11  Level-3 Planform Analysis

๐Ÿ”ด Advanced

The purpose of this SOP is to demonstrate the workflow of fluvial geomorphology (fluvgeo) rapid watershed assessment in ArcGIS Pro. This approach uses a suite of planning analysis tools to rapidly assess and identify sediment sources, pathways, and sinks for watershed analysis. Level 1 is to extract basic channel dimensions. This stage develops terrain, defines the stream reach, creates cross sections and identifies features along the reach. The output is a report of the dimensions for each cross section on a reach.

Application and Data Setup

๐Ÿ”ง Practical

Applications

Level-2 Data

  1. Sites must have had up through Level-2 analysis run. That data is essential to completing Level_3 analysis.
  2. Software application and tools from Level-1 will be needed for Level-3 analysis.

Data access in ArcGIS Pro

  1. Fluvgeo toolbox requires the use of a mapped drive for accessing the data in ArcGIS Pro. UNC connection will create errors with some of the Fluvgeo tools.
  2. Create a mapped drive and use that connection in ArcCatalog.

Analysis Workflow

๐Ÿ”ง Practical

Define Valley Line

Develop Candidate Valleylines

The following steps are performed in the site geodatabase for the base year. This is done to ensure that a valleyline feature class is created smoothly through all of the reaches in a site.

  1. Use the flowline to determine the valley line for the reach.
  2. Open the ESRI ๐Ÿ› ๏ธ Smooth Line tool to smooth the reach ๐Ÿ—บ๏ธ flowline feature class from the most recent year as the input feature.
  3. For the first candidate valleyline, use a ๐Ÿ“Š Smoothing Tolarance value of ๐Ÿงฎ 200 meters. In this case you would name the output feature class valleyline_200 and put in the same feature dataset.
NoteWhat Smoothing Tolerance Value?

It depends! See Tech Manual for discussion on determining planform scale.

  1. Choose the ๐Ÿงฎ PAEK smoothing algorithm.
  2. Set the ๐Ÿ“Š smooth tolerance to ๐Ÿงฎ 200
  3. Click Run.
    1. Repeat the previous step using the ๐Ÿ“Š Smoothing Tolerance values such as ๐Ÿงฎ 400, ๐Ÿงฎ 800, and ๐Ÿงฎ 1000.
    2. Depending on the detail of the ๐Ÿ—บ๏ธ flowline feature class geometry, you may need to select a different range or set of step values of the ๐Ÿ“Š Smoothing Tolerance parameter values to evaluate.
  4. The goal is to create a wide degree of flowline smoothing in the candidate valleyline feature classes to select from in the next step.
  5. Choose Final ๐Ÿ—บ๏ธ Valleyline feature class.
  6. Add the ๐Ÿ—บ๏ธ floodplain polygon (higher bank_raw_###) and all of the candidate ๐Ÿ—บ๏ธ valleyline feature classes to the current map.
  7. Identify the ๐Ÿ—บ๏ธ valleyline feature class that has the highest smoothing tolerance value that also is mostly contained within the extent of the ๐Ÿ—บ๏ธ floodplain polygon feature class.

Valleyline Buffer

The valleyline should be considered a fuzzy area representing the center of the valley.

  1. Add the ๐Ÿ—บ๏ธ valleyline feature class as the input.
  2. Add the output multi-ring buffer to the newest year gdb. Name it ๐Ÿ—บ๏ธ multiring_buffer feature class.
  3. Use the identifies valleyline to create a multi-ring buffer. Use the the distance at a narrow part of the reach as the first buffer distance. The following increments can be set 5, 10, or desired distances. Create 3 to 5 rings.
  4. Leave the remaining settings as the defaults.
  5. Hit Run.
  6. Add the bankline layer to the map.
  7. Identify the buffer ring that best shows the baklines looping out of the buffer ring from side to side. The chosen ring should show the loops at a smaller scale.
NoteScale and distance to use to define valleyline buffers!

It depends on your reach! See Tech Manual for discussion on determining planform scale.

  1. Select and export the chosen buffer ring as new layer in the gdb.
  2. In the site geodatabase of the base year, rename the selected buffer ring to distance_buffer_year. Ex. 20ft_buffer_2012
  3. Delete the multi-ring buffer feature classes from the site geodatabase of the base year.
  4. Copy the selected distance buffer feature class you just created from the site geodatabase to each of the base year reach geodatabases.

Define Meander Loops

The stage defines meander loops and bends for the base year for each reach.

Define Loop Points Layer

  1. Create a new point feature class named ๐Ÿ—บ๏ธ loop_points feature class. ๐Ÿ“Š Enable ๐Ÿงฎ z and m values. The feature class should contain the following fields:
    1. ๐Ÿ“Š ReachName: ๐Ÿงฎ Text (50) - The purpose of this field is to store the reach name.
    2. ๐Ÿ“Š loop: ๐Ÿงฎ Long Integer - The purpose of this field is to store the loop unique identifier for the point.
    3. ๐Ÿ“Š bend: ๐Ÿงฎ Long Integer - The purpose of the field is to store the bend identifier for the point.
    4. ๐Ÿ“Š position: ๐Ÿงฎ Text (10) - The purpose of this field is to store position identifier for the point. This field must have one three values: ๐Ÿงฎstart, ๐Ÿงฎend, or ๐Ÿงฎapex.

