I am using a time series of S1 images to extract backscatter above a point like location, but…these radar images are acquired from ascending orbits with 44 and 34 degree and descending orbits with 41 and 30 degree incidence angles. I think some of you may have come across similar issues while processing a time series. My question is how is it possible to correct for this incidence angle differences and use all the images as one dataset?
you can calibrate to Beta0 and then perform Terrain Flattening in order to reduce the effect of topography on your image.
But generally, information in shadow areas (slopes facing away from the sensor) is lost and cannot be restored.
Hi, ABraun.
Your above answer solved my present part of confusion, thank you! I have a few more questions to ask you. I used sentinel-1 data(VV+VH,IW,GRD) to do long time soil moisture inversion.The yellow area is the research area. The study area is located at the intersection of the image data of two different orbits. The incident angles of the study area in the left image range from 36 to 36.7 degrees, while the right image ranges from 45.5 to 46 degrees.
Here’s what I did:
Orbit correction > Radiometric- Calibrate>Multilooking > Terrain Correction— Range-Doppler Terrain Correction > subset > To dB > Fliter ;
Question 1: Is the sentinel1 data corrected for its incident Angle effect at the ground station or during the processing I mentioned above?
Question 2: In the same research area, are the pre-processed results of images with different incident angles obtained from different orbits greatly affected by the incident Angle effect? If so, do you have a good solution?
Radiometric calibration to Sigma0 corrects for changes in the global (image wide) incidence angle, yes. But it is advisable only to combine images with the same looking direction.
If you want to correct topographic changes as well, you calibrate to Beta0 and apply Radiometric Terrain Flattening. This operator makes use of a DEM (ideally SRTM 1Sec) to adjust the local incidence angle as well and produces Gamma0 as a higher level calibrated product.
Thank you very much for your answer,ABraun.
I’d like to confirm some further information.
Both of my left and right images are descent data. Both images are viewed from left to right. I want to make sure that this is the same looking direction as you said?
In terrain correction, I have used SRTM 1Sec for topographic changes correction. Gamma0 can be converted to sigma0 in SNAP? Because the algorithms I studied in the field of soil moisture inversion mostly use sigma0.
When you have a comparably flat study area (or at least the areas in the image which are analyzed), there is no need to calibrate to Gamma0. So radiometric calibration to Sigma0 in the beginning would be ok.
I would like to integrate S1 SLC images from both orbits to increase dates available to study an eruption sequence at Semeru Indonesia. The objective would be to create RGB amplitude images with amplitude before after and difference between dates respectively in each band. Is it therefore possible to combine images from both orbits for interesting results ?
If so, what is the correct workflow to follow ?
Orbit filter>Calibration (sigma or beta ?) > Split>deburst>radiometric terrain flattening ? > range doppler correction
I have seen also your previous post [S1 radiometric correction] but I am still slightly confused on what the suitable workflow is for a steep volcano.