<?xml version="1.0" encoding='utf-8'?>
<!DOCTYPE wml PUBLIC "-//WAPFORUM//DTD WML 1.1//EN" "http://www.wapforum.org/DTD/wml_1.1.xml">
<wml>
<card id="card1" title="Air-mass thunderstorm - Page 11 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Air-mass_thunderstorm&amp;p=10">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Air-mass_thunderstorm&amp;p=12">3.Next</a>
</p>
<p>they tend not to be as tall. If the gust front, or leading edge of the outflow boundary, moves ahead of the thunderstorm, the thunderstorm's motion will move in tandem with the gust front. This is more of a factor with thunderstorms with heavy precipitation (HP), such as air-mass thunderstorms. When thunderstorms merge, which is most likely when numerous thunderstorms exist in proximity to each other, the motion of the stronger thunderstorm normally dictates future motion of the merged cell. The stronger the mean wind, the less likely other processes</p><p>
<a accesskey="1" href="page.php?w=Air-mass_thunderstorm&amp;p=10">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Air-mass_thunderstorm&amp;p=12">3.Next</a>
</p>

<do type="prev" label="Search">
        <go href="search.wml"/>
</do>

</card>
</wml>