Create Loop Points

NoteHow to Identify Loops.
  1. ๐Ÿ—บ๏ธ Loop_points features are used to define the start and end location of loop bends and the location of a loopโ€™s apex.
  2. ๐Ÿ—บ๏ธ Loop_points features are always placed along (i.e., snapped to) an outer bankline of the feature.
  1. Begin numbering loops starting at the downstream end of the reach and increment the loop integer values moving upstream.
  2. Beginning and end of loops are delineated where the valleyline definitively crosses the flowline.

Step 2

Step 2
  1. If the flowline crosses the valleyline and then crosses back over in a short distance, this is not considered a definitive crossing. A definitive crossing is one where the flowline approaches the valleyline, crosses it, and then continues to move away from the valleyline for a significant longitudinal distance.
  2. Loops must alternate from one bank to the opposite bank. For example, if loop 1 is delineated along the right descending bank, then loop 2 is delineated along the left descending bank.
  3. Loops are composed of one or more bends (bends nest inside of loops). For example, loop 1 can have bends 1, 2, and 3 (i.e., loop 1, bend 1; loop 1, bend 2; loop 1, bend 3).
  4. Bend numbering restarts within each loop. The first bend value within a loop always begins with the value 1.
  5. Create start, end, and apex points (complete all attribute information).
  6. Save Edits.
NoteMultiple Reaches:
  • For a site with multiple reaches, loops must be uniquely numbered across all reaches. The loop field values of loop_points should not repeat within the reaches of a site.
  • The downstream-most loop in the site should be numbered starting with the loop field value of 1 and increase moving upstream.
  • Set the loop field value for each upstream reach to the upstream-most value (i.e., the highest loop value of the downstream reachโ€™s ๐Ÿ—บ๏ธ loop_points feature class) of the downstream reach. For example, set the value of the field loop of the first Reach-2 loop_points feature to 8 if the maximum value of Reach-1โ€™s loop_points feature class loop field is 7.

Check Loop Points:

  • Use the ๐Ÿ› ๏ธ Check Loop Points tool in the ๐Ÿงฐ Check toolset to verify that loops and bends are defined correctly.
  • Review the messages produced by this tool to identify and correct problems with loop and bend delineation.

Derive Bankline Points

The purpose of this step is to convert the banklines to a set of bankline_points and assign elevations and loop and bend locations to these features.

  1. Open the ๐Ÿ› ๏ธ Bankline Points tool to assign loops, bends, elevations and valley line positions to the ๐Ÿ—บ๏ธ bankline_points feature class.
  2. Add the feature dataset for the most recent year.
  3. Add the ๐Ÿ—บ๏ธ loop point, ๐Ÿ—บ๏ธ banklines, and ๐Ÿ—บ๏ธ valleyline feature classes from the most recent year.
  4. Add the ๐Ÿ—บ๏ธ demhydro raster for the mosts recent year.
  5. Set the ๐Ÿ“Š station_distance at ๐Ÿงฎ 1.
  6. Hit Run.
  7. In the ๐Ÿงฐ Check toolset run the ๐Ÿ› ๏ธ Check Bankline Points tool.
    1. The check tool ensures that the ๐Ÿ“Š loop, ๐Ÿ“Š bend, ๐Ÿ“Š position, ๐Ÿ“Š valley_POINT_X, ๐Ÿ“Š valley_POINT_Y, and ๐Ÿ“Š valley_POINT_M fields are populated. Only bankline_points features within loops and bends will have values in the ๐Ÿ“Š loop, ๐Ÿ“Š bend, and๐Ÿ“Š position` fields.
    2. All records should have values in the ๐Ÿ“Š valley_POINT_X, ๐Ÿ“Š valley_POINT_Y, and ๐Ÿ“Š valley_POINT_M fields.
  8. Apply the following definition query to the ๐Ÿ—บ๏ธ bankline_points feature class: โ€œloop IS NOT NULLโ€. Only bankline_points features between loop_points features should be visible.

Assign Cross Section Loops

The purpose of this step is to assign loop and bend identifiers to regularly spaced and riffle cross section feature classes for each reach.

  1. Open the ๐Ÿ› ๏ธ Assign Loops tool to assign loops and bends to a ๐Ÿ—บ๏ธ XS line feature class.
  2. Add the ๐Ÿ—บ๏ธ cross_section feature class from the the most recent survey event dataset.
  3. Add the ๐Ÿ—บ๏ธ bankline_points feature class to the most recent survey event dataset
  4. Once the tool completes check the regular cross section feature class attribute table correctly assigned the loop and bend field values.
  5. Repeat this step for both the ๐Ÿ—บ๏ธ riffle_channel and ๐Ÿ—บ๏ธriffle_floodplain feature classes.

