Today is a beautiful sunny day in Missouri, so I brought my laptop out to the porch. When I work outside, I can’t help but watch the wind and the clouds, hyper-aware of the sounds in my surroundings. As the distant whir of a jet passed far above, I whimsically observed that the sound was coming from a point well behind the plane itself. Replacing whimsiness with my insufferable engineering mindset, I started rattling off some quick calculations, literally on the back of an envelope.
The source of the sound was approximately 30 seconds behind the plane as it flew overhead, which means that the plane was about 6 miles straight up because sound travels a mile every 5 seconds. This is a reasonable answer since it is close to 40,000 feet, the cruising altitude for commercial jetliners. The speed of sound is a useful conversion factor, and I use it all the time to tell me the distance of lightning strikes. There are a few ways to calculate the jet’s speed: you could again use the speed of sound when the jet is in the distance, or you can estimate its angular velocity as it passes overhead at a known altitude. I used the latter, comparing the perceived length of the plane’s vapor tail a minute apart to estimate an angle. This calculation pegged the plane at 550 mph, again reasonable at around 90% of the speed of sound. It took 6 minutes for the plane to leave my view after passing directly overhead, which means I could see it when it was over 100 miles away. Not coincidentally, you can often see over 100 miles from the window seat of a plane. The farthest view from a mountaintop I have ever seen was another mountain 80 miles away, but increasing in altitude from 1 to 6 miles does wonders for visibility, due to both the curvature of the earth and the lower particulate matter concentrations higher up in the atmosphere.
A line of clouds materialized in the distance. To me, it’s no mystery how far away they are or how long they would take to approach. Meteorologists use a metric called “lifted condensation level” (which basically means cloud height) to forecast rain showers and severe thunderstorms, and due to the sharp temperature gradients in our atmosphere, the base height of cumulus clouds is almost guaranteed to fall between 1-2 kilometers. Lower LCL values beget higher chances for severe weather, and, conversely, thunderstorms have lower cloud bases than fair-weather cumulus. You can calculate the LCL using the dew point or relative humidity…I used to tell my chemical engineering students that those weather apps that tell you temperature, humidity, and dew point are redundant because with two of those values you can calculate the third. I also used to tell them to, when they’re having deep conversations with a significant other while gazing into the sky, impress their date by calculating the cloud height on the spot. Anyway, the point of all this, if there is one at all: there are a lot of interesting things to learn by keenly observing your surroundings. The world is full of not only fascinating math but also a natural beauty that defies calculation.