[{"name":"frampton-2015-pathways-1","title":"Numerically modelled transport pathways in degrading permafrost","summary":"A numerical model which couples heat and water conservation equations combined with a post-processing routine for particle tracking of water pathways is used to calculate travel times of solutes in degrading permafrost systems. The models are two-dimensional subsurface representations corresponding to 30 m depth and 100 m lateral extent. Modelling assumptions and details of the configurations are provided in the manuscript. The data set contains (i) spatially and temporally resolved subsurface water fluxes, (ii) spatially and temporally resolved subsurface phase saturations and temperatures, and (iii) subsurface pathway travel times.","citations":"Frampton, A., Destouni, G., 2015. Impact of degrading permafrost on subsurface solute transport pathways and travel times. Water Resources Research 51, 7680\u20137701. DOI: 10.1002\/2014WR016689","comments":"","category":"Terrestrial","subcategory":"Hydrology","keywords":"Earth science; Terrestrial; Hydrology; Cryology; Numerical modelling; Permafrost hydrogeology; Active layer dynamics; Travel times; Flow pathways; Climate change","scientist":"Andrew Frampton","firstname":"Andrew","lastname":"Frampton","address":"Department of Physical Geography; Stockholm University","postalcode":"SE-106 91","city":"Stockholm","province":"","country":"Sweden","parameters":"Land Surface > Soils > Permafrost","location":"Vertical Location > Land Surface","progress":"Completed","language":"English","project":"This study was funded by the Swedish Geological Survey (SGU), and is part of the research within the Climate Community of the Swedish e-Science Research Centre (SeRC).","publisher":"Bolin Centre Database","version":"1","constrains":"None","access":"Free"}]