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add a note about coarsening the grid (ncol)
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emorway-usgs committed Sep 18, 2024
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17 changes: 12 additions & 5 deletions scripts/ex-gwe-barends.py
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# 19–22 September 2010.
# https://doi.org/10.2118/134670-MS
#
# Below is a diagram of the model cell numbering, which is helpful for this
# Below is a diagram of the model cell numbering (assuming delr = 1.0; values
# for other ncol discretizations will be different), which is helpful for this
# DISU setup since the groundwater reservoir is flowing in a 1D, left-to-right
# manner with no flow in the overburden. Additionally, heat "bleeds" into
# the overburden from the flowing reservoir. Heat bleeds in a 1D upward
# manner and does not conduct laterally once in the overburden. Thus, the
# manner with no flow in the overburden. Additionally, heat "bleeds"
# (conduction) into the overburden from the flowing reservoir. Conduction, or
# "thermal bleeding" as Barends (2010) refers to it, only occurs in a 1D
# vertical manner and does not conduct laterally once in the overburden. Thus, the
# connections in the DISU grid are such that cells in the overburden are not
# connected to their lateral neighbors, but only the cells above and below.
# connected to their lateral neighbors, but only to the cells above and below.
#
# +-------+-------+-------+ +-------+-------+-------+ \
# Cell IDs | 0 | 1 | 2 | ... | 997 | 998 | 999 | Layer 1 |
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# | | | | | | | | Layer 3 |
# +-------+-------+-------+ +-------+-------+-------+ /
# ----> gw flow direction ---->
#
# NOTE: In the current example, ncol is specified as 250. If users are not
# satisfied with GWE fits to the analytical solution, this value may be
# increased to 500, 1,000, or more for an improved solution. Currently,
# ncol is kept low for faster run times.
# -

# +
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