Global Astronomical M2 Tide - Revision history

Wpringle: /* Options/Features Tested */

2020-07-06T21:37:34Z

Options/Features Tested

← Older revision		Revision as of 17:37, 6 July 2020
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	== Options/Features Tested ==		== Options/Features Tested ==
	*<code>[[ICS]]</code> = -22: Uses the Mercator projection with a coordinate rotation to remove the pole singularity (need to provide a [[fort.rotm]].		*<code>[[ICS]]</code> = -22: Uses the Mercator projection with a coordinate rotation to remove the pole singularity (need to provide a [[fort.rotm]]).
	*<code>[[IM]]</code> = 513113: Uses the fully implicit scheme for the gravity wave term (computational time step is 12 minutes).		*<code>[[IM]]</code> = 513113: Uses the fully implicit scheme for the gravity wave term (computational time step is 12 minutes).
	*<code>[[NTIP]]</code> = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).		*<code>[[NTIP]]</code> = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).

Wpringle at 22:17, 8 June 2020

2020-06-08T22:17:18Z

← Older revision		Revision as of 18:17, 8 June 2020
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	This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The results of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation. Find the test at the [https://github.com/adcirc/adcirc-cg-testsuite/tree/~~master~~/adcirc/adcirc_global-tide-2d GitHub test suite].		This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The results of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation. Find the test at the [https://github.com/adcirc/adcirc-cg-testsuite/tree/v55/adcirc/adcirc_global-tide-2d GitHub test suite].

	== Mesh ==		== Mesh ==

Wpringle: /* Options/Features Tested */

2020-05-05T22:24:30Z

Options/Features Tested

← Older revision		Revision as of 18:24, 5 May 2020
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	== Options/Features Tested ==		== Options/Features Tested ==
	*[[ICS]] = -22: Uses the Mercator projection with a coordinate rotation to remove the pole singularity (need to provide a [[fort.rotm]].		*<code>[[ICS]]</code> = -22: Uses the Mercator projection with a coordinate rotation to remove the pole singularity (need to provide a [[fort.rotm]].
	*[[IM]] = 513113: Uses the fully implicit scheme for the gravity wave term (computational time step is 12 minutes).		*<code>[[IM]]</code> = 513113: Uses the fully implicit scheme for the gravity wave term (computational time step is 12 minutes).
	*[[NTIP]] = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).		*<code>[[NTIP]]</code> = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).
	*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.		*<code>[[A00, B00, C00]]</code> = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.
	*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.		*<code>[[ESLM]]</code> = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.
	*[[NHAGE]] = 5: outputs the harmonic constituent elevations into a netCDF4 [[fort.53 file]].		*<code>[[NHAGE]]</code> = 5: outputs the harmonic constituent elevations into a netCDF4 [[fort.53 file]].
	*[[NHAGV]] = 5: outputs the harmonic constituent velocities into a netCDF4 [[fort.54 file]].		*<code>[[NHAGV]]</code> = 5: outputs the harmonic constituent velocities into a netCDF4 [[fort.54 file]].
	*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.		*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.
	*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.		*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.

Wpringle at 22:05, 5 May 2020

2020-05-05T22:05:20Z

← Older revision		Revision as of 18:05, 5 May 2020
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	This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The results of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation.		This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The results of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation. Find the test at the [https://github.com/adcirc/adcirc-cg-testsuite/tree/master/adcirc/adcirc_global-tide-2d GitHub test suite].

	== Mesh ==		== Mesh ==

Wpringle at 22:03, 5 May 2020

2020-05-05T22:03:41Z

← Older revision		Revision as of 18:03, 5 May 2020
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	This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The ~~result~~ of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation.		This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The results of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation.

	== Mesh ==		== Mesh ==

Wpringle: /* Options/Features Tested */

2020-05-05T22:03:14Z

Options/Features Tested

← Older revision		Revision as of 18:03, 5 May 2020
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	*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.		*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.
	*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.		*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.
	*[[NHAGE]] = 5: outputs the harmonic constituent elevations into a netCDF4 [[fort.53]] ~~file~~.		*[[NHAGE]] = 5: outputs the harmonic constituent elevations into a netCDF4 [[fort.53 file]].
	*[[~~NHAVE~~]] = 5: outputs the harmonic constituent velocities into a netCDF4 [[fort.54]] ~~file~~.		*[[NHAGV]] = 5: outputs the harmonic constituent velocities into a netCDF4 [[fort.54 file]].
	*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.		*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.
	*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.		*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.

Wpringle: /* Options/Features Tested */

2020-05-05T22:01:14Z

Options/Features Tested

← Older revision		Revision as of 18:01, 5 May 2020
Line 10:		Line 10:
	*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.		*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.
	*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.		*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.
			*[[NHAGE]] = 5: outputs the harmonic constituent elevations into a netCDF4 [[fort.53]] file.
			*[[NHAVE]] = 5: outputs the harmonic constituent velocities into a netCDF4 [[fort.54]] file.
	*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.		*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.
	*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.		*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.

Wpringle: /* Options/Features Tested */

2020-05-05T21:59:04Z

Options/Features Tested

← Older revision		Revision as of 17:59, 5 May 2020
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	*[[NTIP]] = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).		*[[NTIP]] = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).
	*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.		*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.
	*[[~~ELSM~~]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.		*[[ESLM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.
	*[[internal tide ~~wave drag~~]]:		*[[fort.13_file#Internal_Tide_Energy_Conversion\|internal_tide_friction]]: spatially varying linear wave drag [[fort.13 file]] attribute accounting for energy conversion due to internal tide generation in the deep ocean.
			*[[fort.13_file#Quadratic_Friction_coefficient\|quadratic_friction_coefficient]]: spatially varying quadratic bottom friction [[fort.13 file]] attribute.

Wpringle: Created page with "This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with..."

2020-05-05T21:52:50Z

Created page with "This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with..."

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This example tests ADCIRC version 55 (and beyond). It tests the simulation of the astronomical M2 tidal constituent on the spherical Earth under equilibrium tidal forcing with the inclusion of the self-attraction and loading tide. The result of interest are the M2 tidal constituent amplitudes and phases of elevations and velocities from the least-squares harmonic analysis. The test finishes in about 5 minutes in serial ADCIRC for a full month of simulation.

== Mesh ==
The mesh is a coarse representation of the spherical Earth with minimum resolution of approximately 50 km, comprised of 27,330 vertices and 50,859 triangular elements.

== Options/Features Tested ==
*[[ICS]] = -22: Uses the Mercator projection with a coordinate rotation to remove the pole singularity (need to provide a [[fort.rotm]].
*[[IM]] = 513113: Uses the fully implicit scheme for the gravity wave term (computational time step is 12 minutes).
*[[NTIP]] = 2: equilibrium tide + self-attraction and loading tide forcing (read from a [[fort.24 file]]).
*[[A00, B00, C00]] = 0.5, 0.5, 0: Ensures that the fully implicit scheme is stable with a large time step.
*[[ELSM]] = -0.2: enables the Smagorinsky turbulence closure with a coefficient of 0.2.
*[[internal tide wave drag]]: