Changes in Soil Cohesion due to Water Vapor Exchange: A Proposed Dry-flow Trigger Mechanism for Recurring Slope Lineae on Mars

This file contains the modeling and experimental datasets to accompany the paper "Changes in Soil Cohesion due to Water Vapor Exchange: A Proposed Dry-flow Trigger Mechanism for Recurring Slope Lineae on Mars" currently in review at Geophysical Research Letters. The model datasets are MarsWRF diurnal simulations of the near-surface and surface conditions at Ls = 180 and Ls = 240 degrees at Hale Crater, Mars. The experimental datasets are Raman spectra and microscope images of lab simulations of these same seasons.