_04-ex.Rmd

```{r 04-ex-e0, include=TRUE, message=FALSE}
library(sf)
library(dplyr)
library(spData)
```

E1. It was established in Section \@ref(spatial-vec) that Canterbury was the region of New Zealand containing most of the 100 highest points in the country.
How many of these high points does the Canterbury region contain?

**Bonus:** plot the result using the `plot()` function to show all of New Zealand, `canterbury` region highlighted in yellow, high points in Canterbury represented by red crosses (hint: `pch = 7`) and high points in other parts of New Zealand represented by blue circles. See the help page `?points` for details with an illustration of different `pch` values.

```{r 04-ex-e1}
library(tmap)
# tmap_mode("view")
qtm(nz) + qtm(nz_height)
canterbury = nz |> filter(Name == "Canterbury")
canterbury_height = nz_height[canterbury, ]
nz_not_canterbury_height = nz_height[canterbury, , op = st_disjoint]
nrow(canterbury_height) # answer: 70

plot(st_geometry(nz))
plot(st_geometry(canterbury), col = "yellow", add = TRUE)
plot(nz_not_canterbury_height$geometry, pch = 1, col = "blue", add = TRUE)
plot(canterbury_height$geometry, pch = 4, col = "red", add = TRUE)
```

E2. Which region has the second highest number of `nz_height` points, and how many does it have?

```{r 04-ex-e2}
nz_height_count = aggregate(nz_height, nz, length)
nz_height_combined = cbind(nz, count = nz_height_count$elevation)
nz_height_combined |> 
  st_drop_geometry() |> 
  dplyr::select(Name, count) |> 
  arrange(desc(count)) |> 
  slice(2)
```

E3. Generalizing the question to all regions: how many of New Zealand's 16 regions contain points which belong to the top 100 highest points in the country? Which regions?

- Bonus: create a table listing these regions in order of the number of points and their name.

```{r 04-ex-e3}
# Base R way:
nz_height_count = aggregate(nz_height, nz, length)
nz_height_combined = cbind(nz, count = nz_height_count$elevation)
plot(nz_height_combined)

# Tidyverse way:
nz_height_joined = st_join(nz_height, nz |> select(Name))
# Calculate n. points in each region - this contains the result
nz_height_counts = nz_height_joined |> 
  group_by(Name) |> 
  summarise(count = n())

# Optionally join results with nz geometries:
nz_height_combined = left_join(nz, nz_height_counts |> sf::st_drop_geometry())
# plot(nz_height_combined) # Check: results identical to base R result

# Generate a summary table
nz_height_combined |> 
  st_drop_geometry() |> 
  dplyr::select(Name, count) |> 
  arrange(desc(count)) |> 
  na.omit()
```

E4. Test your knowledge of spatial predicates by finding out and plotting how US states relate to each other and other spatial objects.

The starting point of this exercise is to create an object representing Colorado state in the USA. Do this with the command 
`colorado = us_states[us_states$NAME == "Colorado",]` (base R) or with with the  `filter()` function (tidyverse) and plot the resulting object in the context of US states.

- Create a new object representing all the states that geographically intersect with Colorado and plot the result (hint: the most concise way to do this is with the subsetting method `[`).
- Create another object representing all the objects that touch (have a shared boundary with) Colorado and plot the result (hint: remember you can use the argument `op = st_intersects` and other spatial relations during spatial subsetting operations in base R).
- Bonus: create a straight line from the centroid of the District of Columbia near the East coast to the centroid of California near the West coast of the USA (hint: functions `st_centroid()`, `st_union()` and `st_cast()` described in Chapter 5 may help) and identify which states this long East-West line crosses.

```{r 04-ex-4-1}
colorado = us_states[us_states$NAME == "Colorado", ]
plot(us_states$geometry)
plot(colorado$geometry, col = "grey", add = TRUE)
```

```{r 04-ex-4-2}
intersects_with_colorado = us_states[colorado, , op = st_intersects]
plot(us_states$geometry, main = "States that intersect with Colorado")
plot(intersects_with_colorado$geometry, col = "grey", add = TRUE)
```

```{r 04-ex-4-3}
# Alternative but more verbose solutions
# 2: With intermediate object, one list for each state
sel_intersects_colorado = st_intersects(us_states, colorado)
sel_intersects_colorado_list = lengths(sel_intersects_colorado) > 0
intersects_with_colorado = us_states[sel_intersects_colorado_list, ]

# 3: With intermediate object, one index for each state
sel_intersects_colorado2 = st_intersects(colorado, us_states)
sel_intersects_colorado2
us_states$NAME[unlist(sel_intersects_colorado2)]

# 4: With tidyverse
us_states |> 
  st_filter(y = colorado, .predicate = st_intersects)
```

```{r 04-ex-4-4}
touches_colorado = us_states[colorado, , op = st_touches]
plot(us_states$geometry, main = "States that touch Colorado")
plot(touches_colorado$geometry, col = "grey", add = TRUE)
```


```{r 04-ex-4-5}
washington_to_cali = us_states |> 
  filter(grepl(pattern = "Columbia|Cali", x = NAME)) |> 
  st_centroid() |> 
  st_union() |> 
  st_cast("LINESTRING")
states_crossed = us_states[washington_to_cali, , op = st_crosses]
states_crossed$NAME
plot(us_states$geometry, main = "States crossed by a straight line\n from the District of Columbia to central California")
plot(states_crossed$geometry, col = "grey", add = TRUE)
plot(washington_to_cali, add = TRUE)
```


