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Coriolis Effect: Air Circulation in the Atmosphere - Earth How

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aria-current="page">Coriolis Effect: Air Circulation in the Atmosphere</span></span></div><h1 class="entry-title">Coriolis Effect: Air Circulation in the Atmosphere</h1><div class="entry-meta entry-meta-divider-customicon"> <div class="meta-comments"><span class="kadence-svg-iconset"><svg class="kadence-svg-icon kadence-comments-alt-svg" fill="currentColor" version="1.1" xmlns="http://www.w3.org/2000/svg" width="28" height="28" viewBox="0 0 28 28"><title>Comments</title><path d="M10 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM16 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM22 14c0 1.109-0.891 2-2 2s-2-0.891-2-2 0.891-2 2-2 2 0.891 2 2zM14 6c-6.5 0-12 3.656-12 8 0 2.328 1.563 4.547 4.266 6.078l1.359 0.781-0.422 1.5c-0.297 1.109-0.688 1.969-1.094 2.688 1.578-0.656 3.016-1.547 4.297-2.672l0.672-0.594 0.891 0.094c0.672 0.078 1.359 0.125 2.031 0.125 6.5 0 12-3.656 12-8s-5.5-8-12-8zM28 14c0 5.531-6.266 10-14 10-0.766 0-1.531-0.047-2.266-0.125-2.047 1.813-4.484 3.094-7.187 3.781-0.562 0.156-1.172 0.266-1.781 0.344h-0.078c-0.313 0-0.594-0.25-0.672-0.594v-0.016c-0.078-0.391 0.187-0.625 0.422-0.906 0.984-1.109 2.109-2.047 2.844-4.656-3.219-1.828-5.281-4.656-5.281-7.828 0-5.516 6.266-10 14-10v0c7.734 0 14 4.484 14 10z"></path> </svg></span><a class="meta-comments-link anchor-scroll" href="#comments">4 Comments</a></div></div></header> <div class="entry-content single-content"> <figure class="wp-block-image is-style-default"><img fetchpriority="high" decoding="async" width="678" height="378" src="https://earthhow.com/wp-content/uploads/2018/12/Coriolis-Effect-Feature-678x378.png" alt="Coriolis Effect" class="wp-image-2503"/></figure> <div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What is the Coriolis Effect?</h3> <p>The Coriolis effect is the deflection of air because of <a href="https://earthhow.com/earth-rotation-day-night-boundary/">Earth&#8217;s rotation</a>. In the northern hemisphere, air deflects to the right. But in the southern hemisphere, air veers to the left.</p> <p>It&#8217;s a myth that the Coriolis effect determines the direction a toilet flushes like on the Simpsons. But the Coriolis effect does impact air circulation, weather patterns, and <a href="https://earthhow.com/ocean-currents/">ocean currents</a>.</p> <p>What would happen to the Coriolis effect if Earth stopped rotating? Or what would happen if Earth&#8217;s rotation sped up? Before we answer those questions, let&#8217;s first understand how the Coriolis effect works.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">How the Coriolis effect works</h3> <div class="wp-block-image is-style-default"> <figure class="alignright"><img decoding="async" width="290" height="300" src="https://earthhow.com/wp-content/uploads/2018/09/Coriolis-Effect-0-290x300.png" alt="Coriolis Effect" class="wp-image-1523" srcset="https://earthhow.com/wp-content/uploads/2018/09/Coriolis-Effect-0-290x300.png 290w, https://earthhow.com/wp-content/uploads/2018/09/Coriolis-Effect-0.png 407w" sizes="(max-width: 290px) 100vw, 290px"/></figure></div><p>If you stand at the equator, you <a href="https://earthhow.com/how-fast-does-the-earth-spin/">spin at about 1000 miles per hour</a>. But if you stand on the North Pole, you move at a rate of 0 miles/hr. This is because you鈥檙e basically spinning on the same spot for 24 hours straight. Either way, our bodies are used to the motion so we don&#8217;t necessarily feel the velocity.</p> <p><strong>NORTHERN HEMISPHERE</strong>: So if an object travels through the air from the equator to the north, it will start to veer off to the right in the northern hemisphere due to Earth&#8217;s rotation.</p> <p><strong>SOUTHERN HEMISPHERE</strong>: But in the southern hemisphere, it鈥檚 the opposite. It would veer off to the left.</p> <p>But the Coriolis effect often refers to air circulation. So instead of <a href="https://earthhow.com/solar-radiation-electromagnetic/">hot air transferring from the equator</a> to the colder poles, it deflects away. Eventually, air starts to swirl in a circular pattern. This circular pattern is the convection cells caused by the Coriolis effect.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What if Earth stopped rotating?