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      <title>Concepts of Hydrological Cycle by hariharan sibisharan</title>
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      <description>Made with Dedication</description>
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      <pubDate>2020-05-27 06:28:31 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <description><![CDATA[<div><strong>Water cycle</strong>, also called <strong>hydrologic cycle</strong>, cycle that involves the continuous circulation of water in the Earth-atmosphere system. Of the many processes involved in the water cycle, the most important are evaporation, transpiration, condensation, precipitation, and runoff. Although the total amount of water within the cycle remains essentially constant, its distribution among the various processes is continually changing.<br><br></div>]]></description>
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         <pubDate>2020-05-27 06:45:10 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 06:56:12 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <description><![CDATA[<div>Evapotranspiration can be defined as the sum of all forms of evaporation plus transpiration, but here at the Water Science School, we'll be defining it as the sum of evaporation from the land surface plus transpiration from plants.</div>]]></description>
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         <pubDate>2020-05-27 06:56:52 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <description><![CDATA[<div>When rain falls onto the landscape, it doesn't just sit there and wait to be evaporated by the sun or lapped up by the local wildlife—it begins to move (due to gravity). Some of it seeps into the ground to refresh groundwater, but most of it flows down gradient as surface runoff. Runoff is an intricate part of the natural water cycle.</div>]]></description>
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         <pubDate>2020-05-27 07:00:31 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 07:01:39 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 07:09:07 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <description><![CDATA[<div><strong>Infiltration</strong> is the process by which water on the ground surface enters the soil. It is commonly used in both hydrology and soil sciences. The <strong>infiltration</strong> capacity is defined as the maximum rate of <strong>infiltration</strong>.</div>]]></description>
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         <pubDate>2020-05-27 07:09:29 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <description><![CDATA[<div>1.evapotranspiration<br>2. condensation<br>3. precipitation<br>4. infiltration<br>5. percolation <br>6. runoff.</div>]]></description>
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         <pubDate>2020-05-27 07:58:58 UTC</pubDate>
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         <description><![CDATA[<div><strong>Percolation</strong> is the movement of <strong>water</strong> through the soil itself. Finally, as the <strong>water</strong> percolates into the deeper layers of the soil, it reaches ground <strong>water</strong>, which is <strong>water</strong> below the surface. The upper surface of this underground <strong>water</strong> is called the "<strong>water</strong> table".</div>]]></description>
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         <pubDate>2020-05-27 08:04:08 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 08:04:21 UTC</pubDate>
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         <author>sibisharan2000</author>
         <link>https://padlet.com/sibisharan2000/cx8qx0fmxnjxodt8/wish/596377631</link>
         <description><![CDATA[<div>The air is full of water, as water vapor, even if you can't see it. Condensation is the process of water vapor turning back into liquid water, with the best example being those big, fluffy clouds floating over your head. And when the water droplets in clouds combine, they become heavy enough to form raindrops to rain down onto your head.</div>]]></description>
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         <pubDate>2020-05-27 08:07:20 UTC</pubDate>
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         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 08:08:13 UTC</pubDate>
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         <title></title>
         <author>sibisharan2000</author>
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         <pubDate>2020-05-27 08:10:46 UTC</pubDate>
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         <title></title>
         <author>sibisharan2000</author>
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         <description><![CDATA[<div>The air is full of water, even if you can't see it. Higher in the sky where it is colder than at the land surface, invisible water vapor condenses into tiny liquid water droplets—clouds. When the cloud droplets combine to form heavier cloud drops which can no longer "float" in the surrounding air, it can start to rain, snow, and hail... all forms of precipitation, the superhighway moving water from the sky to the Earth's surface.</div>]]></description>
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         <pubDate>2020-05-27 08:12:04 UTC</pubDate>
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