modtran
Differences
This shows you the differences between two versions of the page.
| Both sides previous revisionPrevious revisionNext revision | Previous revision | ||
| modtran [2025/02/19 11:19] – admin | modtran [2025/02/19 13:33] (current) – admin | ||
|---|---|---|---|
| Line 1: | Line 1: | ||
| ===== Radiative Forcing Experiments with Modtran ===== | ===== Radiative Forcing Experiments with Modtran ===== | ||
| - | **work in progress** | + | |
| + | Reproduce with: {{ : | ||
| + | |||
| + | Also at [[https:// | ||
| ==== Using Modtran online at U. Chicago ==== | ==== Using Modtran online at U. Chicago ==== | ||
| Line 40: | Line 43: | ||
| | {{ : | | {{ : | ||
| + | ==== Experiments at 70 km ==== | ||
| + | ^At 70 km, there is a spike in the CO< | ||
| + | |{{ : | ||
| - | ==== The GUI ==== | + | ^ Double CO< |
| + | {{ : | ||
| + | |||
| + | ^Smaller temperature increase is needed to restore equilibrium. Increasing stratospheric temperature is not a good approximation for what happens in restored equilibrium. The stratopsphere would cool. ^ | ||
| + | | {{ :: | ||
| + | |||
| + | ==== The GUIs ==== | ||
| Line 53: | Line 65: | ||
| ^ 0ppm20km ^ 300ppm20kmch136 ^ | ^ 0ppm20km ^ 300ppm20kmch136 ^ | ||
| |{{ :: | |{{ :: | ||
| + | |||
| + | ^ 600ppm70kmt105rh ^ | ||
| + | |{{ : | ||
modtran.1739985572.txt.gz · Last modified: by admin
