[{"data":1,"prerenderedAt":76},["ShallowReactive",2],{"category-page:\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean":3},{"category":4,"seo":11,"breadcrumbs":16,"childCategories":23,"topicPreview":24,"topicCount":62},{"path":5,"title":6,"description":7,"shortDescription":8,"parentPath":9,"accentToken":10},"\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean","大気と海洋","大気の層構造、地球の熱収支、大気と海洋の大循環、深層循環を扱うカテゴリです。","大気・海洋と地球規模の熱輸送を見る","\u002Fhigh-school\u002Fbasic-earth-science","signal-blue",{"title":12,"description":13,"canonicalUrl":14,"ogImage":15},"大気と海洋 | 地学基礎 学習カテゴリ | Zeqnilo","高校地学基礎の大気構造、熱収支、大気循環、海洋循環を短い学習ページで整理します。","https:\u002F\u002Fzeqnilo.com\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean","https:\u002F\u002Fzeqnilo.com\u002Fassets\u002Fsite\u002Fdefault-og.svg",[17,20,22],{"title":18,"path":19},"高校","\u002Fhigh-school",{"title":21,"path":9},"地学基礎",{"title":6,"path":5},[],[25,39,48,57,67],{"id":26,"title":27,"summary":28,"canonicalPath":29,"categoryPath":5,"categoryTitle":6,"difficulty":30,"targetAudience":31,"estimatedMinutes":32,"publishedAt":33,"updatedAt":33,"reviewStatus":34,"tags":35},"high-school-basic-earth-science-atmosphere-and-ocean-atmospheric-layers-and-vertical-profile","大気の層構造と気温・気圧の鉛直変化","高度に伴う気圧・気温の変化をグラフから読み、対流圏・成層圏・中間圏・熱圏を区分して、雲・オゾン・流星などの現象を対応させます。","\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Fatmospheric-layers-and-vertical-profile","beginner","student_high",6,"2026-07-28","ai_generated",[21,6,36,37,38],"大気の層構造","気圧は高度とともに低下","対流圏は気温低下",{"id":40,"title":41,"summary":42,"canonicalPath":43,"categoryPath":5,"categoryTitle":6,"difficulty":30,"targetAudience":31,"estimatedMinutes":32,"publishedAt":33,"updatedAt":33,"reviewStatus":34,"tags":44},"high-school-basic-earth-science-atmosphere-and-ocean-radiation-budget-albedo-and-greenhouse","地球の放射収支・アルベド・温室効果","太陽放射の受熱、反射、地球放射の放熱を整理し、温室効果が地表温度を保つ仕組みを学びます。","\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Fradiation-budget-albedo-and-greenhouse",[21,6,45,46,47],"地球の放射収支","太陽放射の一部は反射","アルベドは反射割合",{"id":49,"title":50,"summary":51,"canonicalPath":52,"categoryPath":5,"categoryTitle":6,"difficulty":30,"targetAudience":31,"estimatedMinutes":32,"publishedAt":33,"updatedAt":33,"reviewStatus":34,"tags":53},"high-school-basic-earth-science-atmosphere-and-ocean-latitudinal-heat-imbalance-and-atmospheric-circulation","緯度別の熱収支と大気大循環","緯度による受熱量の違いから、ハドレー循環、貿易風、偏西風と熱輸送を関連付けます。","\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Flatitudinal-heat-imbalance-and-atmospheric-circulation",[21,6,54,55,56],"大気大循環","低緯度は受熱が大きい","高緯度は放熱が相対的に大きい",{"id":58,"title":59,"summary":60,"canonicalPath":61,"categoryPath":5,"categoryTitle":6,"difficulty":30,"targetAudience":31,"estimatedMinutes":62,"publishedAt":33,"updatedAt":33,"reviewStatus":34,"tags":63},"high-school-basic-earth-science-atmosphere-and-ocean-surface-ocean-currents-and-heat-transport","表層海流と熱輸送","海面近くの海流を暖流・寒流に分け、大気とともに低緯度から高緯度へ熱を運ぶ働きを整理します。","\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Fsurface-ocean-currents-and-heat-transport",5,[21,6,64,65,66],"表層海流","暖流は低緯度側から","寒流は高緯度側から",{"id":68,"title":69,"summary":70,"canonicalPath":71,"categoryPath":5,"categoryTitle":6,"difficulty":30,"targetAudience":31,"estimatedMinutes":32,"publishedAt":33,"updatedAt":33,"reviewStatus":34,"tags":72},"high-school-basic-earth-science-atmosphere-and-ocean-ocean-layering-and-deep-circulation","海洋の層構造と深層循環","海洋を表層、水温躍層、深層に分け、沈み込みと湧昇が深層までつなぐ循環を整理します。","\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Focean-layering-and-deep-circulation",[21,6,73,74,75],"海洋の層構造","表層は風で混合","水温躍層で急低下",1785565313729]