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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/tcd-3-181-2009</doi>
	<article_url>http://www.the-cryosphere-discuss.net/3/181/2009/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/3/181/2009/tcd-3-181-2009.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/3/181/2009/tcd-3-181-2009.pdf</fulltext_pdf>
	<start_page>181</start_page>
	<end_page>222</end_page>
	<publication_date>2009-02-05</publication_date>
	<article_title content_type="html">Estimating basal properties of glaciers from surface measurements:  a non-linear Bayesian inversion approach</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. J. Raymond</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. H. Gudmundsson</name>
			<email>ghg@bas.ac.uk</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie (VAW), ETH Zürich, 8092 Zürich, Switzerland</affiliation>
		<affiliation numeration="2" content_type="html">British Antarctic Survey, High Cross, Madingley Rd., Cambridge CB3 0ET, UK</affiliation>
	</affiliations>
	<abstract content_type="html">We propose a new approach to indirectly estimate basal properties of
a glacier, i.e. bedrock topography and basal slipperiness, from
observations of surface topography and surface velocities. We
demonstrate how a maximum a posteriori estimate of basal conditions
can be determined using a Bayesian inference approach in a
combination with an analytical linearisation of the forward
model. Using synthetic data we show that for non-linear media and
non-linear sliding law only a few forward-step model evaluations are
needed for convergence.  The forward step is solved with a numerical
finite-element model using the full Stokes equations. Forward Fréchet
derivatives are approximated through analytical small-perturbation
solutions. This approximation is a key feature of the method and the
effects of this approximation on model performance are analyzed. The number
of iterations needed for convergence increases with the amplitude of the basal
perturbations, but generally less than ten iterations are needed.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Gouveia, W P. and Scales, J A.: Bayesian seismic waveform inversion: Parameter estimation and uncertainty analysis, J. Geophys. Res., 103, 2759–2780, doi:10.1029/97JB02933, 1998. </reference>
		<reference numeration="2" content_type="text"> Gudmundsson, G H.: Transmission of basal variability to a glacier surface, J. Geophys. Res., 108(B5), 2253, doi:10.129/2002JB002107, 2003. </reference>
		<reference numeration="3" content_type="text"> Gudmundsson, G H.: Glacier Science and Environmental Change, chap.\ Estimating basal properties of glaciers from surface measurements, Blackwell Publishing, Oxford, p. 415, 2006. </reference>
		<reference numeration="4" content_type="text"> Gudmundsson, G H. and Raymond, M J.: On the limit to resolution and information on basal properties obtainable from surface data on ice streams, The Cryosphere Discuss., 2, 413–445, 2008. </reference>
		<reference numeration="5" content_type="text"> Hutter, K.: Theoretical glaciology; material science of ice and the mechanics of glaciers and ice sheets, D. Reidel Publishing Company/Tokyo, Terra Scientific Publishing Company, 1983. </reference>
		<reference numeration="6" content_type="text"> Joughin, I., MacAyeal, D R., and Tulaczyk, S.: Basal shear stress of the Ross ice streams from control method inversions, J. Geophys. Res., 109, B09405, doi:10.1029/2003JB002960, 2004. </reference>
		<reference numeration="7" content_type="text"> Kitanidis, A K.: Introduction to geostatistics: applications to hydrogeology, Cambridge University Press, 1997. </reference>
		<reference numeration="8" content_type="text"> Leysinger Vieli, G. J.-M C. and Gudmundsson, G H.: On estimating length fluctuations of glaciers caused by changes in climatic forcing, J. Geophys. Res., 109, F01007, doi:10.1029/2003JF000027, 2004. </reference>
		<reference numeration="9" content_type="text"> MacAyeal, D R.: The Basal Stress Distribution of Ice Stream E, Antarctica, inferred by control methods, J. Geophys. Res., 97, 596–603, 1992. </reference>
		<reference numeration="10" content_type="text"> MacAyeal, D R., Bindschadler, R A., and Scambos, T A.: Basal friction of Ice Stream E, West Antartica, J. Glaciol., 41, 247–262, 1995. </reference>
		<reference numeration="11" content_type="text"> Paterson, W. S B.: The physics of glaciers, Butterworth-Heinemann, Oxford, third edn., 1994. </reference>
		<reference numeration="12" content_type="text"> Raymond, M J.: Estimating basal properties of glaciers and ice streams from surface measurements, Mitteilung 202, VAW, 152 pp., 2007. </reference>
		<reference numeration="13" content_type="text"> Raymond, M J. and Gudmundsson, G H.: On the relationship between surface and basal properties on glaciers, ice sheets, and ice streams., J. Geophys. Res., 110, B08411, doi:10.1029/2005JB003681, 2005. </reference>
		<reference numeration="14" content_type="text"> Rodgers, C D.: Inverse Methods for Atmospheric Sounding. Theory and Practice, World Scientific Publishing Co. Pte. Ltd. Singapore, 2000. </reference>
		<reference numeration="15" content_type="text"> Smith, G D. and Morland, L W.: Viscous relations for the steady creep of polycrystalline ice, Cold Reg. Sci. Technol., 5, 141–150, 1981. </reference>
		<reference numeration="16" content_type="text"> Tarantola, A.: Inverse Problem Theory and Methods for Model Parameter Estimation, Society for Industrial and Applied Mathematics, 2005. </reference>
		<reference numeration="17" content_type="text"> Thorsteinsson, T., Raymond, C F., Gudmundsson, G H., Bindschadler, R B., Vornberger, P., and Joughin, I.: Bed topography and lubrication inferred from surface measurements on fast flowing ice streams, J. Glaciol., 49, 481–490, 2003. </reference>
		<reference numeration="18" content_type="text"> Truffer, M.: The basal speed of valley glaciers: an inverse approach, J. Glaciol., 50, 236–242, 2004. </reference>
		<reference numeration="19" content_type="text"> Van~der Veen, C J. and Whillans, I M.: Force Budget: I. Theory and Numerical Methods, J. Glaciol., 35, 53–60, 1989. </reference>
		<reference numeration="20" content_type="text"> Vieli, A. and Payne, A J.: Application of control methods for modelling the flow of Pine Island Glacier, West Antarctica, Ann. Glaciol., 36, 197–204, 2003. </reference>
	</references>
</article>

