Variable penetration depth of interferometric synthetic aperture radar signals on Alaska glaciers: a cold surface layer hypothesis

MLA

Mark Sanford, et al. “Variable Penetration Depth of Interferometric Synthetic Aperture Radar Signals on Alaska Glaciers: A Cold Surface Layer Hypothesis.” Annals of Glaciology, vol. 54, Jan. 2013, pp. 218–23. EBSCOhost, https://doi.org/10.3189/2013aog64a114.

APA

Mark Sanford, Anthony Arendt, Donald K. Atwood, Bert Kampes, Alessio Gusmeroli, & Joanna C. Young. (2013). Variable penetration depth of interferometric synthetic aperture radar signals on Alaska glaciers: a cold surface layer hypothesis. Annals of Glaciology, 54, 218–223. https://doi.org/10.3189/2013aog64a114

Chicago

Mark Sanford, Anthony Arendt, Donald K. Atwood, Bert Kampes, Alessio Gusmeroli, and Joanna C. Young. 2013. “Variable Penetration Depth of Interferometric Synthetic Aperture Radar Signals on Alaska Glaciers: A Cold Surface Layer Hypothesis.” Annals of Glaciology 54 (January): 218–23. doi:10.3189/2013aog64a114.