Appendix: A Appendix: B Appendix: C Appendix: D
Considerations For Developing Riparian Setbacks
Appendix A
REASONS to Establish Riparian SETBACKS:
PURPOSE OF Riparian Setbacks:
BENEFITS PROVIDED BY RIPARIAN AREAS:
USES THAT MAY BE ALLOWED IN RIPARIAN SETBACKS:
1. Without A Permit:
2. With A Permit:
USES THAT MAY BE PROHIBITED IN RIPARIAN SETBACKS:
ESTABLISHMENT OF DESIGNATED WATERCOURSES AND RIPARIAN SETBACKS:
Stream setback widths are based on stream processes that cause streams to adjust to their meander pattern and maintain dynamic stability (erosion = deposition). It best estimates the corridor in which stream meander migration is likely to occur over time and it provides a minimum level of protection for each streambank.
There are two methods for establishing setback widths. Both methods use the size of a stream’s drainage area to establish the dimensions of the setback. In the first method, fixed widths are assigned based on a drainage area range, while in the second method; an empirically derived equation is employed to calculate the setback area.
Two ordinances employing the fixed width method have been developed in Northeast Ohio, one by the Chagrin River Watershed Partners, Inc. and the other by Summit County. Either would be an excellent model to consider.
The Chagrin River Watershed Partners, Inc. Model:
1. Designated watercourses shall include those watercourses meeting any one of the following criteria:
2. Riparian setbacks on designated watercourses are established as follows:
3. The following conditions should apply in riparian setbacks:
1. An affected stream is defined as a surface watercourse with a well-defined bed and bank, either natural or artificial, which confines and conducts continuous or periodical flowing water in such a way that terrestrial vegetation cannot establish roots within the channel.
2. Widths of setbacks are measured as horizontal map distance outward from the ordinary high water mark on each side of a stream and are established as follows:
3. Where the 100-year floodplain is wider than the Riparian Setback on either or both sides of the stream, the Riparian Setback should be extended to the outer edge of the 100-year floodplain.
4. Because the gradient of the riparian corridor significantly influences impacts on the stream, the following adjustment for steep slopes will be integrated into the Riparian Setback formulae for width determination:
|
Average Percent Slope |
Width of Setback |
|
15% - 20% |
Add 25 feet |
|
21% - 25% |
Add 50 feet |
|
> 25% |
Add 100 feet |
The setback area width is a total width, which crosses the channel and is calculated according to the drainage area (miles2) of the stream using the following equation:
Setback Area Width = 129 Drainage Area0.43
1. When calculating the setback width:
2. If there are wetlands or floodplains on the site, the setback area should ideally be expanded from the minimum width calculated to include these and associated buffer areas, since they provide hydrologic and other benefits.
3. Locate the setback area by placing the centerline of the area over the centerline of the watercourse. Move the area based on the site topography and changes in stream and valley direction.
The map on the following page shows the main streams running through Seville:
Chippewa Creek (Ch), Hubbard Creek (Hb), and 4 unnamed streams that will be referred to as streams A, B, C and D.
The drainage areas of these streams have been calculated up to each of the labeled dots. Table “1” compares of the setback widths determined by each of the 3 models.

|
Stream Point |
Drainage Area (sq mi) |
Setback Width in Feet |
||
|
Chagrin Model |
Summit Model |
Calculated |
||
|
on both sides of watercourse |
from high water mark on each side |
total width across channel |
||
|
Chippewa 1 |
45.7 |
120 |
100 |
667 |
|
Chippewa 2 |
36.9 |
120 |
100 |
609 |
|
Chippewa 3 |
36.4 |
120 |
100 |
605 |
|
Chippewa 4 |
35.7 |
120 |
100 |
600 |
|
Hubbard 1 |
8.4 |
75 |
75 |
322 |
|
Hubbard 2 |
8.2 |
75 |
75 |
319 |
|
A |
0.23 |
25 |
50 |
69 |
|
B1 |
0.64 |
75 |
75 |
106 |
|
B2 |
0.45 |
25 |
50 |
92 |
|
B3 |
0.26 |
25 |
50 |
72 |
|
B4 |
0.12 |
25 |
50 |
52 |
|
C1 |
0.86 |
75 |
75 |
121 |
|
C2 |
0.73 |
75 |
75 |
113 |
|
D1 |
0.23 |
25 |
50 |
69 |
|
D2 |
0.11 |
25 |
50 |
50 |
Appendix: A Appendix: B Appendix: C Appendix: D