- #1
DielsAlder
- 5
- 0
Hi
I am currently involved in atmospheric remote sensors on board a satellite which collect back-scattered and reflected solar radiation to provide atmospheric composition measurements through an algorithm based on Differential Spectroscoy. I am currently involved in studying the physical principles behind the operation principle and retrieval step for these instruments. Examples are TROPOMI on board the Sentinel-5P and OMI (Aura). I would like to clarify some general aspects through some questions regarding their viewing. I would like to post an exercise and I would appreciate it very much if you could assess if my conclusions are correct . Thanks very much.
I am currently involved in atmospheric remote sensors on board a satellite which collect back-scattered and reflected solar radiation to provide atmospheric composition measurements through an algorithm based on Differential Spectroscoy. I am currently involved in studying the physical principles behind the operation principle and retrieval step for these instruments. Examples are TROPOMI on board the Sentinel-5P and OMI (Aura). I would like to clarify some general aspects through some questions regarding their viewing. I would like to post an exercise and I would appreciate it very much if you could assess if my conclusions are correct . Thanks very much.