http://www.colloquiam.com/wd/index.php?action=history&feed=atom&title=Vicario_et_al_2020aVicario et al 2020a - Revision history2026-05-11T23:22:17ZRevision history for this page on the wikiMediaWiki 1.27.0-wmf.10http://www.colloquiam.com/wd/index.php?title=Vicario_et_al_2020a&diff=172947&oldid=prevLeticiavicario at 23:21, 2 October 20202020-10-02T23:21:03Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==Abstract==</div></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==Abstract==</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Precipitation is considered the main variable for the evaluation of meteorological drought in a basin. <del class="diffchange diffchange-inline">Droughts </del>is a <del class="diffchange diffchange-inline">phenomena </del>of different spatial scale, so <del class="diffchange diffchange-inline">that </del>is convenient to have simultaneous rainfall <del class="diffchange diffchange-inline">records in time and </del>in different locations, in order to analyze <del class="diffchange diffchange-inline">their </del>evolution in space, depending on the size and the variability of the characteristics in the basin. In Argentina, specifically in the central region, the availability of information on the spatial variability of rainfall is not usual, so drought studies in this region are limited. Due to this it is convenient to validate the rainfall information obtained through satellite missions. The present work evaluates the validity and applicability of monthly rainfall data estimated through TRMM in ten stations in the basin of the Carcarañá river in the central region of Argentina and its subsequent application to studies on meteorological droughts through a representative index (SPI). Statistical parameters such as the concordance coefficient, the correlation coefficient and the bias were used for this analysis. There was a significant variation of the parameters with respect to the height. <del class="diffchange diffchange-inline">Was observed </del>better coefficients in stations located in plain compared with stations located in mountainous areas.</div></td><td class='diff-marker'>+</td><td style="color:black; 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;"><div>Precipitation is considered the main variable for the evaluation of meteorological drought in a basin. <ins class="diffchange diffchange-inline">Drought </ins>is a <ins class="diffchange diffchange-inline">phenomenon </ins>of different spatial scale, so <ins class="diffchange diffchange-inline">it </ins>is convenient to have simultaneous <ins class="diffchange diffchange-inline">time </ins>rainfall <ins class="diffchange diffchange-inline">series </ins>in different locations, in order to analyze <ins class="diffchange diffchange-inline">its </ins>evolution in space, depending on the size and the variability of the characteristics in the basin. In Argentina, specifically in the central region, the availability of information on the spatial variability of rainfall is not usual, so drought studies in this region are limited. Due to this it is convenient to validate the rainfall information obtained through satellite missions. The present work evaluates the validity and applicability of monthly rainfall data estimated through TRMM in ten stations in the basin of the Carcarañá river in the central region of Argentina and its subsequent application to studies on meteorological droughts through a representative index (SPI). Statistical parameters such as the concordance coefficient, the correlation coefficient and the bias were used for this analysis. There was a significant variation of the parameters with respect to the height. <ins class="diffchange diffchange-inline">In addition, </ins>better coefficients in stations located in plain compared with stations located in mountainous areas<ins class="diffchange diffchange-inline">, were observed</ins>.</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==Key words: Monthly precipitation - Meteorological drought - Validation TRMM - basin of the central region of Argentina==</div></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==Key words: Monthly precipitation - Meteorological drought - Validation TRMM - basin of the central region of Argentina==</div></td></tr>
</table>Leticiavicariohttp://www.colloquiam.com/wd/index.php?title=Vicario_et_al_2020a&diff=172945&oldid=prevLagodoy: Lagodoy moved page Review 521930852811 to Vicario et al 2020a2020-10-02T22:05:42Z<p>Lagodoy moved page <a href="/public/Review_521930852811" class="mw-redirect" title="Review 521930852811">Review 521930852811</a> to <a href="/public/Vicario_et_al_2020a" title="Vicario et al 2020a">Vicario et al 2020a</a></p>
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<td colspan='1' style="background-color: white; color:black; text-align: center;">Revision as of 22:05, 2 October 2020</td>
