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  <title type="html">Euro-Mediterranean Information System on know-how in the Water sector - Evapotranspiration &amp;amp; soil moisture</title>
  <subtitle type="html">&lt;P&gt;- &lt;U&gt;&lt;STRONG&gt;Evapotranspiration&lt;/STRONG&gt;&lt;/U&gt; is the process of water loss in vapour form from a unit surface of land both directly by evaporation from the ground and by transpiration through leaf surfaces during a specific period of time. &lt;/P&gt;
&lt;P&gt;- &lt;STRONG&gt;&lt;U&gt;Soil moisture&lt;/U&gt;&lt;/STRONG&gt; is defined as the water stored in or at the continental surface and available for evaporation. &lt;/P&gt;</subtitle>
  <updated>2011-08-09T17:54:27Z</updated>
  <id>tag:www.emwis.net,2011-08-09:/topics/agriculture/ET</id>
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        href="http://www.emwis.net/topics/agriculture/ET"/>
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  <generator version="1.0" uri="http://www.emwis.net">Euro-Mediterranean Information System on know-how in the Water sector</generator>

  <entry>
    

  <title type="html">Facts and figures about Evapotranspiration and soil moisture</title>
  <link type="text/html" rel="alternate"
        href="http://www.emwis.net/topics/agriculture/ET/doc936252" />
  <id>tag:www.emwis.net,2008-09-02:/topics/agriculture/ET/doc936252</id>
  <updated>2008-09-02T18:05:52Z</updated>
  <author>
    <name>Jauad El-Kharraz</name>
  </author>
  <contributor>
    <name>Jauad El-Kharraz</name>
  </contributor>
  <summary type="html" xml:lang="en">by &lt;A href="http://www.unesco.org/water/"&gt;UNESCO Water Portal&lt;/A&gt;.</summary>



  </entry>
  <entry>
    

  <title type="html">Basics of evapotranspiration</title>
  <link type="text/html" rel="alternate"
        href="http://www.emwis.net/topics/agriculture/ET/basics-evapotranspiration" />
  <id>tag:www.emwis.net,2008-09-02:/topics/agriculture/ET/basics-evapotranspiration</id>
  <updated>2008-09-02T18:05:52Z</updated>
  <author>
    <name>Jauad El-Kharraz</name>
  </author>
  <contributor>
    <name>Jauad El-Kharraz</name>
  </contributor>
  <summary type="html" xml:lang="en">&lt;span&gt;
&lt;div class="centrado"&gt;
By &lt;a href="http://www.environmental-expert.com/author_file.aspx?idproducttype=6&amp;amp;cmp=1&amp;amp;idauthor=136814&amp;amp;fname=Keith&amp;amp;lname=Bellingham" class="enlaceNormal"&gt;Keith&amp;nbsp;Bellingham&lt;/a&gt;
&lt;/div&gt;
&lt;/span&gt;
&lt;span&gt;Courtesy of &lt;a href="http://www.environmental-expert.com/STSE_resultEach.aspx?cid=7850&amp;amp;idproducttype=1&amp;amp;idmainpage=0&amp;amp;level=0"&gt;Stevens Water Monitoring Systems, Inc.&lt;/a&gt;&lt;/span&gt;
&lt;span&gt;&lt;br /&gt;
Originally published Aug. 2008&lt;/span&gt;
&lt;br /&gt;
&lt;span&gt;
&lt;div style="width: 85%; text-align: justify"&gt;
Evapotranspiration
(ET) represents the loss of water from the Earth&amp;rsquo;s surface from the
combination of direct evaporation and plant transpiration. ET is
usually expressed as a rate such as inches per day. Knowledge of ET is
important for irrigation scheduling but it is also an important factor
for other land use applications such as septic tank drain fields, water
shed water budgeting, and climate and weather models. ET can be used as
a historical tool but usually it is predicted or used in a forecast to
help irrigators optimize irrigation.
&lt;/div&gt;
&lt;/span&gt;
</summary>



