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(16 Posts)
GinaO_Neil
Esri Contributor

Introducing the new home for Arc Hydro Docs! 

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SophieAubry
Esri Contributor

The Flood Impact Analysis Solution (FIAS) is a workflow allowing users to visualize high peak flow events and quantify the impacts. The workflow assumes that the user posses predefined flood depth rasters for their area of interest; however, a common question amongst users is how to derive this data. Consider this document as the prequel to FIAS as it will assist users in generating the necessary input depth rasters. 

 

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ChristaCampbell
Esri Contributor

Manage email preferences and print subscriptions so that you only receive what is relevant to you. 

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GinaO_Neil
Esri Contributor

WIM for Pro 3+ is here! You can now leverage point ground truth data, postprocess predictions, use Continuous Flow, and use Surface Parameters' adaptive neighborhoods.

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DeanDjokic
Esri Contributor

How to report Arc Hydro tools issues.

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GinaO_Neil
Esri Contributor

Predict the Impervious, Pervious, and Open Water Areas for Any WatershedBlog - Impervious Surfaces (2).png

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GinaO_Neil
Esri Contributor

Walk through the WIM workflow with jupyter notebooks

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DeanDjokic
Esri Contributor

Following the release of Arc Hydro for ArcGIS Pro 2.5 earlier this year, here is the Arc Hydro for ArcGIS Pro 2.6 formal release.  The major advancements include implementation of Trace Network capabilities fully released in Pro 2.6, addition of functionality for hydrologic modeling support, LAS to DEM creation toolset, two new functions for terrain ruggedness quantification, and several other functions transitioned from the ArcMap version.  This release is identified as “ArcHydroPro2.0.221_signed” release in the Arc Hydro Pro download setup directory.

Check out a separate blog on the ruggedness measurements and an extensive document presenting the hydrologic processing workflows, including export to HEC-HMS basin file.  If you did not get a chance to recently review “Arc Hydro – Project Development Best Practices” and, specifically for Pro, the “Arc Hydro – ArcGIS Pro Project Startup Best Practices” document, now would be good time to do so.  Both documents, as well as all others in the Arc Hydro documentation series, are available on the Arc Hydro GeoNet page.

Arc Hydro Pro development continues and plans for the 2.7 release focus on including additional floodplain delineation and hydraulic modeling support tools, advanced Trace Network tools, and more extensive documentation.  If you have any questions or comments, please contact the Arc Hydro team either via the GeoNet page or directly via email using archydro@esri.com.

The Arc Hydro Team.

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EzraBosworth-Ahmet
Esri Contributor

The Importance of Terrain Analyses

Quantifying the characteristics of terrain can be beneficial in many analysis workflows including sediment transport modelling, ecological studies, geomorphological evaluation of land forms, and landslide hazards assessment. To help with terrain analysis, Arc Hydro is adding a Terrain Ruggedness Index (TRI) tool and a Vector Ruggedness Measure (VRM) tool to its terrain pre-processing capabilities.

 

How TRI and VRM contribute to Terrain Analyses

Terrain Ruggedness Index:

   TRI expresses the amount of elevation difference between adjacent cells of a DEM. Using methodology developed by Riley et al (1999) and published in the paper “A Terrain ruggedness Index That Quantifies Topographic heterogeneity”, the tool measures the difference in elevation values from a center cell and eight cells directly surrounding it. Then, the eight elevation differences are squared and averaged. The square root of this average results is a TRI measurement for the center cell. This calculation is then conducted on every cell of the DEM.

 

 Vector Ruggedness Measure:

   VRM provides a way to measure terrain ruggedness as the variation in three-dimensional orientation of grid cells within a neighborhood. Slope and aspect are captured into a single measure and used to decouple terrain ruggedness from just slope or elevation. The VRM was first proposed by Hobson (1972) in “Surface roughness in topography: quantitative approach” and was later adapted by Sappington et al (2007) in “Quantifying landscape ruggedness for animal habitat analysis: A case study using bighorn sheep in the Mojave Desert.”

 

   Both tool scripts use geoprocessing workflows developed by Dr. Barry Nickel, a professor at University of California Santa Cruz.

 

Where to Find TRI and VRM

Many ecologists and geologists have employed TRI and VRM to further their research and understanding of terrain. Prior to this tool release, analysts had to derive both TRI and VRM through a series of geoprocessing steps or had to write their own custom tool. Now, both tools are available under Arc Hydro's Terrain Preprocessing toolbox in ArcMap 10.8.0.37 and ArcGIS Pro in Arc Hydro build 2.6.26. Future releases of Arc Hydro will also support the tools.

 

 

How to Use the Tools

  The TRI tool requires only a DEM as an input. The output is a TRI raster data set that expresses the amount of elevation difference between adjacent cells of the DEM in meters. Output values are dependent on input DEM resolution.

 

 

   The VRM tool has two input parameters. One is the DEM for analyses, and the other is an integer specifying neighborhood size for analyses. A larger window size can be useful, but often causes a smoothing effect on the landscape, so as a default, the window size is set to 3. The output is a VRM raster data set that is a dimensionless ruggedness value between 0 (flat) and 1 (most rugged). Typical values for natural terrains range between 0 and 0.5, with rugged landscape defined to be greater than 0.02.

 

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DeanDjokic
Esri Contributor

      Over the last few years, we have been working towards integrating Arc Hydro into the ArcGIS Pro platform.  The release of Arc Hydro for ArcGIS Pro 2.5 includes over 200 Arc Hydro functions in the domain of terrain preprocessing, watershed and stream delineation, and characterization.  Most of the “old friends” from the Arc Hydro 10.x implementation are there, but some of the new functionality is not available in 10.x.  For example, only available in Arc Hydro in Pro is a whole toolset dedicated to wetlands identification using a machine learning approach – check out Gina’s blog on that.

      Also, Arc Hydro for Pro 2.5 leverages the new Trace Network functionality that is available by participating in the Trace Network Beta program for ArcGIS Pro 2.5.  This core ArcGIS Pro functionality enables the Pro implementation of Arc Hydro functions that were previously unavailable due to dependency on geometric networks.  If you are interested in testing and reviewing the Trace Network and Arc Hydro tools built on top of it, please e-mail archydro@esri.com and we will get you registered in the Trace Network Beta program.

      If you did not get a chance to recently review “Arc Hydro – Project Development Best Practices” and, specifically for Pro, the “Arc Hydro – ArcGIS Pro Project Startup Best Practices” documents, now would be a good time to do so.  Both documents, as well as all others in the Arc Hydro documentation series, are available on the Arc Hydro GeoNet page.

      Arc Hydro Pro development continues and plans for the 2.6 release focus on including additional hydrologic and hydraulic modeling support tools and more extensive documentation.  If you have any questions or comments, please contact the Arc Hydro team either via the GeoNet page or directly via email using archydro@esri.com.

The Arc Hydro Team

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