Problem with loading screen for S-1 Back Geocoding

sorry, this goes beyond my mandate in this forum. If I offered this to you, other would expect it as well.
Maybe you have a colleague or a supervisor who can discuss this with you?

In this moment don’t, do you know someone who you can recommend me?

Thank you.

not really, because this procedure is not so complex and actually should work.

What happens when you select GETASSE30 (AutoDownload) in the BackGeocoding?

I am going to show everything that I have done today:

For Images
S1A_IW_SLC__1SDV_20191212T105226_20191212T105253_030314_03779B_9982.zip
S1A_IW_SLC__1SDV_20191224T105225_20191224T105252_030489_037DA8_6D12.zip
which are that I have showed you in these days, GETASSE30 (AutoDownload) didn’t work, because slave image doesn’t show data.

But I tried with images of another time, specifically of november and december of 2020
S1A_IW_SLC__1SDV_20201112T105233_20201112T105300_035214_041C93_A76F.zip
S1A_IW_SLC__1SDV_20201230T105231_20201230T105258_035914_0434D0_59AF.zip
GETASSE30 (AutoDownload) worked and showed data for both images, master and slave


So for those images the problem doesn’t persist, but for images of 2019 it does. Still we don’t have an absolute solution but I am more quiet that in some images I don’t have that problem.

I need to know until what time of the year what images don’t show this problem, because I need to create a time-series and as you told me in few weeks I have to use at least 20 SAR images, I have two that I can use haha.

But now I have another problem. It is about Unwrapping step.

For the images of final 2020, in snaphu unwrapping happens this:

image
I put Phase_ifg_VV_30Dec2020_12Nov2020.snaphu.hdr as source product, that file is in a folder that I created in snapphu export step

image
When I run in Processing Parameters appears this message, I think that something went wrong.


And I know that in the folder that I used has to appear another file,
UnwPhase_ifg_VV_30Dec2020_12Nov2020.snaphu.img, but it doesn´t exist


For that reason I can´t continue with the process in snaphu import, because I need
UnwPhase_ifg_VV_30Dec2020_12Nov2020.snaphu.img file

So I don’t know what to do here.

if GETASSE30 worked for the one pair, it should also work for the other. Maybe it is worth to download both zip files again and repeat the processing from the beginning.

About the snaphu error - have you filtered your data before unwrapping? How does the interferogram look at all? Snaphu abnormal abortion while unwrapping

Yes I filtered before the unwrapping, with Goldstein Phase Filtering

Interferometric > Filtering > Goldstein Phase Filtering

image

I used those parameters.

Now it worked.

I am going to say what I made:
I changed the method to MST and it worked

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Another thing, I generated a displacement map of the zone. I exported it to Google Earth


As you can see in the west there is a volcano and in the east a city.
With displacement map both (volcano and city are in color gray) and scale is in meters, I would like to know if the results could be possible. I think that displacement in volcano is between 0.034 meters to 0.093, so that means that deformation was positive, but I don’t know how to interprate it right.

Could you help me please?

Thank you.

I have repeated the process for the same area and the same pair and the result is different, now the deformation is negative. I don’t know what is the correct answer.

I can’t tell if the displacement is feasible in your region. How does the interferogram look? Maybe you can share screenshots, also of the unwrapped interferogram.

I have done for same pair the exercise, and the results were different, why could happen that?

This is the differential interferogram for first exercise

Unwrapped interferogram

This is the differential interferogram for another exercise

Unwrapped interferogram

You can see that are different, very strange because they are the same images.
The only thing that I changes in the process was:
For first exercise I put derampDemodPhase_mst file when I made Back Geocoding, for second exercise I didn’t, and for first exercise I put topo_phase_VV file in Goldstein Filtering step, for second exercise I didn’t, as you can see below

I realizedt that I made a mistake in stack, because the name of the file for second exercise is S1A_IW_SLC__1SDV_20201230T105231_20201230T105258, I have done something wrong because it should be like the first exercise
S1A_IW_SLC__1SDV_20201112T105233_20201112T105300, because master image for me is november image. probably the problem is related with that, but I don’t know.

According to my understanding, the interferogram contains too much noisy areas. Unwapping will lead to random patterns here which are not related to surface deformation. Especially completely isolated patches of noisy areas are a problem.
As you see, the phase variation on the areas of highe coherence (those which have a clear pattern in the interferogram) are hardly effecting the patterns in the unwrapped interferograms, and the random phase variations superimpose the actual signal which you want to see.

Is your study area covered by vegetation? Such areas suffer from low coherence and therefore phase decorrelation which leads to the observed noise.

Almost all my country has a lot of vegetation, Colombia is a tropical country with a lot of biodiversity , the only place with low vegetation is in the north of Colombia, in the desert of La Guajira, but its an exception.

My study area is a volcano, I searched active volcanos and in Colombia we have many, the best study volcanes are volcanoes of the South of Colombia, one of the most important is Volcán Galeras, the volcano that I have showed you, it’s a volcano near to the city of San Juan de Pasto, I just need to apply interferometry in the volcano, not in another area and I saw that the vegetation is not so much like in suround area.

So, only for volcano area, what do you think, the result could be possible?


blue circle shows volcano zone

I’m not an expert for volcanoes, sorry. I recommend comparing your results to some of the published results for similar volcano types (strato, shield or dome volcano). It depends on what kind of displacement you expect with respect to the looking direction. A general uplift, a redistribution of materials, a tilting of the volcano? Each of them results in different fringe patterns.
It also makes a difference if there is a caldera or not.

Examples:
grafik
source

grafik
source

grafik
source


source

If you are only interested in the area within the blue circle, I recommend to clip the interferogram before unwrapping.
The smaller the proportion of noisy areas, the lower is the chance for false patterns induced by vegetated areas.

Can I clip the interferogram with subset tool before unwrappe it?
If I can do that, in what step do you suggest me? deburst, dinsar, multilooking…? or when I after to create the interferogram?

you can clip after debursting the interferogram.

Just make sure you select the subset in the export and also as reference in the import.

“Just make sure you select the subset in the export and also as reference in the import.” Sorry I didn’t understand good.

I just created clip file and it worked.

Thank you mister.

good job!
I just wanted to emphasize that you need the subset as reference product when you want to import the unwrapped phase again.

Ok.

I am going to make other proofs with other pairs and see if the initial problem doesn’t persist with other images.

Thank you for your guide.