One advantage of the API method is that it allows high resolution vertical velocities to be measured between 50-120 km. Here is an example plot from our 9.12.2011 measurement. Around noon (7000 seconds in to the measurement) there are also some tropospheric echos.
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjHkAC6jSpgmxI-hXKkQmrhfDpeuGHjmbcvpnG_3dmXDQknqDyS3x5u7ddRdUEZDew22vkkcHJ4t0y-QlPc705opN2-JoDI81NBUB6IZjnSU5HhOHq8l7cIhJbSh18dGs7qtJ-en2GXeNA/s400/Screen+shot+2011-12-10+at+8.02.34+PM.png) |
Vertical velocities in the 60-120 km region measured using the API method with the EISCAT heater. |
No comments:
Post a Comment
Note: only a member of this blog may post a comment.