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cyschneck committed Jan 6, 2025
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10 changes: 5 additions & 5 deletions _preview/168/_sources/ncl/ncl_entries/meteorology.ipynb
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Expand Up @@ -82,11 +82,11 @@
"\n",
"Where the maximum number of daylight hours, N, is calculated as:\n",
"\n",
"{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`\n",
"{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`\n",
"\n",
"Where {math}`{\\omega}_{s}` is the sunset hour angle in radians [(Chapter 3, Equation 25)](https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data) {footcite}`allan_fao_1998`\n",
"\n",
"{math}`N = \\frac{24}{{\\pi}} {\\omega}_{s}`"
"{math}`{\\omega}_{s} = arccos[-tan({\\phi})tan({\\delta})]`"
]
},
{
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"\n",
"NCL's `satvpr_temp_fao56` calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 11)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n",
"\n",
"Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature {math}`T` (°C) is calculated as:\n",
"Where the saturation vapor pressure, {math}`e^°` (kPa), at air temperature, {math}`T` (°C), is calculated as:\n",
"\n",
"{math}`e^°(T) = 0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]`"
]
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"\n",
"NCL's `satvpr_tdew_fao56` calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 [(Chapter 3, Equation 14)](https://www.fao.org/4/x0490e/x0490e07.htm) {footcite}`allan_fao_1998`\n",
"\n",
"Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C) which is calculated as:\n",
"Where the actual vapor pressure, {math}`e_{a}` (kPa), is saturation vapor pressure at a specific dewpoint temperature, {math}`T_{dew}` (°C), which is calculated as:\n",
"\n",
"{math}`e_{a} = e^°(T_{dew}) = 0.6108 {\\exp}[\\frac{17.27 T_{dew}}{T_{dew} + 237.3}]`"
]
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"\n",
"Where the slope of saturation vapor pressure curve, {math}`{\\Delta}` (kPa), at air temperature {math}`T` (°C) is calculated as:\n",
"\n",
"{math}`{\\Delta} = \\frac{4098 [0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}]}{(T + 237.3)^2}`"
"{math}`{\\Delta} = \\frac{4098 (0.6108 {\\exp}[\\frac{17.27T}{T + 237.3}])}{(T + 237.3)^2}`"
]
},
{
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74 changes: 37 additions & 37 deletions _preview/168/applications/climatology.html
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6 changes: 3 additions & 3 deletions _preview/168/applications/datetime.html
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Expand Up @@ -450,7 +450,7 @@ <h2>The <code class="docutils literal notranslate"><span class="pre">datetime</s
</div>
<div class="cell_output docutils container">
<div class="output stream highlight-myst-ansi notranslate"><div class="highlight"><pre><span></span>datetime.date.today() -&gt; 2025-01-06
datetime.datetime.now() -&gt; 2025-01-06 23:01:04.434005
datetime.datetime.now() -&gt; 2025-01-06 23:21:44.173662
</pre></div>
</div>
</div>
Expand Down Expand Up @@ -481,10 +481,10 @@ <h3><code class="docutils literal notranslate"><span class="pre">strftime()</spa
2025

now.strftime(&#39;%A, %B %d %Y %I:%M:%S %p&#39;)
Monday, January 06 2025 11:01:04 PM
Monday, January 06 2025 11:21:44 PM

now.strftime(&#39;%c&#39;)
Mon Jan 6 23:01:04 2025
Mon Jan 6 23:21:44 2025
</pre></div>
</div>
</div>
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2 changes: 1 addition & 1 deletion _preview/168/applications/general_applied_math.html
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Expand Up @@ -608,7 +608,7 @@ <h3><code class="docutils literal notranslate"><span class="pre">cosecant</span>
</div>
<div class="output stderr highlight-myst-ansi notranslate"><div class="highlight"><pre><span></span>&lt;&gt;:14: SyntaxWarning: invalid escape sequence &#39;\M&#39;
&lt;&gt;:14: SyntaxWarning: invalid escape sequence &#39;\M&#39;
/tmp/ipykernel_2219/1093943048.py:14: SyntaxWarning: invalid escape sequence &#39;\M&#39;
/tmp/ipykernel_2243/1093943048.py:14: SyntaxWarning: invalid escape sequence &#39;\M&#39;
print(&quot;\Multiple Value Input (array/list)&quot;)
</pre></div>
</div>
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34 changes: 17 additions & 17 deletions _preview/168/applications/humid_heat_metrics.html
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22 changes: 11 additions & 11 deletions _preview/168/applications/spectral_analysis.html
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10 changes: 5 additions & 5 deletions _preview/168/ncl/ncl_entries/meteorology.html
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Expand Up @@ -490,9 +490,9 @@ <h3>Grab and Go<a class="headerlink" href="#grab-and-go" title="Link to this hea
<h2>daylight_fao56<a class="headerlink" href="#daylight-fao56" title="Link to this heading">#</a></h2>
<p>NCL’s <code class="docutils literal notranslate"><span class="pre">daylight_fao56</span></code> calculates the maximum number of daylight hours as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 <a class="reference external" href="https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data">(Chapter 3, Equation 34)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id2" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p>Where the maximum number of daylight hours, N, is calculated as:</p>
