Spatial Analysis Techniques in ArcGIS for Elevation and Precipitation Data

exercise 3 overview n.w
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Explore the process of slope calculations, verification using ArcGIS, automation with ModelBuilder, and analysis of San Marcos elevation and precipitation data. Learn about projecting rasters, topography visualization, zonal average calculations, Thiessen polygons, and more.

  • Spatial Analysis
  • ArcGIS
  • Elevation
  • Precipitation
  • ModelBuilder

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  1. Exercise 3 Overview Slope calculations by hand Verifying using ArcGIS Automating and applying to larger dataset using Modelbuilder Spatial Analysis of San Marcos Elevation and Precipitation Projecting rasters Examining and visualizing topography Zonal average calculations Thiessen polygons Surface smoothing to average precipitation

  2. Slope and Aspect ? ? ? = aspect clockwise from North ? ? ? https://pro.arcgis.com/en/pro-app/tool-reference/spatial-analyst/how-slope-works.htm

  3. ArcGIS Slope tool y a b c +? ? 2 2 ? ? 2 +? ? 2 2 ? ? 2 d e f + 2 g h i x dz dx= a + 2d + g c + 2f + i 8 ? ? 2 Similarly ? ? 2 dz dy= g + 2h + i a + 2b + c 8 ? ? 2 c b f Slope magnitude = a e i 2 2 d h ?? ?? ?? ?? + g 2 x y

  4. ArcGIS Aspect the steepest downslope direction dz dz / dx x ? = = atan atan dy dz / dy y dz ? = ? dx ? ? Use atan2 to resolve ambiguity in atan direction ? + 180? ( ) , y atan2 x ? ? https://pro.arcgis.com/en/pro-app/tool-reference/spatial-analyst/how-aspect-works.htm

  5. Example dz = 30 + * 8 + + + (a 2d g) - (c 2f i) a b c dx x_mesh_spa cing 80 74 63 + + + + 80 ( 2 * 69 60 ) ( 63 2 * 56 48 ) = d e f 145.2o 8 * 30 69 67 56 = . 0 229 + g h i i) + 2b + + dz (g 2h - (a c) 60 52 48 = dy y_mesh_sp * 8 + acing + + + ( 60 2 * 52 48 ) 80 ( 2 * 74 63 ) = = + 8 * 30 2 2 Slope . 0 229 . 0 329 = . 0 329 = . 0 401 = o atan . 0 ( 401 ) 21 8 . + o 180 . 0 229 = = o Aspect atan 34 8 . o . 0 329 145 2 .

  6. Hydrologic Slope (Flow Direction Tool) - Direction of Steepest Descent 30 30 80 74 63 80 74 63 69 67 56 69 67 56 60 52 48 60 52 48 67 48 67 52 = Slope: . 0 45 = . 0 50 30 2 30

  7. Eight Direction Pour Point Model 32 64 128 16 1 8 4 2 ESRI Direction encoding

  8. The D Algorithm Steepest direction downslope z0 Elevations at each vertex zi z2 z1 3 2 4 2 z z = atan 1 2 1 0 1 z z 1 5 0 1 2 2 z z z z 8 = + 0 1 S 1 2 6 7 If 1 does not fit within the triangle the angle is chosen along the steepest edge or diagonal resulting in a slope and direction equivalent to D8

  9. D Example 30 z z 80 74 63 = 7 8 atan 1 z z 0 7 eo 52 48 69 67 56 = = o atan 14 9 . 67 52 e8 e7 60 52 48 2 2 52 48 67 52 284.9o = + S 30 30 14.9o = . 0 517 From ArcGIS Pro Help:

  10. 10 z0 4 3 2 ?5 ?6 ?0 ?5 ? = atan z5 5 1 26.0 26.4 ? 2 2 ?5 ?6 ?? ?5 ? = + 6 25.8 7 8 z6

  11. Subwatershed Precipitation by Thiessen Polygons P2 Thiessen Polygons Intersect with Subwatersheds Evaluate A*P Product Summarize by subwatershed P1 A2 A1 A3 P3 ? =?1 ?1 + ?2 ?2 + ?3 ?3 ?1 + ?2 + ?3

  12. Subwatershed Precipitation by Thiessen Polygons Thiessen Polygons Intersect with Subwatersheds Evaluate A*P Product Summarize by subwatershed ??= ?????? ????

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