{"id":173,"date":"2015-08-06T21:43:42","date_gmt":"2015-08-06T21:43:42","guid":{"rendered":"http:\/\/54.245.251.220\/?p=173"},"modified":"2023-12-26T21:59:06","modified_gmt":"2023-12-26T21:59:06","slug":"what-is-the-solar-wind","status":"publish","type":"post","link":"https:\/\/blog.aurorasaurus.org\/?p=173","title":{"rendered":"What is the solar wind?"},"content":{"rendered":"<p>By Sean McCloat<\/p>\n<p>Greetings, Aurorasaurans! In our recent <a target=\"_blank\" rel=\"noopener noreferrer\" href=\"https:\/\/blog.aurorasaurus.org\/blog\/aurorachat-qs-during-summer-solstice-storm-622\/\">#tweetchat about the aurora<\/a>, we received a tweet requesting more information about what Bz, Kp and solar wind density are, and how they relate to the aurora. Since these are good questions that cannot adequately be answered in tweet form, we will be publishing a series of blog posts that explain what these terms are and how they relate to aurora. \u00a0We will also include discussions of other related concepts to help flesh out more of the science about aurora.<\/p>\n<p>If you have been keeping up with our<a target=\"_blank\" rel=\"noopener noreferrer\" href=\"https:\/\/blog.aurorasaurus.org\/\"> Aurorasaurus blog posts<\/a> (which if you have not been, you are seriously missing out), or have read through our <a target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/aurorasaurus.org\/learn\">learn section<\/a>, then you are probably familiar with the general mechanisms that create auroras. But just to recap, here is a broad overview: the Sun\u2019s constant stream of energetic particles, called the solar wind, can sometimes be bolstered by events called coronal mass ejections (CMEs), which are usually cone-shaped explosions of fast moving, electrically charged solar particles.<\/p>\n<p><iframe loading=\"lazy\" style=\"float: left;\" src=\"https:\/\/www.youtube.com\/embed\/i_x3s8ODaKg\" width=\"420\" height=\"315\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n<p>Once a CME reaches Earth, it interacts with Earth\u2019s magnetic field \u2013 known as the magnetosphere. CMEs can compress the magnetosphere, causing changes in the configuration (e.g. shape and direction) of Earth\u2019s magnetic field lines. Some particles, which are trapped along these field lines, are accelerated into Earth\u2019s atmosphere where they collide with atmospheric particles, such as nitrogen and oxygen molecules. The atmospheric particles are then able to emit light, which is what we know as the aurora. Check out our<a target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/aurorasaurus.org\/learn\"> Learn Page<\/a> to get a more in depth look at this process.<\/p>\n<p>Not all CMEs are created equal and you might say that each one is a unique ten million degree snowflake. Some are hotter, some are ejected with more speed, some are ejected with (generally speaking) more solar matter, and the magnetic fields they carry can be all over the place. \u00a0As a result of the variation in CME properties, not all interactions between CMEs and Earth are the same. There are certain properties that have more bearing on how strong of an impact they have on the Earth\u2019s magnetosphere.<\/p>\n<p>The next few blog posts that will be coming out will discuss how we measure the properties of CMEs and the solar wind as they fly from the Sun to Earth and which properties in particular Aurorasaurus uses in order to anticipate aurora activity. In this post, we talk about how we measure the properties that can dictate the nature of those interactions and what some of those properties are.<\/p>\n<p><strong><em>CATCHING THE SOLAR WIND<\/em><\/strong><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" style=\"float: right;\" src=\"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/b\/bf\/Lagrangianpointsanimated.gif\" alt=\"\" width=\"150\" height=\"152\" \/><\/p>\n<p>At the moment, we have no way to measure the properties of a CME as it is first seen erupting off the surface of the Sun. Scientists have to wait until the CME blows past the <a target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.nasa.gov\/mission_pages\/sunearth\/news\/ace-15th.html\">Advanced Composition Explorer (ACE)<\/a> satellite in order get this data. It takes a day or two for the CME to reach ACE. Once it reaches ACE, there is only about an hour until the CME reaches Earth! ACE does not orbit Earth, but instead orbits a gravitationally stable point that is always between Earth and the Sun called Lagrangian point 1, or L1 for short (as shown in figure to the right). \u00a0That way, it is always in the best place to intercept the solar wind before it reaches Earth.