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The Order Stream A Classification of the Rank of Streams and Rivers VideoStream Order Animation Die Fantasy-Teenie-Serie hatte durchaus ihre Fans. Schauspieler Jake Manley Jack Morton. Handicap Deutsch kannst "The Order" bei Broswergames im Abo streamen. Beschreibung Classic-stream-order.
Vera leads the Order in a spell to summon Rogwan, a powerful demon. But when her plan goes awry, she needs the Knights on her side.
Vera negotiates a deal with the Sons of Prometheus — a rival magic society — and sends Jack and Alyssa to their compound as hostages.
Amid a standoff with the Prometheans, Alyssa goes into withdrawal. Meanwhile, Randall, Hamish and Gabrielle track professor Foley.
The Knights weigh whether to join the Order. Alyssa suspects that her feelings for Jack might be blocking her magic. Kepler pulls rank on Vera.
The Knights try to prevent a strange affliction from spreading. Kepler schemes to strip Vera of her power, and Alyssa searches Vera's house.
Jack tries to broker a deal between Vera and Salvador. As chaos reigns, the Knights must convince Vera and Alyssa to work together to seal the eruption and save Lilith from the demon realm.
Call Netflix Netflix. Creators: Dennis Heaton. Watch all you want. Videos The Order. Season 2 Trailer: The Order. The Order: Season 1 Trailer 1.
Season 1 Recap: The Order. Episodes The Order. Season 1 Season 2. Release year: Hell Week: Part 1 51m. Hell Week: Part 2 47m. Introduction to Ethics: Part 1 49m.
It is, however, scale-dependent. The larger the map scale , the more orders of stream may be revealed. A general lower boundary for the definition of a "stream" may be set by defining its width at the mouth or, referencing a map, by limiting its extent.
The system itself is also applicable for other small-scale structures outside of hydrology. The Shreve system also gives the outermost tributaries the number "1".
Unlike the Strahler method, at a confluence the two numbers are added together. Shreve stream order is preferred in hydrodynamics : it sums the number of sources in each catchment above a stream gauge or outflow, and correlates roughly to the discharge volumes and pollution levels.
Like the Strahler method, it is dependent on the precision of the sources included, but less dependent on map scale. It can be made relatively scale-independent by using suitable normalization and is then largely independent of an exact knowledge of the upper and lower courses of an area.
Other systems include the Horton stream order, an early top down system devised by Robert E. Horton ,  and the topological stream order system, which is "a bottom up" system, and where the stream order number increases by one at every confluence.
Classical or topological ordering systems are assigned a dimensionless numerical order of "one", starting at the mouth of a stream, which is its lowest elevation point.
The vector order then increases as it traces upstream and converges with other smaller streams, resulting in a correlation of higher-order numbers to more highly-elevated headwaters.
Horton proposed to establish a reversal of that order. Horton's research report established a stream ordering method based on vector geometry.
In , Arthur Strahler proposed a modification to Horton's method. Both Horton's and Strahler's methods established the assignment of the lowest order, number 1, starting at the river's headwater, which is the highest elevation point.
Classical order number assignment correlates to height and elevation and traces upstream, but Horton and Strahler's stream ordering methods correlate to gravity flow and trace downstream.
Both Horton's and Strahler's stream ordering methods rely on principles of vector point-line geometry. Horton's and Strahler's rules form the basis of programming algorithms that interpret map data as queried by Geographic Information Systems.
The algorithm, developed in , uses vectors lines to represent the various streams and connects them using nodes the place on the map where the two vectors meet.
By using the different options available in ArcGIS, users can then change the line width or color to show the different stream orders. The result is a topologically correct depiction of the stream network that has a wide variety of applications.