{"id":40741,"date":"2026-01-26T08:00:24","date_gmt":"2026-01-26T12:00:24","guid":{"rendered":"https:\/\/www.fondriest.com\/news\/?p=40741"},"modified":"2026-02-11T14:04:52","modified_gmt":"2026-02-11T18:04:52","slug":"using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences","status":"publish","type":"post","link":"https:\/\/www.fondriest.com\/news\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm","title":{"rendered":"Using Buoys to Measure the AMOC: An Ocean Current with Global Climate Consequences"},"content":{"rendered":"<p>Nicholas Foukal stands on the bridge of a long, pale white boat overlooking the choppy Denmark Strait, the water a greenish-blue hue and dotted with towering icebergs.<\/p>\n<p>The deck and boat interior are loaded with research equipment\u2013several large yellow mooring buoys, a remote underwater vehicle, and a plethora of water quality measurement instruments, just to name a few.<\/p>\n<p>They\u2019re a reminder of what Foukal has come to this formidable ocean passage to do: study the changes befalling the Atlantic Meridional Overturning Current (AMOC), one of the world\u2019s most important ocean current systems.<\/p>\n<p>But as he stares at the massive, rugged snow-capped fjords and glaciers of East Greenland crashing into a seemingly endless turbulent sea, the scale of his task hits him.<\/p>\n<div id=\"attachment_40748\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40748\" class=\"size-full wp-image-40748\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8239_ForWeb.jpg\" alt=\"The East Greenland coastline from the site at 71\u00b0N where the VBB system was deployed.\" width=\"940\" height=\"705\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8239_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8239_ForWeb-300x225.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8239_ForWeb-600x450.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8239_ForWeb-768x576.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40748\" class=\"wp-caption-text\"><span style=\"color: #808080;\">The East Greenland coastline from the site at 71\u00b0N where the VBB system was deployed. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n<p>Six carefully placed buoys, spanning dozens of miles across the southern edge of one of the harshest seas in the world, will help provide new information on an oceanic current that stretches from pole to pole, impacting the lives of billions of people.<\/p>\n<p>The captain stops the ship at precisely the correct location, even 10 feet makes a difference to Foukal, and his team prepares to drop a buoy into the waves.<\/p>\n<p>Constructed of several small, connected spheres and loaded with sensors to measure water temperature, salinity, and velocity, the buoys will track freshwater melting off Greenland\u2019s plentiful ice sheets.<\/p>\n<p>What Foukal and his team aim to discover is how much freshwater is intruding on the AMOC, and whether those changes represent a climate tipping point with global consequences.<\/p>\n<div id=\"attachment_40747\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40747\" class=\"size-full wp-image-40747\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8229-2_ForWeb.jpg\" alt=\"An ocean bottom tripod (yellow, left) and a Stablemoor buoy (red, right). The Stablemoor buoy is a portion of the \u201cVariable Ballast Buoy\u201d system in which an instrument package (not shown) moves vertically depending on how deep the ice is above this Stablemoor buoy. The ice thickness is calculated using the upward-looking ADCP on the Stablemoor.\" width=\"940\" height=\"705\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8229-2_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8229-2_ForWeb-300x225.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8229-2_ForWeb-600x450.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8229-2_ForWeb-768x576.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40747\" class=\"wp-caption-text\"><span style=\"color: #808080;\">An ocean bottom tripod (yellow, left) and a Stablemoor buoy (red, right). The Stablemoor buoy is a portion of the \u201cVariable Ballast Buoy\u201d system in which an instrument package (not shown) moves vertically depending on how deep the ice is above this Stablemoor buoy. The ice thickness is calculated using the upward-looking ADCP on the Stablemoor. