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Further Reading

Found 51 results
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Miege, C., Forster R., Brucker L., Koenig L., Solomon D. K., Paden J., et al. (2016).  Spatial extent and temporal variability of the Greenland firn aquifer detected by ground and airborne radars. J. Geophys. Res. Earth Surf.. 121,
Miege, C., Forster R., Brucker L., Koenig L., Solomon D. K., Paden J., et al. (2016).  Spatial extent and temporal variability of the Greenland firn aquifer detected by ground and airborne radars. J. Geophys. Res. Earth Surf.. 121,
Miege, C., Forster R., Brucker L., Koenig L., Solomon D. K., Paden J., et al. (2016).  Spatial extent and temporal variability of the Greenland firn aquifer detected by ground and airborne radars. J. Geophys. Res. Earth Surf.. 121,
Miege, C., Forster R., Brucker L., Koenig L., Solomon D. K., Paden J., et al. (2016).  Spatial extent and temporal variability of the Greenland firn aquifer detected by ground and airborne radars. J. Geophys. Res. Earth Surf.. 121,
Kidd, C., Becker A., Huffman G. J., Muller C. L., Joe P., Skofronick-Jackson G., et al. (2017).  So, How Much of the Earth’s Surface Is Covered by Rain Gauges? . Bull. Amer. Meteor. Soc. 98(1), 69-78.
Magand, O., Picard G., Brucker L., Fily M., & Genthon C. (2008).  Snow melting bias in microwave mapping of Antarctic snow accumulation. The Cryosphere. 2(2), 109-115.
Brucker, L., Picard G., & Fily M. (2010).  Snow grain size profile deduced from microwave snow emissivities in Antarctica. Journal of Glaciology. 56(197), 514-524.
Picard, G., Brucker L., Roy A., Dupont F., Fily M., Royer A., et al. (2013).  Simulation of the microwave emission of multi-layered snowpacks using the Dense Media Radiative transfer theory: the DMRT-ML model. Geosci. Model Dev.. 6, 1061-1078.
Langlois, A., Brucker L., Kohn J., Royer A., Derksen C., Cliche P., et al. (2009).  Simulation of snow water equivalent (SWE) using thermodynamic snow models in Québec, Canada. Journal of Hydrometeorology. 10(6), 1447-1463.
P
Tan, S., Aksoy M., Brogioni M., Macelloni G., Durand M., Jezek K. C., et al. (2015).  Physical Models of Layered Polar Firn Brightness Temperatures from 0.5 GHz to 2 GHz. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing. 8(7), 3681-3691.
Tan, S., Aksoy M., Brogioni M., Macelloni G., Durand M., Jezek K. C., et al. (2015).  Physical Models of Layered Polar Firn Brightness Temperatures from 0.5 GHz to 2 GHz. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing. 8(7), 3681-3691.