Commands
10
Queries
22.14 ms
Query time
0
Failed Queries
| # | Time | Connection | Command |
|---|---|---|---|
| 1 | 0.53 ms | cache | CONNECT redis.internal 6379 5 <null> 5 5 |
| 2 | 0.29 ms | cache | SELECT 0 |
| 3 | 0.20 ms | cache | MGET wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=www |
| 4 | 0.52 ms | cache | INFO Memory |
| 5 | 0.02 ms | cache | MULTI 2 |
| 6 | 0.09 ms | cache | SETEX wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=www 2678399 ��L �_ 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:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/378-6545f33eaabf9231597235.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/378-6545f33eaabf9231597235.webp";s:5:"title";s:153:"https://www.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's atmosphere is divided by scientists into 5 theoretical layers:</p> <ul> <li>The <strong>Troposphere</strong> contains 80% of the 5 trillion tons of air! In direct contact with and heated by the ground, this layer of air is where the important thermal exchanges responsible for meteorological 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. In absorbing this energy, they increase in temperature and ionize. This is the ionosphere. This part of the Thermosphere has important electromagnetic properties. 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. The majority of satellites are 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:890;s:5:"title";s:35:"Interactive Earth: Oceanic currents";s:4:"slug";s:34:"interactive-earth-oceanic-currents";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/890-6545f466c09f1737431820.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/890-6545f466c09f1737431820.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/890-6545f466c09f1737431820.webp";}s:19:"thumbnailBackground";s:7:"#00a751";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2017-09-12 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:416:"<ul> <li>To know and locate the main oceanic currents.</li> <li>To describe the influence of oceanic currents on climate.</li> <li>To introduce some important concepts such as density, salinity, oceanic gyres, deep currents, etc.</li> <li>To offer an overview of the marine dynamics of our planet.</li> <li>To discuss the effects of human activity on the oceans and the risks of global warming.</li> </ul>";}i:1;a:9:{s:2:"id";i:842;s:5:"title";s:19:"4 seasons in a year";s:4:"slug";s:19:"4-seasons-in-a-year";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/842-6545f45e4c608863883364.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/842-6545f45e4c608863883364.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/842-6545f45e4c608863883364.webp";}s:19:"thumbnailBackground";s:7:"#413994";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2016-05-29 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:515:"<ul> <li>To observe the effect of the seasons on the vegetation throughout the year.</li> <li>To understand that there is a 6-month shift in seasons between the northern and the southern hemisphere.</li> <li>To study the life cycle of living beings according to the seasons (germination of seed plants, reproduction cycle, ...).</li> </ul> <p>"The seasons" from Italian painter Giuseppe Arcimbolodo is an interesting approach on the subject: https://en.wikipedia.org/wiki/Giuseppe_Arcimboldo</p>";}i:2;a:9:{s:2:"id";i:286;s:5:"title";s:25:"Weight / Mass on the Moon";s:4:"slug";s:23:"weight-mass-on-the-moon";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/286-6545f308c8283788141644.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/286-6545f308c8283788141644.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/286-6545f308c8283788141644.webp";}s:19:"thumbnailBackground";s:7:"#b51d8e";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2025-05-01 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:226:"<ul> <li>To distinguish between the weight (Intensity of the force in N) and the mass of a body (Fundamental property in kg).</li> <li>To simulate the influence of the gravitational constant on the weight.</li> </ul>";}i:3;a:9:{s:2:"id";i:661;s:5:"title";s:31:"Emission and absorption spectra";s:4:"slug";s:31:"emission-and-absorption-spectra";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/661-6545f3f6542b7006188991.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/661-6545f3f6542b7006188991.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/661-6545f3f6542b7006188991.webp";}s:19:"thumbnailBackground";s:7:"#462f92";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:313:"<ul> <li>To distinguish between absorption spectra and emission spectra.</li> <li>To characterize an atom by its light spectrum and to introduce spectroscopy.</li> <li>To understand that the spectral emission lines of an element have the same frequencies as the lines of the absorption spectrum.</li> </ul>";}i:4;a:9:{s:2:"id";i:891;s:5:"title";s:27:"Interactive Earth: Climates";s:4:"slug";s:26:"interactive-earth-climates";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/891-6545f46754731332555945.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/891-6545f46754731332555945.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/891-6545f46754731332555945.webp";}s:19:"thumbnailBackground";s:7:"#f487b9";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2017-09-27 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:241:"<ul> <li>To illustrate the distribution of all the climates on Earth.</li> <li>To make hypotheses about the link between the climate of a region and its latitude.</li> <li>To address the effects and risks of global warming.</li> </ul>";}i:5;a:9:{s:2:"id";i:377;s:5:"title";s:23:"Landscapes and climates";s:4:"slug";s:23:"landscapes-and-climates";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/377-6545f33e1de44389596892.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/377-6545f33e1de44389596892.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/377-6545f33e1de44389596892.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";s:545:"<ul> <li>To identify the major types of climates on Earth and to know how to locate them on a map.</li> <li>To list the factors that determine a climate.</li> <li>To explain seasonal variations for the same region. One could use annual temperature and precipitation curves taken from specific locations.</li> <li>To make the distinction between Climate (a study of averages, on a global scale) and weather (values that are nearly instantaneous, and local).</li> <li>To introduce the risks involved in climate changes.</li> </ul>";}}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:33:"Environmental science and Ecology";} |
| 7 | 0.03 ms | cache | SADD wJo3GJ9dRH:tagscache-service wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=www |
| 8 | 0.02 ms | cache | SADD wJo3GJ9dRH:tagscache-service-data > anonymous-media wJo3GJ9dRH:data > anonymous-media > id=2559,locale=en,domain=www |
| 9 | 19.56 ms | cache | EXEC |
| 10 | 0.89 ms | cache | MGET wJo3GJ9dRH:data > locale-page-groups > locale=en |