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 <!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.0 20120330//EN" "http://jats.nlm.nih.gov/publishing/1.0/JATS-journalpublishing1.dtd"> <article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" article-type="research-article" dtd-version="1.0" xml:lang="en">
  <front>
    <journal-meta>
      <journal-id journal-id-type="publisher-id">JWC</journal-id>
      <journal-title-group>
        <journal-title>Journal of Weather Changes</journal-title>
      </journal-title-group>
      <issn pub-type="epub">3070-3379</issn>
      <publisher>
        <publisher-name>Open Access Pub</publisher-name>
        <publisher-loc>United States</publisher-loc>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.14302/issn.3070-3379.jwc-24-5072</article-id>
      <article-id pub-id-type="publisher-id">JWC-24-5072</article-id>
      <article-categories>
        <subj-group>
          <subject>research-article</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title>Dragonhead Cyclone in The Falkland Islands (Malvines Islands) has Double Cote's Spiral Like NGC 5247</article-title>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author">
          <name>
            <surname>Ricardo</surname>
            <given-names>Gobato</given-names>
          </name>
          <xref ref-type="aff" rid="idm1841500020">1</xref>
          <xref ref-type="aff" rid="idm1841512020">*</xref>
        </contrib>
        <contrib contrib-type="author">
          <name>
            <surname>Abhijt</surname>
            <given-names>Mitra</given-names>
          </name>
          <xref ref-type="aff" rid="idm1841499876">2</xref>
        </contrib>
        <contrib contrib-type="author">
          <name>
            <surname>Sana</surname>
            <given-names>Ahmed</given-names>
          </name>
          <xref ref-type="aff" rid="idm1841498580">3</xref>
        </contrib>
      </contrib-group>
      <aff id="idm1841500020">
        <label>1</label>
        <addr-line>Green Land Landscaping and Gardening, Seedling Growth Laboratory, 86130-000, Parana, Brazil.</addr-line>
      </aff>
      <aff id="idm1841499876">
        <label>2</label>
        <addr-line>Department of Marine Science, University of Calcutta, 35 B. C Road, Kolkata, 700019, West Bengal, India.</addr-line>
      </aff>
      <aff id="idm1841498580">
        <label>3</label>
        <addr-line>Department of Oceanography, Techno India University, West Bengal, EM 4 Salt Lake, Sector V, Kolkata 700091, India.</addr-line>
      </aff>
      <aff id="idm1841512020">
        <label>*</label>
        <addr-line>Corresponding Author </addr-line>
      </aff>
      <contrib-group>
        <contrib contrib-type="editor">
          <name>
            <surname>Sasho</surname>
            <given-names>Stoleski</given-names>
          </name>
          <xref ref-type="aff" rid="idm1841357028">1</xref>
        </contrib>
      </contrib-group>
      <aff id="idm1841357028">
        <label>1</label>
        <addr-line>Institute of Occupational Health of R. Macedonia, WHO CC and Ga2len CC.</addr-line>
      </aff>
      <author-notes>
        <corresp>
    
    Ricardo Gobato, <addr-line>Green Land Landscaping and Gardening, Seedling Growth Laboratory, 86130-000, Parana, Brazil</addr-line>, <email>ricardogobato@hotmail.com</email></corresp>
        <fn fn-type="conflict" id="idm1849342116">
          <p>The authors have declared that no competing interests exist.</p>
        </fn>
      </author-notes>
      <pub-date pub-type="epub" iso-8601-date="2024-07-10">
        <day>10</day>
        <month>07</month>
        <year>2024</year>
      </pub-date>
      <volume>1</volume>
      <issue>1</issue>
      <fpage>18</fpage>
      <lpage>29</lpage>
      <history>
        <date date-type="received">
          <day>12</day>
          <month>04</month>
          <year>2024</year>
        </date>
        <date date-type="accepted">
          <day>29</day>
          <month>06</month>
          <year>2024</year>
        </date>
        <date date-type="online">
          <day>10</day>
