Variable penetration depth of interferometric synthetic aperture radar signals on Alaska glaciers: a cold surface layer hypothesis. Gusmeroli, A., Arendt, A., Atwood, D., Kampes, B., Sanford, M., & Young, J. C. Annals of Glaciology, 54(64):218–223, September, 2013.
Variable penetration depth of interferometric synthetic aperture radar signals on Alaska glaciers: a cold surface layer hypothesis [link]Paper  doi  bibtex   
@article{gusmeroli_variable_2013,
	title = {Variable penetration depth of interferometric synthetic aperture radar signals on {Alaska} glaciers: a cold surface layer hypothesis},
	volume = {54},
	issn = {02603055, 17275644},
	shorttitle = {Variable penetration depth of interferometric synthetic aperture radar signals on {Alaska} glaciers},
	url = {http://openurl.ingenta.com/content/xref?genre=article&issn=0260-3055&volume=54&issue=64&spage=218},
	doi = {10.3189/2013AoG64A114},
	language = {English},
	number = {64},
	urldate = {2014-05-30},
	journal = {Annals of Glaciology},
	author = {Gusmeroli, Alessio and Arendt, Anthony and Atwood, Donald and Kampes, Bert and Sanford, Mark and Young, Joanna C.},
	month = sep,
	year = {2013},
	pages = {218--223},
}

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