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n<h3><span style=\"color: #4d4d4d;\">Why Study the AMOC\u2019s Hydrology?<\/span><\/h3>\n<p>Dr. Nicholas Foukal is an assistant professor at the University of Georgia\u2019s <a href=\"https:\/\/www.skio.uga.edu\/\" target=\"_blank\" rel=\"noopener\">Skidaway Institute of Oceanography<\/a>. He studies how the ocean stores and transports heat, which sparked an interest in the AMOC, leading to his current four-year National Science Foundation-funded project.<\/p>\n<p>In the northern hemisphere, this global ocean current transports warmer surface water from the Gulf of Mexico toward northern Europe, before the cold climate around Iceland and Greenland plunges it deeper and turns it around. This deep water then surges south past the US East Coast and toward South America.<\/p>\n<p>\u201cGenerally speaking, it&#8217;s just this northward flow of surface waters, and then a net southward flow of deeper waters,\u201d Foukal says. \u201cBut the really important part is the fact that those two water masses have very different temperatures and salinities.\u201d<\/p>\n<p>It was long thought that these differences remained relatively stable, and the current wasn\u2019t extremely variable. But Foukal says recent research has shown intraseasonal variations in both of these water masses.<\/p>\n<p>The warmer surface current has been measured by the <a href=\"https:\/\/rapid.ac.uk\/\" target=\"_blank\" rel=\"noopener\">RAPID mooring array<\/a> since 2004, stretching from Florida to Western Africa.<\/p>\n<p>Further north, the <a href=\"https:\/\/www.o-snap.org\/\" target=\"_blank\" rel=\"noopener\">OSNAP array<\/a> stretches from Canada to Greenland\u2019s southern tip, then toward Scotland. This younger mooring array measures the AMOC, where much of the deep water is formed. Together, data from these arrays have shown that the AMOC.<\/p>\n<div id=\"attachment_40746\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40746\" class=\"size-full wp-image-40746\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb.jpg\" alt=\"A set of ocean bottom tripods awaits deployment on the back deck of the R\/V \u00de\u00f3runn \u00de\u00f3r\u00f0ard\u00f3ttir (Iceland). Upward-looking ADCPs are visible on each tripod. Yellow spheres provide flotation for mooring recovery when the anchor is released after a year of deployment.\" width=\"940\" height=\"940\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb-300x300.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb-600x600.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb-150x150.jpg 150w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8224_ForWeb-768x768.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40746\" class=\"wp-caption-text\"><span style=\"color: #808080;\">A set of ocean bottom tripods awaits deployment on the back deck of the R\/V \u00de\u00f3runn \u00de\u00f3r\u00f0ard\u00f3ttir (Iceland). Upward-looking ADCPs are visible on each tripod. Yellow spheres provide flotation for mooring recovery when the anchor is released after a year of deployment. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n<p>Overall, Foukal says the massive current is becoming <a href=\"https:\/\/www.theguardian.com\/environment\/2018\/apr\/11\/critical-gulf-stream-current-weakest-for-1600-years-research-finds\" target=\"_blank\" rel=\"noopener\">weaker<\/a> and stronger on a more variable time scale. The problem is that no one is confident about what is causing these changes around AMOC&#8217;s current northern terminus.<\/p>\n<p>\u201cThe question is, \u2018what causes the variability in those time series?\u2019\u201d Foukal explains. \u201cAnd to understand that, you need to look at other things, like a stressor or something that&#8217;s a physical force on [the] AMOC.\u201d<\/p>\n<p>This question led to a hypothesis within the scientific community: global warming-induced ice melt is flowing off East Greenland, introducing too much freshwater to the salty ocean current and changing its density.<\/p>\n<p>\u201cGlobally, if you look at the density structure, temperature is a much larger control on density than salinity is,\u201d Foukal says, which is why a warm surface water current flows north from the Gulf.<\/p>\n<p>He continues, \u201cBut in certain regions, like the polar regions, salinity is more important.