https://jams.uni-jena.de/ilmswiki/index.php?action=history&feed=atom&title=Land_use_parameterLand use parameter - Revision history2026-07-24T09:45:57ZRevision history for this page on the wikiMediaWiki 1.17.0https://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12321&oldid=prevDanielS at 20:36, 20 November 20122012-11-20T20:36:02Z<p></p>
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<tr><td colspan="2"> </td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div><ins style="color: red; font-weight: bold; text-decoration: none;">[[pt:Parâmetro_do_uso_da_terra]]</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The major classification required for the J2000 hydrological model is provided in the Table below.  </div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The major classification required for the J2000 hydrological model is provided in the Table below.  </div></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12320&oldid=prevDanielS at 20:16, 20 November 20122012-11-20T20:16:13Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>----</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>----</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The information of these variables <del class="diffchange diffchange-inline">are </del>used to calculate different hydrological components during the modelling application. The LAI is used for Interception Module to calculate interception storage. Similarly, RSC0_1...12, effHeight, and root depth is required for estimation of evapotranspiration and soil module. The relevancies of these variables in calculation of different water cycle components are provided in the following documents.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The information of these variables <ins class="diffchange diffchange-inline">is </ins>used to calculate different hydrological components during the modelling application. The LAI is used for Interception Module to calculate interception storage. Similarly, RSC0_1...12, effHeight, and root depth is required for estimation of evapotranspiration and soil module. The relevancies of these variables in calculation of different water cycle components are provided in the following documents.</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Krause 2001, Krause 2010, Nepal 2012</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Krause 2001, Krause 2010, Nepal 2012</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12319&oldid=prevDanielS at 20:15, 20 November 20122012-11-20T20:15:18Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The information of these variables are used to calculate different hydrological components during the modelling application. The LAI is used for Interception Module to calculate interception storage. Similarly, RSC0_1...12, effHeight, and root depth is required for estimation of evapotranspiration and soil module. The relevancies of these variables in calculation of <del class="diffchange diffchange-inline">differnt </del>water cycle components are provided in the following documents.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The information of these variables are used to calculate different hydrological components during the modelling application. The LAI is used for Interception Module to calculate interception storage. Similarly, RSC0_1...12, effHeight, and root depth is required for estimation of evapotranspiration and soil module. The relevancies of these variables in calculation of <ins class="diffchange diffchange-inline">different </ins>water cycle components are provided in the following documents.</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Krause 2001, Krause 2010, Nepal 2012</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Krause 2001, Krause 2010, Nepal 2012</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12318&oldid=prevDanielS at 20:07, 20 November 20122012-11-20T20:07:38Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany, the value of LAI is low during winter as most of the leaves fall due to low temperature, whereas in tropical regions, few leaves fall off trees during the cold season. However, certain information, such as root depth, remains the same for each vegetation type for different zones. You are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and <del class="diffchange diffchange-inline">the </del>application in different modules <del class="diffchange diffchange-inline">are </del>provided in the table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany, the value of LAI is low during winter as most of the leaves fall due to low temperature, whereas in tropical regions, few leaves fall off trees during the cold season. However, certain information, such as root depth, remains the same for each vegetation type for different zones. You are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and <ins class="diffchange diffchange-inline">their </ins>application in different modules <ins class="diffchange diffchange-inline">is </ins>provided in the table below.</div></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12317&oldid=prevDanielS at 19:58, 20 November 20122012-11-20T19:58:58Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany the value of LAI is low during winter <del class="diffchange diffchange-inline">season </del>as most of the leaves fall due to low temperature<del class="diffchange diffchange-inline">. Conversely</del>, in tropical regions, few leaves fall off trees during <del class="diffchange diffchange-inline">winter</del>. However, certain information such as root depth remains same for each vegetation type for different zones. <del class="diffchange diffchange-inline">Users </del>are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in <del class="diffchange diffchange-inline">Table </del>below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany<ins class="diffchange diffchange-inline">, </ins>the value of LAI is low during winter as most of the leaves fall due to low temperature, <ins class="diffchange diffchange-inline">whereas </ins>in tropical regions, few leaves fall off trees during <ins class="diffchange diffchange-inline">the cold season</ins>. However, certain information<ins class="diffchange diffchange-inline">, </ins>such as root depth<ins class="diffchange diffchange-inline">, </ins>remains <ins class="diffchange diffchange-inline">the </ins>same for each vegetation type for different zones. <ins class="diffchange diffchange-inline">You </ins>are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in <ins class="diffchange diffchange-inline">the table </ins>below.