The dry air absorbs moisture from the lake, which fuels the snowfall and gives the air more latent heat energy that is released as it condenses into a cloud.
Flowing over the warmer lake water, the temperature of the cold air rises, and as it warms, the air lifts higher into the sky and becomes more unstable.
After blowing over the smooth surface of the lake, the air plows into the uneven surface of the land, slows down in the friction, and piles up, rising farther into the sky.
And the cold air gets another lift from the hills and higher terrain it encounters above the far shores.
In the summer, the Great Lakes have a very different effect on the weather of the region. Because the water of the lakes is often cooler than the surrounding air this time of year, they can dampen thunderstorm activity.
Maritime tropical air masses from the Pacific sometimes sweep northeastward over California, and when they do, they can bring heavy rains and flooding. Similarly, maritime tropical air from out of the Gulf of Mexico and Caribbean Sea can fuel flooding storms as it moves up the Mississippi and Ohio valleys.
Summer air masses
The continental polar air that brought frigid misery during winter often has a welcome cooling effect over much of the United States in summer. Fair weather generally prevails over the Northern Plains and Midwest when continental polar air is around, occasionally reaching even the Gulf of Mexico with pleasant dry air.
Maritime tropical air masses from the Atlantic Ocean, the Caribbean Sea, and the Gulf of Mexico spend a lot of time over the eastern two-thirds of the United States during summer, especially the Southeast, bringing warm temperatures and high humidity.
Continental tropical air forms over the big desert regions of northern Mexico and the U.S. Southwest in summer, keeping things hot and dry.
News from the Fronts
During the most powerful storms of winter and summer you will probably find two air masses of very different qualities — different temperatures and humidities — crashing into one another. When upper winds and other conditions are right, this is where you will see a powerful mid-latitude cyclone with well-defined fronts that bring rain or snow over big sections of the country. In spring and summer, along these fronts can be long lines of severe thunderstorms that can form tornadoes when conditions are right — or wrong!
It might look like a rainy or snowy mess from down below, but a front, the transition zone or line between two distinct air masses, has a certain shape or structure to it, depending on what’s going on.
Cold fronts
When a cold front moves into space occupied by warmer air, it forces the warmer air to rise up and over the leading cold wedge. This is because cold air is denser, or heavier, than warm air and sort of bullies it out of the way. As the warm air rises, it mixes with the cold air and condenses into big clouds. Figure 3-3 shows what happens with the passage of a typical cold front.
FIGURE 3-3: These diagrams illustrate what usually happens when cold fronts and warm fronts come along.
Often, these cold fronts are carried along by westerly winds, which tear away the tops of these clouds and carry them out far in advance of the approaching front. The first sign of an advancing cold front can be the appearance of these high clouds, followed quickly by a thickening sky. And then a line of heavy thundershowers develops as the front passes, followed by steadier and gradually lighter rain. A typical cold front moves about 30 miles an hour, often traveling to the south and east.
Warm fronts
When a warm front moves into the space occupied by a retreating cold air mass, it develops a completely different precipitation pattern than an advancing cold front would. While a cold front digs in underneath a warm air mass, because its air is denser, the lighter air of a warm front rides up above the cold air it is replacing. In this rising warm air, clouds form far out ahead of the advancing warm front’s boundary. Hundreds of miles ahead of the surface edge of a warm front, the cloud cover slowly thickens, finally bringing rain or snow. All this happens long before the surface edge of the warm front finally passes. When that happens, the sky is usually clear. A typical warm front can travel about 10 to 20 miles per hour, most often moving north and east.
THERE GOES THE MOON
Sailors and poets and ancient thinkers all favored the idea that the moon has a lot to do with how things go here on Earth. A “ring around the moon” was seen as a sign of impending storminess, for example, but none of it is the moon’s doing.
That ring or halo is moonlight — sunshine reflecting off of the moon’s surface — scattering as it encounters thin clouds in the atmosphere. They might be high in the atmosphere, those clouds, but they are nowhere near the moon.
But the moon has this important indirect impact on weather: The tug of its gravity makes the tides of oceans and very large lakes rise and fall, and during powerful coastal storms, high tides can make the difference between inconvenience and natural disaster.
Stationary fronts
A stationary front, as you might expect, isn’t going anywhere, at least for the time being. But don’t let its lack of motion fool you. A stationary or slow-moving front can mean real trouble. A lot of weather can be happening around a front that isn’t moving. Sometimes, when warm humid air travels over the frontal boundary, rainfall can occur over large areas, and because the front isn’t moving, the rain may stay long enough to cause flooding.
Occluded fronts
As a winter storm progresses, the large wedge of warmer air between the warm front and the cold front gets narrower. The cold front travels faster than the warm front, and beginning near the low-pressure center of a mature storm, it eventually overtakes it. This new boundary is called an occluded front. On one side is cold air from behind the cold front. On the other is cool air that the warm front was flowing over. Above the front is warm air that has been cut off from the ground.
Here Comes the Sun
