{"id":442941,"date":"2026-05-07T10:02:38","date_gmt":"2026-05-07T17:02:38","guid":{"rendered":"https:\/\/climatescience.press\/?p=442941"},"modified":"2026-05-07T15:19:24","modified_gmt":"2026-05-07T22:19:24","slug":"western-tibetan-vortex-drives-spring-warming-through-cloud-reduction-and-increased-sunshine","status":"publish","type":"post","link":"https:\/\/climatescience.press\/?p=442941","title":{"rendered":"Western Tibetan Vortex Drives Spring Warming Through Cloud Reduction and Increased Sunshine"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" width=\"723\" height=\"485\" data-attachment-id=\"442942\" data-permalink=\"https:\/\/climatescience.press\/?attachment_id=442942\" data-orig-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?fit=1168%2C784&amp;ssl=1\" data-orig-size=\"1168,784\" 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 Western Tibetan Vortex Drives Spring Warming Through Cloud Reduction and Increased Sunshine\" data-image-description=\"\" data-image-caption=\"\" data-large-file=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?fit=723%2C485&amp;ssl=1\" src=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?resize=723%2C485&#038;ssl=1\" alt=\"\" class=\"wp-image-442942\" srcset=\"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?resize=1024%2C687&amp;ssl=1 1024w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?resize=300%2C201&amp;ssl=1 300w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?resize=768%2C516&amp;ssl=1 768w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?resize=640%2C430&amp;ssl=1 640w, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?w=1168&amp;ssl=1 1168w\" sizes=\"auto, (max-width: 723px) 100vw, 723px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">The Tibetan Plateau, often called the \u201cThird Pole,\u201d experiences rapid warming that influences water resources, ecosystems, and weather patterns across Asia. While greenhouse gas forcing contributes to long-term trends, internal variability driven by atmospheric circulation patterns can dominate interannual and decadal fluctuations.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The <strong>Western Tibetan Vortex (WTV)<\/strong>, also linked to the<strong> Karakoram Zonal Index<\/strong>, is a large-scale circulation feature centered over the western TP. Previous studies identified its influence on temperature, snow cover, and precipitation. However, the precise radiative mechanisms connecting the WTV to surface warming remained underexplored. This study quantifies the radiative forcing pathway, emphasizing cloud modulation of shortwave radiation.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">A 2026 study (Wang et al.) published in Geophysical Research Letters, highlighted on sites like NoTricksZone and Watts Up With That.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The paper examines the <strong>Western Tibetan Vortex (WTV)<\/strong>, a dominant atmospheric circulation pattern over the western<strong> Tibetan Plateau (TP)<\/strong> and adjacent southwest Asia. It strongly influences springtime surface air temperature (T2m) variability in that region.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The study focuses on <strong>regional circulation-driven variability<\/strong> (especially spring), using surface energy balance diagnostics. It does not attribute global or long-term TP warming primarily to this, nor does it rule out other factors like greenhouse gases for broader trends. It highlights how natural atmospheric dynamics control cloudiness and thus surface solar input in this elevated, sensitive region.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Cloud Radiative Forcing (CRF)<\/strong>, also called <strong>Cloud Radiative Effect (CRE)<\/strong>, quantifies the impact of clouds on Earth&#8217;s energy balance by comparing the net radiative fluxes (energy entering\/leaving the system) under all-sky (cloudy + clear) conditions versus clear-sky (no clouds) conditions.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">It is typically calculated at the <strong>Top of the Atmosphere (TOA) <\/strong>but can also be evaluated at the <strong>surface<\/strong> (relevant to the Tibetan Plateau study). Data sources include satellites like <strong>ERBE, CERES, and GEWEX SRB<\/strong> (used in the Wang et al. 2026 paper).<\/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>Radiative Forcing of Western Tibetan Vortex on Surface Air Temperature in Spring<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>The paper &#8220;Radiative Forcing of Western Tibetan Vortex on Surface Air Temperature in Spring&#8221; by Jingzhi Wang et al. (2026, Geophysical Research Letters, DOI: 10.1029\/2025GL119603) is an open-access research letter.<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The paper examines the <strong>Western Tibetan Vortex (WTV)<\/strong>, a dominant atmospheric circulation pattern over the western <strong>Tibetan Plateau (TP)<\/strong> and adjacent southwest Asia. It strongly influences springtime<strong> surface air temperature (T2m) <\/strong>variability in that region.