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12316&oldid=prevDanielS at 19:55, 20 November 20122012-11-20T19:55:38Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. <del class="diffchange diffchange-inline">However</del>, in <del class="diffchange diffchange-inline">the </del>tropical <del class="diffchange diffchange-inline">reagions</del>, few leaves <del class="diffchange diffchange-inline">are left in </del>trees during winter <del class="diffchange diffchange-inline">season</del>. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. <ins class="diffchange diffchange-inline">Conversely</ins>, in tropical <ins class="diffchange diffchange-inline">regions</ins>, few leaves <ins class="diffchange diffchange-inline">fall off </ins>trees during winter. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12315&oldid=prevDanielS at 19:51, 20 November 20122012-11-20T19:51:13Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical <del class="diffchange diffchange-inline">reason</del>, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). You have to adjust the parameter values, which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) regions. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical <ins class="diffchange diffchange-inline">reagions</ins>, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12312&oldid=prevDanielS at 21:00, 19 November 20122012-11-19T21:00:05Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). <del class="diffchange diffchange-inline">The </del>parameter values which differ in different ecological zones <del class="diffchange diffchange-inline"> has to be adjusted by users </del>based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) <del class="diffchange diffchange-inline">region</del>. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every part of the world (such as root depth). <ins class="diffchange diffchange-inline">You have to adjust the </ins>parameter values<ins class="diffchange diffchange-inline">, </ins>which differ in different ecological zones based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) <ins class="diffchange diffchange-inline">regions</ins>. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12311&oldid=prevDanielS at 20:57, 19 November 20122012-11-19T20:57:21Z<p></p>
<table style="background-color: white; color:black;">
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<td colspan='2' style="background-color: white; color:black;">Revision as of 20:57, 19 November 2012</td>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every <del class="diffchange diffchange-inline">parts </del>of the world (such as root depth). The parameter values which differ in different ecological zones  has to be adjusted by users based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) region. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information is primarily similar in every <ins class="diffchange diffchange-inline">part </ins>of the world (such as root depth). The parameter values which differ in different ecological zones  has to be adjusted by users based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) region. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
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</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Land_use_parameter&diff=12310&oldid=prevDanielS at 20:57, 19 November 20122012-11-19T20:57:09Z<p></p>
<table style="background-color: white; color:black;">
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<td colspan='2' style="background-color: white; color:black;">← Older revision</td>
<td colspan='2' style="background-color: white; color:black;">Revision as of 20:57, 19 November 2012</td>
</tr><tr><td colspan="2" class="diff-lineno">Line 18:</td>
<td colspan="2" class="diff-lineno">Line 18:</td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The land-use classes with similar features (such as agriculture and its rainfed  and irrigated varieties) can be merged, which behaves similarly to hydrological dynamics. In case of few classes be available in the data (such as only Forest class), you can exclude other sub-classes such as deciduous or coniferous.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information <del class="diffchange diffchange-inline">are </del>primarily similar in every parts of the world (such as root depth). The parameter values which differ in different ecological zones  has to be adjusted by users based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) region. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The J2000 hydrological model requires information of each land-cover type as provided in the table below. Some information might differ in ecological zones such as LAI. However, some information <ins class="diffchange diffchange-inline">is </ins>primarily similar in every parts of the world (such as root depth). The parameter values which differ in different ecological zones  has to be adjusted by users based on the climatic and ecological conditions of the study area. For example, the LAI value is different in tropical (India) and temperate (Germany) region. In Germany the value of LAI is low during winter season as most of the leaves fall due to low temperature. However, in the tropical reason, few leaves are left in trees during winter season. However, certain information such as root depth remains same for each vegetation type for different zones. Users are free to change these values based on direct field measurement or literature. The detailed information about the land-use parameters and the application in different modules are provided in Table below.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
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</table>DanielS