• After witnessing the continued decrease of involvement in the SpotterNetwork staff in serving SN members with troubleshooting issues recently, I have unilaterally decided to terminate the relationship between SpotterNetwork's support and Stormtrack. I have witnessed multiple users unable to receive support weeks after initiating help threads on the forum. I find this lack of response from SpotterNetwork officials disappointing and a failure to hold up their end of the agreement that was made years ago, before I took over management of this site. In my opinion, having Stormtrack users sit and wait for so long to receive help on SpotterNetwork issues on the Stormtrack forums reflects poorly not only on SpotterNetwork, but on Stormtrack and (by association) me as well. Since the issue has not been satisfactorily addressed, I no longer wish for the Stormtrack forum to be associated with SpotterNetwork.

    I apologize to those who continue to have issues with the service and continue to see their issues left unaddressed. Please understand that the connection between ST and SN was put in place long before I had any say over it. But now that I am the "captain of this ship," it is within my right (nay, duty) to make adjustments as I see necessary. Ending this relationship is such an adjustment.

    For those who continue to need help, I recommend navigating a web browswer to SpotterNetwork's About page, and seeking the individuals listed on that page for all further inquiries about SpotterNetwork.

    From this moment forward, the SpotterNetwork sub-forum has been hidden/deleted and there will be no assurance that any SpotterNetwork issues brought up in any of Stormtrack's other sub-forums will be addressed. Do not rely on Stormtrack for help with SpotterNetwork issues.

    Sincerely, Jeff D.

Why is Death Valley so hot?

The rain shadow effect from the Sierra Nevadas, when air encounters the Sierras, on the windward side, it is force to rise, orographic uplift, moisture is condensed out and when air descends on the back side or leeward side of the mountains, air is compressed which leads to warming of the air, and the moisture is evaporated, helping to make Death Valley a desert. To some degree the influence of the nearby subtropical high, which is around 30 deg N latitude Death Valley is around 35-36 deg N latitude. which promotes subsidence in the atmosphere, leads to air being compressed and is warm and less relative humidiites. Also being below sea level can lead to further heating. Be interesting to see a sounding from Death Valley, to what the lapse rates would be with all the stong surface heating.

Mike
 
Be interesting to see a sounding from Death Valley, to what the lapse rates would be with all the stong surface heating.

There is a RAOB site at Desert Rock NV, which is about 35 mi east of Death Valley.

If you extrapolate the temperature trace on the Desert Rock NV sounding dry adiabatically down to 1020mb you'd probably have a good idea of what a sounding from Death Valley would look like. Sure enough, that would have worked today - the high at Desert Rock at 3200 feet above sea level was 102F, while the high at Death Valley at 194 feet below sea level was 118F.

Here is Sunday afternoon's sounding for Desert Rock NV....note how the lapse rates are pretty much dry adiabatic from the surface up to about 630mb.

[Broken External Image]:http://home.earthlink.net/~jckssjeff/DRA04071900.gif
 
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