Closed
Description
I am interested in modeling clear sky irradiance at different altitudes, including the stratosphere. My test run using my current clear sky setup with ineichen at an altitude of 20km produced an answer significantly greater than the dni_et I used.
I'd appreciate any hints as to whether I need use something other than the default linke turbidities table, or whether there is a better algorithm for clear sky to use for high altitude modeling.