{"slip": { "id": 103, "advice": "Respect your elders."}}
{"type":"standard","title":"Madden–Julian oscillation","displaytitle":"Madden–Julian oscillation","namespace":{"id":0,"text":""},"wikibase_item":"Q1170041","titles":{"canonical":"Madden–Julian_oscillation","normalized":"Madden–Julian oscillation","display":"Madden–Julian oscillation"},"pageid":1666522,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/8/8d/MJO_5-day_running_mean_through_1_Oct_2006.png/330px-MJO_5-day_running_mean_through_1_Oct_2006.png","width":320,"height":320},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/8/8d/MJO_5-day_running_mean_through_1_Oct_2006.png","width":700,"height":700},"lang":"en","dir":"ltr","revision":"1233582272","tid":"f9178e3d-3e36-11ef-85ec-3d2fd6932221","timestamp":"2024-07-09T21:05:30Z","description":"Tropical atmosphere element of variability","description_source":"local","content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Madden%E2%80%93Julian_oscillation","revisions":"https://en.wikipedia.org/wiki/Madden%E2%80%93Julian_oscillation?action=history","edit":"https://en.wikipedia.org/wiki/Madden%E2%80%93Julian_oscillation?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Madden%E2%80%93Julian_oscillation"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Madden%E2%80%93Julian_oscillation","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Madden%E2%80%93Julian_oscillation","edit":"https://en.m.wikipedia.org/wiki/Madden%E2%80%93Julian_oscillation?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Madden%E2%80%93Julian_oscillation"}},"extract":"The Madden–Julian oscillation (MJO) is the largest element of the intraseasonal variability in the tropical atmosphere. It was discovered in 1971 by Roland Madden and Paul Julian of the American National Center for Atmospheric Research (NCAR). It is a large-scale coupling between atmospheric circulation and tropical deep atmospheric convection. Unlike a standing pattern like the El Niño–Southern Oscillation (ENSO), the Madden–Julian oscillation is a traveling pattern that propagates eastward, at approximately 4 to 8 m/s, through the atmosphere above the warm parts of the Indian and Pacific oceans. This overall circulation pattern manifests itself most clearly as anomalous rainfall.","extract_html":"
The Madden–Julian oscillation (MJO) is the largest element of the intraseasonal variability in the tropical atmosphere. It was discovered in 1971 by Roland Madden and Paul Julian of the American National Center for Atmospheric Research (NCAR). It is a large-scale coupling between atmospheric circulation and tropical deep atmospheric convection. Unlike a standing pattern like the El Niño–Southern Oscillation (ENSO), the Madden–Julian oscillation is a traveling pattern that propagates eastward, at approximately 4 to 8 m/s, through the atmosphere above the warm parts of the Indian and Pacific oceans. This overall circulation pattern manifests itself most clearly as anomalous rainfall.
"}{"slip": { "id": 102, "advice": "Tell it like it is."}}
{"fact":"Lions are the only cats that live in groups, called prides. Every female within the pride is usually related.","length":109}
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{"fact":"Jaguars are the only big cats that don't roar.","length":46}
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