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<!DOCTYPE html>
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<meta name="Description" CONTENT="Author: Leobardo Oscar Alc�ntara Oca�a, Category: Work Gallery">
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<title>Clouds spotted in Guadalajara Jalisco</title>
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<h1 id="subtitle">Clouds spotted in Guadalajara Jalisco, Mexico </h1> <!-- <p>(20.6752° N, 103.3473° W). </p> -->
</header>
<div class="wrapper">
<!-- Column 1-->
<div class="box a"> <h4> High</h4>
(12,000 m.) </br>
<small> (40,000 ft) </small>
</div>
<!-- Column 2-->
<!-- Cumulonimbus -->
<div class="box c_n">
<!-- Cumulonimbus -->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#cumulonimbus" title="Go to CUMULONIMBUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" data-bs-placement="right" title=" <hr> <strong> Cumulonimbus: </strong> </br> The thunderstorm cloud, this is a heavy and dense cloud in the form of a mountain or huge tower. The upper portion is usually smoothed, fibrous, or striated and nearly always flattened in the shape of an anvil or vast plume.
Under the base of this cloud, which is often very dark, there are commonly low ragged clouds that may or may not merge with the base. They produce precipitation, which sometimes is in the form of virga.
Cumulonimbus clouds also produce hail and tornadoes.<hr>">
<img src = "img/svg/clouds/cumulonimbus_rain.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption> Cumulonimbus </figcaption>
</figure>
</div>
<div class="box b high_clouds "> <!-- High clouds -->
<!-- Column Subgrid -->
<div class="subgrid_1">
<div class="box aa a_cirrocumulus">
<!-- Cirrocumulus -->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Cirrocumulus" title="Go to CIRROCUMULUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Cirrocumulus: </strong> </br> Thin and white, these clouds look like a patchy sheet or layer arranged somewhat-regularly into grains or ripples without shading. Most of these elements have an apparent width of less than one degree (approximately width of the little finger held at arm's length).
Predominantly made of ice crystals, cirrocumulus often form in connection with cirrus or cirrostratus or from a degraded state of these cloud types and are short-lived.<hr> ">
<img src = "img/svg/clouds/cirrocumulus.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption>Cirrocumulus</figcaption>
</figure>
</div>
<div class="box bb b_cirrostratus">
<!-- Cirrostratus -->
</figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Cirrustratus" title="Go to CIRROSTRATUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Cirrostratus: </strong> </br> Transparent, whitish veil-like clouds with a fibrous (hair-like) or smooth appearance. A sheet of cirrostratus is very extensive and can cover the whole sky.
During the day, when the sun is sufficiently high above the horizon, the sheet is never thick enough to prevent shadows of objects on the ground.
A veil of cirrostratus may have a similar appearance to a milky veil of fog (or thin stratus), but is distinguished by a halo phenomena nearly always produced around the Sun or Moon shining through a layer of cirrostratus. <hr> ">
<img src = "img/svg/clouds/cirrostratus.svg" height = "auto" width = "auto" /> </a>
</span>
<figcaption>Cirrostratus</figcaption>
</figure>
</div>
<div class="box cc c_cirrus">
<!-- Cirrus -->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Cirrus" title="Go to CIRRUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" data-bs-placement="right" title=" <hr> <strong> Cirrus: </strong> </br> Detached clouds in the form of white, delicate filaments, mostly in patches or narrow bands. They may have a fibrous (hair-like) and/or silky sheen appearance.
Cirrus clouds are always composed of ice crystals, and their transparent character depends upon the degree of separation of the crystals. As a rule, when these clouds cross the sun's disk, they hardly diminish its brightness. When they are exceptionally thick, they may veil its light and obscure its contour. <hr> ">
<img src = "img/svg/clouds/cirrus.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption>Cirrus</figcaption>
</figure>
</div>
</div>
</div>
<div class="box c "> <h4> Middle</h4>
(7,000 m.) </br>
<small>(23,000 ft)</small>
</div>
<div class="box d middle_clouds"> <!-- Middle Clouds -->
<div class="subgrid_2">
<div class="box aa a_altocumulus">
<!-- Altocumulus -->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Altocumulus" title="Go to ALTOCUMULUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Altocumulus: </strong> </br> White and/or gray patchy, sheet, or layered clouds generally composed of laminae (plates), rounded masses, or rolls. They may be partly fibrous or diffuse and may or may not be merged.
Most of these regularly arranged small elements have an apparent width of one to five degrees (larger than the little finger and smaller than three fingers held at arm's length).
When the edge or a thin semitransparent patch of altocumulus passes in front of the sun or moon, a corona appears. This colored ring has red on the outside and blue inside and occurs within a few degrees of the sun or moon. <hr> ">
<img src = "img/svg/clouds/altocumulus.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption>Altocumulus</figcaption>
</figure>
</div>
<div class="box bb b_cirrostratus">
<!-- Altostratus -->
<figure>
<a href="" title="Go to ALTOSTRATUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Altostratus: </strong> </br> Gray or bluish cloud sheets or layers of striated or fibrous clouds that totally or partially cover the sky. They are thin enough to regularly reveal the sun as if seen through ground glass.
