{"id":330,"date":"2021-09-26T20:35:56","date_gmt":"2021-09-26T20:35:56","guid":{"rendered":"http:\/\/ciresblogs.colorado.edu\/lidarexploration\/?p=330"},"modified":"2021-09-26T20:35:56","modified_gmt":"2021-09-26T20:35:56","slug":"lets-talk-about-gravity-waves","status":"publish","type":"post","link":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/2021\/09\/26\/lets-talk-about-gravity-waves\/","title":{"rendered":"Let’s Talk About Gravity Waves"},"content":{"rendered":"\n

And no, I\u2019m not talking about gravitational waves like those created by the collisions of blackholes and measured by the incredible LIGO instrument (Fun fact: LIGO is basically a gigantic Michelson interferometer which, on a much smaller scale, our group uses to measure the wavelengths of our lasers). <\/p>\n\n\n\n

I\u2019m referring to atmospheric gravity waves which are generated when some force pushes air up or down from its equilibrium height. Even those who haven\u2019t heard of atmospheric gravity waves have probably seen the characteristic, rippled cloud pattern that they generate.\u00a0<\/p>\n\n\n\n

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Rippled clouds like these above McMurdo Station, Antarctica are signs of gravity waves in the lower atmosphere.<\/strong><\/figcaption><\/figure>\n\n\n\n

Gravity waves are a key piece of the puzzle to the dynamics of the upper atmosphere because these waves can transfer energy and momentum from the lower atmosphere to extreme heights. This energy transfer is so significant that computer models of the upper atmosphere must incorporate some representation of these waves to be accurate. <\/p>\n\n\n\n

As gravity waves travel through the atmosphere they perturb the pressure, density, and temperature of the air. Lidars are a fantastic tool for studying gravity waves because they can make high-resolution measurements of these perturbations. Our group has been making lidar observations of gravity waves in the upper atmosphere above McMurdo Station, Antarctica for 10+ years to study how these waves fit into the big picture of atmospheric dynamics and impact other atmospheric processes.\u00a0<\/p>\n\n\n\n

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Example of density and temperature perturbations associated with gravity waves measured by our Fe Boltzmann lidar system at McMurdo Station (Chen et al., 2016).<\/strong><\/figcaption><\/figure><\/div>\n\n\n\n

So how are gravity waves generated? To answer that question, we first have to understand a key concept called hydrostatic equilibrium. In an average sense, the Earth\u2019s atmosphere can be considered to be in a state of hydrostatic equilibrium. That is, the gravitational force pulling air down towards Earth is balanced by the pressure gradient force that wants to suck the air back out into space. This balance of forces acts to keep a volume of air at a specific altitude where it is in equilibrium. This concept also explains why atmospheric density and pressure decrease exponentially with altitude. The gravitational force acting on the air decreases as you go higher up in the atmosphere, so if the pressure gradient force didn\u2019t also decrease the air would be accelerated out into space. Therefore, atmospheric pressure, and consequently density, must decrease with altitude in order to keep these forces balanced. <\/p>\n\n\n\n

However, consider what happens when some additional force acts on a volume of air to displace it from its equilibrium altitude. Any force or disruption that displaces air from its equilibrium height can result in the generation of gravity waves! A good example is when air is blown over a mountain. As an air parcels flows over a mountain it enters a region where the surrounding air is less dense and gravity acts to pull it back towards its equilibrium height. However, gravity pulls the air parcel down a little too far so that it is now surrounded by denser air, resulting in a buoyancy force which pushes the parcel back up. In fact, gravity waves are also called buoyancy waves because gravity and buoyancy are both restoring forces. Similar to a stretched or compressed spring that is then released, this oscillation continues and is what we call a gravity wave!<\/p>\n\n\n\n

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Diagram of how a mountain wave is formed where the red circle represents a volume of air being displaced over a mountain.<\/strong><\/figcaption><\/figure>\n\n\n\n

This kind of motion is responsible for the fantastic cap and lenticular clouds that form over mountain tops. The air parcel also cools as it is pushed over the obstruction and if the air is moist enough it can cool sufficiently to condense into clouds.\u00a0<\/p>\n\n\n\n

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Cap cloud over Mt. Discovery in the Transantarctic Mountain Range.<\/strong><\/figcaption><\/figure>\n\n\n\n
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Lenticular clouds over Mt. Erebus as seen on the way to the Arrival Heights lidar lab<\/strong>.<\/figcaption><\/figure>\n\n\n\n

So not only are gravity waves responsible for these cool cloud phenomena, they have far-reaching impacts on atmospheric processes, hence the reason we go all the way to Antarctica to study them!\u00a0\u00a0\u00a0<\/p>\n","protected":false},"excerpt":{"rendered":"

And no, I\u2019m not talking about gravitational waves like those created by the collisions of blackholes and measured by the incredible LIGO instrument (Fun fact: LIGO is basically a gigantic Michelson interferometer which, on a much smaller scale, our group uses to measure the wavelengths of our lasers).  I\u2019m referring to atmospheric gravity waves which… Read More<\/a><\/p>\n","protected":false},"author":158,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[2,6,4,3,5],"class_list":["post-330","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-antarctica","tag-atmospheric-science","tag-gravity-waves","tag-lidar","tag-mcmurdo"],"jetpack_featured_media_url":"","publishpress_future_action":{"enabled":false,"date":"2026-05-21 14:25:51","action":"change-status","newStatus":"draft","terms":[],"taxonomy":"category"},"publishpress_future_workflow_manual_trigger":{"enabledWorkflows":[]},"_links":{"self":[{"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/posts\/330","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/users\/158"}],"replies":[{"embeddable":true,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/comments?post=330"}],"version-history":[{"count":2,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/posts\/330\/revisions"}],"predecessor-version":[{"id":337,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/posts\/330\/revisions\/337"}],"wp:attachment":[{"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/media?parent=330"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/categories?post=330"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ciresblogs.colorado.edu\/lidarexploration\/wp-json\/wp\/v2\/tags?post=330"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}