Hi Guys,
I have a question for you weather guys out there. I flew on Saturday around noon and there were some strong thermals around 200ft AGL. It made the approach very uncomfortable and was really tossing the plane around. If I would have known the conditions were going to be like that, I would have not brought a passenger. Especially one who has never flown in a small airplane.
My questions is, what is the best way to check for conditions like this?
Anyone have any advice?
Kevin
Other than the rules-of-thumb mentioned above, you can do what we glider pilots do: add a skew-T check to your wx briefing. In a nutshell, a skew-T graph will show you what you most want to know: at what altitude you can expect strong lift. They're also handy for predicting cloud base altitudes... because (unfortunately for VFR pilots) where lift peters out is usually where the clouds start to form.
Here is a good source, although there are many:
http://www.drjack.info/BLIP/RUC/
...and here's one of the clearer explanations I've seen on how to read and use them. Tailored for pilots
seeking lift, but just replace "good" with "bad" wherever mentioned, and it will work for you.
https://www.ssa.org/myhome.asp?mbr=3981940746&show=blog&id=141
... these diagrams can yield a ton of varied info, but for your flight planning purposes, you just need the trigger temp (surface temp at which the conditions aloft will most likely occur) and the altitude where lift (unstable air) will be less energetic. Hint: that altitude is usually where the two most important lines on the graph intersect.
Because these graphs are only based on twice-a-day balloon soundings , and covering a fairly limited area, you should always keep the thumbnail rules in mind and pay attention to what the sky is doing as you fly along.
Best thumbnail-rule advice I can give you is that if you see flat or concave-bottom cumulus clouds with "crisp"-looking tops, the air is going to be bumpy below them, possibly all the way down to the surface. They don't have to be very big clouds... in fact, once you start looking for these visual signs, you will learn how to spot "newborn" Cus, and they often can indicate a very strong thermal that has just pushed a moist parcel of air up to where it's cold enough for the cloud to become visible. And if there is wind present, the cloud itself might be downwind a ways from the surface "hotspot" that is warming the air... thermals "lean" downwind to some extent.