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The Order Stream Navigation menu VideoStream Order Animation Klicke auf einen Zeitpunkt, Em Quali Gruppe H diese Version zu laden. Steve Bacic Malachai. Folgende Änderungen wurden vorgenommen: vectorized. Mathias Herndl. The classic stream order, also called Hack's stream order or Gravelius' stream order, is a "bottom up" hierarchy that allocates the number "1" to the river with its mouth at the sea (the main stem).Its tributaries are given a number one greater than that of the river or stream into which they discharge. So, for example, all immediate tributaries of the main stem are given the number "2".
But her new pledges prove hard to control. While the Knights look for ways to protect themselves, Alyssa gives Jack a job: find the "magic tourist" who's been wreaking havoc on campus.
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.
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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 classic use of stream order is in general hydrological cartography. Stream order systems are also important for the systematic mapping of a river system, enabling the clear labelling and ordering of streams.
The Strahler and Shreve methods are particularly valuable for the modelling and morphometric analysis of river systems, because they define each section of a river.
That allows the network to be separated at each gauge or outflow into upstream and downstream regimes, and for these points to be classified.
These systems are also used as a basis for modelling the water budget using storage models or time-related, precipitation-outflow models and the like.
In the GIS-based earth sciences these two models are used because they show the graphical extent of a river object. These are the streams that flow into and "feed" larger streams but do not normally have any water flowing into them.
Also, first- and second-order streams generally form on steep slopes and flow quickly until they slow down and meet the next order waterway. First- through third-order streams are also called headwater streams and constitute any waterways in the upper reaches of the watershed.
Going up in size and strength, streams that are classified as fourth- through sixth-order are medium streams, while anything larger up to 12th-order is considered a river.
For example, to compare the relative size of these different streams, the Ohio River in the United States is an eighth-order stream while the Mississippi River is a 10th-order stream.
Unlike the smaller order streams, these medium and large rivers are usually less steep and flow more slowly. They do however tend to have larger volumes of runoff and debris as it collects in them from the smaller waterways flowing into them.
If, however, two streams of different order join neither increases in order. For example, if a second-order stream joins a third-order stream, the second-order stream simply ends by flowing its contents into the third-order stream, which then maintains its place in the hierarchy.
Stream order also helps people like biogeographers and biologists in determining what types of life might be present in the waterway.