Working with indices#
Indices calculated from multispectral satellite imagery are powerful ways to
quantitatively analyze these data.
They take advantage of different spectral properties of materials to
differentiate between them.
Many of these indices can be calculated with simple arithmetic operations.
So now that our data are in xarray.Dataset
’s, it’s fairly easy to
calculate them.
As an example, we’ll use two example scenes from before and after the
Brumadinho tailings dam disaster
to try to image and quantify the total area flooded by the damn collapse.
Trigger warning
This tutorial uses data from the tragic Brumadinho tailings dam disaster, in which over 250 people lost their lives. We use this dataset to illustrate the usefulness of remote sensing data for monitoring such disasters but we want to acknowledge its tragic human consequences. Some readers may find this topic disturbing and may not wish to read futher.
First, we must import the required packages, download our two sample scenes,
and load them with xlandsat.load_scene
:
import xlandsat as xls
import matplotlib.pyplot as plt
path_before = xls.datasets.fetch_brumadinho_before()
path_after = xls.datasets.fetch_brumadinho_after()
before = xls.load_scene(path_before)
after = xls.load_scene(path_after)
after
<xarray.Dataset> Size: 1MB Dimensions: (easting: 400, northing: 300) Coordinates: * easting (easting) float64 3kB 5.844e+05 5.844e+05 ... 5.963e+05 5.964e+05 * northing (northing) float64 2kB -2.232e+06 -2.232e+06 ... -2.223e+06 Data variables: blue (northing, easting) float16 240kB 0.0686 0.07043 ... 0.0564 green (northing, easting) float16 240kB 0.1027 0.09839 ... 0.07043 red (northing, easting) float16 240kB 0.09778 0.09778 ... 0.06177 nir (northing, easting) float16 240kB 0.2988 0.2715 ... 0.2637 0.251 swir1 (northing, easting) float16 240kB 0.2311 0.2274 ... 0.1608 0.142 swir2 (northing, easting) float16 240kB 0.145 0.1442 ... 0.09961 0.08655 Attributes: (12/19) Conventions: CF-1.8 title: Landsat 8 scene from 2019-01-30 (path/row=218... digital_object_identifier: https://doi.org/10.5066/P9OGBGM6 origin: Image courtesy of the U.S. Geological Survey landsat_product_id: LC08_L2SP_218074_20190130_20200829_02_T1 processing_level: L2SP ... ... ellipsoid: WGS84 date_acquired: 2019-01-30 scene_center_time: 12:57:09.1851220Z wrs_path: 218 wrs_row: 74 mtl_file: GROUP = LANDSAT_METADATA_FILE\n GROUP = PROD...
Let’s make RGB composites to get a sense of what these two scenes contain:
rgb_before = xls.composite(before, rescale_to=(0.03, 0.2))
rgb_after = xls.composite(after, rescale_to=(0.03, 0.2))
fig, axes = plt.subplots(2, 1, figsize=(10, 12), layout="tight")
for ax, rgb in zip(axes, [rgb_before, rgb_after]):
rgb.plot.imshow(ax=ax)
ax.set_title(rgb.attrs["title"])
ax.set_aspect("equal")
plt.show()
The dam is located at around 592000 east and -2225000 north. The after scene clearly shows all of the red mud that flooded the region to the southwest of the dam. Notice also the red tinge of the Paraopeba River in the after image as it was contaminated by the mud flow.
Tip
See Making composites for more information on what we did above.
