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dev/_downloads/343c0344834d69ed1d752ddfeaa49067/Complex-Sounding-Plot.py
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# Copyright (c) 2015,2016,2017 MetPy Developers. | ||
# Distributed under the terms of the BSD 3-Clause License. | ||
# SPDX-License-Identifier: BSD-3-Clause | ||
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""" | ||
================================== | ||
Sounding Plot with Complex Layout | ||
================================== | ||
This example combines simple MetPy plotting functionality, `metpy.calc` | ||
computation functionality, and a few basic tricks to create an | ||
advanced sounding plotter with a clean layout & high readability. | ||
""" | ||
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import matplotlib.pyplot as plt | ||
import numpy as np | ||
import pandas as pd | ||
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import metpy.calc as mpcalc | ||
from metpy.cbook import get_test_data | ||
from metpy.plots import add_metpy_logo, Hodograph, SkewT | ||
from metpy.units import units | ||
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########################################### | ||
# Upper air data can easily be obtained using the siphon package, | ||
# but for this example we will use some of MetPy's sample data. | ||
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col_names = ['pressure', 'height', 'temperature', 'dewpoint', 'direction', 'speed'] | ||
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df = pd.read_fwf(get_test_data('may4_sounding.txt', as_file_obj=False), | ||
skiprows=5, usecols=[0, 1, 2, 3, 6, 7], names=col_names) | ||
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# Drop any rows with all NaN values for T, Td, winds | ||
df = df.dropna(subset=('temperature', 'dewpoint', 'direction', 'speed'), | ||
how='all').reset_index(drop=True) | ||
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########################################### | ||
# We will pull the data out of the example dataset into | ||
# individual variables and assign units. | ||
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p = df['pressure'].values * units.hPa | ||
z = df['height'].values * units.m | ||
T = df['temperature'].values * units.degC | ||
Td = df['dewpoint'].values * units.degC | ||
wind_speed = df['speed'].values * units.knots | ||
wind_dir = df['direction'].values * units.degrees | ||
u, v = mpcalc.wind_components(wind_speed, wind_dir) | ||
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########################################### | ||
# Now lets make a Skew-T Log-P diagram using some simply | ||
# MetPy functionality | ||
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# Create a new figure. The dimensions here give a good aspect ratio | ||
fig = plt.figure(figsize=(9, 9)) | ||
add_metpy_logo(fig, 430, 30, size='large') | ||
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skew = SkewT(fig, rotation=45, rect=(0.1, 0.1, 0.55, 0.85)) | ||
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# Plot the data using normal plotting functions, in this case using | ||
# log scaling in Y, as dictated by the typical meteorological plot | ||
skew.plot(p, T, 'r') | ||
skew.plot(p, Td, 'g') | ||
skew.plot_barbs(p, u, v) | ||
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# Change to adjust data limits and give it a semblance of what we want | ||
skew.ax.set_adjustable('datalim') | ||
skew.ax.set_ylim(1000, 100) | ||
skew.ax.set_xlim(-20, 30) | ||
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# Add the relevant special lines | ||
skew.plot_dry_adiabats() | ||
skew.plot_moist_adiabats() | ||
skew.plot_mixing_lines() | ||
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# Create a hodograph | ||
ax = plt.axes((0.7, 0.75, 0.2, 0.2)) | ||
h = Hodograph(ax, component_range=60.) | ||
h.add_grid(increment=20) | ||
h.plot(u, v) | ||
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########################################### | ||
# This layout isn't bad, especially for how little code it required, | ||
# but we could add a few simple tricks to greatly increase the | ||
# readability and complexity of our Skew-T/Hodograph layout. Lets | ||
# try another Skew-T with a few more advanced features: | ||
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########################################### | ||
# STEP 1: CREATE THE SKEW-T OBJECT AND MODIFY IT TO CREATE A | ||
# NICE, CLEAN PLOT | ||
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# Create a new figure. The dimensions here give a good aspect ratio | ||
fig = plt.figure(figsize=(18, 12)) | ||