          <month>07</month>
          <year>2024</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© </copyright-statement>
        <copyright-year>2024</copyright-year>
        <copyright-holder>Ricardo Gobato, et.al</copyright-holder>
        <license xlink:href="http://creativecommons.org/licenses/by/4.0/" xlink:type="simple">
          <license-p>This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
        </license>
      </permissions>
      <self-uri xlink:href="http://openaccesspub.org/jwc/article/2233">This article is available from http://openaccesspub.org/jwc/article/2233</self-uri>
      <abstract>
        <p>Extratropical cyclones are common in the South Atlantic. They generally arise with the passage of cold fronts to the south of the South American continent, crossing the south of Chile and Argentina, in the regions of Puerto Natales, Punta Arenas (Chile), Rio Galegos, Rio Grande, El Calafate and Ushuaia (Argentina). The extratropical cyclone analyzed presented at its peak the very characteristic shape of a Chinese dragon. Other cyclones in the form of a Cote's spiral curve are part of this analysis (Gobato et al., 2018-2023).  They present a mathematical form of a double Cotes Spiral curve. Here called the Dragonhead cyclone,                      indicate a structural similarity with spiral galaxies, especially NGC 5247, in the constellation Virgo. With an area of influence and a size of around 3,247                            thousand km<sup>2</sup> at its peak, it moved quickly in a west-northwest (WNW) direction, with an average speed of 76 km/h, with winds of 84 km/h at 100 km from the nucleus, as it passed north of the Falkland Islands (Malvinas Islands). The                  cyclone temperature during its trajectory varies from -45ºC to -50ºC at its edge, while at its core it varies between -10ºC to -25ºC.</p>
        <p>In the data collected (Gobato et al., 2018-2023), and analyzed from the Dragonhead cyclone, it is clear that all extratropical cyclones that appear south of the South American continent, below 40° latitude,  have the shape of a spiral curve, like the spiral galaxy. Most of these are in the form of a double Cote’s             spiral curve.</p>
      </abstract>
      <kwd-group>
        <kwd>Cyclones</kwd>
        <kwd>South American</kwd>
        <kwd>Spiral Galaxy</kwd>
        <kwd>NGC 5247</kwd>
        <kwd>South Atlantic</kwd>
        <kwd>Chinese dragon</kwd>
      </kwd-group>
      <counts>
        <fig-count count="7"/>
        <table-count count="1"/>
        <page-count count="11"/>
      </counts>
    </article-meta>
  </front>
  <body>
    <sec id="idm1841361924" sec-type="intro">
      <title>Introduction</title>
      <sec id="idm1841361492">
        <title>Cyclone </title>
        <p>A cyclone is a large air mass that rotates around a strong center of low                atmospheric pressure, counterclockwise in the Northern Hemisphere and               clockwise in the Southern Hemisphere as viewed from above (opposite to an  anticyclone). <xref ref-type="bibr" rid="ridm1849391076">1</xref><xref ref-type="bibr" rid="ridm1849395396">2</xref><xref ref-type="bibr" rid="ridm1849396124">3</xref><xref ref-type="bibr" rid="ridm1849470708">4</xref><xref ref-type="bibr" rid="ridm1849110268">27</xref><xref ref-type="bibr" rid="ridm1849066340">29</xref> Subtropical cyclone is a weather system that can form between the equator and the 50th parallel. <xref ref-type="bibr" rid="ridm1849391076">1</xref><xref ref-type="bibr" rid="ridm1849499076">5</xref><xref ref-type="bibr" rid="ridm1849247492">6</xref><xref ref-type="bibr" rid="ridm1849244828">7</xref><xref ref-type="bibr" rid="ridm1849235772">8</xref><xref ref-type="bibr" rid="ridm1849237356">9</xref><xref ref-type="bibr" rid="ridm1849098532">26</xref><xref ref-type="bibr" rid="ridm1849110268">27</xref> These storms usually have a                  radius of maximum winds that is larger than what is observed in purely tropical systems, and their maximum sustained winds have not been observed to exceed about 32 m/s (64 knots). Subtropical cyclones in