</h3> <div class="wp-block-image is-style-default"> <figure class="alignright"><img decoding="async" width="290" height="300" src="https://earthhow.com/wp-content/uploads/2018/12/Coriolis-Effect-No-Rotation-290x300.png" alt="Coriolis Effect No Rotation" class="wp-image-4304" srcset="https://earthhow.com/wp-content/uploads/2018/12/Coriolis-Effect-No-Rotation-290x300.png 290w, https://earthhow.com/wp-content/uploads/2018/12/Coriolis-Effect-No-Rotation.png 407w" sizes="(max-width: 290px) 100vw, 290px"/></figure></div><p>What if the Earth didn&#8217;t rotate at all, would there still be a Coriolis effect? If the Earth didn鈥檛 rotate, warm air at the equator would simply transfer to the poles. This would be just a simple exchange of hot and cold air back and forth.</p> <p>Instead of our current 6 convection cells on Earth, we would have 2 convection cells driven by thermal convection. As warm air moves from the equator to the poles, cool air from the poles would sink back down to the equator. So each hemisphere would have a convection cell on its own.</p> <hr class="wp-block-separator has-css-opacity is-style-default"/> <blockquote class="wp-block-quote has-text-align-center is-style-large is-layout-flow wp-block-quote-is-layout-flow"> <p>&#8220;If Earth stopped rotating, there would be 2 separate convection cells split at the equator. One cell would occupy the northern hemisphere. Then, the other one would be in the southern hemisphere.&#8221;</p> </blockquote> <hr class="wp-block-separator has-css-opacity is-style-default"/></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">What if Earth stopped rotating?</h3> <p>Now, what if the Earth rotated more rapidly? If Earth spun faster, what would happen to the Coriolis effect?</p> <p>The same fundamental concepts would hold true. Again, air veers off to the right in the northern hemisphere. But it would deflect faster.</p> <p>Instead of the 6 convection cells we experience on Earth, it would have more due to a faster rotation. Simply, the number of convection cells is a function of how fast it rotates.</p> <hr class="wp-block-separator has-css-opacity is-style-default"/> <blockquote class="wp-block-quote has-text-align-center is-style-large is-layout-flow wp-block-quote-is-layout-flow"> <p>&#8220;If the Earth spun faster, there would be several more convection cells than there currently is.&#8221;</p> </blockquote> <hr class="wp-block-separator has-css-opacity is-style-default"/></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">Air circulation patterns from the Coriolis effect</h3> <div class="wp-block-image is-style-default"> <figure class="alignright"><img loading="lazy" decoding="async" width="290" height="300" src="https://earthhow.com/wp-content/uploads/2018/12/Hadley-Ferrel-Polar-Cells-290x300.png" alt="Hadley Ferrel Polar Cells" class="wp-image-4306" srcset="https://earthhow.com/wp-content/uploads/2018/12/Hadley-Ferrel-Polar-Cells-290x300.png 290w, https://earthhow.com/wp-content/uploads/2018/12/Hadley-Ferrel-Polar-Cells.png 407w" sizes="(max-width: 290px) 100vw, 290px"/></figure></div><p>Earth has a total of 6 convection cells. Each hemisphere has 3 on its own.</p> <ul class="wp-block-list"> <li>From 0-30掳 north/south, these are Hadley cells.</li> <li>Then from 30-60掳 north/south are Ferrel cells.</li> <li>Finally from 60-90掳 are the polar cells.</li> </ul> <p>For Hadley cells, the sun shines down at the equator. It evaporates and begins to rise bringing water vapor. More or less, it provides rain until about 30掳 latitude when it loses most of its moisture.</p> <p>The equator area is damp and moist. But at about 30掳 latitude, the air is much dryer. Then at 50-60掳, it&#8217;s a sub-polar low. In the Ferrel cell, air moves north at 30掳 latitude, then comes down at 60掳 north.</p> <p>Air is deflected from the Coriolis effect causing the Westerlies to move east to west. Finally, the air that comes down from the North Pole is very dry. The North Pole is like a desert because it has some of the lowest precipitation rates on the planet.</p></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">The Coriolis effect on Jupiter</h3> <div class="wp-block-image is-style-default"> <figure class="alignright"><img loading="lazy" decoding="async" width="290" height="300" src="https://earthhow.com/wp-content/uploads/2019/01/Planet-Jupiter-290x300.png" alt="Planet Jupiter" class="wp-image-3156" srcset="https://earthhow.com/wp-content/uploads/2019/01/Planet-Jupiter-290x300.png 290w, https://earthhow.com/wp-content/uploads/2019/01/Planet-Jupiter.png 407w" sizes="(max-width: 290px) 100vw, 290px"/></figure></div><p>Jupiter spins at an incredible pace. The velocity at Jupiter鈥檚 equator is about 28,000 miles per hour, compared to Earth&#8217;s 1000 mph.</p> <p>This means that one day on Jupiter takes a bit less than 10 hours. Because of its fast rotation and heaping size, the Coriolis effect is extraordinary in size.