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GDL Traditional Cache

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neco_cachero: This one had a really good journey bringing people close to one of the 4 big Doppler radars in the state of Kansas. Hopefully the area has more caches now than when placed this one so more people can see the big golf ball.

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Hidden : 9/23/2011
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   small (small)

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Geocache Description:

GDL is the designated code for the Goodland Weather Doppler Radar Station located in Armory Rd, Goodland Kansas near the Regional Airport.

Visit GDL page in NOAA


From the distance it looks like a water tower. When I got closer I noticed it looks more like a soccer ball with the hexagons and heptagons sewn patches. Then it hit me. It is a RADAR, but what type? I started a small research and found out that this one of the four doppler radars that NOAA has in KS. I have found this things before so I identified it. NOAA has a bunch of radars in the state but there are four big ones. One is here in Goodland. The other three are in Wichita, Dodge City and Alma.

Its designtaion is GDL and it is fully automatic. From this distance you can clearly notice the patches. This is an easy park and grab. You are looking for a small camouflaged pill bottle hide in the branches of a tree. There is room for small things. Please bring your own pen (BYOP).

Doppler Radar

A Doppler radar is a specialized radar that makes use of the doppler effect to produce velocity data about objects at a distance. It does this by beaming a microwave signal towards a desired target and listening for its reflection, then analyzing how the frequency of the returned signal has been altered by the object's motion. This variation gives direct and highly accurate measurements of the radial component of a target's velocity relative to the radar. Doppler radars are used in aviation, sounding satellites, meteorology, police speed guns, and radiology.

The specific term "Doppler Radar", due in part to its extremely common use by television meteorologists in on-air weather reporting, has erroneously become popularly synonymous with the type of radar used in meteorology. Most modern weather radars use the pulse-doppler technique to examine the motion of precipitation, but it is only a part of the processing of their data. So, while these radars use a highly specialized form of doppler radar, the term is much broader in its meaning and its applications.

Doppler Effect

The Doppler effect (or Doppler shift), named after Austrian physicist Christian Doppler who proposed it in 1842, is the change in frequency of a wave for an observer moving relative to the source of the waves. It is commonly heard when a vehicle sounding a siren approaches, passes and recedes from an observer. The received frequency is increased (compared to the emitted frequency) during the approach, it is identical at the instant of passing by, and it is decreased during the recession. This variation of frequency also depends on the direction the wave source is moving with respect to the observer; it is maximum when the source is moving directly toward or away from the observer, and diminishes with increasing angle between the direction of motion and the direction of the waves, until when the source is moving at right angles to the observer, there is no shift.

An analogy would be pitcher throwing one ball every second in a person's direction (a frequency of 1 ball per second). Assuming that the balls travel at a constant velocity, if the pitcher is stationary, the man will catch one ball every second. However, if the pitcher is jogging towards the man, he will catch balls more frequently because the balls will be less spaced out (the frequency increases). The inverse is true if the pitcher is moving away from the man; he will catch balls less frequently due to the pitcher's backward motion (the frequency decreases). If the pitcher were to move at an angle but with the same speed, the variation of the frequency at which the receiver would catch the ball would be less as the distance between the two would change more slowly. Note that, from the point of view of the pitcher, the frequency remains constant (whether he's throwing balls or transmitting microwaves). Since with electromagnetic radiation like microwaves frequency is inversely proportional to wavelength, the wavelength of the waves is also affected. Thus, the relative difference in velocity between a source and an observer is what gives rise to the doppler effect.

The cache is hidden in the branches of the nearest pine tree. I used some wiring holding ties to keep the cache from falling on the ground or being blown away because of the wind. It is not by the old machinery behind the pine tree. You can park right next to the cache. There is no need to walk away from the road and venture into the field or garden.

From here you can appreciate this fine piece of technology that helps us forecast the weather, track nasty storms, and helps prevent so much damage even saving lives. Take some time to check it out. Next time you watch the news and the forecast report at home you will know where that information comes from and that you have visited one of the stations here in Kansas.

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