E5. Use `dem = rast(system.file("raster/dem.tif", package = "spDataLarge"))`, and reclassify the elevation in three classes: low (<300), medium and high (>500).
Secondly, read the NDVI raster (`ndvi = rast(system.file("raster/ndvi.tif", package = "spDataLarge"))`) and compute the mean NDVI and the mean elevation for each altitudinal class.

```{r 04-ex-e5}
library(terra)
dem = rast(system.file("raster/dem.tif", package = "spDataLarge"))
ndvi = rast(system.file("raster/ndvi.tif", package = "spDataLarge"))

#1
dem_rcl = matrix(c(-Inf, 300, 0, 300, 500, 1, 500, Inf, 2), ncol = 3, byrow = TRUE)
dem_reclass = classify(dem, dem_rcl)
levels(dem_reclass) = data.frame(id = 0:2, cats = c("low", "medium", "high"))
plot(dem_reclass)

#2
zonal(c(dem, ndvi), dem_reclass, fun = "mean")
```

E6. Apply a line detection filter to `rast(system.file("ex/logo.tif", package = "terra"))`.
Plot the result.
Hint: Read `?terra::focal()`.

```{r 04-ex-e6}
# from the focal help page (?terra::focal()):
# Laplacian filter: filter=matrix(c(0,1,0,1,-4,1,0,1,0), nrow=3)
# Sobel filters (for edge detection): 
# fx=matrix(c(-1,-2,-1,0,0,0,1,2,1), nrow=3) 
# fy=matrix(c(1,0,-1,2,0,-2,1,0,-1), nrow=3)

# just retrieve the first channel of the R logo
r = rast(system.file("ex/logo.tif", package = "terra"))
# compute the Sobel filter
filter_x = matrix(c(-1, -2, -1, 0, 0, 0, 1, 2, 1), nrow = 3)
sobel_x = focal(r, w = filter_x)
plot(sobel_x, col = c("white", "black"))

filter_y = matrix(c(1, 0, -1, 2, 0, -2, 1, 0, -1), nrow = 3)
sobel_y = focal(r, w = filter_y)
plot(sobel_y, col = c("black", "white"))
```

E7. Calculate the Normalized Difference Water Index	(NDWI; `(green - nir)/(green + nir)`) of a Landsat image. 
Use the Landsat image provided by the **spDataLarge** package (`system.file("raster/landsat.tif", package = "spDataLarge")`).
Also, calculate a correlation between NDVI and NDWI for this area (hint: you can use the `layerCor()` function).

```{r 04-ex-e7}
file = system.file("raster/landsat.tif", package = "spDataLarge")
multi_rast = rast(file)

ndvi_fun = function(nir, red){
  (nir - red) / (nir + red)
}
ndvi_rast = lapp(multi_rast[[c(4, 3)]], fun = ndvi_fun)
plot(ndvi_rast)

ndwi_fun = function(green, nir){
    (green - nir) / (green + nir)
}

ndwi_rast = lapp(multi_rast[[c(2, 4)]], fun = ndwi_fun)
plot(ndwi_rast)

two_rasts = c(ndvi_rast, ndwi_rast)
names(two_rasts) = c("ndvi", "ndwi")

# correlation -- option 1
layerCor(two_rasts, fun = cor)

# correlation -- option 2
two_rasts_df = as.data.frame(two_rasts)
cor(two_rasts_df$ndvi, two_rasts_df$ndwi)
```

E8. A StackOverflow [post](https://stackoverflow.com/questions/35555709/global-raster-of-geographic-distances) shows how to compute distances to the nearest coastline using `raster::distance()`.
Try to do something similar but with `terra::distance()`: retrieve a digital elevation model of Spain, and compute a raster which represents distances to the coast across the country (hint: use `geodata::elevation_30s()`).
Convert the resulting distances from meters to kilometers.
Note: it may be wise to increase the cell size of the input raster to reduce compute time during this operation (`aggregate()`).

```{r 04-ex-e8}
# Fetch the DEM data for Spain
spain_dem = geodata::elevation_30s(country = "Spain", path = ".", mask = FALSE)

# Reduce the resolution by a factor of 20 to speed up calculations
spain_dem = aggregate(spain_dem, fact = 20)

# According to the documentation, terra::distance() will calculate distance
# for all cells that are NA to the nearest cell that are not NA. To calculate
# distance to the coast, we need a raster that has NA values over land and any
# other value over water
water_mask = is.na(spain_dem)
water_mask[water_mask == 0] = NA

# Use the distance() function on this mask to get distance to the coast
distance_to_coast = distance(water_mask)
# convert distance into km
distance_to_coast_km = distance_to_coast / 1000

# Plot the result
plot(distance_to_coast_km, main = "Distance to the coast (km)")
```

E9. Try to modify the approach used in the above exercise by weighting the distance raster with the elevation raster; every 100 altitudinal meters should increase the distance to the coast by 10 km.
Next, compute and visualize the difference between the raster created using the Euclidean distance (E7) and the raster weighted by elevation.

```{r 04-ex-e9}
# now let's weight each 100 altitudinal meters by an additional distance of 10 km
distance_to_coast_km2 = distance_to_coast_km + ((spain_dem / 100) * 10)
# plot the result
plot(distance_to_coast_km2)
# visualize the difference
plot(distance_to_coast_km - distance_to_coast_km2)
```