{"id":441820,"date":"2026-04-29T04:19:32","date_gmt":"2026-04-29T11:19:32","guid":{"rendered":"https:\/\/climatescience.press\/?p=441820"},"modified":"2026-04-29T04:19:34","modified_gmt":"2026-04-29T11:19:34","slug":"snowball-earth-may-hide-a-far-stranger-climate-cycle-than-anyone-expected","status":"publish","type":"post","link":"https:\/\/climatescience.press\/?p=441820","title":{"rendered":"Snowball Earth May Hide a Far Stranger Climate Cycle Than Anyone Expected"},"content":{"rendered":"<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"687\" height=\"1024\" data-attachment-id=\"441821\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=441821\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?fit=784%2C1168&amp;ssl=1\" data-orig-size=\"784,1168\" data-comments-opened=\"1\" data-image-meta=\"{&quot;aperture&quot;:&quot;0&quot;,&quot;credit&quot;:&quot;&quot;,&quot;camera&quot;:&quot;&quot;,&quot;caption&quot;:&quot;&quot;,&quot;created_timestamp&quot;:&quot;0&quot;,&quot;copyright&quot;:&quot;&quot;,&quot;focal_length&quot;:&quot;0&quot;,&quot;iso&quot;:&quot;0&quot;,&quot;shutter_speed&quot;:&quot;0&quot;,&quot;title&quot;:&quot;&quot;,&quot;orientation&quot;:&quot;0&quot;}\" data-image-title=\"0 Snowball Earth May Hide a Far Stranger Climate Cycle Than Anyone Expected\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?fit=687%2C1024&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected-687x1024.jpg?resize=687%2C1024&#038;ssl=1\" alt=\"\" class=\"wp-image-441821\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?resize=687%2C1024&amp;ssl=1 687w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?resize=201%2C300&amp;ssl=1 201w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?resize=768%2C1144&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?resize=640%2C953&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?w=784&amp;ssl=1 784w\" sizes=\"auto, (max-width: 687px) 100vw, 687px\" \/><\/figure>\n<\/div>\n\n\n<p class=\"wp-block-paragraph\"><strong>A new study published in the Proceedings of the National Academy of Sciences (PNAS) in 2026 proposes that the famous &#8220;Snowball Earth&#8221; events\u2014particularly the long Sturtian glaciation (~717\u2013658 million years ago)\u2014may have involved a far stranger, oscillating climate cycle than the traditional &#8220;one long freeze followed by rapid thaw&#8221; model.<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Traditional Snowball Earth View<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">During the Cryogenian Period (part of the Neoproterozoic), Earth experienced extreme glaciations where ice sheets reached the tropics, and the planet was largely (or entirely) encased in ice for millions of years.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The classic mechanism:<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Runaway cooling:<\/strong> Increased ice cover raised <strong>Earth&#8217;s albedo (reflectivity)<\/strong>, reflecting more sunlight and causing further cooling in a positive feedback loop.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Escape from snowball:<\/strong> Volcanic CO\u2082 built up over millions of years because silicate weathering (a major CO\u2082 sink) largely stopped under ice. Eventually, the greenhouse effect overwhelmed the ice, leading to rapid deglaciation and extremely hot &#8220;hothouse&#8221; conditions afterward.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">This explained glacial deposits at low latitudes and cap carbonates (unusual rock layers formed during rapid warming). However, it struggled with some observations, such as the very long duration of the Sturtian (~56\u201360 million years) and evidence that life (including oxygen-dependent processes) persisted.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>The New &#8220;Limit Cycle&#8221; Model: A Stranger, Repeating Climate Oscillation<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The recent modeling study suggests the Sturtian wasn&#8217;t one monolithic deep freeze. Instead, it featured <strong>repeated &#8220;limit cycles&#8221;<\/strong>\u2014oscillations between glacial (cold, icy) and interglacial\/hothouse (warmer) states driven by interactions between <strong>volcanism, the Franklin Large Igneous Province (LIP)<\/strong>, and <strong>silicate weathering<\/strong>.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Key dynamics:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Weathering of fresh basaltic rocks from the Franklin LIP (a massive volcanic event) acted as a powerful CO\u2082 sink, drawing down atmospheric carbon and triggering or prolonging glaciation.<\/li>\n\n\n\n<li>During full glaciation, weathering slowed or halted \u2192 CO\u2082 from ongoing volcanism built up \u2192 warming eventually occurred.<\/li>\n\n\n\n<li>Upon partial deglaciation, remaining unweathered basalt from the LIP became available again for rapid weathering \u2192 CO\u2082 drawdown resumed \u2192 cooling restarted the cycle.