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API Documentation: https://therundown.docs.stoplight.io/ Real-time odds and scores from major sportsbooks. NFL, NBA, WNBA, MLB, NHL, NCAA Football, & NCAA Basketball with more sports soon. Over a dozen sportsbooks currently integrated: 5Dimes, Pinnacle, Matchbook, Betcris, Lowvig, TheGreek, YouWager, Justbet, Tigergaming, Betonline, Bookmaker, Sportsbetting, Intertops & more coming soon. Moneyline, Spread, & Total for full-games, 1st half, 2nd half, 1st Quarter/Period, 2nd Quarter/Period, 3rd Quarter/Period, and 4th Quarter/Period with more markets coming soon. See more at https://therundown.io/.
A better Face detection service! Provides coordinates for all faces detected and associated facial features such as eyes, nose, mouth, skin tone, and hair color. This API also returns several biometric features still in development to include gender, race, and age estimation.
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IPIX LMS provides companies and organizations with a technology-enhanced learning management solution that is compatible with every platform, allowing trainers to build and distribute courses, training programs, assessments, and other learning materials that suit their respective teaching styles and pace.
It consists of balls or irregular lumps of ice, each of which is called a hailstone. Ice pellets fall generally in cold weather while hail growth is greatly inhibited during cold surface temperatures. Unlike other forms of water ice such as graupel, which is made of rime, and ice pellets, which are smaller and translucent, hailstones usually measure between 5 mm (0.2 in) and 15 cm (6 in) in diameter. Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least 1 millimetre (0.039 in) thick, which are deposited upon the hailstone as it travels through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the updraft and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5 cm (1 in) and golf ball-sized (1.75 in). Hail is most common within continental interiors of the mid-latitudes, as hail formation is considerably more likely when the freezing level is below the altitude of 11,000 feet (3,400 m).Movement of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in. Accordingly, hail is less common in the tropics despite a much higher frequency of thunderstorms than in the mid-latitudes because the atmosphere over the tropics tends to be warmer over a much greater altitude. As hail stones are not perfect spheres it is difficult to calculate their speed accurately.Megacryometeors, large rocks of ice that are not associated with thunderstorms, are not officially recognized by the World Meteorological Organization as "hail," which are aggregations of ice associated with thunderstorms, and therefore records of extreme characteristics of megacryometeors are not given as hail records.
Hail Website Summary:
Welcome to the Hail Developer Centre. For the content that our customers create to be truly reusable and future-proofed, it needs to be accessible by anything at any time; not bound by our features and interfaces. Want to pull your Hail content through to your website, put your recent headlines up on your office TV, or even create an old-school print publication with your content? [...] We encourage the developer community to subscribe to our mailing list to receive updates on the API and other goings-on.