The advantage of radar is that it is not affected by clouds to the same degree that optical remote sensing is, and there is also useful information gained by the polarisation.
As an example, I downloaded a Sentinel 1B product covering Cornwall and Devon which was taken on 7th October 2016, from the Copernicus data hub.
The type of product I used is the Interferometric Wide Swath mode (further detail).
I used the Sentinel Toolbox to perform orthorectification automatically, and visualise as a RGB with VH polarisation in the red channel, VV in the green, and the ratio between the two in the blue.
Here is an image from 11th December 2014, with the same colour scheme used.
|Returning to the interferometric wide swath mode, overlaying roads and placenames for context. The colour scaling is slightly different in this image, making the green band less strong.|
|A portion from a Sentinel 2A image from 30th September 2016, using bands 11, 8 and 4 (1610nm, 842nm, 655nm).|
|The Level 2A product includes a basic pixel level land cover classification - there are some errors here note some cloud shadow has been classified as water or cloud, and spurious snow/ice around Porthtowan.|