Copy
www.rotorworks.com                                                                     (780) 778 6600

December 2017

A very merry Christmas from everyone at Rotorworks. We hope you've all had a great 2017 and are looking forward to 2018. We've had a busy end to the year so far and have been working from Rainbow Lake, Alberta to Snow Lake, Manitoba. This month we are going to have a refresh on wind shear and temperature inversions.

For those of you who have regularly driven through Whitecourt over the years you'll know we used to have a billboard by the side of the road. It blew down in the wind a few years ago and we've finally got a new one made and put up. Here's the before and after.
Review
 
Wind shear is a "difference in wind between two separate points." It can be vertical or horizontal and the difference can be in speed and/or direction. 

Taken from Air Command Weather Manual Page 11-1
Temperature Inversions

I'm sure you all remember the international standard atmospheric lapse rate from your ground school (it's 1.98°C per 1000 ft in case you need a hint) but it's that time of year again when you may have noticed your outside air temperature gauge increasing with altitude.
 
This year in Whitecourt we've been getting a lot and many with some big temperature changes. Some days it's been 15 degrees centigrade warmer at circuit height than on the ground. So how are these inversions formed and what does it mean for your flying?

The most common way this time of year is on a clear night (although thunderstorms and frontal systems can also cause wind shear). With the suns rays no longer heating the surface the ground radiates it heat out and the now cold ground cools the air above it. Typically these inversions are fairly shallow. Usually between 1000 - 2000 ft above ground level although can go much higher.
You may have noticed the horizon looking a little like the photo on the right. A flat mountain top with valleys and ridges that appear and disappear as you climb or descend. This is due to the different air temperatures having different densities. The light traveling through is bent or refracted causing you to see things that aren't really there.
With this change in temperature and air density you can expect to encounter some wind shear. This change in wind speed and/or direction can be barely noticeable to quite dramatic. It may change the height you were planning to fly at. By climbing or descending you may be able to switch from a headwind to a tailwind. You may find it considerably smoother above the inversion than below it. The most important consideration with wind shear is when making your approach to land. Always keep an eye on where the wind is from. Just because you started your approach into wind doesn't mean you'll still be into wind closer to the ground. If you're aware of this you might not need to change your approach but the wind can bite you when it's not where you think it is.
Review
 
Low Level Wind Shear (LLWS). If wind shear is reported or forecast to be at or below 1500 ft above ground level it will be shown as LLWS. If it is reported by a pilot it will be issued as an Urgent Pirep. 
 
Jonathan came back at the start of the month to finish up his Bell 206 Jet Ranger endorsement. Thank you to Ridge Rotors for the use of the Jet Ranger. Give us a call if you've ever considered getting an Astar or 206 endorsement on your licence.
Share
Tweet
Forward
Copyright © *|2017|* *|Rotorworks|*, All rights reserved.


Want to change how you receive these emails?
You can update your preferences or unsubscribe from this list

Email Marketing Powered by Mailchimp