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The Order Stream A Classification of the Rank of Streams and Rivers Video1- What is Stream Order?
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. Share Flipboard Email. Amanda Briney.
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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.
Research activity following Strahler's report has focused on solving some challenges when converting two-dimensional maps into three-dimensional vector models.