\u201d<\/p>\n<p>Freshwater is less dense than saltwater, so <a href=\"https:\/\/www.nature.com\/articles\/s41558-022-01328-2\" target=\"_blank\" rel=\"noopener\">some believe<\/a> that freshwater intrusion is throwing these salty currents off their normal circulation pattern, therefore weakening the southbound deep water formations.<\/p>\n<p>Yet no one has successfully tested this hypothesis and measured how much freshwater is actually flowing into the Denmark Strait, something that astounded Foukal as he researched this project.<\/p>\n<p>\u201cIt&#8217;s certainly well known that this is a really sensitive component of our climate system, yet no one&#8217;s been able to actually measure, not only the variability, but what the mean [of freshwater input] is,\u201d Foukal says.<\/p>\n<p>Months later, as he floats along Greenland&#8217;s treacherous east coast and deploys buoys further north than most have ever tried, he understands why. But Foukal knows this data is important, and hopes some intuitive system designs will overcome the harsh Arctic conditions.<\/p>\n<div id=\"attachment_40752\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40752\" class=\"size-full wp-image-40752\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8309_ForWeb.jpg\" alt=\"The East Greenland coastline near the site where the VBB was deployed at 71\u00b0N.\" width=\"940\" height=\"705\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8309_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8309_ForWeb-300x225.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8309_ForWeb-600x450.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8309_ForWeb-768x576.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40752\" class=\"wp-caption-text\"><span style=\"color: #808080;\">The East Greenland coastline near the site where the VBB was deployed at 71\u00b0N. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n<h3><span style=\"color: #4d4d4d;\">Challenges Deploying Buoys and a Density-Measurement System<\/span><\/h3>\n<p>The biggest obstacle for Foukal\u2019s team when deploying their buoys is also, quite literally, the biggest obstacle in the strait: massive icebergs.<\/p>\n<p>Large, unpredictable, and capable of stretching deep below the surface, icebergs can wreak havoc on unattended monitoring systems, especially with the parameters his team is measuring.<\/p>\n<p>\u201cSalinity is tricky because you have to have an instrument that&#8217;s in the part of the water column where you need that data, and ideally you want the salinity near the surface,\u201d Foukal explains. \u201cThe problem is, there&#8217;s ice up there, and icebergs tend to just destroy moorings.\u201d<\/p>\n<p>Foukal\u2019s systems include the buoys and their moorings, with a rope system snaking beneath the waves. The rope houses several CTD sensors to measure water salinity and temperature, while an <a href=\"https:\/\/www.nexsens.com\/systems\/water_current_monitoring\" target=\"_blank\" rel=\"noopener\">ADCP<\/a> is attached to the bottom to measure water velocity.<\/p>\n<p>Together, Foukal says this will help them understand how much freshwater is coming off Greenland, and where it\u2019s going.<\/p>\n<p>To hopefully get around the iceberg problem, Foukal explains that the links between his instruments are intentionally weak. That way, if an iceberg comes along and knocks off the top instrument, the rest of the mooring will stay in place and continue logging measurements.<\/p>\n<p>He also partnered with the <a href=\"https:\/\/www.whoi.edu\/\" target=\"_blank\" rel=\"noopener\">Woods Hole Oceanographic Institute<\/a> to deploy a variable ballast buoy for one of his moorings. If this buoy, which was programmed to move within the water column based on the presence of icebergs, is successful, Foukal hopes to see more like it deployed in the future.<\/p>\n<p>Foukal\u2019s six buoys are part of a larger network that stretches even further east into the Denmark Strait toward Iceland. These extra seven buoys, which are from <a href=\"https:\/\/www.uib.no\/en\" target=\"_blank\" rel=\"noopener\">Norway <\/a>and <a href=\"https:\/\/www.awi.de\/en\/\" target=\"_blank\" rel=\"noopener\">Germany<\/a>, will help provide a more complete picture of how the AMOC behaves at such a northerly longitude.<\/p>\n<p>Now that Foukal\u2019s exciting but difficult two-week deployment off Greenland is completed, he must wait. The buoys will be in the water for a year before he removes them and extracts the data.