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21 changes: 10 additions & 11 deletions _sources/acknowledgements.rst.txt
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Expand Up @@ -16,20 +16,19 @@ University of Alaska PISM developers; find us in Elvey 410D. The Arctic Region
Supercomputing Center (now RCS) has provided significant computational resources and
technical help in the development of PISM.

Thanks for comments/questions from many PISM users around the world, including these not
already listed as PISM authors:
Thanks for comments and questions from many PISM users around the world, including these
not already listed as PISM authors:


Guðfinna Aðalgeirsdóttir, Antje Fitzner, Nick Golledge, Tore Hattermann,
Moritz Huetten, Thomas Kleiner, Leo van Kampenhout, Marianne Madsen, Malou Maris, Tim
Morey, Mirena Olaizola, Christian Rodehacke, Nathan Shemonski, Sebastian Simonsen,
Anne Solgaard, Ben Sperisen, Synne Høyer Svendsen, Martin Truffer, Shuting Yang,
Ryan Woodard
Guðfinna Aðalgeirsdóttir, Antje Fitzner, Nick Golledge, Tore Hattermann, Moritz
Huetten, Guillaume Jouvet, Thomas Kleiner, Leo van Kampenhout, Marianne Madsen, Malou
Maris, Tim Morey, Mirena Olaizola, Christian Rodehacke, Nathan Shemonski, Sebastian
Simonsen, Anne Solgaard, Ben Sperisen, Synne Høyer Svendsen, Martin Truffer, Shuting
Yang, Ryan Woodard.

for helpful comments and questions on PISM and this *Manual*. Dave Covey, Don Bahls, and
Greg Newby have supported our hardware, software, and computations. Bob Bindschadler,
Sophie Nowicki, Jesse Johnson, and others in the SeaRISE group have motivated and assisted
PISM development in many ways.
Dave Covey, Don Bahls, and Greg Newby have supported our hardware, software, and
computations. Bob Bindschadler, Sophie Nowicki, Jesse Johnson, and others in the SeaRISE
group have motivated and assisted PISM development in many ways.

PISM includes the source code for two external libraries we rely on:

Expand Down
2 changes: 1 addition & 1 deletion _sources/manual/jakobshavn/index.rst.txt
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Expand Up @@ -369,7 +369,7 @@ For this example ``PyPISMTools/colormaps/Full_saturation_spectrum_CCW.cpt`` was
.. rubric:: Footnotes

.. [#] PISM can also do 1 km runs for the whole Greenland ice sheet; see this `news item
<http://www.pism.io/news/2012/04/12/first1km/>`_.
<https://www.pism.io/news/2012/04/12/first1km/>`_.
.. [#] If this file is already present then no actual download occurs, and preprocessing
proceeds. Thus: Do not worry about download time if you need to preprocess again.
Expand Down
97 changes: 56 additions & 41 deletions _sources/manual/simplified-geometry/ismip-hom.rst.txt
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Expand Up @@ -84,51 +84,66 @@ Unlike simplified-geometry experiments A--D, the diagnostic simulation of the fl
the central flowline of Haut Glacier d'Arolla does not require any code modifications and
uses the ``pismr`` executable. Please see ``examples/ismip-hom/e-arolla`` for details.

The complete command used to produce :numref:`fig-ismiphom-e-surface`,
The complete script used to produce data for :numref:`fig-ismiphom-e-surface`,
:numref:`fig-ismiphom-e-no-slip`, and :numref:`fig-ismiphom-e-sliding` is below:

.. code-block:: bash
# set ice softness
A=$(echo "scale=50; 10^(-16) / (365.2524 * 86400.0)" | bc -l)
pismr -i ${input} -bootstrap \
-Mx 401 \
-grid.registration corner \
-grid.periodicity y \
-stress_balance.model blatter \
-stress_balance.blatter.flow_law isothermal_glen \
-flow_law.isothermal_Glen.ice_softness ${A} \
-stress_balance.blatter.coarsening_factor 7 \
-blatter_Mz 50 \
-bp_snes_monitor_ratio \
-bp_ksp_type gmres \
-bp_pc_type mg \
-bp_pc_mg_levels 3 \
-bp_mg_levels_ksp_type richardson \
-bp_mg_levels_pc_type sor \
-bp_mg_coarse_ksp_type preonly \
-bp_mg_coarse_pc_type lu \
-basal_resistance.pseudo_plastic.enabled \
-basal_resistance.pseudo_plastic.q 1.0 \
-basal_resistance.pseudo_plastic.u_threshold 3.1556926e7 \
-basal_yield_stress.model constant \
-energy none \
-geometry.update.enabled false \
-atmosphere uniform \
-atmosphere.uniform.precipitation 0 \
-surface simple \
-y 1e-16 \
-o ${output}
This run uses the `12.5` m grid resolution along the flowline and `50` vertical levels,
which corresponds to the vertical resolution of under `5` meters where the ice is
thickest.

