Gradient management remains, arguably, the most subjective, by-guess-and-by-golly aspect of astronomical image processing. PI has done a great job of making most other processing very mathematically (and scientifically) rigorous. I look forward to gradient management becoming a substantially objective process, as well.Wow, thats great news. I honestly think that the MARS project will be the biggest leap in image processing capabilities since some years!
That's exciting news, thank you. Looking forward to using it. Also cool to hear that custom reference images will be a built-in option. Now to sit and find out how many weeks "weeks" is.We are currently working on the first version of the MultiscaleGradientCorrection tool. It will use a database with preliminary MARS data for most of the northern hemisphere and will also allow you to select custom reference images.
The complexity of this process is considerable, but if all goes as expected (and we have reasons to be optimistic), it's a matter of weeks.
We are currently working on the first version of the MultiscaleGradientCorrection tool. It will use a database with preliminary MARS data for most of the northern hemisphere and will also allow you to select custom reference images.
The complexity of this process is considerable, but if all goes as expected (and we have reasons to be optimistic), it's a matter of weeks.
Great news, but what about the southern hemisphere?
The original MSGR article gives some good info on that. https://pixinsight.com/tutorials/multiscale-gradient-correction/index.htmlJust for future planning purposes, what approximate ratio between focal lengths are we talking about?
I know that this is not a definite number, but a general range of ratios would be helpful to estimate what is needed for generating ones own reference images.
CS Gerrit
We are acquiring the first layer of actual MARS data (so far, we have acquired provisional data for testing/design purposes) under strictly controlled conditions from southern Spain with two dedicated observing stations. This requires significant economic, time, and logistical investments that we can only afford for the northern sky for now.
For the southern sky, we depend on user-contributed data, which we are gathering through the MARS data upload system. Logically, user-contributed images vary largely in all aspects related to acquisition conditions, so they require a lot of work to generate coherent and compatible data sets. We are also working on this, but it requires time and additional development efforts.
It will use local databases, similar to local Gaia and APASS star catalogs and XPEH ephemerides files (although completely different in structure and contents). No Internet connection will be required.Will the process use a downloaded catalog or require an Internet connection?
Great, glad to hear that. All my projects I haven't started are in a holding pattern for the next while.
Or setup a remote pier like I did. (but it is so worth it)I was thinking the same thing.
That, and I won't need to move to a cabin in the Canadian wilderness to get good images.
I image from pristine skies, almost entirely clear of any light pollution induced gradients. But there are plenty of sources of natural gradients, that exist in the darkest of skies. No imaging location on Earth will get us away from needing gradient management tools.I was thinking the same thing.
That, and I won't need to move to a cabin in the Canadian wilderness to get good images.
After I started imaging from New Mexico, I learned how "bright" a quarter moon is. From a city it doesn't look bright, but from a B1 site I don't need any kind of flashlight while walking around.I image from pristine skies, almost entirely clear of any light pollution induced gradients. But there are plenty of sources of natural gradients, that exist in the darkest of skies. No imaging location on Earth will get us away from needing gradient management tools.
I've seen my shadow cast by Venus. I've had gradients from zodiacal light, from gegenschein, from skyglow, from cloud layers too thin to be apparent to the eye. And, of course, from even very crescent moons.After I started imaging from New Mexico, I learned how "bright" a quarter moon is. From a city it doesn't look bright, but from a B1 site I don't need any kind of flashlight while walking around.
I'm in remote Alaska and frequently deal with aurora gradients.I was thinking the same thing.
That, and I won't need to move to a cabin in the Canadian wilderness to get good images.