linear-transfer functions as approximation of model derivatives of a non-linear forward model can work.
However, recent results obtained by Melanie Raymond (shown to the right) suggest that this is nevertheless the case. This makes inversion using a full-system non-linear forward model a feasible option.
![Page 14: Resolution and informational aspects of surface inversion on ice streams G. Hilmar Gudmundsson British Antarctic Survey, Cambridge, UK Melanie Raymond,](https://reader036.fdocuments.in/reader036/viewer/2022070401/56649f1f5503460f94c37765/html5/thumbnails/14.jpg)
Conclusion
•Mixing effects not a problem when solving for both
bedrock and slipperiness simultaneously
•Usefulness of basal slipperiness retrieval seems limited unless ice thickness known to better than
about 10%
•Spatial resolution of slipperiness retrieval about an
order of magnitude less than for a bed-line retrieval
Work that remains to be done: Amplitude effects, and effects due to rheological non-linearities