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Dan Chaffee wrote:
Dan C, Most of my measurements are now from Mt Graham taken at the VATT. I have some data from the ridge at Mt Hopkins, Mt Bigelow and a few hours at kitt peak. I am going to in line mode now, see me below On Sat, 04 Dec 2004 17:03:37 -0700, Dan Mckenna wrote: I have been looking at this for a few years as well and have recently come back from an observing run where I used a SCIDAR to measure the altitude profile of the seeing while also measuring the image quality from one second exposures. Dan, Can you give us the location of these measurements? I am most curious if other regions that experience different combinations of low level buoyancy, Think in terms of atmospheric gravity waves. A good book is An Intro to Atmospheric Gravity Waves C. J Nappo also Small Scale Processes in Geophysical Fluid Flows L H. Kantha & C. A. Clayson Has good information on waves, drainage flows, and flows over complex topography. The nocturnal ground inversion is a place that can have intense wave activity that can dominate the seeing. If the area of interest is driven by a drainage flow it gets more complicated. Drainage flows exist even for slopes less than 1 degree. mid level inversions, and different shear profiles would lead you to the same generalizations. Mid level inversions are also places of gravity wave creation, if it is associated with a jet, becomes a place where ducted waves in the jet propagate up or down. I see wind shear regions in my data and in some cases the wind shear regions are due to propagating Gravity waves. DC |
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On Sun, 05 Dec 2004 09:54:58 -0700, Dan Mckenna
wrote: Think in terms of atmospheric gravity waves. A good book is An Intro to Atmospheric Gravity Waves C. J Nappo also Small Scale Processes in Geophysical Fluid Flows L H. Kantha & C. A. Clayson Thanks, I'll be on the lookout for them. Dan |
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