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The Earth Story

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This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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Why do storms break up and go around (name your town here)?

If you’ve ever watched a line of storms moving into your area on the radar, you may have asked this question yourself. A line of storms may appear solid and menacing at a distance, and then as the storms get closer, gaps appear in the line, and your house may get missed by the rain. After the storms pass, the gaps disappear, and you see a solid line of storms again. The storms are not actually breaking up and reforming around your town. What you are seeing is a result of the changing size of the radar beam as it moves away from the radar. At close range, the beam is narrower and can see finer details, such as gaps in the storms. At a distance, the radar beam is much wider and cannot see the gaps between storms, so a line of storms at a distance appears to be solid, when it is really not.

Think of the radar beam as a beam of light from a flashlight. If you hold a flashlight close to a wall in a dark room, you will see a small beam of light. As you back away from the wall, the beam of light gets larger. The energy coming from the radar works in much the same way. Near the radar, the beam of energy is much narrower, but as the beam moves out away from the radar, it grows in size, much like a flashlight beam.

The spreading radar beam affects the resolution of the image. Small features can be seen close to the location of the radar, but they are often obscured at a greater distance. So, at a distance from the radar, a line of storms may appear solid, because the beam is too wide to resolve the gaps between storms. As the storms get closer to the radar, the narrower beam can “see” the gaps.

Also, the life cycle of a typical thunderstorm is only around 30 minutes to 1 hour. Storms are changing and evolving all the time. A storm at a distance that is an hour away will change considerably by the time it reaches your location. It may weaken and die out before it ever reaches you, or it may change the direction it is moving and miss your location completely.

Here’s just one more thing to keep in mind. Due to the curvature of the earth, the radar beam gets higher in the sky as it moves away from the radar. The radar beam is sampling the upper levels of storms at a distance, and looking at the lower levels of storms close to the radar. This can also affect what you are seeing on the radar screen.

-Amy

For more on how radars work, visit the JetStream mini-course on radars:

Photo credit NOAA/NWS

Source: facebook.com
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