{"id":52116,"date":"2023-12-07T21:21:18","date_gmt":"2023-12-07T20:21:18","guid":{"rendered":"https:\/\/dasgoetheanum.com\/?p=52116"},"modified":"2023-12-08T12:49:36","modified_gmt":"2023-12-08T11:49:36","slug":"what-can-we-learn-from-what-is-happening-in-antarctica","status":"publish","type":"post","link":"https:\/\/dasgoetheanum.com\/en\/what-can-we-learn-from-what-is-happening-in-antarctica\/","title":{"rendered":"What Can We Learn From What is Happening in Antarctica?"},"content":{"rendered":"\n<p><strong>Antarctica is under human protection, but human-induced climate disruption is undermining this endeavour. The melting of the ice-shelf, now categorised as &#8220;unavoidable&#8221;, is a reflection of thinking that is separated from the processes of life.<\/strong><\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>The Antarctic continent was designated and preserved as a place for scientific observation and research by the Antarctic Treaty that came into effect in 1961. It was further protected from the exploitation of raw materials in 1991 through actions initiated by Greenpeace in the 1980s. Over the past two decades, the research community has been heavily involved in documenting changes in sea ice conditions, glacier retreat, and ocean currents in connection with marine life. It is now apparent that the energy conversions set in motion by humans using oil, gas, and coal are leading to the gradual destruction of Antarctic glaciers and the living conditions in the world&#8217;s oceans. An important article was published in the prestigious bulletin <em>Nature Climate Change<\/em> on October 23, 2023\u2014it was immediately judged to be of significance and high quality by the international research community.<span id='easy-footnote-1-52116' class='easy-footnote-margin-adjust'><\/span><span class='easy-footnote'><a href='https:\/\/dasgoetheanum.com\/en\/what-can-we-learn-from-what-is-happening-in-antarctica\/#easy-footnote-bottom-1-52116' title='A Naughten et al., &amp;#8220;&lt;a href=&quot;https:\/\/www.nature.com\/articles\/s41558-023-01818-x&quot; data-type=&quot;URL&quot; data-id=&quot;https:\/\/www.nature.com\/articles\/s41558-023-01818-x&quot; target=&quot;_blank&quot; rel=&quot;noreferrer noopener&quot;&gt;Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century&lt;\/a&gt;&amp;#8220;, Nature Climate Change, 2022.'><sup>1<\/sup><\/a><\/span> The title of the article is \u201cUnavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century\u201d. The use of the word &#8220;unavoidable&#8221; is unusual and new. Antarctic events play a key role in understanding the drama of climate breakdown. This will be explained in a simplified form below.<\/p>\n\n\n\n<p>The Antarctic continent, with the South Pole at its centre, is surrounded by sea ice\u2014a floating mass of ice that grows and shrinks rhythmically with the seasons. This ice mass is encircled by a strong, eastward-moving ocean current that extends from the surface to great ocean depths (see illustration). This current is in a moving relationship with all other oceanic currents. Particularly in the bays of the Antarctic, the ocean current turns around and flows first southwards, then westwards under the sea ice towards the land mass (see illustration). The current now washes beneath the large glaciers that are connected to the mainland and protrude into the sea, and as water temperatures warm up, the glaciers melt away faster and faster from underneath. This melting can lead to glacier instability, so that large sections of glacier break off, enter the Antarctic Circumpolar Current as icebergs, melt and raise the sea level.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" src=\"https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum-1050x1024.jpg\" alt=\"\" class=\"wp-image-51456\" width=\"525\" height=\"512\" srcset=\"https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum-1050x1024.jpg 1050w, https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum-300x293.jpg 300w, https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum-770x751.jpg 770w, https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum-1536x1498.jpg 1536w, https:\/\/dasgoetheanum.com\/wp-content\/uploads\/2023\/11\/SY_DSC1527_Wochenschrift_Anthroposophie_Das_Goetheanum.jpg 1538w\" sizes=\"(max-width: 525px) 100vw, 525px\" \/><\/figure><\/div>\n\n\n<h3 class=\"wp-block-heading\"><strong>Separating Inorganic Processes from Life Processes<\/strong><\/h3>\n\n\n\n<p>The topographical conditions of the subsurface sea areas of the West Antarctic shelf have been well studied. There, the inflowing ocean current has made the overlying glaciers unstable with alarming acceleration.<span id='easy-footnote-2-52116' class='easy-footnote-margin-adjust'><\/span><span class='easy-footnote'><a href='https:\/\/dasgoetheanum.com\/en\/what-can-we-learn-from-what-is-happening-in-antarctica\/#easy-footnote-bottom-2-52116' title='TS Dotto et al., &lt;a href=&quot;http:\/\/doi.org\/10.1038\/s41467-022-35499-5&quot; target=&quot;_blank&quot; rel=&quot;noreferrer noopener&quot;&gt;&amp;#8220;Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength&amp;#8221;&lt;\/a&gt;, Nature Communication, 2022.'