Spring is the time when our local atmosphere is most unstable, often percolating in upward and downward motions like hot cereal in your stove-top saucepan.
The visual expression of such unstable motions is cumulus convection, ranging from relatively benign fair-weather cumulus to towering cumulonimbus.
On Tuesday, the atmosphere became unstable and a full range of cumulus clouds was evident.
During the afternoon, relatively shallow cumulus clouds had formed by 2 PM (see below from the Seattle PanoCam on the Space Needle). No precipitation was evident underneath them.
By 5 PM, following afternoon surface heating, vertical turrets start to form, indicating greater instability and vertical development.
The 6 PM image showed even more vertical development and the formation of two cirrus anvils (the flat, elongated objects at the top of the image.)
30 minutes later the anvils had explored in size. Very impressive! It was raining underneath the big cumulus clouds and lightning was observed
Cumulus clouds like this are a sign of vertical instability driven by large temperature changes in the vertical.
Stability 101
Most of the time the atmosphere is stable. You push some air upwards and it comes back down.
But if the temperature declines with height rapidly enough, the situation changes. In this case, a displaced air parcel can accelerate upwards.
The explanation for this behavior is something we describe in detail in my department's classes, but the essential point is this:
When temperature cools rapidly with height it becomes easier for an air parcel to be warmer and less dense than the surrounding air. And such warm/less dense air parcels tend to be buoyant and rise.
Think of a hot-air balloon! (see below)
Here in the Pacific Northwest, the change in temperature with height is greatest during the spring. That is why this is the best time of the year to see impressive cumulus clouds.
But why spring, you ask?
During the spring, after a long winter, the temperatures aloft are quite cold...in fact, the coldest of the year. To show this, below are the temperatures around 10,000 ft (700 hPa pressure) at Forks, WA, on the NW coast.
Lowest temperatures in March and April. Quite cold in early May.
While temperatures are cold aloft, solar heating is getting very strong now, particularly on days without extensive clouds. Below is the plot of solar radiation reaching the surface in Seattle for the last year. Getting pretty strong lately. Keep you sunscreen handy.
May 2 sun is roughly as intense as early August!
So with strong heating at the surface and cool temperatures aloft, there is often a very large change in temperature with height during early spring, which fosters lots of cumulus clouds....from shallow ones to deep thunderstorm clouds.
Just to drive the point home, here is a plot of the change in observed temperature with height (termed the lapse rate) at Forks/Quillayute between the surface and 3 km (about 10,000 ft). Very high this time of the year.
Finally, you can see the growth of cumulus during the day produced by increasing temperature change with height. Let's start with the visible satellite image over eastern Washington on Wednesday morning around 8 AM. No clouds over the Columbia Basin.
By 2 PM, with plenty of solar heating at the surface, the temperature change with height is greatly enhanced and instability has developed, leading to lots of cumulus clouds.