the Atlantic basin are classiﬁed  by their maximum sustained surface winds: Subtropical depressions have surface winds less than 18 m/s (35 knots), while subtropical storms have surface winds greater than or equal to 18 m/s. <xref ref-type="bibr" rid="ridm1849237356">9</xref>, <xref ref-type="bibr" rid="ridm1849223140">10</xref>, <xref ref-type="bibr" rid="ridm1849227316">11</xref>, <xref ref-type="bibr" rid="ridm1849205604">12</xref>, <xref ref-type="bibr" rid="ridm1849204452">13</xref>, <xref ref-type="bibr" rid="ridm1849214532">14</xref>, <xref ref-type="bibr" rid="ridm1849209420">15</xref>, <xref ref-type="bibr" rid="ridm1849161636">16</xref>, <xref ref-type="bibr" rid="ridm1849157532">17</xref>, <xref ref-type="bibr" rid="ridm1849168692">18</xref>, <xref ref-type="bibr" rid="ridm1849140844">19</xref>, <xref ref-type="bibr" rid="ridm1849137028">20</xref>, <xref ref-type="bibr" rid="ridm1849148332">21</xref>, <xref ref-type="bibr" rid="ridm1849098532">26</xref>, <xref ref-type="bibr" rid="ridm1849110268">27</xref>, <xref ref-type="bibr" rid="ridm1849107460">28</xref>, <xref ref-type="bibr" rid="ridm1849066340">29</xref>, <xref ref-type="bibr" rid="ridm1849069940">39</xref></p>
        <p>Tropical cyclones are compact, circular storms, generally some 320 km (200 miles) in diameter, whose winds swirl around a central region of low atmospheric pressure. The winds are driven by this                       low-pressure core and by the rotation of the Earth, which deﬂects the path of the wind through a phenomenon known as the Coriolis force. As a result, tropical cyclones rotate in a counterclockwise (or cyclonic) direction in the Northern Hemisphere and  clockwise (or anticyclonic) direction in the       Southern Hemisphere. .<xref ref-type="bibr" rid="ridm1849237356">9</xref>, <xref ref-type="bibr" rid="ridm1849223140">10</xref>, <xref ref-type="bibr" rid="ridm1849227316">11</xref>, <xref ref-type="bibr" rid="ridm1849205604">12</xref>, <xref ref-type="bibr" rid="ridm1849204452">13</xref>, <xref ref-type="bibr" rid="ridm1849214532">14</xref>, <xref ref-type="bibr" rid="ridm1849209420">15</xref>, <xref ref-type="bibr" rid="ridm1849161636">16</xref>, <xref ref-type="bibr" rid="ridm1849157532">17</xref>, <xref ref-type="bibr" rid="ridm1849168692">18</xref>, <xref ref-type="bibr" rid="ridm1849140844">19</xref>, <xref ref-type="bibr" rid="ridm1849137028">20</xref>, <xref ref-type="bibr" rid="ridm1849148332">21</xref>, <xref ref-type="bibr" rid="ridm1849098532">26</xref>, <xref ref-type="bibr" rid="ridm1849110268">27</xref>, <xref ref-type="bibr" rid="ridm1849066340">29</xref>, <xref ref-type="bibr" rid="ridm1849069940">39</xref></p>
      </sec>
      <sec id="idm1841362644">
        <title>NGC 5247 Spiral Galaxy</title>
        <p>Spiral galaxies <xref ref-type="bibr" rid="ridm1849013924">40</xref><xref ref-type="bibr" rid="ridm1849012988">41</xref><xref ref-type="bibr" rid="ridm1849009892">42</xref><xref ref-type="bibr" rid="ridm1849005788">43</xref> form a class of galaxy originally described by Edwin Hubble in his 1936 work The Realm of the Nebulae and, as such, form part of the Hubble sequence. Most spiral               galaxies consist of a ﬂat, rotating disk containing stars, gas and dust, and a central concentration of stars known as the bulge. These are often surrounded by a much fainter halo of stars, many of which reside in globular clusters<xref ref-type="bibr" rid="ridm1848954332">54</xref></p>
        <p>Spiral galaxies are named by their spiral structures that extend from the center into the galactic disc. The spiral arms are sites of ongoing star formation and are brighter than the surrounding disc because of the young, hot OB stars that inhabit them <xref ref-type="bibr" rid="ridm1849009892">42</xref><xref ref-type="bibr" rid="ridm1849005788">43</xref><xref ref-type="bibr" rid="ridm1848998300">47</xref><xref ref-type="bibr" rid="ridm1848954332">54</xref>.</p>
