.. DO NOT EDIT. .. THIS FILE WAS AUTOMATICALLY GENERATED BY SPHINX-GALLERY. .. TO MAKE CHANGES, EDIT THE SOURCE PYTHON FILE: .. "auto_meta_modeling/fields_metamodels/plot_viscous_fall_metamodel.py" .. LINE NUMBERS ARE GIVEN BELOW. .. only:: html .. note:: :class: sphx-glr-download-link-note :ref:`Go to the end ` to download the full example code .. rst-class:: sphx-glr-example-title .. _sphx_glr_auto_meta_modeling_fields_metamodels_plot_viscous_fall_metamodel.py: Viscous free fall: metamodel of a field function ================================================ .. GENERATED FROM PYTHON SOURCE LINES 6-12 In this example, we present how to create the metamodel of a field function. This examples considers the :ref:`free fall model `. We first compute the Karhunen-Loève decomposition of a sample of trajectories. Then we create a create a polynomial chaos which takes the inputs and returns the KL decomposition modes as outputs. Finally, we create a metamodel by combining the KL decomposition and the polynomial chaos. .. GENERATED FROM PYTHON SOURCE LINES 15-17 Define the model ---------------- .. GENERATED FROM PYTHON SOURCE LINES 19-26 .. code-block:: Python import openturns as ot import numpy as np import openturns.viewer as viewer from matplotlib import pylab as plt ot.Log.Show(ot.Log.NONE) .. GENERATED FROM PYTHON SOURCE LINES 27-28 We first define the time grid associated with the model. .. GENERATED FROM PYTHON SOURCE LINES 30-35 .. code-block:: Python tmin = 0.0 # Minimum time tmax = 12.0 # Maximum time gridsize = 100 # Number of time steps mesh = ot.IntervalMesher([gridsize - 1]).build(ot.Interval(tmin, tmax)) .. GENERATED FROM PYTHON SOURCE LINES 36-38 .. code-block:: Python vertices = mesh.getVertices() .. GENERATED FROM PYTHON SOURCE LINES 39-40 Creation of the input distribution. .. GENERATED FROM PYTHON SOURCE LINES 42-48 .. code-block:: Python distZ0 = ot.Uniform(100.0, 150.0) distV0 = ot.Normal(55.0, 10.0) distM = ot.Normal(80.0, 8.0) distC = ot.Uniform(0.0, 30.0) distribution = ot.ComposedDistribution([distZ0, distV0, distM, distC]) .. GENERATED FROM PYTHON SOURCE LINES 49-53 .. code-block:: Python dimension = distribution.getDimension() dimension .. rst-class:: sphx-glr-script-out .. code-block:: none 4 .. GENERATED FROM PYTHON SOURCE LINES 54-58 Then we define the Python function which computes the altitude at each time value. In order to compute all altitudes with a vectorized evaluation, we first convert the vertices into a Numpy `array` and use the Numpy functions`exp` and `maximum`: this increases the evaluation performance of the script. .. GENERATED FROM PYTHON SOURCE LINES 61-75 .. code-block:: Python def AltiFunc(X): g = 9.81 z0 = X[0] v0 = X[1] m = X[2] c = X[3] tau = m / c vinf = -m * g / c t = np.array(vertices) z = z0 + vinf * t + tau * (v0 - vinf) * (1 - np.exp(-t / tau)) z = np.maximum(z, 0.0) return [[zeta[0]] for zeta in z] .. GENERATED FROM PYTHON SOURCE LINES 76-79 In order to create a `Function` from this Python function, we use the `PythonPointToFieldFunction` class. Since the altitude is the only output field, the third argument `outputDimension` is equal to `1`. If we had computed the speed as an extra output field, we would have set `2` instead. .. GENERATED FROM PYTHON SOURCE LINES 81-84 .. code-block:: Python outputDimension = 1 alti = ot.PythonPointToFieldFunction(dimension, mesh, outputDimension, AltiFunc) .. GENERATED FROM PYTHON SOURCE LINES 85-86 Compute a training sample. .. GENERATED FROM PYTHON SOURCE LINES 88-93 .. code-block:: Python size = 2000 ot.RandomGenerator.SetSeed(0) inputSample = distribution.getSample(size) outputSample = alti(inputSample) .. GENERATED FROM PYTHON SOURCE LINES 94-96 Compute the KL decomposition of the output ------------------------------------------ .. GENERATED FROM PYTHON SOURCE LINES 98-103 .. code-block:: Python algo = ot.KarhunenLoeveSVDAlgorithm(outputSample, 1.0e-6) algo.run() KLResult = algo.getResult() scaledModes = KLResult.getScaledModesAsProcessSample() .. GENERATED FROM PYTHON SOURCE LINES 104-110 .. code-block:: Python graph = scaledModes.drawMarginal(0) graph.setTitle("KL modes") graph.setXTitle(r"$t$") graph.setYTitle(r"$z$") view = viewer.View(graph) .. image-sg:: /auto_meta_modeling/fields_metamodels/images/sphx_glr_plot_viscous_fall_metamodel_001.png :alt: KL modes :srcset: /auto_meta_modeling/fields_metamodels/images/sphx_glr_plot_viscous_fall_metamodel_001.png :class: sphx-glr-single-img .. GENERATED FROM PYTHON SOURCE LINES 111-112 We create the `postProcessingKL` function which takes coefficients of the K.