band maths and thresholding#

Tip

The script for this tutorial can be found via this direct link.

Alternatively, if you have already added the repository, you can open the script from the Code Editor, by navigating to 03_change_detection/02_thresholding.js under the Reader section.

In this tutorial, we’ll see how we can quantify changes using arithmetic operations, comparing the changes observed using:

  • a simple difference

  • a band ratio

  • a normalized difference

To determine areas where we likely see an increase in vegetation between 1986 and 2022. As in the visual analysis of changes tutorial, we’ll primarily use the SWIR2 band (TM/OLI Band 7), though feel free to modify the script for other bands and applications.

The first two examples calculated in the script are the difference and band ratio, using ee.Image.subtract() and ee.Image.divide(), respectively:

// band maths examples
var diff = oli2022.select('SR_B7').subtract(tm1986.select('SR_B7')).rename('difference');
var ratio = oli2022.select('SR_B7').divide(tm1986.select('SR_B7')).rename('ratio');

Now, we use ee.Image.cat() (documentation) to combine band 7 from each image into a single image:

// add the b7 bands from each year to a single image
var multitemp = ee.Image.cat([
  tm1986.select('SR_B7').rename('1986_B7'),
  oli2022.select('SR_B7').rename('2022_B7')
]);

then we use ee.Image.normalizedDifference() to calculate the normalized difference between 1986 and 2022:

// create a multi-temporal normalized difference
var normdiff = multitemp.normalizedDifference(['2022_B7', '1986_B7']).rename('normDiff');

Just like with examples discussed in the band maths tutorial, such as NDVI1 or NDWI2, this has the effect of stretching the differences so that they vary between -1 and 1, which can help to enhance the changes that we see between the two dates.

interpreting changes#

To see this, run the script, then toggle on the Difference layer:

the difference in SWIR2 reflectance between 1986 and 2022


followed by the Normalized Difference layer:

the normalized difference in SWIR2 reflectance between 1986 and 2022


Toggle back and forth between the two images - you should notice that while the colors don’t change (remember that the sign is the same for both), the colors in the normalized difference image have been stretched to fill the color range compared to the difference image.

Orange colors in both images indicate a negative change in SWIR2 reflectance (i.e., the reflectance was higher in 1986), while purple colors indicate a positive change (i.e., the reflectance was higher in 2022). What types of changes do you see associated with each color?

Remember to look at the ratio image as well:

the ratio of SWIR2 reflectance in 2022 to the reflectance in 1986


how do the changes that you can see in this image compare to the changes displayed in the difference and normalized difference images?

In addition to adding the images to the Map, we have also printed statistics and histograms for these two images to the Console:

a histogram of the difference in NIR reflectance between 1986 and 2022 a histogram of the normalized difference in NIR reflectance between 1986 and 2022


Just like with the images themselves, you should notice that the histogram of the normalized difference image is spread out, or stretched, over a larger range - as a result, it has a much lower, broader peak than the difference image.

Click on Object (under “Difference”/”Normalized Difference”) to show the descriptive statistics calculated for the difference/normalized difference image. Which image has the larger standard deviation? What impact do you think this might have on determining what pixel values represent “normal variation”, and which values represent actual change?

choosing a threshold#

In order to distinguish between “change” and “no change”, we have to pick a threshold value. Here, because we are interested in highlighting areas where vegetation has been replaced by built-up areas, we’ll pick a single threshold value and select only pixels where the pixel value is greater than or equal to the chosen threshold value.

In the script, you should see the following lines of code:

// mask the image based on a threshold
var mask = normdiff.gte(0.5); // select pixels greater than/equal to upper boundary
mask.select('normDiff').rename('changeMask');

mask = mask.updateMask(mask.neq(0));

This uses ee.Image.gte() to select all pixels in normdiff with a value greater than or equal to 0.15, then uses ee.Image.mask() to mask all pixels of the resulting image where this condition is not met.

Later in the script, we add this layer to the Map as urban change mask, then export the vector to a shapefile format that you can use in your GIS software of choice.

To see what this mask looks like, toggle on the urban change mask layer in the Map:

the change mask loaded in the map, showing not very much change


You should probably notice that this threshold hasn’t managed to capture most of the changes that we can see between the two dates - the masked areas are limited to the former rice fields south of Foshan, newly-built islands in the Zhujiang River Estuary, and small patches along some of the other rivers visible in the image.

Hopefully, it’s clear that I’ve deliberately set the threshold too high, which means that a lot of areas of genuine change have been excluded from the mask.

Using the histogram of the normalized difference image, the descriptive statistics, and a bit of trial and error, try to improve on this result. The goal is to include as much of the urban change that you can see as possible, while minimizing differences that are due to natural fluctuations in reflectance.

Once you have a change mask that you feel captures most of the urban growth while minimizing areas where not much change appears to have happened, be sure to click on the Tasks tab and run the task to export the shapefile.

references and notes#

1

Rouse, J.W., et al. (1974). Proceedings, 3rd Earth Resource Technology Satellite Symposium, 1, 48-62. https://ntrs.nasa.gov/citations/19740022614

2

McFeeters, S. K. (1996). Int. J. Rem. Sens., 17(7), 1425–1432. doi: 10.1080/01431169608948714