</p> <p>Earth has 6 convection cells. Whereas <a href="https://earthhow.com/planet-jupiter-facts/">Jupiter has consistent bands of air</a> that whirl around its surface. If you&#8217;ve ever seen Jupiter, the Coriolis effect is why it has its iconic banded appearance.</p> <p>Overall, the weather is at an extreme on Jupiter. For example, astronomers have observed an everlasting hurricane in its atmosphere. It&#8217;s been there since the first time we&#8217;ve looked at Jupiter.</p> <hr class="wp-block-separator has-css-opacity is-style-default"/> <blockquote class="wp-block-quote has-text-align-center is-style-large is-layout-flow wp-block-quote-is-layout-flow"> <p>&#8220;Jupiter spins so fast that it has consistent bands of air whirling around its surface.&#8221;</p> </blockquote> <hr class="wp-block-separator has-css-opacity is-style-default"/></div></div><div class="wp-block-group" style="padding-top:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50)"><div class="wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained"> <h3 class="wp-block-heading">The Coriolis Effect on Earth</h3> <p>The Coriolis effect is the phenomenon that causes a mass on a rotating object to be deflected by a force pointing in the opposite direction of rotation.</p> <p>As such, this effect is only present when the object is moving, and so it only applies to objects moving on Earth.</p> <p>You can also drop us a line in the comment section below.</p></div></div><div class="newsletter1"><span style="color:#FFFFFF">Subscribe to our newsletter:</span> <div class="tnp tnp-subscription-minimal"><form action="https://earthhow.com/wp-admin/admin-ajax.php?action=tnp&amp;na=s" method="post" style="text-align: center"><input type="hidden" name="nr" value="minimal"> <input type="hidden" name="nlang" value=""> <input class="tnp-email" type="email" required name="ne" value="" placeholder="Email"><input class="tnp-submit" type="submit" value="Subscribe" style=""> </form></div></div><div class="kb-row-layout-wrap kb-row-layout-id18087_9ac6f0-08 alignnone wp-block-kadence-rowlayout"><div class="kt-row-column-wrap kt-has-1-columns kt-row-layout-equal kt-tab-layout-inherit kt-mobile-layout-row kt-row-valign-top"> <div class="wp-block-kadence-column kadence-column18087_8adc6b-56 kvs-sm-false kb-section-dir-horizontal"><div class="kt-inside-inner-col"><div class="wp-block-kadence-posts kb-posts kb-posts-id-18087_4ff245-dc content-wrap grid-cols kb-posts-style-unboxed grid-sm-col-2 grid-lg-col-3 item-image-style-above"><article class="entry content-bg loop-entry post-66 post type-post status-publish format-standard has-post-thumbnail hentry category-atmosphere category-outside-earth tag-feature tag-infographic mv-content-wrapper"> <a class="post-thumbnail kadence-thumbnail-ratio-2-3" href="https://earthhow.com/atmosphere-layers-troposphere-stratosphere-mesosphere-thermosphere/"> <div class="post-thumbnail-inner"> <img width="425" height="319" src="https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-425x319.png" class="attachment-medium_large size-medium_large wp-post-image" alt="Earth Atmosphere Layers" decoding="async" loading="lazy" srcset="https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-425x319.png 425w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-300x225.png 300w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-675x507.png 675w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-550x413.png 550w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers.png 678w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-326x245.png 326w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-80x60.png 80w, https://earthhow.com/wp-content/uploads/2017/07/Earth-Atmosphere-Layers-267x200.png 267w" sizes="(max-width: 425px) 100vw, 425px"/></div></a> <div class="entry-content-wrap"> <header class="entry-header"> <h6 class="entry-title"><a href="https://earthhow.com/atmosphere-layers-troposphere-stratosphere-mesosphere-thermosphere/" rel="bookmark">What Are the 4 Layers of the Atmosphere? 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status-publish format-standard has-post-thumbnail hentry category-atmosphere category-climate-change tag-feature mv-content-wrapper"><div class="kt-blocks-post-grid-item-inner-wrap kt-feat-image-align-left kt-feat-image-mobile-align-side"><div class="kadence-post-image"><div class="kadence-post-image-intrisic kt-image-ratio-66-67" style="padding-bottom:66.67%;"><div class="kadence-post-image-inner-intrisic"><a href="https://earthhow.com/milankovitch-cycle/" aria-label="Read More What Are the 3 Milankovitch Cycles?" class="kadence-post-image-inner-wrap"><img width="300" height="225" src="https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-300x225.png" class="attachment-medium size-medium