-L. modes as inputs and returns the trajectories. .. GENERATED FROM PYTHON SOURCE LINES 114-116 .. code-block:: Python karhunenLoeveLiftingFunction = ot.KarhunenLoeveLifting(KLResult) .. GENERATED FROM PYTHON SOURCE LINES 117-118 The `project` method computes the projection of the output sample (i.e. the trajectories) onto the K.-L. modes. .. GENERATED FROM PYTHON SOURCE LINES 120-122 .. code-block:: Python outputSampleChaos = KLResult.project(outputSample) .. GENERATED FROM PYTHON SOURCE LINES 123-124 We limit the sampling size of the Lilliefors selection in order to reduce the computational burden. .. GENERATED FROM PYTHON SOURCE LINES 126-128 .. code-block:: Python ot.ResourceMap.SetAsUnsignedInteger("FittingTest-LillieforsMaximumSamplingSize", 1) .. GENERATED FROM PYTHON SOURCE LINES 129-130 We create a polynomial chaos metamodel which takes the input sample and returns the K.-L. modes. .. GENERATED FROM PYTHON SOURCE LINES 132-136 .. code-block:: Python algo = ot.FunctionalChaosAlgorithm(inputSample, outputSampleChaos) algo.run() chaosMetamodel = algo.getResult().getMetaModel() .. GENERATED FROM PYTHON SOURCE LINES 137-139 The final metamodel is a composition of the KL lifting function and the polynomial chaos metamodel. In order to combine these two functions, we use the `PointToFieldConnection` class. .. GENERATED FROM PYTHON SOURCE LINES 141-143 .. code-block:: Python metaModel = ot.PointToFieldConnection(karhunenLoeveLiftingFunction, chaosMetamodel) .. GENERATED FROM PYTHON SOURCE LINES 144-146 Validate the metamodel ---------------------- .. GENERATED FROM PYTHON SOURCE LINES 148-149 Create a validation sample. .. GENERATED FROM PYTHON SOURCE LINES 151-155 .. code-block:: Python size = 10 validationInputSample = distribution.getSample(size) validationOutputSample = alti(validationInputSample) .. GENERATED FROM PYTHON SOURCE LINES 156-167 .. code-block:: Python graph = validationOutputSample.drawMarginal(0) graph.setColors(["red"]) graph2 = metaModel(validationInputSample).drawMarginal(0) graph2.setColors(["blue"]) graph.add(graph2) graph.setTitle("Model/metamodel comparison") graph.setXTitle(r"$t$") graph.setYTitle(r"$z$") view = viewer.View(graph) plt.show() .. image-sg:: /auto_meta_modeling/fields_metamodels/images/sphx_glr_plot_viscous_fall_metamodel_002.png :alt: Model/metamodel comparison :srcset: /auto_meta_modeling/fields_metamodels/images/sphx_glr_plot_viscous_fall_metamodel_002.png :class: sphx-glr-single-img .. GENERATED FROM PYTHON SOURCE LINES 168-173 We see that the blue trajectories (i.e. the metamodel) are close to the red trajectories (i.e. the validation sample). This shows that the metamodel is quite accurate. However, we observe that the trajectory singularity that occurs when the object touches the ground (i.e. when :math:`z` is equal to zero), makes the metamodel less accurate. .. GENERATED FROM PYTHON SOURCE LINES 175-176 Reset ResourceMap .. GENERATED FROM PYTHON SOURCE LINES 176-177 .. code-block:: Python ot.ResourceMap.Reload() .. _sphx_glr_download_auto_meta_modeling_fields_metamodels_plot_viscous_fall_metamodel.py: .. only:: html .. container:: sphx-glr-footer sphx-glr-footer-example .. container:: sphx-glr-download sphx-glr-download-jupyter :download:`Download Jupyter notebook: plot_viscous_fall_metamodel.ipynb ` .. container:: sphx-glr-download sphx-glr-download-python :download:`Download Python source code: plot_viscous_fall_metamodel.py `