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Core Findings<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The Western <strong>Tibetan Vortex (WTV) <\/strong>is the dominant atmospheric circulation pattern over the western Tibetan Plateau (TP). It strongly controls springtime (MAM) 2 m <strong>surface air temperature (T2m)<\/strong> variability in the western TP and adjacent southwest Asia.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The WTV (measured via the Karakoram Zonal Index, KZI) explains<strong> ~66% of T2m variance<\/strong> (correlation R = 0.81) over the key region (roughly 26\u201336\u00b0N, 63\u201377\u00b0E).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Mechanism (surface energy balance diagnostics):<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Anticyclonic (positive) WTV phases<\/strong> \u2192 Reduced total cloud cover \u2192 Positive cloud radiative forcing (CRF) anomalies \u2192 Increased downward shortwave radiation (DSW) at the surface \u2192 Surface warming.<\/li>\n\n\n\n<li><strong>Cyclonic (negative) WTV phases<\/strong> \u2192 Increased cloud cover \u2192 Negative CRF anomalies \u2192 Decreased DSW \u2192 Cooling.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Downward shortwave radiation (DSW), modulated via clouds\/CRF, is the primary radiative driver. <\/strong>Longwave effects and other terms play lesser roles in this context. The study uses satellite observations (GEWEX SRB) combined with ERA5 and MERRA-2 reanalyses for robust verification, addressing known uncertainties in reanalysis radiation data over the TP.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Quantitative examples <\/strong>(from composites and related reporting):<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>An ~11% decline in total cloud cover (TCC) can yield ~7 W\/m\u00b2 more DSW, linked to substantial regional warming (e.g., ~1.87 K in one highlighted case).<\/li>\n\n\n\n<li>Anticyclonic events: ~7% TCC reduction, +4.4 W\/m\u00b2 DSW CRF contribution, +0.81 K warming (composites). Opposite for cyclonic phases.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Methods Highlights<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Data: <\/strong>GEWEX SRB satellite radiation (all-sky\/clear-sky for CRF), ERA5\/MERRA-2 for meteorology (1988\u20132009 overlap period).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Analysis:<\/strong> Correlations, composites of positive\/negative KZI events, surface energy balance (SEB) equation to link radiation anomalies to T2m\/Ts changes. CRF defined as the cloud-induced difference in fluxes.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Focus is on <strong>interannual variability <\/strong>in spring (when WTV is active with a distinct structure), not long-term trends or global attribution.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Context and Implications<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">This builds on prior work identifying the WTV&#8217;s role in circulation, snow cover, and temperatures. It provides observational support (satellite + reanalysis) for a circulation \u2192 cloud \u2192 shortwave radiation pathway, consistent with Li et al. (2022) theory but now quantified with independent radiation data.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">It illustrates how <strong>natural atmospheric dynamics <\/strong>(internal variability) can drive significant regional temperature fluctuations through cloud modulation and shortwave forcing. This aligns with broader evidence that clouds and shortwave radiation are critical (and uncertain) in the climate system\u2014small cloud cover changes produce large energy budget impacts. The TP warms rapidly overall, but this study highlights a key local\/regional control mechanism independent of uniform greenhouse gas forcing.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Caveats <\/strong>(from the paper&#8217;s scope):<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Regional and seasonal (spring variability focus).<\/li>\n\n\n\n<li>Does not negate other drivers of long-term TP warming (e.g., greenhouse gases, black carbon, elevation feedbacks, snow-albedo).<\/li>\n\n\n\n<li>Models often struggle with clouds and regional circulation details.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">The full paper is freely available on the AGU site (HTML and PDF). It includes figures showing spatial correlations, time series, composites, and SEB breakdowns\u2014highly recommended for details. This adds valuable observational evidence to debates on cloud\/shortwave roles in warming.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Published:<\/strong> Geophysical Research Letters<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>DOI:<\/strong> <a href=\"https:\/\/doi.org\/10.1029\/2025GL119603\">10.1029\/2025GL119603<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Authors:<\/strong> <a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/authored-by\/Wang\/Jingzhi\">Jingzhi Wang<\/a>,&nbsp;<a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/authored-by\/Li\/Xiao%E2%80%90Feng\">Xiao-Feng Li<\/a>,&nbsp;<a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/authored-by\/Wang\/Jing\">Jing Wang<\/a>,&nbsp;<a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/authored-by\/Yang\/Song\">Song Yang<\/a>,&nbsp;<a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/authored-by\/Fowler\/Hayley+J.