GET https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/en/media/378-atmosphere

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3 0.45 ms cache MGET wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=junior
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6 0.15 ms cache SETEX wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=junior 2678399 �5�A�_Oa:2:{i:0;s:13:"cache-service";i:1;s:36:"cache-service-data > anonymous-media";}a:15:{s:2:"id";i:378;s:5:"title";s:10:"Atmosphere";s:4:"slug";s:10:"atmosphere";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/378-6545f33eaabf9231597235.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/378-6545f33eaabf9231597235.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/378-6545f33eaabf9231597235.webp";}s:19:"thumbnailBackground";s:7:"#004387";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:391:"<ul> <li>To illustrate the scale of sizes (knowing that, in this animation, correct proportions are not always respected)</li> <li>To define the Standard Atmosphere (ISA)</li> <li>To become aware that the portion of the atmosphere that concerns us is only a very thin layer at the scale of the planet.</li> <li>To introduce the composition and the function of each layer.</li> </ul>";s:5:"width";i:550;s:6:"height";i:440;s:11:"description";s:1582:"<p>An atmosphere is a layer of gas that surrounds a planet.</p> <p>The Earth&#39;s atmosphere is divided by scientists into&nbsp; 5 &nbsp;theoretical layers:</p> <ul> <li>The <strong>Troposphere</strong> contains 80% of the 5 trillion tons of air!&nbsp;In direct contact with and heated by the ground, this layer of air is where the important thermal exchanges responsible for meteorological&nbsp; phenomena take place.</li> <li>In the<strong> Stratosphere</strong>, the temperature gets higher as altitude increases. This temperature inversion acts as a limit for clouds. It is here that we fiind the Ozone Layer that filters out a large part of the ultraviolet radiation coming from the Sun.</li> <li>In the <strong>Mesosphere</strong>, the temperature once again begins to drop.</li> <li>Those rare particles still present in the<strong> Thermosphere </strong>interact with solar radiation.&nbsp;In absorbing this energy, they increase in temperature and ionize. This is the ionosphere. This part of the Thermosphere has important electromagnetic properties.&nbsp; The International Space Station (ISS) is in orbit in the thermosphere, beyond the ionosphere.</li> <li>Particles are so rare in the <strong>Exosphere</strong> that the probability of collisions among them is negligible. Some even escape the gravitational attraction of the Earth. Although the boundary is not clearly defined, the exosphere marks the beginning of outer space.&nbsp;The majority of satellites are&nbsp;orbiting in the exosphere, at altitudes between 800 km and 36,000 km.</li> </ul>";s:11:"suggestions";a:6:{i:0;a:9:{s:2:"id";i:693;s:5:"title";s:7:"Wegener";s:4:"slug";s:7:"wegener";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";}s:19:"thumbnailBackground";s:7:"#b51d8e";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:399:"<ul> <li>To discover the clues that enabled Alfred Wegener to announce his theory of continental drift.</li> <li>To compare Wegener&rsquo;s hypotheses and those of his detractors of the time (fixism, catastrophism).</li> <li>To complete Wegener&rsquo;s hypotheses in the light of more recent discoveries (topography of the ocean bottoms, geomagnetism, thermal sources, earthquakes)</li> </ul>";}i:1;a:9:{s:2:"id";i:685;s:5:"title";s:17:"Greenhouse effect";s:4:"slug";s:17:"greenhouse-effect";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/685-6545f40743108734012587.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/685-6545f40743108734012587.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/685-6545f40743108734012587.webp";}s:19:"thumbnailBackground";s:7:"#ee1b2e";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:1101:"<ul> <li>To insist that the Greenhouse Effect is a natural phenomenon that has allowed the appearance of Life on Earth.</li> <li>To distinguish the electromagnetic characteristics of radiations. Those from the Sun are primarily in the high infrared, the visible and the near ultraviolet. Those emitted by the Earth are in the low infrared. Molecules of greenhouse gases are little affected by the former.</li> <li>To mention the certitude of climate change resulting from the release of greenhouse gases. (Source: Work done by The Intergovernmental Panel on Climate Change (IPCC) between 1990 and 1997 (Kyoto). To also recognize the uncertainty about the extent and the rapidity of the changes.</li> <li>To remind people of the call of the Kyoto Protocol: 170 countries have agreed to, by 2012, reduce greenhouse gas emissions to levels 5% lower than those existing in 1990. In the he Paris agreement (12 December 2015)&nbsp;all countries agreed to work to limit global temperature rise to well below 2 degrees Celsius, and given the grave risks, to strive for 1.5 degrees Celsius.</li> </ul>";}i:2;a:9:{s:2:"id";i:436;s:5:"title";s:8:"Air pump";s:4:"slug";s:8:"air-pump";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/436-6545f360d0290702689689.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/436-6545f360d0290702689689.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/436-6545f360d0290702689689.webp";}s:19:"thumbnailBackground";s:7:"#f6951d";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:170:"<ul> <li>Illustrate the relationship between pressure and number of molecules.</li> <li>Observe how a gas behaves when it is confined to a certain volume.</li> </ul>";}i:3;a:9:{s:2:"id";i:462;s:5:"title";s:23:"The structure of matter";s:4:"slug";s:23:"the-structure-of-matter";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/462-6545f37056ce0635838598.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/462-6545f37056ce0635838598.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/462-6545f37056ce0635838598.webp";}s:19:"thumbnailBackground";s:7:"#f6951d";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:138:"<ul> <li>To get a simplified view of the structure of matter.</li> <li>To define each of the basic constituents of matter.</li> </ul>";}i:4;a:9:{s:2:"id";i:455;s:5:"title";s:21:"Quiz Earth's interior";s:4:"slug";s:21:"quiz-earth-s-interior";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/455-6545f36c30024678394952.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/455-6545f36c30024678394952.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/455-6545f36c30024678394952.webp";}s:19:"thumbnailBackground";s:7:"#00a751";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:152:"<ul> <li>Review the knowledge on the internal structure of the Earth.</li> <li>Review certain aspects of the theory of plate techtonics.</li> </ul>";}i:5;a:9:{s:2:"id";i:801;s:5:"title";s:19:"Video: Biodiversity";s:4:"slug";s:18:"video-biodiversity";s:9:"mediaType";s:5:"video";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/801-6545f44ade474006787636.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/801-6545f44ade474006787636.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/801-6545f44ade474006787636.webp";}s:19:"thumbnailBackground";s:7:"#00b7ad";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";N;}}s:4:"tags";a:12:{i:0;s:3:"air";i:1;s:8:"aircraft";i:2;s:8:"aviation";i:3;s:7:"climate";i:4;s:5:"cloud";i:5;s:3:"iss";i:6;s:8:"pressure";i:7;s:5:"space";i:8;s:12:"stratosphere";i:9;s:11:"temperature";i:10;s:11:"troposphere";i:11;s:7:"weather";}s:12:"baseNodeName";s:27:"Earth science and astronomy";}
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