The firn densification model IMAU-FDM has been used to simulate the firn density profile around Antarctica. The model is forced at the surface with climate data from the RACMO2.3 regional climate model. Here we provide the depth of three key firn density layers below the surface (750, 800 and 830 kgm^-3), averaged over the period 1979-2013. The data is on a horizontal grid of 27x27 km. The depth of each of these density layers was then subtracted from the surface elevation provided by Bedmap2 to determine where permeable firn exists below sea level. This defines the "brine zone" - the region where seawater may infiltrate the firn layer. We also provide shapefiles mapping the brine zone for each of three stated densities
Thesis (Master's)--University of Washington, 2019Knowledge of firn densification is important for se...
International audienceCorrect estimation of the firn lock-in depth is essential for correctly linkin...
In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennia...
The depth and density of the Antarctic firn layer is modeled, using a combination of regional climat...
A firn densification model is presented that simulates steady-state Antarctic firn density profiles,...
Abstract: To reduce the uncertainty in the calculation of Antarctic solid ice fluxes, the firn depth...
Abstract. A firn densification model is presented that sim-ulates steady-state Antarctic firn densit...
Firn densification model The firn densification model described by (13) is used as the model to simu...
Firn is the transitional product between fresh snow and glacier ice and acts as a boundary between t...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
A firn densification model (FDM) is used to assess spatial and temporal (1979-2200) variations in th...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
Firn simulations are essential for understanding Antarctic ice sheet mass change, as they enable us ...
Thesis (Master's)--University of Washington, 2019Knowledge of firn densification is important for se...
International audienceCorrect estimation of the firn lock-in depth is essential for correctly linkin...
In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennia...
The depth and density of the Antarctic firn layer is modeled, using a combination of regional climat...
A firn densification model is presented that simulates steady-state Antarctic firn density profiles,...
Abstract: To reduce the uncertainty in the calculation of Antarctic solid ice fluxes, the firn depth...
Abstract. A firn densification model is presented that sim-ulates steady-state Antarctic firn densit...
Firn densification model The firn densification model described by (13) is used as the model to simu...
Firn is the transitional product between fresh snow and glacier ice and acts as a boundary between t...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
A firn densification model (FDM) is used to assess spatial and temporal (1979-2200) variations in th...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
Correct estimation of the firn lock-in depth is essential for correctly linking gas and ice chronolo...
Firn simulations are essential for understanding Antarctic ice sheet mass change, as they enable us ...
Thesis (Master's)--University of Washington, 2019Knowledge of firn densification is important for se...
International audienceCorrect estimation of the firn lock-in depth is essential for correctly linkin...
In this study, we focus on the model detection in the Antarctic Peninsula (AP) of so-called perennia...