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高校地学基礎を初学者向けに解説します。","https:\u002F\u002Fzeqnilo.com\u002Fhigh-school\u002Fbasic-earth-science\u002Fatmosphere-and-ocean\u002Fsurface-ocean-currents-and-heat-transport","https:\u002F\u002Fzeqnilo.com\u002Fassets\u002Fsite\u002Fdefault-og.svg",[138,141,142,143],{"title":139,"path":140},"高校","\u002Fhigh-school",{"title":17,"path":130},{"title":18,"path":10},{"title":7,"path":9},[145],{"id":146,"title":147,"summary":148,"canonicalPath":149,"categoryPath":10,"categoryTitle":18,"difficulty":11,"targetAudience":12,"estimatedMinutes":150,"publishedAt":14,"updatedAt":14,"reviewStatus":15,"tags":151},"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",6,[17,18,152,153,154],"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",[156],{"id":123,"title":157,"summary":158,"canonicalPath":159,"categoryPath":10,"categoryTitle":18,"difficulty":11,"targetAudience":12,"estimatedMinutes":150,"publishedAt":14,"updatedAt":14,"reviewStatus":15,"tags":160},"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",[17,18,161,125,126],"海洋の層構造",[],1785565317587]