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Isobath corridors summarize terrain along depth horizons. They are useful when observations are collected along contours or when terrain structure needs to be compared at equivalent depths while retaining along-contour variability.
bathy <- read_bathy(blueterra_example("hitw"))
prepared <- prepare_bathy(bathy, depth_range = c(-220, -25), smooth = TRUE)
terrain <- derive_terrain(
prepared,
metrics = c("slope", "bpi", "curvature", "surface_area_ratio")
)The example bathymetry stores depth as negative elevation, so contour depths are passed as negative values.
isobaths <- extract_isobaths(prepared, depths = c(-50, -80, -120))
isobaths[, c("contour_value", "depth_label")]
#> class : SpatVector
#> geometry : lines
#> dimensions : 3, 2 (geometries, attributes)
#> extent : 137476.2, 137772, 205669.4, 205756.6 (xmin, xmax, ymin, ymax)
#> coord. ref. : NAD83 / Puerto Rico & Virgin Is. (EPSG:32161)
#> names : contour_value depth_label
#> type : <num> <num>
#> values : -50 -50
#> -80 -80
#> -120 -120plot_bathy(
prepared,
contours = TRUE,
contour_interval = 25,
vectors = isobaths,
vector_color = "black",
title = "Isobaths Over Hillshaded Bathymetry"
)Buffers are measured in map units, so the raster should use a projected CRS. The example raster is projected; other rasters should be reprojected explicitly when needed. Corridors use a 5 m buffer around each source isobath.
corridors <- make_isobath_corridors(
prepared,
depths = c(-50, -80, -120),
width = 5
)
corridors[, c("contour_value", "depth_label", "corridor_id")]
#> class : SpatVector
#> geometry : polygons
#> dimensions : 3, 3 (geometries, attributes)
#> extent : 137471.2, 137777, 205664.4, 205761.6 (xmin, xmax, ymin, ymax)
#> coord. ref. : NAD83 / Puerto Rico & Virgin Is. (EPSG:32161)
#> names : contour_value depth_label corridor_id
#> type : <num> <num> <int>
#> values : -50 -50 1
#> -80 -80 2
#> -120 -120 3plot_isobath_corridors(
corridors,
prepared,
isobaths = isobaths,
background_contours = FALSE,
title = "Isobath Corridors and Source Isobaths",
subtitle = "Corridors use a 5 m buffer around each source isobath"
)The black lines are the source isobaths. The corridor polygons buffer those depth horizons by 5 m and define the terrain extraction zones used in the summary.
cells <- extract_isobath_corridors(terrain, corridors)
head(cells)
#> # A tibble: 6 × 10
#> ID level contour_value depth_label corridor_id slope_deg bpi_3x3 bpi_11x11
#> <int> <dbl> <dbl> <dbl> <int> <dbl> <dbl> <dbl>
#> 1 1 -50 -50 -50 1 47.1 -0.336 4.82
#> 2 1 -50 -50 -50 1 46.9 -0.436 4.35
#> 3 1 -50 -50 -50 1 47.0 -0.428 3.78
#> 4 1 -50 -50 -50 1 47.8 -0.378 3.35
#> 5 1 -50 -50 -50 1 48.4 -0.419 3.06
#> 6 1 -50 -50 -50 1 48.2 -0.676 2.73
#> # ℹ 2 more variables: curvature <dbl>, surface_area_ratio <dbl>
summary <- summarize_isobath_terrain(terrain, corridors)
summary[, c("contour_value", "slope_deg_mean", "bpi_3x3_mean", "curvature_mean")]
#> # A tibble: 3 × 4
#> contour_value slope_deg_mean bpi_3x3_mean curvature_mean
#> <dbl> <dbl> <dbl> <dbl>
#> 1 -50 46.2 -0.01000 0.0163
#> 2 -80 40.0 -0.0209 0.0629
#> 3 -120 77.7 1.25 -3.77The summary compares terrain structure at the selected depth horizons. BPI values should be interpreted using the raster’s stored vertical convention.
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