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">This back-and-forth continued until the &#8220;weathering power&#8221; of the LIP was largely exhausted. It better explains the prolonged duration of the Sturtian and how biogeochemical cycles (including oxygen levels supporting life) could continue operating, rather than everything shutting down for tens of millions of years.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">_____________________________________________________________________________________<\/p>\n\n\n\n<p class=\"has-large-font-size wp-block-paragraph\"><strong>Repeated snowball\u2013hothouse cycles within the Neoproterozoic Sturtian glaciation<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>&#8220;Repeated snowball\u2013hothouse cycles within the Neoproterozoic Sturtian glaciation&#8221;<\/strong> is the exact title of a new paper published in the Proceedings of the <strong>National Academy of Sciences (PNAS)<\/strong> in late <strong>April 2026<\/strong> by <strong>Charlotte Minsky and colleagues<\/strong>.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Published:<\/strong> Proceedings of the National Academy of Sciences (PNAS)<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Authors:<\/strong> <a href=\"https:\/\/www.pnas.org\/doi\/10.1073\/pnas.2525919123#con1\">Charlotte&nbsp;Minsky<\/a>,&nbsp;<a href=\"https:\/\/www.pnas.org\/doi\/10.1073\/pnas.2525919123#con2\">Robin&nbsp;Wordsworth<\/a>,&nbsp;<a href=\"https:\/\/www.pnas.org\/doi\/10.1073\/pnas.2525919123#con3\">David T.&nbsp;Johnston<\/a> and&nbsp;<a href=\"https:\/\/www.pnas.org\/doi\/10.1073\/pnas.2525919123#con4\">Andrew H.&nbsp;Knoll<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>DOI:<\/strong> <a href=\"https:\/\/dx.doi.org\/10.1073\/pnas.2525919123\" target=\"_blank\" rel=\"noreferrer noopener\">10.1073\/pnas.2525919123<\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><strong>Abstract<\/strong><\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">The Neoproterozoic Era was a pivotal era of Earth\u2019s history in which multiple severe glaciations profoundly influenced the biosphere, but explaining the duration and nature of these events remains a major challenge. Notably, geochronology indicates that the Sturtian glaciation lasted for \u223c56 Myr\u2014far longer than can be accommodated by canonical \u201cSnowball\u201d or \u201cSlushball\u201d models. Here we use a coupled box model of the Neoproterozoic climate and carbon cycle to develop a hypothesis for Sturtian climate evolution. We show that weathering of the Franklin igneous province would have caused Earth to enter a limit cycle regime, alternating between Snowball and hothouse states for the duration of the Sturtian. This scenario resolves the duration problem, is allowable given currently observed patterns of sedimentation, and predicts syn-Sturtian oxygen stability.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Key Finding<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Instead of viewing the Sturtian glaciation (~717\u2013661 Ma, lasting roughly 56 million years) as one continuous, unbroken &#8220;hard snowball&#8221; state, the authors propose it involved repeated limit cycles \u2014 oscillations between extreme glacial (snowball) conditions and warmer hothouse intervals.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">This dynamic cycling better explains several longstanding puzzles:<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong><em>The unusually long duration of the Sturtian (far longer than the later Marinoan glaciation).<\/em><\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong><em>How biogeochemical cycles (especially oxygen) and life could persist over tens of millions of years.<\/em><\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong><em>Evidence that the climate system was not statically frozen for the entire interval.<\/em><\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>The Role of the Franklin Large Igneous Province (LIP)<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The cycles were driven by the massive <strong>Franklin LIP<\/strong>, a huge volcanic province emplaced around 719\u2013716 Ma in what is now northern Canada and Greenland, just before or overlapping the onset of the Sturtian.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Here\u2019s how the limit cycle worked in the model:<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Initial cooling and snowball onset:<\/strong> Weathering of the fresh, calcium- and magnesium-rich basalts from the Franklin LIP rapidly drew down atmospheric CO\u2082 (silicate weathering is a major CO\u2082 sink). Combined with other factors (low mid-ocean ridge outgassing, continental configuration), this pushed Earth past a tipping point into runaway ice-albedo feedback, triggering global glaciation.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>During full snowball:<\/strong> Ice cover greatly reduced or halted subaerial silicate weathering \u2192 volcanic CO\u2082 (from ongoing volcanism) began to accumulate in the atmosphere.