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</td></tr></table>Lagodoyhttp://www.colloquiam.com/wd/index.php?title=Vicario_et_al_2020a&diff=149495&oldid=prevLeticiavicario: Leticiavicario moved page Draft Vicario 322252791 to Review 5219308528112020-01-08T15:59:01Z<p>Leticiavicario moved page <a href="/public/Draft_Vicario_322252791" class="mw-redirect" title="Draft Vicario 322252791">Draft Vicario 322252791</a> to <a href="/public/Review_521930852811" class="mw-redirect" title="Review 521930852811">Review 521930852811</a></p>
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<td colspan='1' style="background-color: white; color:black; text-align: center;">Revision as of 15:59, 8 January 2020</td>
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</td></tr></table>Leticiavicariohttp://www.colloquiam.com/wd/index.php?title=Vicario_et_al_2020a&diff=149490&oldid=prevLeticiavicario at 15:37, 8 January 20202020-01-08T15:37:07Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>==Evaluación de precipitaciones mensuales estimadas con TRMM para su uso en estudios de sequías meteorológicas <del class="diffchange diffchange-inline">a través de un índice representativo  </del>==</div></td><td class='diff-marker'>+</td><td style="color:black; 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;"><div>==Evaluación de precipitaciones mensuales estimadas con TRMM para su uso en estudios de sequías meteorológicas ==</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>Precipitation is considered the main variable for the evaluation of meteorological drought in a basin. Droughts is a phenomena of different spatial scale, so that is convenient to have simultaneous rainfall records in time and in different locations, in order to analyze their evolution in space, depending on the size and the variability of the characteristics in the basin. In Argentina, specifically in the central region, the availability of information on the spatial variability of rainfall is not usual, so drought studies in this region are limited. Due to this it is convenient to validate the rainfall information obtained through satellite missions. The present work evaluates the validity and applicability of monthly rainfall data estimated through TRMM in ten stations in the basin of the Carcarañá river in the central region of Argentina and its subsequent application to studies on meteorological droughts through a representative index (SPI). Statistical parameters such as the concordance coefficient, the correlation coefficient and the bias were used for this analysis. There was a significant variation of the parameters with respect to the height. Was observed better coefficients in stations located in plain compared with stations located in mountainous areas.</div></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>Precipitation is considered the main variable for the evaluation of meteorological drought in a basin. Droughts is a phenomena of different spatial scale, so that is convenient to have simultaneous rainfall records in time and in different locations, in order to analyze their evolution in space, depending on the size and the variability of the characteristics in the basin. In Argentina, specifically in the central region, the availability of information on the spatial variability of rainfall is not usual, so drought studies in this region are limited. Due to this it is convenient to validate the rainfall information obtained through satellite missions. The present work evaluates the validity and applicability of monthly rainfall data estimated through TRMM in ten stations in the basin of the Carcarañá river in the central region of Argentina and its subsequent application to studies on meteorological droughts through a representative index (SPI). Statistical parameters such as the concordance coefficient, the correlation coefficient and the bias were used for this analysis. There was a significant variation of the parameters with respect to the height. Was observed better coefficients in stations located in plain compared with stations located in mountainous areas.</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"></td></tr>
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<tr><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==INTRODUCCIÓN ==</div></td><td class='diff-marker'> </td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>==INTRODUCCIÓN ==</div></td></tr>
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</table>Leticiavicariohttp://www.colloquiam.com/wd/index.php?title=Vicario_et_al_2020a&diff=149487&oldid=prevLeticiavicario: Created page with "<!-- metadata commented in wiki content ==Evaluación de precipitaciones mensuales estimadas con TRMM para su uso en estudios de sequías meteorológicas a través de un ín..."2020-01-08T15:20:15Z<p>Created page with "<!-- metadata commented in wiki content ==Evaluación de precipitaciones mensuales estimadas con TRMM para su uso en estudios de sequías meteorológicas a través de un ín..."</p>
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