Tucson Lenticular Clouds

Unfortunately, because I took the picture with my iPhone, the clouds are a bit hard to see. But, if you look closely at the clouds in the center of the image, you’ll notice that they’re rounded and somewhat “flying saucer” shaped. Here’s a better picture of the same type of clouds, that I took in Mt Shasta, CA:

Mt Shasta Lenticular Clouds

These types of clouds are called Lenticular clouds, and they are stationary, lens shaped clouds that form at high altitudes. Typically, these clouds form on the downwind side of a mountain where warm, moist air is flowing, creating a series of large-scale standing waves. If the temperature at the crest of the wave drops to the dew point, moisture in the air may condense to form lenticular clouds. As the moist air moves to the trough of the wave, if it’s warm enough, it may evaporate back to vapor. Under certain conditions, long strings of lenticular clouds can form near the crest of each successive wave, creating a formation known as a wave cloud. And, because these clouds have a characteristic lens appearance and smooth saucer-like shape, they are often mistaken for UFOs (or “visual cover” for UFOs).

The air in the area of lenticular clouds is great for gliders, who seek out and ride the updrafts associated with the standing waves, but not so great for pilots of powered aircraft who are concerned with the turbulence. “Wave lift” often found in areas with lenticular clouds is often so smooth and strong that gliders can sail to incredible heights and distances. In fact, the current gliding world records for both distance (over 3,000 km; 1,864 mi) and altitude (15,460 m; 50,721 ft) were set using such lift.

I’ve always loved how lenticular clouds look. In almost every trip past Mt Shasta in California, where I have been able to see the mountain, lenticular clouds are present. I’ve also noted them quite frequently on the top of Mt Rainier in Washington. They are very beautiful clouds, but you can rest assured there are no aliens hiding in them!

I hope you like the new direction of this blog, and I look forward to and welcome your comments. Thanks for visiting “Ive Been Thunderstruck!”

An awesome looking supercell!

As a novice storm chaser, I’ve been learning a lot about what it takes to actually form a thunderstorm each day. Fortunately, some local weather forecasters (ErinJordanKOLD, PickeringKOLD and ChuckGeorgeKOLD) have been providing daily storm updates on Twitter, and have parsed out some science knowledge at the same time. One of the things they constantly mention, and which is an important component of thunderstorm formation, is dew point.

According to Wikipedia, “dew point is the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water (all links courtesty of copying from Wikipedia).” Dew point is also associated with relative humidity, in that a high relative humidity indicates that the dew point is closer to the current air temperative. As noted above, dew point is given in degrees (for instance the current dew point temperature in Tucson is 51F). A relative humidity of 100% means that the dew point temperature (temp at which dew forms) is equal to the current temperature, and that the air is maximally saturated with water (can hold no more water, and thus condenses).

Dew point is important for reasons other than storm formation. The higher the dew point, the more uncomfortable it feels outside. In periods of high relative humidity and high dew points, the ability for sweat to evaporate from the body decreases, which reduces the cooling effect related to sweating. That tends to make us hotter, and makes being outside a bit more dangerous.

That’s all good info, but I really wanted to know how dew point influences thunderstorm formation, because I simply love those storms! With an estimated 40,000 thunderstorms occurring world-wide on any given day, and the high occurrence of such storms in areas where factors influence dew point, there must be a correlation, and a direct one at that.

Turns out that dew point plays a great role in thunderstorm formation. There are three factors – moisture, instability, and a lifting mechanism – that contribute to thunderstorm formation. Typically in the Southwest United States (Arizona in specific), dew point levels are very low…in the teens or lower. But each summer a shift in air flow occurs, drawing moisture up from Mexico. That infusion of moisture into the atmosphere leads to higher dew points, and when they have reached the mid-50s for three consecutive days, then the monsoon has officially begun!

Dew point is essentially the low level moisture that actually fuels thunderstorm development. Severe thunderstorms are more likely to occur when the dew point is 55F or higher, providing more potential fuel for the storm as the dew point increases. There are other moisture factors as well, which change in significance as you move higher in the atmosphere. But, for purposes of this discussion, it’s the low level stuff that counts.

So, there you have it. The more moisture in the lower levels, the higher the dew point, the greater the chances of a thunderstorm developing!

Dunn Says Speed Up!