        <p>The (<xref ref-type="fig" rid="idm1849433332">Figure 1</xref>) shows NGC 5247, a grand design barred spiral galaxy, located 60–70 million light-years away. The galaxy lies face-on towards Earth, thus providing an excellent view of its pinwheel structure and multiple arms. It is in the zodiacal constellation of Virgo (the Maiden) <xref ref-type="bibr" rid="ridm1848952460">55</xref>.</p>
        <fig id="idm1849433332">
          <label>Figure 1.</label>
          <caption>
            <title> HAWK-I image of NGC 5247 Galaxy.</title>
          </caption>
          <graphic xlink:href="images/image1.jpg" mime-subtype="jpg"/>
        </fig>
        <p>The image was made in infrared light with the HAWK-I camera on ESO’s Very Large Telescope at Paranal Observatory in Chile. HAWK-I is one of the most powerful infrared imagers in the world, and this is one of the sharpest and most detailed pictures of this galaxy ever taken from Earth. The filters used were Y (shown here in blue), J (in light blue), H (in green), and K (in red). The field of view of the image is about 6.4 arc minutes. <xref ref-type="bibr" rid="ridm1848952460">55</xref></p>
        <p>NGC 5247 is a face-on unbarred spiral galaxy located some 60 million light years away in the                       constellation Virgo. It is a member of the Virgo II Groups, a series of galaxies and galaxy clusters strung out from the southern edge of the Virgo Super cluster. This grand design spiral galaxy displays no indications of distortion caused by interaction with other galaxies. It has two spiral arms that                  bifurcate after wrapping halfway around the nucleus. The disk is estimated to be 4.9 ± 2.0 kly (1.5 ± 0.6 kpc) in thickness and it is inclined by roughly 28° to the line of sight. <xref ref-type="bibr" rid="ridm1848946844">56</xref></p>
      </sec>
      <sec id="idm1841359188">
        <title>Cote’s spiral</title>
        <p>In physics and in the mathematics of plane curves <xref ref-type="bibr" rid="ridm1849066340">29</xref><xref ref-type="bibr" rid="ridm1849063244">30</xref><xref ref-type="bibr" rid="ridm1849058636">31</xref><xref ref-type="bibr" rid="ridm1849057268">32</xref><xref ref-type="bibr" rid="ridm1849055468">33</xref><xref ref-type="bibr" rid="ridm1849050500">34</xref><xref ref-type="bibr" rid="ridm1849047764">35</xref><xref ref-type="bibr" rid="ridm1849045676">36</xref>, a Cote's spiral (also written Cotes' spiral and Cotes spiral) is one of a family of spirals classified by Roger Cotes.</p>
      </sec>
      <sec id="idm1841358468">
        <title>Development</title>
        <p>After an analysis of the different types of spirals <xref ref-type="bibr" rid="ridm1849066340">29</xref><xref ref-type="bibr" rid="ridm1849063244">30</xref><xref ref-type="bibr" rid="ridm1849058636">31</xref><xref ref-type="bibr" rid="ridm1849057268">32</xref><xref ref-type="bibr" rid="ridm1849055468">33</xref><xref ref-type="bibr" rid="ridm1849050500">34</xref><xref ref-type="bibr" rid="ridm1849047764">35</xref><xref ref-type="bibr" rid="ridm1849045676">36</xref>, it was concluded that the form that came closest the spiral, (<xref ref-type="fig" rid="idm1849433332">Figure 1</xref>, <xref ref-type="fig" rid="idm1849401388">Figure 2</xref>, <xref ref-type="fig" rid="idm1849354812">Figure 4</xref>, <xref ref-type="fig" rid="idm1849352508">Figure 5</xref>, <xref ref-type="fig" rid="idm1849350060">Figure 6</xref>), is a double Cotes's Spiral, for the case <inline-graphic xlink:href="images/image2.png" mime-subtype="png"/>, (<xref ref-type="fig" rid="idm1849401388">Figure 2</xref>) <xref ref-type="bibr" rid="ridm1849098532">26</xref>.</p>
        <p>It was determined the mathematical equation of the shape of the Dragonhead cyclone, in the shape of a spiral called Cotes's Spiral", for the case  <inline-graphic xlink:href="images/image2.png" mime-subtype="png"/> , (<xref ref-type="fig" rid="idm1849401388">Figure 2</xref>) <xref ref-type="bibr" rid="ridm1849101628">24</xref><xref ref-type="bibr" rid="ridm1849099540">25</xref><xref ref-type="bibr" rid="ridm1849098532">26</xref>.</p>
        <p>A spiral that gives the solution to the central orbit problem under a radial force law</p>
        <p><inline-graphic xlink:href="images/image3.png" mime-subtype="png"/> (1)</p>
