Recent formation and evolution of northern Martian polar layered deposits as inferred from a Global Climate Model

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The Polar Deposits of Mars (2009, background): “Levrard et al. 2004, 2007; Forget et al. 2006).”
Subsurface structure of Planum Boreum from Mars Reconnaissance Orbiter Shallow Radar soundings (2009, methodology): “, 2003) deliver lithic material to the polar region and concentrate it as lags during excursions in insolation (Levrard et al., 2007).”
Geologic history of Mars (2010, background): “…appears to reflect geologically recent events, but uncertainty exists as to whether the entire north polar ice deposit is lost during periods of higher obliquity (Levrard et al., 2007), or whether some older parts may remain below the surface, protected by a sublimation lag (Tanaka et al., 2005).”
Amazonian northern mid-latitude glaciation on Mars: A proposed climate scenario (2009, background): “Concurrently, developments in climate modeling are providing robust tools to explore this past water cycle (Haberle et al., 2000; Mischna et al., 2003; Levrard et al., 2007; Forget et al., 2006; Montmessin et al., 2007).”
The High Resolution Imaging Science Experiment (HiRISE) during MRO’s Primary Science Phase (PSP) (2010, background): “North polar region The polar layered deposits on Mars are widely believed to record recent global climate variations (e.g., Thomas et al., 1992; Laskar et al., 2004; Levrard et al., 2007).”