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Deglaciation and hothouse phase:<\/strong> Rising CO\u2082 eventually overwhelmed the high albedo, causing rapid warming and partial or full deglaciation. During this warmer &#8220;hothouse&#8221; interval, the remaining unweathered portions of the Franklin basalts were exposed again to intense tropical weathering.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Repeat:<\/strong> Renewed rapid CO\u2082 drawdown from the fresh basalt triggered cooling and another return to snowball conditions.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">This back-and-forth continued until most of the weatherable basalt volume of the LIP was exhausted, eventually allowing a more stable exit from the glacial regime. The model shows that if only a portion of the LIP was weathered in the first snowball, enough remained to fuel subsequent cycles.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Why This Is a &#8220;Stranger&#8221; Climate Cycle<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Traditional &#8220;canonical&#8221; snowball models assumed a single long freeze followed by one dramatic escape driven by volcanic CO\u2082 buildup.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The new limit-cycle hypothesis introduces internal oscillations within the overall glacial epoch, driven by the interaction of LIP emplacement, weathering feedback, and the carbon cycle.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">It reconciles the extreme length of the Sturtian without requiring implausibly slow CO\u2082 buildup or constant subglacial weathering (though other 2026 papers explore continued subglacial weathering as an additional factor that could prolong glaciation).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong><em>This framework also helps explain how oxygen-dependent life and other processes could continue operating, as full shutdown for 56 million years would have been biologically challenging.<\/em><\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The study highlights how large igneous provinces can drive not just one-off climate shifts but prolonged, self-sustaining oscillatory behavior through carbon cycle feedbacks. It refines our understanding of Earth&#8217;s climate sensitivity in extreme states and provides a testable hypothesis for future geological and geochemical studies of Cryogenian rocks.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>A new study published in the Proceedings of the National Academy of Sciences (PNAS) in 2026 proposes that the famous &#8220;Snowball Earth&#8221; events\u2014particularly the long Sturtian glaciation (~717\u2013658 million years ago)\u2014may have involved a far stranger, oscillating climate cycle than the traditional &#8220;one long freeze followed by rapid thaw&#8221; model.<\/p>\n","protected":false},"author":121246920,"featured_media":441821,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_coblocks_attr":"","_coblocks_dimensions":"","_coblocks_responsive_height":"","_coblocks_accordion_ie_support":"","advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_feature_clip_id":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":true,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2},"jetpack_post_was_ever_published":false},"categories":[1],"tags":[691842626,691842627,691842628,691842632,691833970,691842630,691842629,691842631],"class_list":["post-441820","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-cryogenian-period-part-of-the-neoproterozoic","tag-extreme-glaciations","tag-franklin-large-igneous-province-lip","tag-internal-oscillations","tag-proceedings-of-the-national-academy-of-sciences-pnas","tag-repeating-climate-oscillation","tag-silicate-weathering","tag-volcanism","fallback-thumbnail"],"jetpack_publicize_connections":[],"jetpack_featured_media_url":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Snowball-Earth-May-Hide-a-Far-Stranger-Climate-Cycle-Than-Anyone-Expected.jpg?fit=784%2C1168&ssl=1","jetpack_likes_enabled":true,"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/paxLW1-1QW8","jetpack-related-posts":[{"id":447125,"url":"https:\/\/climatescience.press\/?p=447125","url_meta":{"origin":441820,"position":0},"title":"Warmer Antarctic Regions Amplify Temperature Shifts More Than Colder Interiors \u2013 Due to Temperature-Dependent Greenhouse Feedbacks","author":"uwe.roland.gross","date":"05\/28\/2026","format":false,"excerpt":"A recent study highlights how a bare supercontinent like Rodinia, positioned mostly in the tropics around 700\u2013600 million years ago, could have helped trigger or amplify \"Snowball Earth\" glaciations during the Neoproterozoic era.","rel":"","context":"In \"Bare rock albedo\"","block_context":{"text":"Bare rock 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feedback.","rel":"","context":"In \"biogeochemical model (COPSE)\"","block_context":{"text":"biogeochemical model (COPSE)","link":"https:\/\/climatescience.press\/?tag=biogeochemical-model-copse"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Subduction-on-a-Cooling-Planet-Drove-the-Stepwise-Rise-of-Atmospheric-Oxygen.jpg?fit=1168%2C784&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Subduction-on-a-Cooling-Planet-Drove-the-Stepwise-Rise-of-Atmospheric-Oxygen.jpg?fit=1168%2C784&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Subduction-on-a-Cooling-Planet-Drove-the-Stepwise-Rise-of-Atmospheric-Oxygen.jpg?fit=1168%2C784&ssl=1&resize=525%2C300 1.5x, 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advance using a lunar cycle","author":"uwe.roland.gross","date":"07\/19\/2023","format":false,"excerpt":"In 2007, two Canadian scientists studying the effects of this cycle on the Pacific coast of North America successfully predicted the occurrence of a major El Ni\u00f1o event in 2015 based on lunar data. Remarkably, their prediction proved accurate.","rel":"","context":"In \"2015\"","block_context":{"text":"2015","link":"https:\/\/climatescience.press\/?tag=2015"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/07\/00ENSOblog_Bjerknes-feedback-ElNino_large-pichi-1536x1023-1.jpg?fit=1200%2C799&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/07\/00ENSOblog_Bjerknes-feedback-ElNino_large-pichi-1536x1023-1.jpg?fit=1200%2C799&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/07\/00ENSOblog_Bjerknes-feedback-ElNino_large-pichi-1536x1023-1.jpg?fit=1200%2C799&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/07\/00ENSOblog_Bjerknes-feedback-ElNino_large-pichi-1536x1023-1.jpg?fit=1200%2C799&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/07\/00ENSOblog_Bjerknes-feedback-ElNino_large-pichi-1536x1023-1.jpg?fit=1200%2C799&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":239643,"url":"https:\/\/climatescience.press\/?p=239643","url_meta":{"origin":441820,"position":4},"title":"Ian Plimer Asks, \u201eWhat Climate Crisis?\u201c","author":"uwe.roland.gross","date":"01\/14\/2023","format":false,"excerpt":"No past warming events have been driven by an increase in carbon dioxide in the atmosphere. No past cooling events were driven by a decrease in atmospheric carbon dioxide.","rel":"","context":"Similar post","block_context":{"text":"Similar post","link":""},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/01\/image-634.png?fit=1200%2C848&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/01\/image-634.png?fit=1200%2C848&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/01\/image-634.png?fit=1200%2C848&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/01\/image-634.png?fit=1200%2C848&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/01\/image-634.png?fit=1200%2C848&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":442009,"url":"https:\/\/climatescience.press\/?p=442009","url_meta":{"origin":441820,"position":5},"title":"Dust Storms: Hidden Drivers of Extreme Rainfall and Global Precipitation Shifts","author":"uwe.roland.gross","date":"04\/30\/2026","format":false,"excerpt":"Dust storm activity exhibits pronounced global variability characterized by strong regional contrasts and interdecadal oscillations rather than a uniform worldwide trend. Analyses spanning 1979\u20132023 using reanalysis datasets and ground observations reveal cycles of approximately 10\u201314 years in global dusty weather frequency, with a general decline from the late 1970s to\u2026","rel":"","context":"In \"Atlantic Multidecadal Oscillation (AMO)\"","block_context":{"text":"Atlantic Multidecadal Oscillation (AMO)","link":"https:\/\/climatescience.press\/?tag=atlantic-multidecadal-oscillation-amo"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Dust-Storms-Hidden-Drivers-of-Extreme-Rainfall-and-Global-Precipitation-Shifts.jpg?fit=784%2C1168&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Dust-Storms-Hidden-Drivers-of-Extreme-Rainfall-and-Global-Precipitation-Shifts.jpg?fit=784%2C1168&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Dust-Storms-Hidden-Drivers-of-Extreme-Rainfall-and-Global-Precipitation-Shifts.jpg?fit=784%2C1168&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/04\/0-Dust-Storms-Hidden-Drivers-of-Extreme-Rainfall-and-Global-Precipitation-Shifts.jpg?fit=784%2C1168&ssl=1&resize=700%2C400 2x"},"classes":[]}],"_links":{"self":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/441820","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/users\/121246920"}],"replies":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=441820"}],"version-history":[{"count":21,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/441820\/revisions"}],"predecessor-version":[{"id":441842,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/441820\/revisions\/441842"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/media\/441821"}],"wp:attachment":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=441820"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=441820"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=441820"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}