.. DO NOT EDIT. .. THIS FILE WAS AUTOMATICALLY GENERATED BY SPHINX-GALLERY. .. TO MAKE CHANGES, EDIT THE SOURCE PYTHON FILE: .. "api/gallery/volcanology/plot_15_wilson_sparks_eruption_columns.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 or to run this example in your browser via JupyterLite. .. rst-class:: sphx-glr-example-title .. _sphx_glr_api_gallery_volcanology_plot_15_wilson_sparks_eruption_columns.py: Wilson, Sparks, Huang and Watkins's eruption columns (1978) =========================================================== Wilson, Sparks, Huang and Watkins treated a Plinian eruption column as a buoyant plume driven by the heat of its fragmented magma. Its height grows as the fourth root of the heat flux, about ``8.2 Q**(1/4)`` metres, so a column ten times higher needs ten thousand times the eruption rate. The same height follows from the Morton-Taylor-Turner plume with the buoyancy flux of that heat in the atmosphere. .. GENERATED FROM PYTHON SOURCE LINES 12-34 .. image-sg:: /api/gallery/volcanology/images/sphx_glr_plot_15_wilson_sparks_eruption_columns_001.png :alt: Height grows as the fourth root of heat flux :srcset: /api/gallery/volcanology/images/sphx_glr_plot_15_wilson_sparks_eruption_columns_001.png :class: sphx-glr-single-img .. code-block:: Python import matplotlib.pyplot as plt import numpy as np from earthsciencekit.constants import CP_DRY_AIR, GRAVITY from earthsciencekit.volcanology import column_height, plume_rise_height rate = np.logspace(3, 9, 61) # kg/s of magma heat = rate * 1100 * 1000 # specific heat 1100 J/(kg K), cooled by 1000 K height = column_height(heat) buoyancy_flux = GRAVITY * heat / (1.1 * CP_DRY_AIR * 270) / np.pi # air 1.1 kg/m^3 at 270 K plume = plume_rise_height(buoyancy_flux, 0.01) assert np.allclose(height / plume, height[0] / plume[0]) and abs(height[0] / plume[0] - 1) < 0.15 assert np.isclose(column_height(1e12), 8200) fig, ax = plt.subplots() ax.loglog(rate, height / 1e3, label="8.2 Q^(1/4)") ax.loglog(rate, plume / 1e3, "--", label="MTT plume, N = 0.01 1/s") ax.set(xlabel="mass eruption rate [kg/s]", ylabel="column height [km]", title="Height grows as the fourth root of heat flux") ax.legend() plt.show() .. rst-class:: sphx-glr-timing **Total running time of the script:** (0 minutes 0.223 seconds) .. _sphx_glr_download_api_gallery_volcanology_plot_15_wilson_sparks_eruption_columns.py: .. only:: html .. container:: sphx-glr-footer sphx-glr-footer-example .. container:: lite-badge .. image:: images/jupyterlite_badge_logo.svg :target: ../../../lite/lab/index.html?path=api/gallery/volcanology/plot_15_wilson_sparks_eruption_columns.ipynb :alt: Launch JupyterLite :width: 150 px .. container:: sphx-glr-download sphx-glr-download-jupyter :download:`Download Jupyter notebook: plot_15_wilson_sparks_eruption_columns.ipynb ` .. container:: sphx-glr-download sphx-glr-download-python :download:`Download Python source code: plot_15_wilson_sparks_eruption_columns.py ` .. container:: sphx-glr-download sphx-glr-download-zip :download:`Download zipped: plot_15_wilson_sparks_eruption_columns.zip ` .. only:: html .. rst-class:: sphx-glr-signature `Gallery generated by Sphinx-Gallery `_