toolbox
Differences
This shows you the differences between two versions of the page.
| Both sides previous revision Previous revision | Next revision Both sides next revision | ||
|
mark:main [2014/12/10 12:06] mdw12 |
mark:main [2014/12/10 12:07] mdw12 |
||
|---|---|---|---|
| Line 98: | Line 98: | ||
| This effect can be clearly seen in an example of APS (Figure ##), where differences in delay of up to 12cm can exist across a scene, arising from differential changes in the water vapor content of the air. Figure ## shows the map of average apparent velocities that would result from the application of a StaMPS-like algorithm to a series of 12 APS made from 13 maps of atmospheric delay. Differences in velocity on the order of 2 cm/yr are seen over short length scales (~5km), smaller than the StaMPS scene over St Helens (Pictured). | This effect can be clearly seen in an example of APS (Figure ##), where differences in delay of up to 12cm can exist across a scene, arising from differential changes in the water vapor content of the air. Figure ## shows the map of average apparent velocities that would result from the application of a StaMPS-like algorithm to a series of 12 APS made from 13 maps of atmospheric delay. Differences in velocity on the order of 2 cm/yr are seen over short length scales (~5km), smaller than the StaMPS scene over St Helens (Pictured). | ||
| + | |||
| + | {{:mark:av_vel.jpg}} | ||
| **Discussion and Conclusions** | **Discussion and Conclusions** | ||