NDVI#
We can calculate the NDVI for these scenes to see if we can isolate the effect of the flood following the dam collapse. NDVI highlights vegetation, which we assume will have decreased in the after scene due to the flood. NDVI is defined as:
which we can calculate with xarray as:
ndvi_before = (before.nir - before.red) / (before.nir + before.red)
ndvi_before
<xarray.DataArray (northing: 300, easting: 400)> Size: 240kB array([[0.4604, 0.4507, 0.5728, ..., 0.545 , 0.594 , 0.554 ], [0.445 , 0.478 , 0.479 , ..., 0.628 , 0.5664, 0.4626], [0.4734, 0.494 , 0.4739, ..., 0.6387, 0.596 , 0.588 ], ..., [0.5044, 0.5186, 0.4983, ..., 0.527 , 0.4824, 0.474 ], [0.4883, 0.47 , 0.4724, ..., 0.525 , 0.476 , 0.4553], [0.5024, 0.476 , 0.4934, ..., 0.479 , 0.4536, 0.458 ]], dtype=float16) Coordinates: * easting (easting) float64 3kB 5.835e+05 5.835e+05 ... 5.954e+05 5.955e+05 * northing (northing) float64 2kB -2.232e+06 -2.232e+06 ... -2.223e+06
Now we can do the same for the after scene:
ndvi_after = (after.nir - after.red) / (after.nir + after.red)
ndvi_after
<xarray.DataArray (northing: 300, easting: 400)> Size: 240kB array([[0.5073, 0.4705, 0.4907, ..., 0.515 , 0.4946, 0.4565], [0.4277, 0.478 , 0.4817, ..., 0.4949, 0.5166, 0.5474], [0.37 , 0.4304, 0.441 , ..., 0.522 , 0.5786, 0.6226], ..., [0.57 , 0.594 , 0.595 , ..., 0.328 , 0.462 , 0.54 ], [0.5845, 0.5796, 0.583 , ..., 0.4995, 0.566 , 0.572 ], [0.61 , 0.5664, 0.5938, ..., 0.609 , 0.5903, 0.605 ]], dtype=float16) Coordinates: * easting (easting) float64 3kB 5.844e+05 5.844e+05 ... 5.963e+05 5.964e+05 * northing (northing) float64 2kB -2.232e+06 -2.232e+06 ... -2.223e+06
And add some metadata for xarray to find when making plots:
for ndvi in [ndvi_before, ndvi_after]:
ndvi.attrs["long_name"] = "normalized difference vegetation index"
ndvi.attrs["units"] = "dimensionless"
ndvi_before.attrs["title"] = "NDVI before"
ndvi_after.attrs["title"] = "NDVI after"
Now we can make pseudo-color plots of the NDVI from before and after the disaster:
fig, axes = plt.subplots(2, 1, figsize=(10, 12), layout="tight")
for ax, ndvi in zip(axes, [ndvi_before, ndvi_after]):
# Limit the scale to [-1, +1] so the plots are easier to compare
ndvi.plot(ax=ax, vmin=-1, vmax=1, cmap="RdBu_r")
ax.set_title(ndvi.attrs["title"])
ax.set_aspect("equal")
plt.show()
Tracking differences#
An advantage of having our data in xarray.DataArray
format is that we
can perform coordinate-aware calculations. This means that taking the
difference between our two arrays will take into account the coordinates of
each pixel and only perform the operation where the coordinates align.
We can calculate the change in NDVI from one scene to the other by taking the difference:
ndvi_change = ndvi_before - ndvi_after
# Add som metadata for xarray
ndvi_change.name = "ndvi_change"
ndvi_change.attrs["long_name"] = "NDVI change"
ndvi_change.attrs["title"] = (
f"NDVI change between {before.attrs['date_acquired']} and "
f"{after.attrs['date_acquired']}"
)
ndvi_change
<xarray.DataArray 'ndvi_change' (northing: 300, easting: 370)> Size: 222kB array([[ 0.05908 , 0.06323 , 0.0542 , ..., 0.004395, -0.009766, 0.07324 ], [ 0.0498 , 0.07764 , 0.07495 , ..., 0.0957 , 0.012695, 0.003906], [-0.010254, 0.11743 , 0.0747 , ..., 0.03125 , 0.01807 , 0.04004 ], ..., [-0.000977, 0.01123 , 0.000977, ..., 0.00928 , 0.01367 , 0.00708 ], [ 0.00879 , 0.02344 , 0.01318 , ..., 0.006836, 0.00586 , 0.001221], [-0.01221 , 0.02637 , 0.006836, ..., 0.01343 , 0.01221 , 0.0105 ]], dtype=float16) Coordinates: * easting (easting) float64 3kB 5.844e+05 5.844e+05 ... 5.954e+05 5.955e+05 * northing (northing) float64 2kB -2.232e+06 -2.232e+06 ... -2.223e+06 Attributes: long_name: NDVI change title: NDVI change between 2019-01-14 and 2019-01-30
Did you notice?
The keen-eyed among you may have noticed that the number of points along
the "easting"
dimension has decreased. This is because xarray
only makes the calculations for pixels where the two scenes coincide. In
this case, there was an East-West shift between scenes but our calculations
take that into account.
Now lets plot the difference:
fig, ax = plt.subplots(1, 1, figsize=(10, 6))
ndvi_change.plot(ax=ax, vmin=-1, vmax=1, cmap="PuOr")
ax.set_aspect("equal")
ax.set_title(ndvi_change.attrs["title"])
plt.show()
There’s some noise in the cloudy areas of both scenes in the northeast but otherwise this plots highlights the area affected by flooding from the dam collapse in purple at the center.
