Maximum potential sublimation rate [kg/m^2/Gyr]
	polar_north_80_Emax.grd
	polar_south_80_Emax.grd

Time averaged potential sublimation rate [kg/m^2/Gyr]
	polar_north_80_Emean.grd
	polar_south_80_Emean.grd

Maximum temperature after Fourier smoothing [K]
	polar_north_80_Tmax.grd
	polar_south_80_Tmax.grd

Mean temperature, averaged over ecliptic and subsolar longitudes [K]
	polar_north_80_Tmean.grd
	polar_south_80_Tmean.grd
	
Pumping differential [m/Gyr]
	polar_north_80_pump.grd
	polar_south_80_pump.grd

Depth to sublimation loss rate of 100 kg/m^2/Gyr [m]
	polar_north_80_zit-100.grd
	polar_south_80_zit-100.grd

Depth to sublimation loss rate of 1 kg/m^2/Gyr [m]
	polar_north_80_zit-1.grd
	polar_south_80_zit-1.grd
	
	
References: For the methodology and the south polar maps see
Schorghofer, N., & Williams, J.-P. (2020). Mapping of ice storage processes on the Moon with time-dependent temperatures. Planetary Science Journal 1, 54. https://doi.org/10.3847/PSJ/abb6ff
For the north polar maps, a manuscript is in preparation.