This grid is small enough to perform the diagnostic computation serially, avoiding
dependence on parallel direct solvers (e.g. MUMPS) that may be needed in parallel.

We use 3 multigrid levels with a *very* aggressive coarsening factor (`7`).
# The ISMIP-HOM paper uses 1e-16
A=$(echo "scale=50; 10^(-16) / (365 * 86400.0)" | bc -l)
input=$1
output=$2
# number of grid points in the X direction
Mx=$3
# number of MG levels
M=$4
# coarsening factor
C=4
# number of vertical levels in the stress balance solver
bp_Mz=$(echo "$C^($M - 1) + 1" | bc)
echo "Using ${bp_Mz} vertical levels..."
mpiexec -n 8 pismr -i ${input} -bootstrap \
-Mx ${Mx} \
-Mz 216 \
-Lz 215 \
-z_spacing equal \
-grid.registration corner \
-grid.periodicity y \
-stress_balance.model blatter \
-stress_balance.blatter.flow_law isothermal_glen \
-flow_law.isothermal_Glen.ice_softness ${A} \
-stress_balance.blatter.coarsening_factor ${C} \
-blatter_Mz ${bp_Mz} \
-bp_snes_monitor_ratio \
-bp_ksp_type gmres \
-bp_pc_type mg \
-bp_pc_mg_levels ${M} \
-bp_mg_levels_ksp_type richardson \
-bp_mg_levels_pc_type sor \
-bp_mg_coarse_ksp_type cg \
-bp_mg_coarse_pc_type gamg \
-basal_resistance.pseudo_plastic.enabled \
-basal_resistance.pseudo_plastic.q 1.0 \
-basal_resistance.pseudo_plastic.u_threshold 1m.s-1 \
-basal_yield_stress.model constant \
-energy none \
-geometry.update.enabled false \
-atmosphere uniform \
-atmosphere.uniform.precipitation 0 \
-surface simple \
-y 1e-16 \
-o_size big \
-o ${output}
This run uses the `12` m grid resolution along the flowline and `65` vertical levels in
the stress balance solver, which corresponds to the vertical resolution of under `4`
meters where the ice is thickest.

We use 4 multigrid levels with a rather aggressive coarsening factor (`4`).

.. figure:: figures/uvelsurf.png
:name: fig-ismiphom-e-surface
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7 changes: 6 additions & 1 deletion _sources/manual/std-greenland/run-1-watching.rst.txt
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Expand Up @@ -53,7 +53,12 @@ we do:

.. code-block:: none
ncdump -h g20km_10ka.nc |grep history
ncdump -h g20km_10ka.nc | grep history
which prints

.. code-block:: none
:history = "user@machine 2017-10-04 19:16:08 AKDT: PISM done. Performance stats: 0.1784 wall clock hours, 0.7136 proc.-hours, 14005.0054 model years per proc.-hour.\n",
.. figure:: figures/g20km-10ka-usurf-csurf-mask.png
Expand Down
8 changes: 4 additions & 4 deletions _sources/manual/std-greenland/run-2.rst.txt
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Expand Up @@ -78,8 +78,8 @@ because of relatively-recent advances in radar and image technology and processi

So, how good is our model result ``velsurf_mag``? :numref:`fig-csurfvsobserved` compares
the radar-observed ``surfvelmag`` field in the downloaded SeaRISE-Greenland data file
``Greenland_5km_v1.1.nc`` with the just-computed PISM result. The reader might agree with
these broad qualitative judgements:
``Greenland_5km_v1.1.nc`` with the just-computed PISM result (20 km) and results from the next step in the tutorial (10 km).
The reader might agree with these broad qualitative judgements:

- the model results and the observed surface velocity look similar, and
- slow near-divide flow is generally in the right areas and of generally the right
Expand All @@ -95,8 +95,8 @@ these broad qualitative judgements:

:Left: :var:`surfvelmag`, the observed values from SeaRISE data file
``Greenland_5km_v1.1.nc``.
:Middle: :var:`velsurf_mag` from ``g20km_10ka_hy.nc``.
:Right: :var:`velsurf_mag` from ``g10km_10ka_hy.nc``.
:Middle: :var:`velsurf_mag` from ``g10km_10ka_hy.nc`` (will be run in next step of tutorial).
:Right: :var:`velsurf_mag` from ``g20km_10ka_hy.nc``.

