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• W1580735197 abstract "Small-scale variations of seasonal ice are explored at different geomorphic units on the Northern Polar Seasonal Cap (NPSC). We use seasonal rock shadow measurements, combined with visible and thermal observations, to calculate density over time. The coupling of volume density and albedo allows us to determine the microphysical state of the seasonal CO2 ice. We find two distinct end-members across the NPSC: (1) Snow deposits may anneal to form an overlying slab layer that fractures. These low-density deposits maintain relatively constant densities over springtime. (2) Porous slab deposits likely anneal rapidly in early spring and fracture in late spring. These high-density deposits dramatically increase in density over time. The end-members appear to be correlated with latitude." @default.
• W1580735197 created "2016-06-24" @default.
• W1580735197 creator A5040317324 @default.
• W1580735197 creator A5047013394 @default.
• W1580735197 date "2015-07-01" @default.
• W1580735197 modified "2023-10-18" @default.
• W1580735197 title "Evolution of Mars' northern polar seasonal CO₂deposits: Variations in surface brightness and bulk density" @default.
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• W1580735197 doi "https://doi.org/10.1002/2014je004706" @default.
• W1580735197 hasPublicationYear "2015" @default.
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