<p><span class="math notranslate nohighlight">\({\omega}_{s} = arccos[-tan({\phi})tan({\delta})]\)</span></p>
<p>Where <span class="math notranslate nohighlight">\({\omega}_{s}\)</span> is the sunset hour angle in radians <a class="reference external" href="https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data">(Chapter 3, Equation 25)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id3" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p><span class="math notranslate nohighlight">\(N = \frac{24}{{\pi}} {\omega}_{s}\)</span></p>
<p>Where <span class="math notranslate nohighlight">\({\omega}_{s}\)</span> is the sunset hour angle in radians <a class="reference external" href="https://www.fao.org/4/X0490E/x0490e07.htm#chapter%203%20%20%20meteorological%20data">(Chapter 3, Equation 25)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id3" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p><span class="math notranslate nohighlight">\({\omega}_{s} = arccos[-tan({\phi})tan({\delta})]\)</span></p>
<section id="id4">
<h3>Grab and Go<a class="headerlink" href="#id4" title="Link to this heading">#</a></h3>
<div class="cell docutils container">
Expand Down Expand Up @@ -540,7 +540,7 @@ <h3>Grab and Go<a class="headerlink" href="#id4" title="Link to this heading">#<
<section id="satvpr-temp-fao56">
<h2>satvpr_temp_fao56<a class="headerlink" href="#satvpr-temp-fao56" title="Link to this heading">#</a></h2>
<p>NCL’s <code class="docutils literal notranslate"><span class="pre">satvpr_temp_fao56</span></code> calculates saturation vapor pressure using temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 <a class="reference external" href="https://www.fao.org/4/x0490e/x0490e07.htm">(Chapter 3, Equation 11)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id5" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p>Where the saturation vapor pressure, <span class="math notranslate nohighlight">\(e^°\)</span> (kPa), at air temperature <span class="math notranslate nohighlight">\(T\)</span> (°C) is calculated as:</p>
<p>Where the saturation vapor pressure, <span class="math notranslate nohighlight">\(e^°\)</span> (kPa), at air temperature, <span class="math notranslate nohighlight">\(T\)</span> (°C), is calculated as:</p>
<p><span class="math notranslate nohighlight">\(e^°(T) = 0.6108 {\exp}[\frac{17.27T}{T + 237.3}]\)</span></p>
<section id="id6">
<h3>Grab and Go<a class="headerlink" href="#id6" title="Link to this heading">#</a></h3>
Expand Down Expand Up @@ -583,7 +583,7 @@ <h3>Grab and Go<a class="headerlink" href="#id6" title="Link to this heading">#<
<section id="satvpr-tdew-fao56">
<h2>satvpr_tdew_fao56<a class="headerlink" href="#satvpr-tdew-fao56" title="Link to this heading">#</a></h2>
<p>NCL’s <code class="docutils literal notranslate"><span class="pre">satvpr_tdew_fao56</span></code> calculates the actual saturation vapor pressure using dewpoint temperature as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 <a class="reference external" href="https://www.fao.org/4/x0490e/x0490e07.htm">(Chapter 3, Equation 14)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id7" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p>Where the actual vapor pressure, <span class="math notranslate nohighlight">\(e_{a}\)</span> (kPa), is saturation vapor pressure at a specific dewpoint temperature, <span class="math notranslate nohighlight">\(T_{dew}\)</span> (°C) which is calculated as:</p>
<p>Where the actual vapor pressure, <span class="math notranslate nohighlight">\(e_{a}\)</span> (kPa), is saturation vapor pressure at a specific dewpoint temperature, <span class="math notranslate nohighlight">\(T_{dew}\)</span> (°C), which is calculated as:</p>
<p><span class="math notranslate nohighlight">\(e_{a} = e^°(T_{dew}) = 0.6108 {\exp}[\frac{17.27 T_{dew}}{T_{dew} + 237.3}]\)</span></p>
<div class="cell docutils container">
<div class="cell_input docutils container">
Expand Down Expand Up @@ -624,7 +624,7 @@ <h2>satvpr_tdew_fao56<a class="headerlink" href="#satvpr-tdew-fao56" title="Link
<h2>satvpr_slope_fao56<a class="headerlink" href="#satvpr-slope-fao56" title="Link to this heading">#</a></h2>
<p>NCL’s <code class="docutils literal notranslate"><span class="pre">satvpr_slope_fao56</span></code> calculates the slope of the saturation vapor pressure curve as described in the Food and Agriculture Organization (FAO) Irrigation and Drainage Paper 56 <a class="reference external" href="https://www.fao.org/4/x0490e/x0490e07.htm">(Chapter 3, Equation 13)</a> <a class="footnote-reference brackets" href="#footcite-allan-fao-1998" id="id8" role="doc-noteref"><span class="fn-bracket">[</span>2<span class="fn-bracket">]</span></a></p>
<p>Where the slope of saturation vapor pressure curve, <span class="math notranslate nohighlight">\({\Delta}\)</span> (kPa), at air temperature <span class="math notranslate nohighlight">\(T\)</span> (°C) is calculated as:</p>
<p><span class="math notranslate nohighlight">\({\Delta} = \frac{4098 [0.6108 {\exp}[\frac{17.27T}{T + 237.3}]}{(T + 237.3)^2}\)</span></p>
<p><span class="math notranslate nohighlight">\({\Delta} = \frac{4098 (0.6108 {\exp}[\frac{17.27T}{T + 237.3}])}{(T + 237.3)^2}\)</span></p>
<div class="cell docutils container">
<div class="cell_input docutils container">
<div class="highlight-ipython3 notranslate"><div class="highlight"><pre><span></span><span class="c1"># Input: Single Value</span>
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