Altostratus clouds do not produce a halo phenomenon nor are the shadows of objects on the ground visible.
Sometimes virga (streaks of rain) is seen hanging from altostratus and at times may even reach the ground, causing very light precipitation.<hr> ">
<img src = "img/svg/clouds/altostratus.svg" height = "auto" width = "auto" /> </span>
</a>
<figcaption>Altostratus</figcaption>
</figure>
</div>
</div>
</div>
<div class="box e"> <h4> Low </h4>
(2,000 m.) </br>
<small>(6,500 ft) </small>
</div>
<div class="box f low_clouds"><!-- Low Clouds -->
<div class="subgrid_3">
<div class="box aa a_cumulus">
<!-- Cumulus button -->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Cumulus" title="Go to CUMULUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Cumulus: </strong> </br> Detached, generally dense clouds and with sharp outlines that develop vertically in the form of rising mounds, domes, or towers with bulging upper parts often resembling a cauliflower.<hr> ">
<img src = "img/svg/clouds/cumulus.svg" height = "auto" width = "auto" /> </span>
</a>
<figcaption> Cumulus </figcaption>
</figure>
</div>
<div class="box bb b_stratocumulus">
<!-- Stratucumulus-->
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Stratocumulus" title="Go to STRATOCUMULUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Stratocumulus: </strong> </br> Gray or whitish patchy, sheet, or layered clouds that almost always have dark tessellations (honeycomb appearance), rounded masses, or rolls. Except for virga, they are non-fibrous and may or may not be merged.<hr>">
<img src = "img/svg/clouds/stratocumulus.svg" height = "auto" width = "auto" /> </span>
</a>
<figcaption>Stratocumulus</figcaption>
</figure>
</div>
<div class="box cc c_stratus">
<!-- Stratus -->
<figure>
<a href="" title="Go to STRATUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" title=" <hr> <strong> Stratus: </strong> </br> A generally gray cloud layer with a uniform base which may, if thick enough, produce drizzle, ice prisms, or snow grains. When the sun is visible through this cloud, its outline is clearly discernible.<hr> ">
<img src = "img/svg/clouds/stratus.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption>
Stratus
</figcaption>
</figure>
</div>
</div>
</div>
<!-- Radar -->
<div class="radar">
<figure>
<figcaption> Doppler Radar </figcaption>
<a href="http://iam.cucei.udg.mx/radar/iam/" title="Doppler Radar, Universidad de Guadalajara, Jalisco Mexico">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" data-bs-placement="right" title=" <hr> <strong> Radar Doppler: </strong> </br> Operated by the Meteorology and Astronomy Institute. University of Guadalajara. <hr> ">
<img src="img/svg/radar/dome_radar_tower.svg" height = "auto" width = "80wh"> </span>
</a>
</figure>
</div>
<!-- Nimbostratus -->
<div class="box n_s">
<figure>
<a href="https://leobardooscar.github.io/clouds/browse.html#Nimbostratus" title="Go to NIMBOSTRATUS collection ">
<span class=" tt" data-bs-toggle="tooltip" data-bs-html="true" data-bs-placement="left" title="
<hr>
<strong>Nimbostratus: </strong> </br>
Resulting from thickening altostratus, this is a dark gray cloud layer diffused by falling rain or snow. It is thick enough throughout to blot out the sun. Low, ragged clouds frequently occur beneath this cloud and sometimes merge with its base.
<hr>
">
<img src = "img/svg/clouds/nimbostratus.svg" height = "auto" width = "auto" />
</span>
</a>
<figcaption> Nimbostratus </figcaption>
</figure>
</div>
<div class="horizonte">
<!-- Landscape - Horizon <img src = "img/svg/clouds/horizonte.svg" height = "100%" width = "100%" /> -->
<div id="cc_licence">
<span>
<small>
Clouds classification illustration by Valentin de Bruin <small> [CC BY-SA 3.0]. </small> <a href="https://commons.wikimedia.org/wiki/File:Cloud_types_en.svg" title="">Wikimedia Commons Repository</a>
</br> <img src = "img/svg/c_commons/by-sa.svg" height = "28px" width = "80px" title="Creative Commons licence" style="float: right; margin-top: 10px"/>
</span>
</div>
</div>
</div>
<div class="balloon">
<!-- Hot-air-balloon -->
<img src = "img/svg/objects/hot_air_balloon.svg" height = "auto" width = "60vw" />
</div>
<!-- Footer -->
<footer class="text-center text-lg-start bg-body-tertiary text-muted">
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ABOUT THIS COLLECTION
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<p> In meteorology, a phenomenon observed in the atmosphere or on the surface of the Earth is known as a <i>meteor</i>. It may be a form of precipitation, a suspension or a deposit of liquid or solid particles. </p>
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The present collection consists of <i>meteors</i> observed from 2010 to 2024.
Sighting point: Guadalajara Metropolitan Area (Northwest zone). Western Mexico region (20.6752° N, 103.3473° W). 1,500 MAMSL.
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<p><i class="fas fa-home me-3"></i> Guadalajara Jalisco, Mexico.</p>
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© 2024, Leobardo Óscar Alcántara Ocaña.
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