wp-post-image" alt="Milankovitch Cycle" decoding="async" loading="lazy" srcset="https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-300x225.png 300w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-675x507.png 675w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-425x319.png 425w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-550x413.png 550w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle.png 678w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-326x245.png 326w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-80x60.png 80w, https://earthhow.com/wp-content/uploads/2018/12/Milankovitch-Cycle-267x200.png 267w" sizes="(max-width: 300px) 100vw, 300px"/></a></div></div></div><div class="kt-blocks-post-grid-item-inner"><header><h6 class="entry-title"><a href="https://earthhow.com/milankovitch-cycle/">What Are the 3 Milankovitch Cycles?</a></h6><div class="kt-blocks-post-top-meta"></div></header><div class="entry-content"></div><footer class="kt-blocks-post-footer"><div class="kt-blocks-post-footer-left"></div><div class="kt-blocks-post-footer-right"></div></footer></div></div></article></div></div></div></div></div></div></div></div></article> <div id="comments" class="comments-area"> <h2 class="comments-title">4 Comments</h2> <ol class="comment-list"> <li id="comment-42654" class="comment even thread-even depth-1"> <article id="div-comment-42654" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">kyle</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/coriolis-effect-air-circulation/#comment-42654"><time datetime="2024-10-09T12:53:23-06:00">October 9, 2024 at 12:53 pm</time></a></div></footer> <div class="comment-content"> <p>Wrong Wrong Wrong, There would be 1 convection cell to the planet if it stopped spinning, the dark side. Cold air from the dark side would side under hot air from the Sunny side around the longitude. Please stop teaching.</p></div></article> </li> <li id="comment-16490" class="comment odd alt thread-odd thread-alt depth-1"> <article id="div-comment-16490" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">Don Taylor</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/coriolis-effect-air-circulation/#comment-16490"><time datetime="2022-09-12T10:01:27-06:00">September 12, 2022 at 10:01 am</time></a></div></footer> <div class="comment-content"> <p>Describing the wind direction as left or right depends on the vantage point. Describing direction as eastward or westward would be less ambiguous.</p></div></article> </li> <li id="comment-12966" class="comment byuser comment-author-earthhow bypostauthor even thread-even depth-1"> <article id="div-comment-12966" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">earthhow</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/coriolis-effect-air-circulation/#comment-12966"><time datetime="2022-04-05T18:45:51-06:00">April 5, 2022 at 6:45 pm</time></a></div></footer> <div class="comment-content"> <p>Here&#8217; more info on how to cite &#8211; <a href="https://earthhow.com/how-to-cite/" rel="ugc">https://earthhow.com/how-to-cite/</a></p></div></article> </li> <li id="comment-12940" class="comment odd alt thread-odd thread-alt depth-1"> <article id="div-comment-12940" class="comment-body"> <footer class="comment-meta"> <div class="comment-author vcard"> <b class="fn">Kayleigh</b> <span class="says">says:</span></div><div class="comment-metadata"> <a href="https://earthhow.com/coriolis-effect-air-circulation/#comment-12940"><time datetime="2022-04-03T04:28:40-06:00">April 3, 2022 at 4:28 am</time></a></div></footer> <div class="comment-content"> <p>Hello! Who wrote this article may I ask? I need it for a school project.</p></div></article> </li> </ol> <div id="respond" class="comment-respond"> <h3 id="reply-title" class="comment-reply-title">Leave a Reply</h3><form action="https://earthhow.com/wp-comments-post.php" method="post" id="commentform" class="comment-form" novalidate><p class="comment-notes"><span id="email-notes">Your email address will not be published.</span> <span class="required-field-message">Required fields are marked <span class="required">*</span></span></p><p class="comment-form-comment comment-form-float-label"><textarea autocomplete="new-password" id="i477054932" name="i477054932" placeholder="Leave a comment..." cols="45" rows="8" maxlength="65525" aria-required="true" required="required"></textarea><textarea id="comment" aria-label="hp-comment" aria-hidden="true" name="comment" autocomplete="new-password" style="padding:0 !important;clip:rect(1px, 1px, 1px, 1px) !important;position:absolute !important;white-space:nowrap !important;height:1px 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