><sup>2<\/sup><\/a><\/span> <span id='easy-footnote-3-52116' class='easy-footnote-margin-adjust'><\/span><span class='easy-footnote'><a href='https:\/\/dasgoetheanum.com\/en\/what-can-we-learn-from-what-is-happening-in-antarctica\/#easy-footnote-bottom-3-52116' title='J Lauber et al., &lt;a href=&quot;http:\/\/doi.org\/10.1038\/s41561-023-01273-5&quot; target=&quot;_blank&quot; rel=&quot;noreferrer noopener&quot;&gt;&amp;#8220;Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice&amp;#8221;&lt;\/a&gt;, Nature Geoscience, 2023.'><sup>3<\/sup><\/a><\/span> Measurements show that the water temperature and the speed of ocean currents around Antarctica have risen rapidly and severely. This is linked to anthropogenic global warming, which, with a certain delay, is now also affecting the vast water masses of the oceans.<\/p>\n\n\n\n<p>If the water that flows under the Antarctic sea ice is getting warmer, it is not only the existence of the Antarctic glaciers that is being disrupted\u2014there are other connections to consider. When the water flows back to the submarine continental margin, an important event occurs. There, we find the rhythmically pulsating life and death of unicellular plant and animal plankton, combined with a diverse bacterial life. The sinking of the above-mentioned water masses to depths of several kilometres is related to this life metabolism. This sinking water stimulates and brings rhythm into the entirety of all ocean water currents at the surface and at intermediate depths, as well as the important bottom current.<span id='easy-footnote-4-52116' class='easy-footnote-margin-adjust'><\/span><span class='easy-footnote'><a href='https:\/\/dasgoetheanum.com\/en\/what-can-we-learn-from-what-is-happening-in-antarctica\/#easy-footnote-bottom-4-52116' title='HU Schmutz, &amp;#8220;10. Klasse \u2013 Die Erde in Bewegung&amp;#8221; [Year 10 \u2013 The Earth in Motion] in &lt;em&gt;Erdkunde in der 9. bis 12. Klasse an Waldorfschulen, eine Gesamtkonzeption &lt;\/em&gt;[Geography in Year 9 to 12 at Waldorf Schools, an Integrated Concept], (Stuttgart, 2001).'><sup>4<\/sup><\/a><\/span><\/p>\n\n\n\n<p>The sinking has weakened in recent times and, in addition, the uptake and transport of carbon compounds to the depths of the sinking zones is decreasing due to the rising water temperature in the area of the sea ice. Less of the greenhouse gas, carbon dioxide, is absorbed from the air into the sinking water. The rise in the temperature of the ocean water and its effect in the Antarctic region is therefore linked to all the processes that climate researchers are investigating for regions inhabited by humans.<\/p>\n\n\n\n<p>This connection is not a simple one, where a cause is simply followed by a certain effect. These are processes where causes and effects are in constant reciprocal interaction. In this way, Antarctic events can give us the incentive to train agile thinking, so that processes in the inorganic realm are not separated from rhythmically driven life processes, however inconspicuously they may appear in the Antarctic. Such living thinking can be the key to recognising climate breakdown and changing the way we treat the earth.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p><strong><strong>Key to the Antarctic map<\/strong><\/strong>, created by HU Schmutz<\/p>\n\n\n\n<p>White at the edge of the Antarctic: glacier resting on water<br>Pale blue: sea depth up to 200m<br>Light blue: sea depth up to 2000m<br>Dark blue: sea depth up to 6000m<br>Red broken line: extent of sea ice in January<br>Red dot-dash line: extent of sea ice in July<br>Purple wavy line: Antarctic Circumpolar Current<br>Purple line: surface currents<br>Black crosses: sinking zones of surface water<br>Black double line: bottom currents<\/p>\n\n\n\n<p><strong>Translation<\/strong> Christian von Arnim<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Antarctica is under human protection, but human-induced climate disruption is undermining this endeavour. The melting of the ice-shelf, now categorised as &#8220;unavoidable&#8221;, is a reflection of thinking that is separated from the processes of life. The Antarctic continent was designated and preserved as a place for scientific observation and research by the Antarctic Treaty that came into effect in 1961. It was further protected from the exploitation of raw materials in 1991 through actions initiated by Greenpeace in the 1980s. [&hellip;]<\/p>\n","protected":false},"author":9298,"featured_media":51455,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[8825,8815],"tags":[11400,8824],"class_list":["post-52116","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-natural-sciences","category-world-situation","tag-2023-46-en","tag-spotlights"],"acf":[],"_links":{"self":[{"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/posts\/52116","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/users\/9298"}],"replies":[{"embeddable":true,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/comments?post=52116"}],"version-history":[{"count":0,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/posts\/52116\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/media\/51455"}],"wp:attachment":[{"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/media?parent=52116"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/categories?post=52116"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/dasgoetheanum.com\/en\/wp-json\/wp\/v2\/tags?post=52116"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}