Run Report

๐Ÿ”ง Practical

XS Dimensions Level 3

The purpose of this stage is to calculate the Level 3 dimensions for each reach.

Calculate Cross Section L3 Dimensions

The purpose of this step is to calculate the L3 dimensions for the regularly spaced and ๐Ÿ—บ๏ธ riffle _XS feature classes for each reach.

Note

If any ๐Ÿ—บ๏ธ *_dims_L3 feature classes exist in the reach geodatabase (created during a previous run), delete these feature classes.

  1. Open the ๐Ÿ› ๏ธ XS Planform, Level 3 tool to calculate the L3 dimensions.
  2. Add the ๐Ÿ—บ๏ธ level 2 XS_Dimensions feature class from the same survey event to ๐Ÿ—บ๏ธ xs_dimesions.
  3. Add the ๐Ÿ—บ๏ธ bankline_points feature class from the same survey event to ๐Ÿ—บ๏ธ bankline_points feature class.
  4. Refresh the Survey event year folder to update with the ๐Ÿ“ˆ XS-Planform Level 3 csv.
  5. Verify in the attribute table that the L3 dimensions have been calculated

Join from CSV (Data Management toolbox)

  1. Open the ๐Ÿ› ๏ธ Join from CSV tool in the ๐Ÿงฐ Data Management toolbox.
  2. Add the feature dataset for the current survey event.
  3. Add the ๐Ÿ—บ๏ธ level 2 XS_Dimensions feature class from the same survey event to ๐Ÿ“Š fc.
  4. Select the ๐Ÿงฎ Seq in the dropdown for the ๐Ÿ“Š fc_field.
  5. Add the ๐Ÿ“ˆ level 3 dimension csv spreadsheet to the ๐Ÿ“Š csv_file.
  6. Type ๐Ÿงฎ Seq into the ๐Ÿ“Š csv_field.
  7. Hit Run.
  8. Verify in the attribute table joined of the L3 dimensions csv have been added.

Add Modeled Water Surface Elevation (Optional)

  1. Open the ๐Ÿ› ๏ธ RAS Watersurface tool.
  2. Add the feature dataset for the current survey event.
  3. Add the ๐Ÿ—บ๏ธ xs_dimensions_l3 feature class to ๐Ÿ“Š xs_dims.
  4. Add a ๐Ÿ—บ๏ธ ras HEC model raster containing water surface elevation field.
  5. Name the model ouput (Use the RAS_model_name parameter to distinguish between multiple RAS model scenarios)

Generate Level 3 Report

The purpose of this stage is to run the Level 3 report for each reach.

  1. Open the ๐Ÿ› ๏ธ Level 3 Report tool to produce the Level 3 Report.
  2. Add the value of the ๐Ÿ“Š ReachName field used in the ๐Ÿ—บ๏ธ flowline feature class to ๐Ÿ“Š stream.
  3. Add the ๐Ÿ—บ๏ธ flowline feature class for the base year survey to ๐Ÿ“Š flowline_fc.
  4. Add the ๐Ÿ—บ๏ธ XS line feature class to ๐Ÿ“Š xs_fc.
  5. Add the ๐Ÿ—บ๏ธ *_dims_L3 feature class calculated for the regular cross sections of the most recent survey event.
  6. Add the ๐Ÿ—บ๏ธ xs_points_* feature class for the most recent survey event first (i.e., the base year) and then the previous surveys in reverse chronological order (e.g., 2016, 2010, 2006).
  7. Enter the most recent survey event first and then the the previous surveys in reverse chronological order (e.g., 2016, 2010, 2006).
  8. Add the ๐Ÿ—บ๏ธ DEM raster for the most recent survey event.
  9. Add the ๐Ÿ—บ๏ธ banklines feature class created for the most recent survey event.
  10. Add the ๐Ÿ—บ๏ธ features point feature class for the site to the ๐Ÿ“Š features_fc.
  11. Enter the same ๐Ÿงฎ bf_estimate from level 2 report into the ๐Ÿ“Š bf_estimate box.
  12. Enter the same regions used in level 2 report or as others as needed.
  13. Check show map box.
  14. Set the profile units to the units of the surface raster.
  15. Leave ๐Ÿงฎ aerial and ๐Ÿงฎ elevation boxes ๐Ÿ“Š checked.
  16. Leave the ๐Ÿงฎ defaults for ๐Ÿ“Š xs_label_freq, ๐Ÿ“Š exaggeration, and ๐Ÿ“Š extent_factor.
  17. Select the folder that the report should be written to.
  18. Select ๐Ÿงฎ word as the ๐Ÿ“Š output format for the report.
  19. Hit Run.

Next Steps

โ˜‘๏ธ Evaluate

Review the report.

  1. Go to chapter Level 3 Planform Report under Report Reviews.
  2. Refer to the FG Technical Manual as need for more detailed information.
  3. Revise and/or rerun as needed.