{"id":792886,"date":"2025-01-22T08:35:06","date_gmt":"2025-01-22T13:35:06","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=792886"},"modified":"2025-01-22T08:35:06","modified_gmt":"2025-01-22T13:35:06","slug":"swarm-detects-tidal-signatures-of-our-oceans","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=792886","title":{"rendered":"Swarm detects tidal signatures of our oceans"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div id=\"\">\n\t<span class=\"pillar article__item\">Applications<\/span><\/p>\n<p>\t\t\t\t\t\t<span>22\/01\/2025<\/span><br \/>\n\t\t\t\t<span><span id=\"viewcount\">160<\/span><small> views<\/small><\/span><br \/>\n\t\t\t\t\t\t\t\t\t\t<span><span id=\"ezsr_total_26545588\">4<\/span><small> likes<\/small><\/span><\/p>\n<\/div>\n<div>\n<p>A study using data from ESA\u2019s Swarm mission suggests that faint magnetic signatures created by Earth\u2019s tides can help us determine magma distribution under the seabed and could even give us insights into long-term trends in global ocean temperatures and salinity.<\/p>\n<\/div>\n<div>\n<p>Swarm is a constellation of three satellites that study Earth\u2019s geomagnetic field. This magnetic field that extends from Earth\u2019s interior into space is thought to be produced largely by an ocean of liquid iron in the planet\u2019s outer core. Other sources of magnetism include magnetised rocks in the crust.<\/p>\n<p>And although we might not normally think of oceans as generating magnetism, the salty sea water is a moderate electrical conductor. This means that as tides flow across Earth\u2019s magnetic field, they generate weak electric currents, which in turn induce small magnetic signals \u2013 that can be detected from space.<\/p>\n<\/p><\/div>\n<div>\n<figure class=\"article__image article__image--right\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tSwarm constellation<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p>With its satellites flying at an altitude between 462 km and 511 km, Swarm measures Earth\u2019s magnetic field more accurately than ever before. It can detect faint tidal signatures and distinguish them from other stronger magnetic field sources from Earth\u2019s interior.<\/p>\n<p>\u201cThis study shows that Swarm can provide data on properties of the entire water column of our oceans.\u201d says Anja Str\u00f8mme, ESA\u2019s Swarm Mission Manager.<\/p>\n<p>Swarm\u2019s data can also provide insights into the distribution of magma, which could in future support better understanding of events such as the Hunga-Tonga volcanic eruption of 2022.<\/p>\n<p>The study of these signatures made the front cover of the world\u2019s oldest scientific journal, Philosophical Transactions of the Royal Society A, and was conducted by a team from the University of Cologne and the Technical University of Denmark.<\/p>\n<h4>Swarm gets better with age<\/h4>\n<p>The mission, launched in 2013, was only meant to fly for four years but is now in its 12th year. Anja adds: \u201cThis is one of the benefits of flying missions for longer than originally planned. So, by flying as long as the scientific output is of excellent quality and resources allow, you can tackle scientific questions that weren\u2019t originally envisaged.\u201d<\/p>\n<p>Swarm is, however, slowly nearing the natural end of its lifespan as drag gradually brings the satellites physically closer to Earth. This has enabled the mission\u2019s instruments \u2013 the satellites carry state-of-the-art sensors including magnetometers that measure the strength, magnitude and direction of the magnetic field \u2013 to capture faint signals that would be more difficult to detect from the higher orbits at the start of the mission.<\/p>\n<\/p><\/div>\n<div>\n<h2 class=\"heading\">Less solar interference<\/h2>\n<figure class=\"article__image article__image--left\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tSwarm detects tidal magnetic signatures<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p>Swarm\u2019s ability to detect the faint ocean signals was also helped by the Sun\u2019s less active period around 2017. \u201cThese are among the smallest signals detected by the Swarm mission so far,\u201d says lead author Alexander Grayver, of the University of Cologne.<\/p>\n<p>\u201cThe data are particularly good because they were gathered during a period of solar minimum, when there was less noise due to space weather.\u201d<\/p>\n<p>The \u2018minimum\u2019 period of the Sun\u2019s 11-year solar cycle is when the Sun\u2019s surface is least active. During this \u2018quiet\u2019 period, it emits less solar matter \u2013 including electromagnetic radiation and charged particles \u2013 so \u2018space weather\u2019 phenomena such as the Northern Lights are less frequent. And with less electromagnetic radiation from the Sun, the geomagnetic signals from Earth are more easily detectable by Swarm\u2019s magnetometers and other instruments.<\/p>\n<p>The hope is that, when the next solar minimum comes around after 2030, Swarm might still be flying \u2013 albeit at a lower altitude \u2013 and will be able to continue detecting the faint signals that can help us understand more about the temperatures and salinity deep within our oceans.<\/p>\n<\/p><\/div>\n<div>\n<p><button id=\"ezsr_26545588_5_5\" class=\"btn ezsr-star-rating-enabled\" title=\"Like\">Like<\/button><\/p>\n<p id=\"ezsr_just_rated_26545588\" class=\"ezsr-just-rated hide\">Thank you for liking<\/p>\n<p id=\"ezsr_has_rated_26545588\" class=\"ezsr-has-rated hide\">You have already liked this page, you can only like it once!<\/p>\n<\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/www.esa.int\/Applications\/Observing_the_Earth\/FutureEO\/Swarm\/Swarm_detects_tidal_signatures_of_our_oceans?rand=771654\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Applications 22\/01\/2025 160 views 4 likes A study using data from ESA\u2019s Swarm mission suggests that faint magnetic signatures created by Earth\u2019s tides can help us determine magma distribution under&hellip; <\/p>\n","protected":false},"author":1,"featured_media":792887,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[],"class_list":["post-792886","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ESA"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/792886","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=792886"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/792886\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/792887"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=792886"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=792886"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=792886"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}