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		<id>https://wocatpedia.net/index.php?action=history&amp;feed=atom&amp;title=Precipitation</id>
		<title>Precipitation - Revision history</title>
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		<updated>2026-04-19T14:26:08Z</updated>
		<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://wocatpedia.net/index.php?title=Precipitation&amp;diff=4133&amp;oldid=prev</id>
		<title>Irena Irmler at 13:43, 18 March 2013</title>
		<link rel="alternate" type="text/html" href="https://wocatpedia.net/index.php?title=Precipitation&amp;diff=4133&amp;oldid=prev"/>
				<updated>2013-03-18T13:43:48Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Older revision&lt;/td&gt;
			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Revision as of 13:43, 18 March 2013&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background: #eee; color:black; font-size: smaller;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;The most direct impact of global climate change on agricultural water supply is its alteration of [[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Climate_Change_and_Agriculture&lt;/del&gt;|climate change]]. Changes will occur in average annual amount, temporal distribution, and intensity and duration of individual events. The effects will be felt directly, in the case of [[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Rainfed_Agriculture&lt;/del&gt;|rainfed agriculture]], and indirectly, through their effect on [[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Watershed_management&lt;/del&gt;|watershed]] hydrology and runoff, in the case of [[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Irrigated_Agriculture&lt;/del&gt;|irrigated agriculture]]. Higher global temperatures will evaporate more water and increase the moisture-holding capacity of the atmosphere. Annual precipitation will increase in some areas and decrease in others. In general, areas which are already humid will receive more rainfall and already dry areas will receive less. [[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Regional_Climate_Models&lt;/del&gt;|Regional climate models]] can provide more detailed predictions, but their resolution is still relatively coarse. Worldwide, the expectation is for more intense precipitation events and longer dry periods between events.&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;The most direct impact of global climate change on agricultural water supply is its alteration of [[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Climate Change and Agriculture&lt;/ins&gt;|climate change]]. Changes will occur in average annual amount, temporal distribution, and intensity and duration of individual events. The effects will be felt directly, in the case of [[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Rainfed Agriculture&lt;/ins&gt;|rainfed agriculture]], and indirectly, through their effect on [[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Watershed management&lt;/ins&gt;|watershed]] hydrology and runoff, in the case of [[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Design_for_irrigation&lt;/ins&gt;|irrigated agriculture]]. Higher global temperatures will evaporate more water and increase the moisture-holding capacity of the atmosphere. Annual precipitation will increase in some areas and decrease in others. In general, areas which are already humid will receive more rainfall and already dry areas will receive less. [[&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Regional Climate Models&lt;/ins&gt;|Regional climate models]] can provide more detailed predictions, but their resolution is still relatively coarse. Worldwide, the expectation is for more intense precipitation events and longer dry periods between events.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Irena Irmler</name></author>	</entry>

	<entry>
		<id>https://wocatpedia.net/index.php?title=Precipitation&amp;diff=4131&amp;oldid=prev</id>
		<title>Irena Irmler: Created page with &quot; The most direct impact of global climate change on agricultural water supply is its alteration of climate change. Changes will occur in ave...&quot;</title>
		<link rel="alternate" type="text/html" href="https://wocatpedia.net/index.php?title=Precipitation&amp;diff=4131&amp;oldid=prev"/>
				<updated>2013-03-18T10:14:22Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot; The most direct impact of global climate change on agricultural water supply is its alteration of &lt;a href=&quot;/wiki/Climate_Change_and_Agriculture&quot; title=&quot;Climate Change and Agriculture&quot;&gt;climate change&lt;/a&gt;. Changes will occur in ave...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&lt;br /&gt;
The most direct impact of global climate change on agricultural water supply is its alteration of [[Climate_Change_and_Agriculture|climate change]]. Changes will occur in average annual amount, temporal distribution, and intensity and duration of individual events. The effects will be felt directly, in the case of [[Rainfed_Agriculture|rainfed agriculture]], and indirectly, through their effect on [[Watershed_management|watershed]] hydrology and runoff, in the case of [[Irrigated_Agriculture|irrigated agriculture]]. Higher global temperatures will evaporate more water and increase the moisture-holding capacity of the atmosphere. Annual precipitation will increase in some areas and decrease in others. In general, areas which are already humid will receive more rainfall and already dry areas will receive less. [[Regional_Climate_Models|Regional climate models]] can provide more detailed predictions, but their resolution is still relatively coarse. Worldwide, the expectation is for more intense precipitation events and longer dry periods between events.&lt;/div&gt;</summary>
		<author><name>Irena Irmler</name></author>	</entry>

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