<\/p>\n<p>When ACE measures the solar wind, it sends data to Earth that looks like the graph below.\u00a0These graphs are measuring 5 properties of the solar wind (listed on the left side) over time (specified on the bottom). What we\u2019re going to focus on in this blog post are the density (in orange) and speed (in yellow) components. These, along with the Bz (which we\u2019ll cover next time!), are the most important solar wind quantities to keep tabs on for most aurora hunters.<\/p>\n<p><a target=\"_blank\" rel=\"noopener noreferrer\" href=\"https:\/\/blog.aurorasaurus.org\/wp-content\/uploads\/2015\/08\/ace-mag-swepam-24-hour.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-953\" src=\"https:\/\/blog.aurorasaurus.org\/wp-content\/uploads\/2015\/08\/ace-mag-swepam-24-hour.gif\" alt=\"ace-mag-swepam-24-hour\" width=\"640\" height=\"512\" \/><\/a><\/p>\n<p><strong>Now, what about the solar wind density?<\/strong><\/p>\n<p>The density of the incoming solar particles influences how compressed the CME causes the Earth\u2019s magnetosphere will become. Density, as measured by ACE, is looking at how many particles are in a cubic centimeter (roughly the size of a sugar cube). Typical densities of the solar wind are usually around 1 &#8211; 10 microscopic solar particles per sugar cube-sized area. \u00a0This may not sound like very much, and indeed space is mostly empty, but remember the solar wind is blowing a constant stream of these particles. \u00a0When the density of these particles is higher (like when a CME plows through and pushes the solar wind particles in front of it), it creates more pressure on Earth\u2019s magnetosphere and the result is a stronger aurora.<\/p>\n<p><strong>A quick word on speed<\/strong><\/p>\n<p>The speed of the incoming solar wind also plays a major in role in driving the aurora, and may be a bit more intuitive than the role of density. If you imagine that generating the aurora is like getting a windmill to spin, then naturally the wind speed plays a central role: the faster the wind, the faster and more easily the blades of the windmill turn. Similarly, higher solar wind speeds (like when a gusty CME blows through space) can more easily drive the processes that generate aurora. Typical solar wind speed is about 1 million miles per hour, or 400 &#8211; 1000 kilometers per second.<\/p>\n<p><a href=\"https:\/\/blog.aurorasaurus.org\/blog\/understanding-the-aurora-what-is-bz\/\" target=\"_blank\" rel=\"noopener\">Next time: the role of magnetism and how it relates to speed to calculate the solar wind power!\u00a0<\/a><\/p>\n<p>***<\/p>\n<p>Sean McCloat interned with Aurorasaurus in the summer of 2015 while\u00a0pursuing his masters degree in\u00a0Space Studies at the University of North Dakota with a\u00a0focus on the planetary sciences and astrobiology. He\u00a0helped analyze the project\u2019s data, contributed to scientific papers, presentations, and blog posts, and became good friends with Rory, the Aurorasaurus plush doll mascot.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>What is the solar wind and what does it have to do with the aurora?<\/p>\n","protected":false},"author":1,"featured_media":23,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"rop_custom_images_group":[],"rop_custom_messages_group":[],"rop_publish_now":"initial","rop_publish_now_accounts":[],"rop_publish_now_history":[],"rop_publish_now_status":"pending","neve_meta_sidebar":"","neve_meta_container":"","neve_meta_enable_content_width":"off","neve_meta_content_width":70,"neve_meta_title_alignment":"","neve_meta_author_avatar":"","neve_post_elements_order":"","neve_meta_disable_header":"","neve_meta_disable_footer":"","neve_meta_disable_title":"","footnotes":""},"categories":[12],"tags":[],"class_list":["post-173","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-understanding-the-aurora"],"_links":{"self":[{"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/posts\/173","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=173"}],"version-history":[{"count":0,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/posts\/173\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=\/wp\/v2\/media\/23"}],"wp:attachment":[{"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=173"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=173"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.aurorasaurus.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=173"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}