Estimating area#
One things we can do with indices and their differences in time is calculated area estimates. If we know that the region of interest has index values within a given value range, the area can be calculated by counting the number of pixels within that range (a pixel in Landsat 8/9 scenes is 30 x 30 = 900 m²).
First, let’s slice our NDVI difference to just the flooded area to avoid the
effect of the clouds in North. We’ll use the xarray.DataArray.sel
method to slice using the UTM coordinates of the scene:
flood = ndvi_change.sel(
easting=slice(587000, 594000),
northing=slice(-2230000, -2225000),
)
fig, ax = plt.subplots(1, 1, figsize=(10, 6))
flood.plot(ax=ax, vmin=-1, vmax=1, cmap="PuOr")
ax.set_aspect("equal")
plt.show()
Now we can create a mask of the flood area by selecting pixels that have a high
NDVI difference. Using a >
comparison (or any other logical operator in
Python), we can create a boolean (True
or False
)
xarray.DataArray
as our mask:
# Threshold value determined by trial-and-error
flood_mask = flood > 0.3
# Add some metadata for xarray
flood_mask.attrs["long_name"] = "flood mask"
flood_mask
<xarray.DataArray 'ndvi_change' (northing: 167, easting: 234)> Size: 39kB array([[False, False, False, ..., False, False, False], [False, False, False, ..., False, False, False], [False, False, False, ..., False, False, False], ..., [False, False, False, ..., False, False, False], [False, False, False, ..., False, False, False], [False, False, False, ..., False, False, False]]) Coordinates: * easting (easting) float64 2kB 5.87e+05 5.87e+05 ... 5.94e+05 5.94e+05 * northing (northing) float64 1kB -2.23e+06 -2.23e+06 ... -2.225e+06 Attributes: long_name: flood mask
Plotting boolean arrays will use 1 to represent True
and 0 to represent
False
:
fig, ax = plt.subplots(1, 1, figsize=(10, 6))
flood_mask.plot(ax=ax, cmap="gray")
ax.set_aspect("equal")
ax.set_title("Flood mask")
plt.show()
See also
Notice that our mask isn’t perfect. There are little bloobs classified as flood pixels that are clearly outside the flood region. For more sophisticated analysis, see the image segmentation methods in scikit-image.
Counting the number of True
values is as easy as adding all of the boolean
values (remember that True
corresponds to 1 and False
to 0), which
we’ll do with xarray.DataArray.sum
:
flood_pixels = flood_mask.sum().values
print(flood_pixels)
2095
Note
We use .values
above because sum
returns an
xarray.DataArray
with a single value instead of the actual number.
This is usually not a problem but it looks ugly when printed, so we grab
the number with .values
.
Finally, the flood area is the number of pixels multiplied by the area of each pixel (30 x 30 m²):
flood_area = flood_pixels * 30**2
print(f"Flooded area is approximately {flood_area:.0f} m²")
Flooded area is approximately 1885500 m²
Values in m² are difficult to imagine so a good way to communicate these numbers is to put them into real-life context. In this case, we can use the football pitches as a unit that many people will understand:
flood_area_pitches = flood_area / 7140
print(f"Flooded area is approximately {flood_area_pitches:.0f} football pitches")
Flooded area is approximately 264 football pitches
Warning
This is a very rough estimate! The final value will vary greatly if you change the threshold used to generate the mask (try it yourself). For a more thorough analysis of the disaster using remote-sensing data, see Silva Rotta et al. (2020).
Other indices#
Calculating other indices will follow a very similar strategy to NDVI since most of them only involve arithmetic operations on different bands. As an example, let’s calculate and plot the Modified Soil Adjusted Vegetation Index (MSAVI) for our two scenes:
import numpy as np
# This time, use a loop and put them in a list to avoid repeated code
msavi_collection = []
for scene in [before, after]:
msavi = (
(
2 * scene.nir + 1 - np.sqrt(
(2 * scene.nir + 1) * 2 - 8 * (scene.nir - scene.red)
)
) / 2
)
msavi.name = "msavi"
msavi.attrs["long_name"] = "modified soil adjusted vegetation index"
msavi.attrs["units"] = "dimensionless"
msavi.attrs["title"] = scene.attrs["title"]
msavi_collection.append(msavi)
# Plotting is mostly the same
fig, axes = plt.subplots(2, 1, figsize=(10, 12), layout="tight")
for ax, msavi in zip(axes, msavi_collection):
msavi.plot(ax=ax, vmin=-0.5, vmax=0.5, cmap="RdBu_r")
ax.set_title(msavi.attrs["title"])
ax.set_aspect("equal")
plt.show()
With this same logic, you could calculate NBR and dNBR, other variants of NDVI, NDSI, etc.