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Hydrological Modeling. Overview Introduction Watershed delineation Automatic delineation Flow length.

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Presentation on theme: "Hydrological Modeling. Overview Introduction Watershed delineation Automatic delineation Flow length."— Presentation transcript:

1 Hydrological Modeling

2 Overview Introduction Watershed delineation Automatic delineation Flow length

3 Introduction

4 Watershed management

5 Definition of watershed “The region draining into a river, river system, or body of water” -American Heritage Dictionary The upstream area of any given point on the landscape Physically defined by drainage point and upstream area Also known as basin, sub-basin, catchment, and contributing area

6

7

8 Watershed delineation

9 How it works Water always flows downhill For any point on a grid representing a landscape, a drop of water can be traced downhill  direction of flow is known for every DEM cell For any point on a grid representing a landscape, a flow pathway can be traced back uphill  flow accumulation is known for every DEM cell Uphill back-tracing proceeds to a ridgeline or to the edge of the grid Termination of uphill back-tracing defines watershed boundary

10 Watershed delineation Steps (with ArcToolbox): 1.Create a depressionless DEM 2.Calculate flow direction 3.Calculate flow accumulation 4.Create watershed Pour points 5.Delineate watersheds

11 1. Creating a depressionless DEM DEM must eventually drain off edge of grid Areas of internal drainage will result in unprocessed areas FILL routine fills in sinks or cuts off peaks creating a new grid with no drainage errors elevation

12 2. Flow direction Every cell flows into another cell or off the grid edge Flow direction is calculated as the direction of steepest downward descent Flow direction is calculated for each cell, resulting in a new grid theme

13 2. Flow direction flow moves out of a cell in one of 8 directions direction of flow is saved as a code number

14 2. Flow direction north-flowing cells coded as 64

15 2. Flow direction Flow direction grid

16 3. Flow accumulation Each cell has been coded for direction of flow Cumulative flow is calculated from flow direction Output grid is created where values are the number of upstream cells Lower accumulation values are ridge tops Higher accumulation values are valleys & stream channels

17 3. Flow accumulation 1 3 5

18

19 single class legend shows high flow cells 3. Flow accumulation

20 Fit depends on accuracy of the DEM and stream layers 3. Flow accumulation

21 4. Watershed “Pour points” Watersheds are defined by outlets (pour points) Pour points should be placed in high-flow pathways Basins will be generated from pour point to ridgeline or to upstream sub-basin Pour points should be numerically coded per sub-basin Pour points must be converted to a grid layer

22 4. Watershed Pour points Zoom in to place pour point in center of high-flow cell Create as many pour points as necessary

23 5. Delineating watersheds Preliminary steps are completed –Filled DEM –Flow direction –Flow accumulation –Pour points created & converted to grid Run tool to create watersheds

24 5. Delineating watersheds Watersheds represent area upstream from Pour points and terminate at ridgelines, uphill sub- basin boundary, or edge of the grid

25 5. Delineating watersheds

26 Automatic delineation

27 Pour points automatically selected by “intersection” of highest-flow pathways and grid edge

28 Automatic delineation

29 Flow length

30 Flow distance for every cell to outlet

31 Flow length Flow distance for every cell to closest stream

32 Flow length Euclidean distance vs. flow distance

33 Homework Read: Hydrological Modeling & Watershed Delineation, Map Layouts Study for the exam Presentations: 3/5 Luke, Jennifer, Josh 3/7 Chris, Prati, Carolyn


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