skew = SkewT(fig, rotation=45, rect=(0, 0, 0.50, 0.90)) | ||
# add the metpy logo | ||
add_metpy_logo(fig, 100, 80, size='small') | ||
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# Change to adjust data limits and give it a semblance of what we want | ||
skew.ax.set_adjustable('datalim') | ||
skew.ax.set_ylim(1000, 100) | ||
skew.ax.set_xlim(-20, 30) | ||
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# Set some better labels than the default to increase readability | ||
skew.ax.set_xlabel(str.upper(f'Temperature ({T.units:~P})'), weight='bold') | ||
skew.ax.set_ylabel(str.upper(f'Pressure ({p.units:~P})'), weight='bold') | ||
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# Set the facecolor of the Skew Object and the Figure to white | ||
fig.set_facecolor('#ffffff') | ||
skew.ax.set_facecolor('#ffffff') | ||
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# Here we can use some basic math and Python functionality to make a cool | ||
# shaded isotherm pattern. | ||
x1 = np.linspace(-100, 40, 8) | ||
x2 = np.linspace(-90, 50, 8) | ||
y = [1100, 50] | ||
for i in range(0, 8): | ||
skew.shade_area(y=y, x1=x1[i], x2=x2[i], color='gray', alpha=0.02, zorder=1) | ||
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########################################### | ||
# STEP 2: PLOT DATA ON THE SKEW-T. TAKE A COUPLE EXTRA STEPS TO | ||
# INCREASE READABILITY | ||
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# Plot the data using normal plotting functions, in this case using | ||
# log scaling in Y, as dictated by the typical meteorological plot | ||
# set the linewidth to 4 for increased readability. | ||
# We will also add the 'label' kew word argument for our legend. | ||
skew.plot(p, T, 'r', lw=4, label='TEMPERATURE') | ||
skew.plot(p, Td, 'g', lw=4, label='DEWPOINT') | ||
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# again we can use some simple python math functionality to 'resample' | ||
# the wind barbs for a cleaner output with increased readability. | ||
# Something like this would work. | ||
interval = np.logspace(2, 3, 40) * units.hPa | ||
idx = mpcalc.resample_nn_1d(p, interval) | ||
skew.plot_barbs(pressure=p[idx], u=u[idx], v=v[idx]) | ||
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# Add the relevant special lines native to the Skew-T Log-P diagram & | ||
# provide basic adjustments to linewidth and alpha to increase readability | ||
# first we add a matplotlib axvline to highlight the 0 degree isotherm | ||
skew.ax.axvline(0 * units.degC, linestyle='--', color='blue', alpha=0.3) | ||
skew.plot_dry_adiabats(lw=1, alpha=0.3) | ||
skew.plot_moist_adiabats(lw=1, alpha=0.3) | ||
skew.plot_mixing_lines(lw=1, alpha=0.3) | ||
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# Calculate LCL height and plot as black dot. Because `p`'s first value is | ||
# ~1000 mb and its last value is ~250 mb, the `0` index is selected for | ||
# `p`, `T`, and `Td` to lift the parcel from the surface. If `p` was inverted, | ||
# i.e. start from low value, 250 mb, to a high value, 1000 mb, the `-1` index | ||
# should be selected. | ||
lcl_pressure, lcl_temperature = mpcalc.lcl(p[0], T[0], Td[0]) | ||
skew.plot(lcl_pressure, lcl_temperature, 'ko', markerfacecolor='black') | ||
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# Calculate full parcel profile and add to plot as black line | ||
prof = mpcalc.parcel_profile(p, T[0], Td[0]).to('degC') | ||
skew.plot(p, prof, 'k', linewidth=2, label='SB PARCEL PATH') | ||
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# Shade areas of CAPE and CIN | ||
skew.shade_cin(p, T, prof, Td, alpha=0.2, label='SBCIN') | ||
skew.shade_cape(p, T, prof, alpha=0.2, label='SBCAPE') | ||
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########################################### | ||
# STEP 3: CREATE THE HODOGRAPH INSET. TAKE A FEW EXTRA STEPS TO | ||
# INCREASE READABILITY | ||
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# Create a hodograph object: first we need to add an axis | ||
# then we can create the metpy Hodograph | ||
hodo_ax = plt.axes((0.43, 0.40, 0.5, 0.5)) | ||
h = Hodograph(hodo_ax, component_range=80.) | ||
# Add two separate grid increments for a cooler look. This also | ||
# helps to increase readability | ||
h.add_grid(increment=20, ls='-', lw=1.5, alpha=0.5) | ||
h.add_grid(increment=10, ls='--', lw=1, alpha=0.2) | ||
# The next few steps makes for a clean hodograph inset, removing the | ||
# tick marks, tick labels and axis labels | ||
h.ax.set_box_aspect(1) | ||
h.ax.set_yticklabels([]) | ||
h.ax.set_xticklabels([]) | ||
h.ax.set_xticks([]) | ||
h.ax.set_yticks([]) | ||
