Repository for the Parallel Ice Sheet Model (PISM)
Notable changes since v2.0.7
:
Implement the diurnal energy balance model dEBM-simple (see M. Zeitz, R. Reese, J. Beckmann, U. Krebs-Kanzow, and R. Winkelmann, "Impact of the melt-albedo feedback on the future evolution of the Greenland Ice Sheet with PISM-dEBM-simple," The Cryosphere, vol. 15, no. 12, pp. 5739-5764, Dec. 2021, doi: 10.5194/tc-15-5739-2021.)
Implement the isochronal layer tracing scheme (see A. Born and A. Robinson, "Modeling the Greenland englacial stratigraphy," The Cryosphere, vol. 15, no. 9, pp. 4539-4556, 2021, doi: 10.5194/tc-15-4539-2021.)
Support 2D precipitation offsets in -atmosphere ...,delta_P
. If the input file set using atmosphere.delta_P.file
contains a scalar time series delta_P
, use that as a time-dependent constant-in-space forcing. If the input file contains a 2D variable delta_P
, use that as a time-and-space-dependent forcing.
Support 2D air temperature offsets in -atmosphere ...,delta_T
. If the input file set using atmosphere.delta_T.file
contains a scalar time series delta_T
, use that as a time-dependent constant-in-space forcing. If the input file contains a 2D variable delta_T
, use that as a time-and-space-dependent forcing.
Support piecewise-constant temporal interpolation of near-surface air temperatures in -atmosphere given
: set atmosphere.given.air_temperature_interpolation
to piecewise_constant
.
Fix a bug reported by Christian Rodehacke: calving mechanisms should not remove ice at ice fronts adjacent to isolated patches of ice-free water (see issue #521).
Add CITATION.cff
to properly acknowledge all contributions and to make it easier to cite PISM.
Changes since v2.0.6
:
examples/std-greenland
.examples/searise-antarctica
with examples/antarctica
based on ALBMAP v1 data. This avoids a dependency on SeaRISE data hosted by the University of Montana.Implement a flux limiter ensuring strict preservation of non-negativity of ice thickness and therefore mass conservation up to rounding error.
This is a Zalesak-style (see flux corrected transport or FCT) limiter described in
P.K. Smolarkiewicz, "Comment on 'A Positive Definite Advection Scheme Obtained by Nonlinear Renormalization of the Advective Fluxes'," Monthly Weather Review, vol. 117, Art. no. 11, 1989.
Note that this approach (unlike modifications of the discretization of SIA diffusivity in the Jarosch et al paper mentioned below) works with all stress balance models.
Implement a benchmark setup checking mass conservation in an "isothermal SIA + mass continuity" model setup with "rough" bed topography (see examples/bedrock_step
).
This benchmark is described in
A.H. Jarosch, C.G. Schoof, and F.S. Anslow, "Restoring mass conservation to shallow ice flow models over complex terrain," The Cryosphere, vol. 7, Art. no. 1, Feb. 2013.
Fix a bug in the code ensuring non-negativity of ice thickness. (The old code added too much ice in an attempt to ensure non-negativity -- so much so that sometimes this caused crashes with error messages stating that ice thickness exceeds Lz
.)
Note that this "projection step" (ice_thickness = max(tentative_ice_thickness, 0)
) should have no effect now: the flux limiter mentioned above is designed to ensure non-negativity. We keep this step, however, to maintain the ability to keep track of ice thickness changes due to conservation errors (if they ever happen).
PISM no longer attempts to correct energy conservation by freezing basal water.
At each time step PISM checks basal enthalpy and if necessary modifies it to ensure continuity of temperature in each bedrock+ice
column. Sometimes this modification creates energy; prior to this change PISM attempted to remove an equivalent amount of energy by modifying the basal melt rate to freeze water stored at the base.
Under some conditions this basal melt rate adjustment created mass by freezing more water than available and even led to crashes with error messages stating that ice thickness exceeds Lz
.
Fix bugs in scalar diagnostics ice_volume_cold
and ice_volume_temperate
.
Several insignificant fixes (compiler warnings, code cleanup, etc).
-bed_def given
.flux_staggered
diagnostic.NaN
or infinity).time_stepping.assume_bed_elevation_changed
. With the default value ("false") PISM tries to avoid re-computing bed-elevation-dependent quantities if it is known that bed elevation did not change. Setting this flag to "true" disables this optimization.eps = 1e-12
to check if a variable in an input file has values that are outside its valid range.n
is the Glen exponent cannot be used for unit conversion. Luckily we don't need to convert from "Pa s^(1/n)" to other units, so we can get away with disabling unit validation in this particular case."pismr -version"
output.pism::IceModel
and IceModelVec.local_part()
to Python bindings."python3 -m nose ..."
.IceModel::basal_yield_stress_model()
and IceModel::bed_deformation_model()
.IceModelVec2T::average()
that affected periodic climate inputs and made PISM stop with an error message saying "invalid integration interval (a >= b)" (reported by Guillaume Jouvet).time_stepping.hit_multiples
.This release includes the following changes compared to v1.0-millennium-study
:
paleo_precip
" in a new modifier paleo_precip_2d
.-atmosphere ...,anomaly
" for a 2D forcing experiment: add atmosphere_anomaly_temp_only
. This flag restricts the effect of "-atmosphere anomaly
" to air temperatures and does not require "precipitation_anomaly
" in the forcing file. Also, use the variable name "delta_T
" instead of "air_temp_anomaly
" (for consistency).2.x
series for new research.Compared to v1.2, the new version includes
... and many more fixes and improvements. Please see the change log for details.