<\/p>\n<p>He\u2019s hopeful that his system will hold up, as even a year\u2019s worth of baseline data about freshwater in the AMOC is crucial for understanding the ocean current\u2019s future.<\/p>\n<div id=\"attachment_40751\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40751\" class=\"size-full wp-image-40751\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8302_ForWeb.jpg\" alt=\"Icebergs choking the exit of Scoresby Sound.\" width=\"940\" height=\"705\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8302_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8302_ForWeb-300x225.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8302_ForWeb-600x450.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8302_ForWeb-768x576.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40751\" class=\"wp-caption-text\"><span style=\"color: #808080;\">Icebergs choking the exit of Scoresby Sound. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n<h3><span style=\"color: #4d4d4d;\">Applying Data From Six Buoys to the Entire Ocean<\/span><\/h3>\n<p>Ultimately, Foukal hopes that his data can be used to better calibrate the computational models that predict how the AMOC will change. In fact, he\u2019s partnered with a professor at <a href=\"https:\/\/www.jhu.edu\/\" target=\"_blank\" rel=\"noopener\">Johns Hopkins University<\/a> to refine these models.<\/p>\n<p>Without baseline data on the amount of freshwater already in the North Atlantic, these models can\u2019t accurately predict how much is needed to significantly alter the AMOC. And because this current is broadly recognized as not only an important ocean system, but also a potentially dangerous climate <a href=\"https:\/\/tos.org\/oceanography\/article\/is-the-atlantic-overturning-circulation-approaching-a-tipping-point\" target=\"_blank\" rel=\"noopener\">tipping point<\/a>, he knows it\u2019s vital to understand this freshwater input.<\/p>\n<p>So as Foukal looked over the North Atlantic waves while sailing away from a tiny, yellow \u201cpinprick\u201d of a buoy dropped in what looks like an endless ocean, it\u2019s both exciting and nerve-wracking.<\/p>\n<p>He sometimes can\u2019t believe that several small systems among the unfathomably large ocean can truly capture global trends, but he also trusts his team\u2019s work. This is the place to take these globally consequential measurements.<\/p>\n<p>\u201cYou have to look for places where there&#8217;s either choke points in the circulation [&#8230;] or where all the circulation condenses into a small area so you can actually measure it,\u201d Foukal explains.<\/p>\n<p>He continues, \u201cOr you need to look for some places where a small geographic area has an outsized role in our climate. And the Northeast Greenland shelf is absolutely that.\u201d<\/p>\n<p>Foukal and his team braved the treacherous conditions to deploy these ocean monitoring systems, and they hope to pull data from them soon.<\/p>\n<p>With the correct instruments, carefully placed locations, and some intuitive system design, they may be on their way to better understand the AMOC and how the global ocean is changing with it.<\/p>\n<p>\u201cI always have to think of myself, \u2018how are we actually measuring this whole system with just [several] instruments?\u2019\u201d Foukal says. \u201cIt&#8217;s kind of mind-boggling to actually do that.\u201d<\/p>\n<div id=\"attachment_40753\" style=\"width: 950px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-40753\" class=\"size-full wp-image-40753\" src=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8313_ForWeb.jpg\" alt=\"The Stablemoor buoy being deployed by the ship\u2019s crew, and the WHOI Mooring Operations and Engineering group.