\">Hayley J. Fowler<\/a><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><strong>Abstract<\/strong><\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">As the dominant atmospheric circulation pattern over the western Tibetan Plateau (TP), the Western Tibetan Vortex (WTV) exerts substantial control on springtime 2&nbsp;m surface air temperature (<em>T<\/em><sub>2m<\/sub>). However, its underlying radiative processes remain unclear. This study integrates GEWEX satellite observations with ERA5 and MERRA-2 reanalysis, applying surface energy balance diagnostics to quantify the WTV&#8217;s radiative forcing on&nbsp;<em>T<\/em><sub>2m<\/sub>&nbsp;variability. We find the WTV explains \u223c66% of&nbsp;<em>T<\/em><sub>2m<\/sub>&nbsp;variance (<em>R<\/em>&nbsp;=&nbsp;0.81) across the western TP and the adjacent Southwest Asia. Downward shortwave radiation (DSW) emerges as the primarily radiative factor modulated by the WTV via cloud radiative forcing (CRF) processes. Specifically, anticyclonic WTV events reduce cloudiness, generating positive CRF anomalies that enhancing surface DSW and cause warming. Conversely, cyclonic events increase cloudiness, producing negative CRF anomalies that diminish DSW and induce cooling. These findings advance understanding of the radiative processes by which the upper circulations modulate the surface climate over the TP.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The Tibetan Plateau, often called the \u201cThird Pole,\u201d experiences rapid warming that influences water resources, ecosystems, and weather patterns across Asia. While greenhouse gas forcing contributes to long-term trends, internal variability driven by atmospheric circulation patterns can dominate interannual and decadal fluctuations.<\/p>\n","protected":false},"author":121246920,"featured_media":442942,"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":[691842853,691842852,691842850,691842849,691820263,691823095,691842851],"class_list":["post-442941","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-cloud-and-circulation-dynamics","tag-cloud-feedback","tag-cloud-radiative-effect-cre","tag-cloud-radiative-forcing-crf","tag-shortwave-radiation","tag-top-of-the-atmosphere-toa","tag-western-tibetan-vortex-wtv","fallback-thumbnail"],"jetpack_publicize_connections":[],"jetpack_featured_media_url":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2026\/05\/0-Western-Tibetan-Vortex-Drives-Spring-Warming-Through-Cloud-Reduction-and-Increased-Sunshine.jpg?fit=1168%2C784&ssl=1","jetpack_likes_enabled":true,"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/paxLW1-1Red","jetpack-related-posts":[{"id":342979,"url":"https:\/\/climatescience.press\/?p=342979","url_meta":{"origin":442941,"position":0},"title":"Studies That \u2018Confirm\u2019 Humans Cause Climate Rely On Imaginary-World Conditions In Their Calculations","author":"uwe.roland.gross","date":"09\/14\/2024","format":false,"excerpt":"To claim that anthropogenic CO2 emissions drive global warming, radiative forcing modeling studies must assume 1) clouds do not ever change, 2) cloud albedo is constant, and\/or 3) clouds do not exist. None of these are real-world conditions.","rel":"","context":"In \"anthropogenic CO2\"","block_context":{"text":"anthropogenic CO2","link":"https:\/\/climatescience.press\/?tag=anthropogenic-co2"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/09\/0clouds-hd.jpg?fit=1200%2C675&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/09\/0clouds-hd.jpg?fit=1200%2C675&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/09\/0clouds-hd.jpg?fit=1200%2C675&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/09\/0clouds-hd.jpg?fit=1200%2C675&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/09\/0clouds-hd.jpg?fit=1200%2C675&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":384904,"url":"https:\/\/climatescience.press\/?p=384904","url_meta":{"origin":442941,"position":1},"title":"BOMBSHELL: Study Reveals Climate Warming Driven by Receding Cloud Cover","author":"uwe.roland.gross","date":"06\/25\/2025","format":false,"excerpt":"The recent paper by Tselioudis et al., titled \u201cContraction of the World\u2019s Storm-Cloud Zones the Primary Contributor to the 21st Century Increase in the Earth\u2019s Sunlight Absorption\u201d, is a fascinating\u2014and deeply problematic\u2014addition to the climate science canon. It offers yet another reminder that so-called \u201csettled science\u201d in climate modeling is\u2026","rel":"","context":"In \"climate modeling\"","block_context":{"text":"climate modeling","link":"https:\/\/climatescience.press\/?tag=climate-modeling"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/OIG1.1C.-1.jpeg?fit=1024%2C1024&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/OIG1.1C.-1.jpeg?fit=1024%2C1024&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/OIG1.1C.-1.jpeg?fit=1024%2C1024&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/OIG1.1C.