<?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="Ocean surface topography - Page 5 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Ocean_surface_topography&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Ocean_surface_topography&amp;p=6">3.Next</a>
</p>
<p><a href="page.php?w=ocean_heat_content">ocean heat content</a>.</p>

<p><big>Applications</big></p>
<p>Ocean surface topography is used to map <a href="page.php?w=ocean_current">ocean current</a>s, which move around the ocean's "hills" and "valleys" in predictable ways. A clockwise sense of rotation is found around "hills" in the northern hemisphere and "valleys" in the southern hemisphere. This is because of the <a href="page.php?w=Coriolis_effect">Coriolis effect</a>. Conversely, a counterclockwise sense of rotation is found around "valleys" in the</p><p>
<a accesskey="1" href="page.php?w=Ocean_surface_topography&amp;p=4">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Ocean_surface_topography&amp;p=6">3.Next</a>
</p>

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

</card>
</wml>