\" width=\"940\" height=\"705\" srcset=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8313_ForWeb.jpg 940w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8313_ForWeb-300x225.jpg 300w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8313_ForWeb-600x450.jpg 600w, https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/01\/Foukal_IMG_8313_ForWeb-768x576.jpg 768w\" sizes=\"auto, (max-width: 940px) 100vw, 940px\" \/><p id=\"caption-attachment-40753\" class=\"wp-caption-text\"><span style=\"color: #808080;\">The Stablemoor buoy being deployed by the ship\u2019s crew, and the WHOI Mooring Operations and Engineering group. (Credit: Nicholas Foukal)<\/span><\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Nicholas Foukal stands on the bridge of a long, pale white boat overlooking the choppy Denmark Strait, the water a greenish-blue hue and dotted with towering icebergs. The deck and boat interior are loaded with research equipment\u2013several large yellow mooring buoys, a remote underwater vehicle, and a plethora of water quality measurement instruments, just to [&hellip;]<\/p>\n","protected":false},"author":48,"featured_media":40818,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2371,23,5,7,8,44],"tags":[2829,2830,2824,91,2391,2354,2826,2828,2825,1463,2823,161,2832,503,2720,2827,2831],"class_list":["post-40741","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-buoy","category-earth-atmosphere","category-featured-articles","category-news","category-newsfeed","category-oceans-coasts","tag-adcp","tag-amoc","tag-atlantic-overturning-meridional-current","tag-buoy","tag-climate-tipping-point","tag-ctd","tag-denmark-strait","tag-density","tag-greenland","tag-north-atlantic","tag-ocean-current","tag-salinity","tag-skidaway-institute-of-oceanography","tag-water-quality","tag-water-temperature","tag-water-velocity","tag-woods-hole-oceanographic-institute"],"remote_post_permalink":false,"remote_post_featured_image":false,"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Using Buoys to Measure the AMOC: An Ocean Current with Global Climate Consequences<\/title>\n<meta name=\"description\" content=\"The AMOC is changing, and scientists are measuring its northern terminus to see if freshwater intrusion is a culprit.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.fondriest.com\/news\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Using Buoys to Measure the AMOC: An Ocean Current with Global Climate Consequences\" \/>\n<meta property=\"og:description\" content=\"The AMOC is changing, and scientists are measuring its northern terminus to see if freshwater intrusion is a culprit.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.fondriest.com\/news\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm\" \/>\n<meta property=\"og:site_name\" content=\"Environmental Monitor\" \/>\n<meta property=\"article:published_time\" content=\"2026-01-26T12:00:24+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-02-11T18:04:52+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/news.fondriest.com\/wp-content\/uploads\/2026\/02\/Foukal_IMG_8239_ForWeb.webp\" \/>\n\t<meta property=\"og:image:width\" content=\"940\" \/>\n\t<meta property=\"og:image:height\" content=\"705\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/webp\" \/>\n<meta name=\"author\" content=\"Sam Norton\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"Sam Norton\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"9 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\\\/\\\/www.fondriest.com\\\/news\\\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm#article\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.fondriest.com\\\/news\\\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm\"},\"author\":{\"name\":\"Sam Norton\",\"@id\":\"https:\\\/\\\/www.fondriest.com\\\/news\\\/#\\\/schema\\\/person\\\/8b594a2654ef33b01e98456d99a980ef\"},\"headline\":\"Using Buoys to Measure the AMOC: An Ocean Current with Global Climate Consequences\",\"datePublished\":\"2026-01-26T12:00:24+00:00\",\"dateModified\":\"2026-02-11T18:04:52+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\\\/\\\/www.fondriest.com\\\/news\\\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm\"},\"wordCount\":1708,\"commentCount\":0,\"image\":{\"@id\":\"https:\\\/\\\/www.fondriest.com\\\/news\\\/using-buoys-to-measure-the-amoc-an-ocean-current-with-global-climate-consequences.htm#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/news.fondriest.com\\\/wp-content\\\/uploads\\\/2026\\\/02\\\/Foukal_IMG_8239_ForWeb.webp\",\"keywords\":[\"ADCP\",\"AMOC\",\"Atlantic Overturning Meridional Current\",\"buoy\",\"climate tipping point\",\"CTD\",\"Denmark Strait\",\"density\",\"Greenland\",\"North Atlantic\",\"ocean current\",\"salinity\",\"Skidaway Institute of Oceanography\",\"water quality\",\"water temperature\",\"water velocity\",\"Woods Hole Oceanographic Institute\"],\"articleSection\":[\"Buoy\",\"Earth &amp; 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