-1.jpeg?fit=1024%2C1024&ssl=1&resize=700%2C400 2x"},"classes":[]},{"id":332619,"url":"https:\/\/climatescience.press\/?p=332619","url_meta":{"origin":442941,"position":2},"title":"How we know the sun changes the climate. III: Theories","author":"uwe.roland.gross","date":"06\/12\/2024","format":false,"excerpt":"Part I\u00a0in this series on the Sun and climate described how we know that the Sun has been responsible for some of the major climate changes that have occurred over the past 11,000 years. In\u00a0Part II, we considered a range of changes that the Sun is causing in the climate\u2026","rel":"","context":"In \"CO2\"","block_context":{"text":"CO2","link":"https:\/\/climatescience.press\/?tag=co2"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/06\/01868412.jpg?fit=1200%2C750&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/06\/01868412.jpg?fit=1200%2C750&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/06\/01868412.jpg?fit=1200%2C750&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/06\/01868412.jpg?fit=1200%2C750&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2024\/06\/01868412.jpg?fit=1200%2C750&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":382563,"url":"https:\/\/climatescience.press\/?p=382563","url_meta":{"origin":442941,"position":3},"title":"Our Atmospheric Heat\u00a0Engine","author":"uwe.roland.gross","date":"06\/10\/2025","format":false,"excerpt":"A previous post presented Michel Thizon\u2019s description of gravity\u2019s effect on the mass of air functioning as a climate thermostat. Some years ago, Dr. Murry Salby wrote in detail about the troposphere operating as a heat engine and the stratosphere as a refrigerator.","rel":"","context":"In \"Atmospheric physics\"","block_context":{"text":"Atmospheric physics","link":"https:\/\/climatescience.press\/?tag=atmospheric-physics"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/ChatGPT-Image-8.-Juni-2025-18_50_51.png?fit=1200%2C800&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/ChatGPT-Image-8.-Juni-2025-18_50_51.png?fit=1200%2C800&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/ChatGPT-Image-8.-Juni-2025-18_50_51.png?fit=1200%2C800&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/ChatGPT-Image-8.-Juni-2025-18_50_51.png?fit=1200%2C800&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/ChatGPT-Image-8.-Juni-2025-18_50_51.png?fit=1200%2C800&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":369299,"url":"https:\/\/climatescience.press\/?p=369299","url_meta":{"origin":442941,"position":4},"title":"Beyond CO\u2082: Unraveling the Roles of Energy, Water Vapor, and Convection in Earth\u2019s Atmosphere","author":"uwe.roland.gross","date":"03\/10\/2025","format":false,"excerpt":"Fundamentally the entire man-made CO2\u00a0global warming concept, boils down to the interaction of energy and matter in Earth\u2019s atmosphere.\u00a0The only reason that CO2\u00a0and other greenhouse gases (GHGs) are special is that they absorb most of the radiation emitted by Earth\u2019s surface. Water vapor absorbs across almost the entire emission spectrum\u2026","rel":"","context":"In \"Atmospheric temperature\"","block_context":{"text":"Atmospheric temperature","link":"https:\/\/climatescience.press\/?tag=atmospheric-temperature"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/03\/0view-edge-earth-atmosphere-layer.jpg?fit=1200%2C800&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/03\/0view-edge-earth-atmosphere-layer.jpg?fit=1200%2C800&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/03\/0view-edge-earth-atmosphere-layer.jpg?fit=1200%2C800&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/03\/0view-edge-earth-atmosphere-layer.jpg?fit=1200%2C800&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/03\/0view-edge-earth-atmosphere-layer.jpg?fit=1200%2C800&ssl=1&resize=1050%2C600 3x"},"classes":[]},{"id":383331,"url":"https:\/\/climatescience.press\/?p=383331","url_meta":{"origin":442941,"position":5},"title":"My Hypothesis Re-Emerges","author":"uwe.roland.gross","date":"06\/15\/2025","format":false,"excerpt":"I wanted to download all of my WUWT posts so I could make them into ebooks on various subjects. Of course, to do that I need to review some of my earliest posts. Bear in mind, this current analysis is the 1,051st post I\u2019ve put up on WUWT, so it\u2019s\u2026","rel":"","context":"In \"Clouds\"","block_context":{"text":"Clouds","link":"https:\/\/climatescience.press\/?tag=clouds"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0941728.jpg?fit=1200%2C800&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0941728.jpg?fit=1200%2C800&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0941728.jpg?fit=1200%2C800&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0941728.jpg?fit=1200%2C800&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/06\/0941728.jpg?fit=1200%2C800&ssl=1&resize=1050%2C600 3x"},"classes":[]}],"_links":{"self":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/442941","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=442941"}],"version-history":[{"count":21,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/442941\/revisions"}],"predecessor-version":[{"id":442963,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/442941\/revisions\/442963"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/media\/442942"}],"wp:attachment":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=442941"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=442941"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=442941"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}