        <p>where µ is a positive constant. There are three solution regimes,</p>
        <p><inline-graphic xlink:href="images/image4.png" mime-subtype="png"/> (2)</p>
        <p>where <inline-graphic xlink:href="images/image5.png" mime-subtype="png"/>, when <inline-graphic xlink:href="images/image2.png" mime-subtype="png"/>  ,</p>
        <p>where A and ɛ are constants, and h is the specific angular momentum <xref ref-type="bibr" rid="ridm1849098532">26</xref><xref ref-type="bibr" rid="ridm1849041932">37</xref><xref ref-type="bibr" rid="ridm1849040852">38</xref>. </p>
        <p>Analyzing the shape of the Spiral shape called "Cotes’s Spiral" for <inline-graphic xlink:href="images/image2.png" mime-subtype="png"/><xref ref-type="bibr" rid="ridm1849101628">24</xref><xref ref-type="bibr" rid="ridm1849099540">25</xref>, it appears that adding two constants to Equation (2) makes the necessary adjustments for the Isobaric ones. In the case of Dragonhead cyclone, the spiral that gives the solution to a radial force law is given by Equation (1).</p>
        <p>An adjustment in Equation (2) is necessary to obtain the graph of (<xref ref-type="fig" rid="idm1849349700">Figure 7</xref>). Then, adding the                         constants </p>
        <p><inline-graphic xlink:href="images/image6.png" mime-subtype="png"/>and C where for <inline-graphic xlink:href="images/image2.png" mime-subtype="png"/>  .</p>
        <p>The equation is defined for the Dragonhead Cyclone:</p>
        <p><inline-graphic xlink:href="images/image7.png" mime-subtype="png"/> (3)</p>
        <p>The Software for creating the graphics was Origin Lab evaluation version 2018, (<xref ref-type="fig" rid="idm1849350060">Figure 6</xref>). <xref ref-type="bibr" rid="ridm1848935756">63</xref></p>
        <p>For calculations the computer used a Desktop with SUSE Linux Enterprise Desktop <xref ref-type="bibr" rid="ridm1848966428">64</xref>, AMD Ryzen 7 1800X processor <xref ref-type="bibr" rid="ridm1848963260">65</xref>, ASUS Prime A320M-K motherboard <xref ref-type="bibr" rid="ridm1848921212">66</xref>, 16GB of RAM, with 500GB SSD <xref ref-type="bibr" rid="ridm1848916748">67</xref>. </p>
        <p>(<xref ref-type="fig" rid="idm1849354812">Figure 4</xref>) and (<xref ref-type="fig" rid="idm1849352508">Figure 5</xref>) were used to determine the speed, atmospheric pressure, temperature, dimensions of the Dragonhead cyclone. </p>
      </sec>
    </sec>
    <sec id="idm1841309804">
      <title>Analysis and Results</title>
      <p>With winds coming from the Pacific Ocean, the cold front crosses southern Chile and Argentina.             Forming from the region of Puerto Natales, Punta Arenas (Chile), El Calafate, Rio Galegos, Rio Grande and Ushuaia (Argentina), as shown in (<xref ref-type="fig" rid="idm1849354812">Figure 4</xref>), 4h UTC on February 7, 2024. The cold               coming from the Pacific collides with a mass of hot air coming from the north of the province of Santa Cruz and central-south of Chubut.</p>
      <p>On February 7, 2024 at 18:00 UTC, the cyclone reached an area of influence of 3,247 thousand km<sup>2</sup>. It had a head/neck of elliptical dimensions measuring 639 km by 552 km, whose core was located at 45°36'S, 21°31'W, north of the Falkland Islands. With winds of 84 km/h, it had already traveled 640 km in 10 hours, with an average of 64 km/h, according to the analyzes and measurements in (<xref ref-type="fig" rid="idm1849354812">Figure 4</xref>, <xref ref-type="fig" rid="idm1849352508">Figure 5</xref>, <xref ref-type="fig" rid="idm1849350060">Figure 6</xref>).</p>
      <p>The variation in temperature and water sality were not studied in the work, leaving their influence on the formation of cyclones in the region for later studies. As for the cyclone temperature during its                  formation, (<xref ref-type="table" rid="idm1849399228">Table 1</xref>) varies from -45ºC to -50ºC at its edge, while at its core it varies between -10ºC            to -25ºC.</p>
