Articles | Volume 10, issue 1
https://doi.org/10.5194/tc-10-103-2016
https://doi.org/10.5194/tc-10-103-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Feasibility of improving a priori regional climate model estimates of Greenland ice sheet surface mass loss through assimilation of measured ice surface temperatures

M. Navari, S. A. Margulis, S. M. Bateni, M. Tedesco, P. Alexander, and X. Fettweis

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Cited articles

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Bamber, J. L. and Layberry, R. L.: 1. Measurement, data reduction, and errors ice sheet was reestimated and found to have a value at a sample, J. Geophys. Res., 106, 33773–33780, 2001.
Bateni, S., Huang, C., and Margulis, S.: Feasibility of Characterizing Snowpack and the Freeze–Thaw State of Underlying Soil Using Multifrequency Active/Passive Microwave Data, IEEE T. Geosci. Remote, 51, 4085–4102, 2013.
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Short summary
An ensemble batch smoother was used to assess the feasibility of generating a reanalysis estimate of the Greenland ice sheet (GrIS) surface mass fluxes (SMF) via integrating measured ice surface temperatures with a regional climate model estimate. The results showed that assimilation of IST were able to overcome uncertainties in meteorological forcings that drive the GrIS surface processes. We showed that the proposed methodology is able to generate posterior reanalysis estimates of the SMF.