h.ax.set_xlabel(' ') | ||
h.ax.set_ylabel(' ') | ||
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# Here we can add a simple python for loop that adds tick marks | ||
# to the inside of the hodograph plot to increase readability! | ||
plt.xticks(np.arange(0, 0, 1)) | ||
plt.yticks(np.arange(0, 0, 1)) | ||
for i in range(10, 120, 10): | ||
h.ax.annotate(str(i), (i, 0), xytext=(0, 2), textcoords='offset pixels', | ||
clip_on=True, fontsize=10, weight='bold', alpha=0.3, zorder=0) | ||
for i in range(10, 120, 10): | ||
h.ax.annotate(str(i), (0, i), xytext=(0, 2), textcoords='offset pixels', | ||
clip_on=True, fontsize=10, weight='bold', alpha=0.3, zorder=0) | ||
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# plot the hodograph itself, using plot_colormapped, colored | ||
# by height | ||
h.plot_colormapped(u, v, c=z, linewidth=6, label='0-12km WIND') | ||
# compute Bunkers storm motion so we can plot it on the hodograph! | ||
RM, LM, MW = mpcalc.bunkers_storm_motion(p, u, v, z) | ||
h.ax.text((RM[0].m + 0.5), (RM[1].m - 0.5), 'RM', weight='bold', ha='left', | ||
fontsize=13, alpha=0.6) | ||
h.ax.text((LM[0].m + 0.5), (LM[1].m - 0.5), 'LM', weight='bold', ha='left', | ||
fontsize=13, alpha=0.6) | ||
h.ax.text((MW[0].m + 0.5), (MW[1].m - 0.5), 'MW', weight='bold', ha='left', | ||
fontsize=13, alpha=0.6) | ||
h.ax.arrow(0, 0, RM[0].m - 0.3, RM[1].m - 0.3, linewidth=2, color='black', | ||
alpha=0.2, label='Bunkers RM Vector', | ||
length_includes_head=True, head_width=2) | ||
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########################################### | ||
# STEP 4: ADD A FEW EXTRA ELEMENTS TO REALLY MAKE A NEAT PLOT | ||
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# First we want to actually add values of data to the plot for easy viewing | ||
# to do this, lets first add a simple rectangle using matplotlib's 'patches' | ||
# functionality to add some simple layout for plotting calculated parameters | ||
# xloc yloc xsize ysize | ||
fig.patches.extend([plt.Rectangle((0.513, 0.00), 0.334, 0.37, | ||
edgecolor='black', facecolor='white', | ||
linewidth=1, alpha=1, transform=fig.transFigure, | ||
figure=fig)]) | ||
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# now lets take a moment to calculate some simple severe-weather parameters using | ||
# metpy's calculations | ||
# here are some classic severe parameters! | ||
kindex = mpcalc.k_index(p, T, Td) | ||
total_totals = mpcalc.total_totals_index(p, T, Td) | ||
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# mixed layer parcel properties! | ||
ml_t, ml_td = mpcalc.mixed_layer(p, T, Td, depth=50 * units.hPa) | ||
ml_p, _, _ = mpcalc.mixed_parcel(p, T, Td, depth=50 * units.hPa) | ||
mlcape, mlcin = mpcalc.mixed_layer_cape_cin(p, T, prof, depth=50 * units.hPa) | ||
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# most unstable parcel properties! | ||
mu_p, mu_t, mu_td, _ = mpcalc.most_unstable_parcel(p, T, Td, depth=50 * units.hPa) | ||
mucape, mucin = mpcalc.most_unstable_cape_cin(p, T, Td, depth=50 * units.hPa) | ||
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# Estimate height of LCL in meters from hydrostatic thickness (for sig_tor) | ||
new_p = np.append(p[p > lcl_pressure], lcl_pressure) | ||
new_t = np.append(T[p > lcl_pressure], lcl_temperature) | ||
lcl_height = mpcalc.thickness_hydrostatic(new_p, new_t) | ||
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# Compute Surface-based CAPE | ||
sbcape, sbcin = mpcalc.surface_based_cape_cin(p, T, Td) | ||
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# Compute SRH | ||
(u_storm, v_storm), *_ = mpcalc.bunkers_storm_motion(p, u, v, z) | ||
*_, total_helicity1 = mpcalc.storm_relative_helicity(z, u, v, depth=1 * units.km, | ||
storm_u=u_storm, storm_v=v_storm) | ||
*_, total_helicity3 = mpcalc.storm_relative_helicity(z, u, v, depth=3 * units.km, | ||
storm_u=u_storm, storm_v=v_storm) | ||
*_, total_helicity6 = mpcalc.storm_relative_helicity(z, u, v, depth=6 * units.km, | ||
storm_u=u_storm, storm_v=v_storm) | ||
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# Copmute Bulk Shear components and then magnitude | ||
ubshr1, vbshr1 = mpcalc.bulk_shear(p, u, v, height=z, depth=1 * units.km) | ||
bshear1 = mpcalc.wind_speed(ubshr1, vbshr1) | ||
ubshr3, vbshr3 = mpcalc.bulk_shear(p, u, v, height=z, depth=3 * units.km) | ||
bshear3 = mpcalc.wind_speed(ubshr3, vbshr3) | ||
ubshr6, vbshr6 = mpcalc.bulk_shear(p, u, v, height=z, depth=6 * units.km) | ||
bshear6 = mpcalc.wind_speed(ubshr6, vbshr6) | ||
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# Use all computed pieces to calculate the Significant Tornado parameter | ||