      <p>It had a pressure of 978 hPa, February 7, 2024 at 08:00 am (UTC), 100 km north of the nucleus (<xref ref-type="fig" rid="idm1849352508">Figure 5</xref>), with winds of 76 km/h, with a nucleus at 970 hPa. Taking off in the WNW direction.</p>
      <p>It appears that the spiral shape of the Dragonhead is very similar to the shape of the spiral galaxy NGC 5247, presenting the same shape.  The analogous shape of Dragonhead cyclone and the NGC 5247 Galaxy, studied here is clear. These present a double Cote's spiral. Studied by Lindblad<xref ref-type="bibr" rid="ridm1848998300">47</xref>, but with the Cote’s spiral form, (Gobato et al. 2022) <xref ref-type="bibr" rid="ridm1849235772">8</xref><xref ref-type="bibr" rid="ridm1849237356">9</xref><xref ref-type="bibr" rid="ridm1849227316">11</xref>.</p>
      <p>The (<xref ref-type="fig" rid="idm1849401388">Figure 2</xref>) show shapes of curves called Cote's spiral gives the solution to the central orbit                 problem.</p>
      <fig id="idm1849401388">
        <label>Figure 2.</label>
        <caption>
          <title> Shapes of curves called Cote's spiral gives the solution to the central orbit problem, where the radial force has the form equation (1).</title>
        </caption>
        <graphic xlink:href="images/image8.jpg" mime-subtype="jpg"/>
      </fig>
      <p>The (<xref ref-type="table" rid="idm1849399228">Table 1</xref>) shows the coordinates of Dragonhead cyclone, February 07, 2024, am/pm, a central             vortex pressure of  951 hPa, with an approximate dimension of 10 km.</p>
      <table-wrap id="idm1849399228">
        <label>Table 1.</label>
        <caption>
          <title> Dragonhead cyclone coordinates/Pressure/Temperature, in accordance with the analyzes and measurements in Figures (4) and (7).</title>
        </caption>
        <table rules="all" frame="box">
          <tbody>
            <tr>
              <td>
                <bold>February 7, 2024</bold>
              </td>
              <td>
                <bold>Coordinates</bold>
              </td>
              <td>
                <bold>Pressure (</bold>
                <bold>hPa</bold>
                <bold>)</bold>
              </td>
              <td>
                <bold>Temperature (ºC)</bold>
              </td>
            </tr>
            <tr>
              <td>08:00 am (UTC)</td>
              <td>52°46’08”S 67°49’48”W</td>
              <td>978</td>
              <td>-50</td>
            </tr>
            <tr>
              <td>06:00 pm (UTC)</td>
              <td>51°33’22”S 65°14’24”W</td>
              <td>970 </td>
              <td>-45</td>
            </tr>
          </tbody>
        </table>
      </table-wrap>
      <p>The (<xref ref-type="fig" rid="idm1849357404">Figure 3</xref>) shows isobaric and wind lines at 500 m height, in the south of the American continent.</p>
      <fig id="idm1849357404">
        <label>Figure 3.</label>
        <caption>
          <title> The Figure shows isobaric and wind lines at 500 m height, in the south of the American continent.</title>
        </caption>
        <graphic xlink:href="images/image9.jpg" mime-subtype="jpg"/>
      </fig>
      <p>The pressure at 500m height in the cities of El Calafate, Puerto Natales, Ushuaia, Rio Grande, Rio Galegos, are 989, 990, 984, 982, 979 and 979 hPa, respectively. In the Falkland Islands (Malvinas             Islands) it is between 984 and 990 hPa.</p>
      <p>The (<xref ref-type="fig" rid="idm1849354812">Figure 4</xref>) and (<xref ref-type="fig" rid="idm1849352508">Figure 5</xref>) show the trajectory of the dragonhead cyclone between 08:00 am (UTC) and 06:00 pm, February 7, 2024.</p>
      <fig id="idm1849354812">
        <label>Figure 4.</label>
        <caption>
          <title> Image of the Dragonhead cyclone, at 8 am (UTC), February 7, 2024.</title>
        </caption>
        <graphic xlink:href="images/image10.jpg" mime-subtype="jpg"/>
      </fig>
      <fig id="idm1849352508">
        <label>Figure 5.</label>
        <caption>
          <title> Image of the Dragonhead cyclone, at 6 pm (UTC), February 7, 2024.</title>
        </caption>
        <graphic xlink:href="images/image11.jpg" mime-subtype="jpg"/>
      </fig>
