Weather For Dummies. John D. Cox
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FIGURE 3-1: Imaginary lines called latitudes divide the world into the Tropics, the polar regions, and between them, the mid-latitudes.
You might think things would be pretty comfortable in the middle of the house, the middle latitudes, where most people live in the world. Not too hot, like Goldilocks said, and not too cold. And certainly it’s true that, on average, the mid-latitudes are less extreme environments to live in. But there’s a catch, of course. In case you haven’t noticed, it is in the middle latitudes where you and I live that a lot of the masses of northbound tropical warm air and southbound cold polar air come together. And when they do, it’s not a pretty picture. In fact, it can get messy.
Those big storms with the long lines that twist together into a whirling low-pressure system on the weather map are called mid-latitude cyclones, or sometimes, extratropical cyclones. You might think of these storms as battles between opposing armies of hot air and cold air. The lines between them are very appropriately referred to as fronts — as in battlefronts. Weather scientists used to think of these storms exactly this way, although now the picture in their minds is more complicated. (The section later in this chapter, “News from the Fronts,” goes into more detail about these clashes.) Nobody who has lived through the devastation of a flood or a blizzard or an especially severe winter needs to be reminded that weather unleashes powerful forces that can do terrible things. You and I are bystanders to all of this, and the only thing to do when a battle is raging is to try to stay safe, warm, and dry.Where the Armies Mass
An air mass is a widespread body of air that has a uniform look to it. Across hundreds if not thousands of miles, all this air looks and acts pretty much alike. This is because it has been parked over a particular region of the Earth long enough to absorb some of its important qualities. It has picked up from the surface a certain temperature and humidity, or moisture content, and like in any good army, these characteristics are fairly evenly distributed. There are no real storms or battles going on or even strong winds — this is all the same army, after all — and pressure, like morale, is fairly high.
Just as different regions of the world have certain characteristics, so do the air masses that form over them. The big differences that make dramatic weather are temperature and humidity — they are warm or cold and moist or dry.
Continental air masses form over land and are dry.
Maritime air masses form over an ocean and are moist.
Polar or Arctic air masses are cold.
Tropical air masses are warm.
The action begins when an air mass moves from its place of origin, usually in response to winds in the upper atmosphere. (To read about what causes wind, check out Chapter 5.) While weather scientists now think of the winds high in the atmosphere as the driving forces behind the storms, the weather in your face still has the look and feel of a battle of air masses. In the Northern Hemisphere, the half of the world north of the Equator, you can be sure that a cold air mass is moving down out of the cooler regions of the north and a warm air mass is moving up from the warmer regions in the south.
A WEATHER WAR ZONE
Every place has its own dangerous weather at one time of the year or another. But did you know that the continental United States gets more violent weather than anyplace else on Earth? This came as a big surprise to early American settlers.
In a typical year, the National Weather Service reports the continental United States can expect these violent weather events:
Roughly 10,000 severe thunderstorms
About 1,000 tornadoes
Approximately ten severe winter storms
An estimated 2,000 flash floods
Plus threats most years from tropical storms and hurricanes in the North Atlantic, the Gulf of Mexico, and the Caribbean Sea
Why all these extreme weather events? It’s like they say about the real estate business: The three most important things are location, location, and location.
As Figure 3-2 illustrates later in this chapter, one region or another of the continental United States is in pathway of a variety of moist and dry and warm and cold air masses coming at it from all directions.
Winter air masses
Continental polar air masses that move down out of the snow-covered regions of northern Canada and Alaska are often in the picture when bitterly cold winter weather visits the United States (see Figure 3-2). Winds of this frigid, dry air blows over the northern plains and through the Midwest and the Northeast and occasionally reaches as far south as Texas and Florida. Out west, the Rockies, Sierra Nevada, and Cascade Mountains usually protect the Pacific Coast. As these air masses move southward, their extreme cold tends to modify, protecting the southern states from the most extreme cold. The barrier of the Appalachians sometimes protects the cities of the East Coast from the worst of it.
Maritime polar air masses regularly sweep over the West Coast from out of the northern Pacific Ocean, bringing cool, moist air that dumps heavy snow in the western mountains. By the time this air crosses east of the Rockies, it is relatively dry. It warms as it blows down the eastern slopes of the mountains and sometimes brings fair weather and warming temperatures to the plains. Maritime polar air also originates in the North Atlantic and occasionally sweeps southwestward into New England and the mid-Atlantic states, bringing rain and snow.
FIGURE 3-2: The map shows the different air masses that affect weather in the continental United States and helps explain why the nation gets so much dramatic weather.
LAKE-EFFECT SNOWS
In late fall and early winter, people who live along the southern and eastern shores of the Great Lakes are very familiar with the effects of big expanses of water on the air. The continental polar air mass that brings cold, clear winter days to the Midwest has a very different look to it by the time it crosses the Great Lakes.
Even after — or if — the lakes freeze over, still they affect the amount of snowfall in the region. Four main weather-generating processes are at work when the cold, dry Canadian air flows over the lakes and the regions along the