sig_tor = mpcalc.significant_tornado(sbcape, lcl_height, | ||
total_helicity3, bshear3).to_base_units() | ||
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# Perform the calculation of supercell composite if an effective layer exists | ||
super_comp = mpcalc.supercell_composite(mucape, total_helicity3, bshear3) | ||
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# there is a lot we can do with this data operationally, so lets plot some of | ||
# these values right on the plot, in the box we made | ||
# first lets plot some thermodynamic parameters | ||
plt.figtext(0.53, 0.32, 'SBCAPE: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.32, f'{int(sbcape.m)} J/kg', weight='bold', | ||
fontsize=15, color='orangered', ha='right') | ||
plt.figtext(0.53, 0.29, 'SBCIN: ', weight='bold', | ||
fontsize=15, color='black', ha='left') | ||
plt.figtext(0.66, 0.29, f'{int(sbcin.m)} J/kg', weight='bold', | ||
fontsize=15, color='lightblue', ha='right') | ||
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plt.figtext(0.53, 0.24, 'MLCAPE: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.24, f'{int(mlcape.m)} J/kg', weight='bold', | ||
fontsize=15, color='orangered', ha='right') | ||
plt.figtext(0.53, 0.21, 'MLCIN: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.21, f'{int(mlcin.m)} J/kg', weight='bold', | ||
fontsize=15, color='lightblue', ha='right') | ||
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plt.figtext(0.53, 0.16, 'MUCAPE: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.16, f'{int(mucape.m)} J/kg', weight='bold', | ||
fontsize=15, color='orangered', ha='right') | ||
plt.figtext(0.53, 0.13, 'MUCIN: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.13, f'{int(mucin.m)} J/kg', weight='bold', | ||
fontsize=15, color='lightblue', ha='right') | ||
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plt.figtext(0.53, 0.08, 'TT-INDEX: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.08, f'{int(total_totals.m)} Δ°C', weight='bold', | ||
fontsize=15, color='orangered', ha='right') | ||
plt.figtext(0.53, 0.05, 'K-INDEX: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.66, 0.05, f'{int(kindex.m)} °C', weight='bold', | ||
fontsize=15, color='orangered', ha='right') | ||
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# now some kinematic parameters | ||
met_per_sec = (units.m * units.m) / (units.sec * units.sec) | ||
plt.figtext(0.68, 0.32, '0-1km SRH: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.32, f'{int(total_helicity1.m)* met_per_sec:~P}', | ||
weight='bold', fontsize=15, color='navy', ha='right') | ||
plt.figtext(0.68, 0.29, '0-1km SHEAR: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.29, f'{int(bshear1.m)} kts', weight='bold', | ||
fontsize=15, color='blue', ha='right') | ||
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plt.figtext(0.68, 0.24, '0-3km SRH: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.24, f'{int(total_helicity3.m)* met_per_sec:~P}', | ||
weight='bold', fontsize=15, color='navy', ha='right') | ||
plt.figtext(0.68, 0.21, '0-3km SHEAR: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.21, f'{int(bshear3.m)} kts', weight='bold', | ||
fontsize=15, color='blue', ha='right') | ||
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plt.figtext(0.68, 0.16, '0-6km SRH: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.16, f'{int(total_helicity6.m)* met_per_sec:~P}', | ||
weight='bold', fontsize=15, color='navy', ha='right') | ||
plt.figtext(0.68, 0.13, '0-6km SHEAR: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.13, f'{int(bshear6.m)} kts', weight='bold', | ||
fontsize=15, color='blue', ha='right') | ||
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plt.figtext(0.68, 0.08, 'SIG TORNADO: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.08, f'{int(sig_tor.m)}', weight='bold', fontsize=15, | ||
color='orangered', ha='right') | ||
plt.figtext(0.68, 0.05, 'SUPERCELL COMP: ', weight='bold', fontsize=15, | ||
color='black', ha='left') | ||
plt.figtext(0.83, 0.05, f'{int(super_comp.m)}', weight='bold', fontsize=15, | ||
color='orangered', ha='right') | ||
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# add legends to the skew and hodo | ||
skewleg = skew.ax.legend(loc='upper left') | ||
hodoleg = h.ax.legend(loc='upper left') | ||
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# add a plot title | ||
plt.figtext(0.40, 0.92, 'OUN | MAY 4TH 1999 - 00Z VERTICAL PROFILE', | ||
weight='bold', fontsize=20, ha='center') | ||
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# Show the plot | ||
plt.show() |
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