      <p>The (<xref ref-type="fig" rid="idm1849350060">Figure 6</xref>) it represents the dimensions of the points collected from (<xref ref-type="fig" rid="idm1849352508">Figure 5</xref>), in km, using the Isobaric <xref ref-type="bibr" rid="ridm1849063244">30</xref><xref ref-type="bibr" rid="ridm1849058636">31</xref> found in (<xref ref-type="fig" rid="idm1849357404">Figure 3</xref>, <xref ref-type="fig" rid="idm1849354812">Figure 4</xref>, <xref ref-type="fig" rid="idm1849352508">Figure 5</xref>).</p>
      <fig id="idm1849350060">
        <label>Figure 6.</label>
        <caption>
          <title> Graphic plot of the dimensions and shape of the Dragonhead cyclone, as at 18 am (UTC), February 7, 2024.</title>
        </caption>
        <graphic xlink:href="images/image12.jpg" mime-subtype="jpg"/>
      </fig>
      <p>The (<xref ref-type="fig" rid="idm1849349700">Figure 7</xref>) show the cyclone temperature during its trajectory, (<xref ref-type="table" rid="idm1849399228">Table 1</xref>), varies from -45ºC                       to -50ºC at its edge, while at its core it varies between -10ºC to -25ºC.</p>
      <fig id="idm1849349700">
        <label>Figure 7.</label>
        <caption>
          <title> Image of atmospheric temperature at 500m altitude of the Dragonhead cyclone, 8:10 am (UTC) at 6:10 pm (UTC), February 7, 2024.</title>
        </caption>
        <graphic xlink:href="images/image13.jpg" mime-subtype="jpg"/>
      </fig>
      <p>Other spiral galaxies, vortex storms, have also been analyzed <xref ref-type="bibr" rid="ridm1848997508">48</xref><xref ref-type="bibr" rid="ridm1848991388">49</xref><xref ref-type="bibr" rid="ridm1848988724">50</xref><xref ref-type="bibr" rid="ridm1849019900">51</xref><xref ref-type="bibr" rid="ridm1848958148">52</xref><xref ref-type="bibr" rid="ridm1848955772">53</xref>.</p>
    </sec>
    <sec id="idm1841303236" sec-type="conclusions">
      <title>Conclusions</title>
      <p>Extratropical cyclones are common in the South Atlantic. They generally arise with the passage of cold fronts to the south of the South American continent, crossing the south of Chile and Argentina, in the regions of Puerto Natales, Punta Arenas (Chile), Rio Galegos, Rio Grande, El Calafate, and Ushuaia (Argentina). The extratropical cyclone analyzed, presented at its peak the very characteristic shape of a Chinese dragon. Mathematical analysis of the way the cyclone pressure curve behaves is that of a                double Cotes's Spiral. Here called the Dragonhead cyclone, indicate structural similarity with spiral galaxies, especially NGC 5247, in the constellation Virgo. With an area of influence and a size of around 3,247 thousand km<sup>2</sup> at its peak, it moved quickly in a WNW direction, with an average speed of 76 km/h, with winds of 84 km/h at 100 km from the nucleus, as it passed north of the Falkland Islands (Malvinas Islands). </p>
      <p>In the data collected <xref ref-type="bibr" rid="ridm1849247492">6</xref><xref ref-type="bibr" rid="ridm1849244828">7</xref><xref ref-type="bibr" rid="ridm1849235772">8</xref><xref ref-type="bibr" rid="ridm1849237356">9</xref><xref ref-type="bibr" rid="ridm1849223140">10</xref><xref ref-type="bibr" rid="ridm1849227316">11</xref><xref ref-type="bibr" rid="ridm1849205604">12</xref><xref ref-type="bibr" rid="ridm1849204452">13</xref><xref ref-type="bibr" rid="ridm1849214532">14</xref><xref ref-type="bibr" rid="ridm1849209420">15</xref><xref ref-type="bibr" rid="ridm1849161636">16</xref><xref ref-type="bibr" rid="ridm1849157532">17</xref><xref ref-type="bibr" rid="ridm1849168692">18</xref><xref ref-type="bibr" rid="ridm1849140844">19</xref><xref ref-type="bibr" rid="ridm1849137028">20</xref><xref ref-type="bibr" rid="ridm1849148332">21</xref> and analyzed from the Dragonhead cyclone, it is clear that all extratropical cyclones that appear south of the South American continent, below 40° latitude, have the shape of a spiral curve, like the spiral galaxy. Most of these are in the form of a double Cote’s spiral curve.</p>
    </sec>
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