We can compare these PISM results to other observed-vs-model comparisons of surface
velocity maps, for example Figure 1 in :cite:`Priceetal2011` and Figure 8 in
Expand Down
13 changes: 8 additions & 5 deletions _sources/manual/std-greenland/run-4.rst.txt
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Expand Up @@ -55,19 +55,22 @@ You will see an impressively-long command, which you can compare to the :ref:`fi
<firstcommand>`. There are several key changes. First, we do not start from scratch but
instead from a previously computed near-equilibrium result:

.. code-block:: none
.. code-block:: bash
-regrid_file g20km_10ka_hy.nc -regrid_vars litho_temp,thk,enthalpy,tillwat,bmelt
-regrid_file g20km_10ka_hy.nc \
-regrid_vars litho_temp,thk,enthalpy,tillwat,basal_melt_rate_grounded
For more on regridding see section :ref:`sec-regridding`. Then we turn on the earth
deformation model with option ``-bed_def lc``; see section :ref:`sec-beddef`. After
that the atmosphere and surface (PDD) models are turned on and the files they need are
identified:

.. code-block:: none
.. code-block:: bash
-atmosphere searise_greenland,delta_T,precip_scaling -surface pdd \
-atmosphere_precip_scaling_file pism_dT.nc -atmosphere_delta_T_file pism_dT.nc
-atmosphere searise_greenland,delta_T,precip_scaling \
-atmosphere_precip_scaling_file pism_dT.nc \
-atmosphere_delta_T_file pism_dT.nc \
-surface pdd
Then the sea level forcing module providing both a time-dependent sea level to the ice
dynamics core, is turned on with ``-sea_level constant,delta_sl`` and the file it needs is
Expand Down
4 changes: 2 additions & 2 deletions _static/documentation_options.js
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@@ -1,7 +1,7 @@
var DOCUMENTATION_OPTIONS = {
URL_ROOT: document.getElementById("documentation_options").getAttribute('data-url_root'),
VERSION: '2.0.6',
LANGUAGE: 'None',
VERSION: '2.0.7',
LANGUAGE: 'en',
COLLAPSE_INDEX: false,
BUILDER: 'html',
FILE_SUFFIX: '.html',
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35 changes: 17 additions & 18 deletions acknowledgements.html
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@@ -1,11 +1,11 @@

<!DOCTYPE html>

<html>
<html lang="en">
<head>
<meta charset="utf-8" />
<meta name="viewport" content="width=device-width, initial-scale=1.0" />
<title>Acknowledgements &#8212; PISM, a Parallel Ice Sheet Model 2.0.6 documentation</title>
<title>Acknowledgements &#8212; PISM, a Parallel Ice Sheet Model 2.0.7 documentation</title>
<link rel="stylesheet" href="_static/pygments.css" type="text/css" />
<link rel="stylesheet" href="_static/alabaster.css" type="text/css" />
<script id="documentation_options" data-url_root="./" src="_static/documentation_options.js"></script>
Expand All @@ -15,7 +15,7 @@
<link rel="index" title="Index" href="genindex.html" />
<link rel="search" title="Search" href="search.html" />
<link rel="next" title="Installing PISM" href="installation/index.html" />
<link rel="prev" title="PISM 2.0.6 documentation" href="index.html" />
<link rel="prev" title="PISM 2.0.7 documentation" href="index.html" />