  </entry>
  <entry>
    

  <title type="html">Integrated Methodology for Estimating Water Use in Mediterranean Agricultural Areas </title>
  <link type="text/html" rel="alternate"
        href="http://www.emwis.net/topics/agriculture/ET/integrated-methodology-estimating-water-use" />
  <id>tag:www.emwis.net,2010-04-23:/topics/agriculture/ET/integrated-methodology-estimating-water-use</id>
  <updated>2010-04-23T17:51:23Z</updated>
  <author>
    <name>Jauad El-Kharraz</name>
  </author>
  <contributor>
    <name>Jauad El-Kharraz</name>
  </contributor>
  <summary type="html" xml:lang="en">&lt;p&gt;Agricultural use is by far the largest consumer of fresh water worldwide,&amp;nbsp;especially in the Mediterranean, where it has reached unsustainable levels, thus posing a&amp;nbsp;serious threat to water resources. Having a good estimate of the water used in an&amp;nbsp;agricultural area would help water managers create incentives for water savings at the&amp;nbsp;farmer and basin level, and meet the demands of the European Water Framework Directive.&lt;/p&gt;&lt;p&gt;This work presents an integrated methodology for estimating water use in Mediterranean&amp;nbsp;agricultural areas. It is based on well established methods of estimating the actual&amp;nbsp;evapotranspiration through surface energy fluxes, customized for better performance under&amp;nbsp;the Mediterranean conditions: small parcel sizes, detailed crop pattern, and lack of&amp;nbsp;necessary data. The methodology has been tested and validated on the agricultural plain of&amp;nbsp;the river Strimonas (Greece) using a time series of Terra MODIS and Landsat 5 TM&amp;nbsp;satellite images, and used to produce a seasonal water use map at a high spatial resolution.&amp;nbsp;&lt;/p&gt;&lt;p&gt;Finally, a tool has been designed to implement the methodology with a user-friendly&amp;nbsp;interface, in order to facilitate its operational use.&lt;/p&gt;</summary>



  </entry>
  <entry>
    

  <title type="html">NDVI 10-day daily composites</title>
  <link type="text/html" rel="alternate"
        href="http://www.emwis.net/topics/agriculture/ET/ndwi-10-day-daily-composites" />
  <id>tag:www.emwis.net,2010-10-27:/topics/agriculture/ET/ndwi-10-day-daily-composites</id>
  <updated>2010-10-27T05:34:08Z</updated>
  <author>
    <name>Jauad El-Kharraz</name>
  </author>
  <contributor>
    <name>Jauad El-Kharraz</name>
  </contributor>
  <summary type="html" xml:lang="en">&lt;p&gt;The Normalized Difference Water Index (NDVI) (Gao, 1996) is a satellite-derived index from the Near-Infrared (NIR) and Short Wave Infrared (SWIR) channels. The SWIR reflectance reflects changes in both the vegetation water content and the spongy mesophyll structure in vegetation canopies, while the NIR reflectance is affected by leaf internal structure and leaf dry matter content but not by water content.&amp;nbsp;&lt;/p&gt;</summary>



  </entry>
  <entry>
    

  <title type="html">Estimating reference evapotranspiration using remote sensing and empirical models in a region with limited ground data availability in Kenya</title>
  <link type="text/html" rel="alternate"
        href="http://www.emwis.net/topics/agriculture/ET/estimating-reference-evapotranspiration-using-remote-sensing-and-empirical" />
  <id>tag:www.emwis.net,2011-04-22:/topics/agriculture/ET/estimating-reference-evapotranspiration-using-remote-sensing-and-empirical</id>
  <updated>2011-04-22T16:36:22Z</updated>
  <author>
    <name>Jauad El-Kharraz</name>
  </author>
  <contributor>
    <name>Jauad El-Kharraz</name>
  </contributor>
  <summary type="html" xml:lang="en">&lt;p&gt;Evapotranspiration is an important component of the hydrological cycle and its accurate quantiﬁcation is&amp;nbsp;crucial for the design, operation and management of irrigation systems. However, the lack of meteorological data from ground stations is a clear barrier to the proper management of water resources in poor&amp;nbsp;countries, increasing the risks of water scarcity and water conﬂicts. In the presented study, three&amp;nbsp;temperature based ET models are evaluated in the Taita Hills, Kenya, which is a particularly important&amp;nbsp;region from the environmental conservation point of view. The Hargreaves, the Thornthwaite and the&amp;nbsp;BlaneyeCriddle are the three tested methods, given that these are the most recommended approaches&amp;nbsp;when only air temperature data are available. Land surface temperature data, retrieved from the MODIS/Terra sensor are evaluated as an alternative input for the models. One weather station with complete&amp;nbsp;climate datasets is used to calibrate the selected model using the FAO-56 PenmaneMonteith method as&amp;nbsp;a reference. The results indicate that the Hargreaves model is the most appropriate for this particular&amp;nbsp;study area, with an average RMSE of 0.47 mm d1, and a correlation coefﬁcient of 0.67. The MODIS LST&amp;nbsp;product was satisfactorily incorporated into the Hargreaves model achieving results that are consistent&amp;nbsp;with studies reported in the literature using air temperature data collected in ground stations.&lt;/p&gt;</summary>



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