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	<id>https://climatewiki.earth/wiki/index.php?action=history&amp;feed=atom&amp;title=Albedo_Effect</id>
	<title>Albedo Effect - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://climatewiki.earth/wiki/index.php?action=history&amp;feed=atom&amp;title=Albedo_Effect"/>
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	<updated>2026-04-13T16:27:35Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://climatewiki.earth/wiki/index.php?title=Albedo_Effect&amp;diff=7902&amp;oldid=prev</id>
		<title>Florez4747 at 05:00, 25 June 2023</title>
		<link rel="alternate" type="text/html" href="https://climatewiki.earth/wiki/index.php?title=Albedo_Effect&amp;diff=7902&amp;oldid=prev"/>
		<updated>2023-06-25T05:00:58Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 05:00, 25 June 2023&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l5&quot;&gt;Line 5:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 5:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;Blockquote&amp;gt;If Earth's climate is colder and there is more snow and ice on the planet, albedo increases, more sunlight is reflected out to space, and the climate gets even cooler. But, when warming causes snow and ice to melt, darker colored surfaces are exposed, albedo decreases, less solar energy is reflected out to space, and the planet warms even more. This is known as the ice-albedo feedback.&amp;lt;Ref&amp;gt;https://scied.ucar.edu/learning-zone/how-climate-works/albedo-and-climate&amp;lt;/Ref&amp;gt;&amp;lt;/Blockquote&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;Blockquote&amp;gt;If Earth's climate is colder and there is more snow and ice on the planet, albedo increases, more sunlight is reflected out to space, and the climate gets even cooler. But, when warming causes snow and ice to melt, darker colored surfaces are exposed, albedo decreases, less solar energy is reflected out to space, and the planet warms even more. This is known as the ice-albedo feedback.&amp;lt;Ref&amp;gt;https://scied.ucar.edu/learning-zone/how-climate-works/albedo-and-climate&amp;lt;/Ref&amp;gt;&amp;lt;/Blockquote&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;= See also =&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[Climate Feedback Loops]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br/&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;= Sources =&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;= Sources =&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Florez4747</name></author>
	</entry>
	<entry>
		<id>https://climatewiki.earth/wiki/index.php?title=Albedo_Effect&amp;diff=6335&amp;oldid=prev</id>
		<title>Florez4747: Created page with &quot;&quot;The  albedo effect is the ability of a surface to reflect sunlight. Light-colored surfaces  (high albedo) reflect more sunlight than dark-colored surfaces (low albedo). Albedo can also be known  as surface albedo.&quot;&lt;Ref&gt;https://greenly.earth/en-us/blog/ecology-news/what-is-the-albedo-effect-and-how-does-it-impact-global-warming&lt;/Ref&gt;  = Effect on Global Heating =   &lt;Blockquote&gt;If Earth's climate is colder and there is more snow and ice on the planet, albedo increases, mo...&quot;</title>
		<link rel="alternate" type="text/html" href="https://climatewiki.earth/wiki/index.php?title=Albedo_Effect&amp;diff=6335&amp;oldid=prev"/>
		<updated>2023-03-17T02:29:10Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&amp;quot;The  albedo effect is the ability of a surface to reflect sunlight. Light-colored surfaces  (high albedo) reflect more sunlight than dark-colored surfaces (low albedo). Albedo can also be known  as surface albedo.&amp;quot;&amp;lt;Ref&amp;gt;https://greenly.earth/en-us/blog/ecology-news/what-is-the-albedo-effect-and-how-does-it-impact-global-warming&amp;lt;/Ref&amp;gt;  = Effect on Global Heating =   &amp;lt;Blockquote&amp;gt;If Earth&amp;#039;s climate is colder and there is more snow and ice on the planet, albedo increases, mo...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;quot;The  albedo effect is the ability of a surface to reflect sunlight. Light-colored surfaces  (high albedo) reflect more sunlight than dark-colored surfaces (low albedo). Albedo can also be known  as surface albedo.&amp;quot;&amp;lt;Ref&amp;gt;https://greenly.earth/en-us/blog/ecology-news/what-is-the-albedo-effect-and-how-does-it-impact-global-warming&amp;lt;/Ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
= Effect on Global Heating = &lt;br /&gt;
&lt;br /&gt;
&amp;lt;Blockquote&amp;gt;If Earth's climate is colder and there is more snow and ice on the planet, albedo increases, more sunlight is reflected out to space, and the climate gets even cooler. But, when warming causes snow and ice to melt, darker colored surfaces are exposed, albedo decreases, less solar energy is reflected out to space, and the planet warms even more. This is known as the ice-albedo feedback.&amp;lt;Ref&amp;gt;https://scied.ucar.edu/learning-zone/how-climate-works/albedo-and-climate&amp;lt;/Ref&amp;gt;&amp;lt;/Blockquote&amp;gt;&lt;br /&gt;
&lt;br /&gt;
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= Sources =&lt;/div&gt;</summary>
		<author><name>Florez4747</name></author>
	</entry>
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