<link rel="stylesheet" href="_static/custom.css" type="text/css" />

Expand All @@ -37,22 +37,21 @@ <h1>Acknowledgements<a class="headerlink" href="#acknowledgements" title="Permal
University of Alaska PISM developers; find us in Elvey 410D. The Arctic Region
Supercomputing Center (now RCS) has provided significant computational resources and
technical help in the development of PISM.</p>
<p>Thanks for comments/questions from many PISM users around the world, including these not
already listed as PISM authors:</p>
<p>Thanks for comments and questions from many PISM users around the world, including these
not already listed as PISM authors:</p>
<blockquote>
<div><p>Guðfinna Aðalgeirsdóttir, Antje Fitzner, Nick Golledge, Tore Hattermann,
Moritz Huetten, Thomas Kleiner, Leo van Kampenhout, Marianne Madsen, Malou Maris, Tim
Morey, Mirena Olaizola, Christian Rodehacke, Nathan Shemonski, Sebastian Simonsen,
Anne Solgaard, Ben Sperisen, Synne Høyer Svendsen, Martin Truffer, Shuting Yang,
Ryan Woodard</p>
<div><p>Guðfinna Aðalgeirsdóttir, Antje Fitzner, Nick Golledge, Tore Hattermann, Moritz
Huetten, Guillaume Jouvet, Thomas Kleiner, Leo van Kampenhout, Marianne Madsen, Malou
Maris, Tim Morey, Mirena Olaizola, Christian Rodehacke, Nathan Shemonski, Sebastian
Simonsen, Anne Solgaard, Ben Sperisen, Synne Høyer Svendsen, Martin Truffer, Shuting
Yang, Ryan Woodard.</p>
</div></blockquote>
<p>for helpful comments and questions on PISM and this <em>Manual</em>. Dave Covey, Don Bahls, and
Greg Newby have supported our hardware, software, and computations. Bob Bindschadler,
Sophie Nowicki, Jesse Johnson, and others in the SeaRISE group have motivated and assisted
PISM development in many ways.</p>
<p>Dave Covey, Don Bahls, and Greg Newby have supported our hardware, software, and
computations. Bob Bindschadler, Sophie Nowicki, Jesse Johnson, and others in the SeaRISE
group have motivated and assisted PISM development in many ways.</p>
<p>PISM includes the source code for two external libraries we rely on:</p>
<ul class="simple">
<li><p><a class="reference external" href="http://cirrus.ucsd.edu/~pierce/calcalcs/index.html">CalCalcs</a>, Copyright © 2010 by David W. Pierce, GPL</p></li>
<li><p><a class="reference external" href="https://cirrus.ucsd.edu/~pierce/calcalcs/index.html">CalCalcs</a>, Copyright © 2010 by David W. Pierce, GPL</p></li>
<li><p><code class="docutils literal notranslate"><span class="pre">cubature.c</span></code>, Copyright © 2005 Steven G. Johnson, GPL</p></li>
</ul>
<table class="colwidths-given docutils align-default" id="tab-funding">
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<html>
<html lang="en">
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<meta name="viewport" content="width=device-width, initial-scale=1.0" />
<title>Authorship &#8212; PISM, a Parallel Ice Sheet Model 2.0.6 documentation</title>
<title>Authorship &#8212; PISM, a Parallel Ice Sheet Model 2.0.7 documentation</title>
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<!DOCTYPE html>

<html>
<html lang="en">
<head>
<meta charset="utf-8" />
<meta name="viewport" content="width=device-width, initial-scale=1.0" />
<title>Atmosphere model components &#8212; PISM, a Parallel Ice Sheet Model 2.0.6 documentation</title>
<title>Atmosphere model components &#8212; PISM, a Parallel Ice Sheet Model 2.0.7 documentation</title>
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</dl>
<p>This modifier implements the SeaRISE-Greenland formula for a precipitation correction from
present; a 7.3% change of precipitation rate for every one degree Celsius of air
temperature change <a class="bibtex reference internal" href="../zzz_references_html.html#huybrechts02" id="id17">[2]</a>. See <a class="reference external" href="http://websrv.cs.umt.edu/isis/index.php/Model_Initialization#Greenland">SeaRISE Greenland model initialization</a> for details. The input file should contain air temperature offsets
temperature change <a class="bibtex reference internal" href="../zzz_references_html.html#huybrechts02" id="id17">[2]</a>. See <a class="reference external" href="https://web.archive.org/web/20221220001121/http://websrv.cs.umt.edu/isis/index.php/Model_Initialization#Greenland">SeaRISE Greenland model initialization</a> for details. The input file should contain air temperature offsets
in the format used by <code class="docutils literal notranslate"><span class="pre">-atmosphere</span> <span class="pre">...,delta_T</span></code> modifier, see section <a class="reference internal" href="#sec-atmosphere-delta-t"><span class="std std-ref">Scalar temperature offsets</span></a>.</p>
<p>This mechanisms increases precipitation by <span class="math notranslate nohighlight">\(100(\exp(C) - 1)\)</span> percent for each degree of
temperature increase, where</p>
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<html>
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<title>Examples and corresponding options &#8212; PISM, a Parallel Ice Sheet Model 2.0.7 documentation</title>
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