Annotation of /MITgcm_contrib/icefront/3D_example/README

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This is an example 3D configuration for a glacier fjord using icefornt pkg.

This example simulates a glacier fjord of 500 m deep, 500 m long along the fjord, and 150 m
wide across the fjord. A tidewater glacier is terminated at the edge of the fjord, with a 
vertical calving face of 150 m wide and 500 m high, in contact with sea water. A channel of 
1-m high and 2-m wide 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.(2013), Subaqueous melting of Store Glacier, west Greenland from three-dimensional, 
 high-resolution numerical modeling and ocean observations. Geophys. Res. Lett., 40, 
 doi:10.1002/grl.50825.)
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3
4			This is an example 3D configuration for a glacier fjord using icefornt pkg.
5
6			This example simulates a glacier fjord of 500 m deep, 500 m long along the fjord, and 150 m
7			wide across the fjord. A tidewater glacier is terminated at the edge of the fjord, with a
8			vertical calving face of 150 m wide and 500 m high, in contact with sea water. A channel of
9			1-m high and 2-m wide exists at the bottom of the glacier, where freshwater at freezing point
10			flows to the ocean at the speed of 0.5 m/s. The channel is created using shelfice pkg, and
11			water T/S/V in the channel is prescribed using obcs pkg. Melt rate at the vertical ice face
12			is calculated using icefront pkg.
13
14			More details of this experiment are described in the paper:
15			(Xu et al.(2013), Subaqueous melting of Store Glacier, west Greenland from three-dimensional,
16			high-resolution numerical modeling and ocean observations. Geophys. Res. Lett., 40,
17			doi:10.1002/grl.50825.)