Contents of /MITgcm_contrib/icefront/2D_example/README

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This is an example 2D (x-z) configuration for a glacier fjord using icefornt pkg.

This example simulates a glacier fjord of 500 m deep and 6.4 km long along the fjord. 
A tidewater glacier is terminated at the edge of the fjord, with its vertical calving face 
in contact with sea water. A 5-m high channel exists at the bottom of the glacier, where 
freshwater at freezing point flows to the ocean at the speed of 0.5 m/s. The channel is 
created using shelfice pkg, and water T/S/V in the channel is prescribed using obcs pkg.
Melt rate at the vertical ice face is calculated using icefront pkg.

More details of this experiment are described in the paper: 
(Xu et al., Numerical experiments on subaqueous melting of Greenland tidewater 
 glaciers in response to ocean warming and enhanced subglacial discharge. 
 Annals of Glaciology, 2012. http://ecco2.org/manuscripts/2012/Xu2012.pdf)
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3
4	This is an example 2D (x-z) configuration for a glacier fjord using icefornt pkg.
5
6	This example simulates a glacier fjord of 500 m deep and 6.4 km long along the fjord.
7	A tidewater glacier is terminated at the edge of the fjord, with its vertical calving face
8	in contact with sea water. A 5-m high channel exists at the bottom of the glacier, where
9	freshwater at freezing point flows to the ocean at the speed of 0.5 m/s. The channel is
10	created using shelfice pkg, and water T/S/V in the channel is prescribed using obcs pkg.
11	Melt rate at the vertical ice face is calculated using icefront pkg.
12
13	More details of this experiment are described in the paper:
14	(Xu et al., Numerical experiments on subaqueous melting of Greenland tidewater
15	glaciers in response to ocean warming and enhanced subglacial discharge.
16	Annals of Glaciology, 2012. http://ecco2.org/manuscripts/2012/Xu2012.pdf)