Friday, December 4, 2009

HAARP Conspiracy


Jesse Ventura, former wrestler and Minnesota governor, is hosting a new TV show about conspiracy theories.

In its premier telecast on December 2, “Conspiracy Theory with Jesse Ventura” investigated the High Frequency Active Auroral Research Program (HAARP) project in Gakona, Alaska.

For many years, the HAARP has been a favorite of the conspiracy set. It is about mind control, weather control, and other insidious plans by the federal government, the program’s opponents say.

On the other hand, it is about researching the physical and electrical properties of the ionosphere, not creating a new weapon, and it does not have the power to control minds or weather, supporters say.

The High Frequency Active Auroral Research Program (HAARP) is an investigation project jointly funded by the US Air Force, the US Navy, the University of Alaska, and the Defense Advanced Research Projects Agency (DARPA).Its purpose is to investigate the ionosphere and establish whether some of its properties can be used for communication or surveillance purposes. Started in 1993, the project is proposed to last for a period of twenty years. The system was designed and built by Advanced Power Technologies[citation needed] (APTI) and since 2003, by BAE Advanced Technologies.

The facility currently operates a VHF and UHF radar, a fluxgate magnetometer, a digisonde, and an induction magnetometer alongside the transmitter facilities.

HAARP's main goal is basic science research of the uppermost portion of the atmosphere, known as the ionosphere. Essentially a transition between the atmosphere and the magnetosphere, the ionosphere is where the atmosphere is thin enough that the sun's x-rays and UV rays can reach it, but thick enough that there are still enough molecules present to absorb those rays. Consequently, the ionosphere consists of a rapid increase in density of free electrons, beginning at ~70 km, reaching a peak at ~300 km, and then falling off again as the atmosphere disappears entirely by ~1000 km. Various aspects of HAARP can study all of the main layers of the ionosphere.

The profile of the ionosphere, however, is highly variable, showing minute-to-minute changes, diurnal changes, seasonal changes, and year-to-year changes. This becomes particularly complicated near the Earth's poles, where a host of physical processes (like auroral lights) are unlocked by the fact that the alignment of the Earth's magnetic field is nearly vertical.

On the other hand, the ionosphere is traditionally very difficult to measure. Balloons cannot reach it because the air is too thin, but satellites cannot orbit there because the air is still too thick. Hence, most experiments on the ionosphere give only small pieces of information. HAARP approaches the study of the ionosphere by following in the footsteps of an ionospheric heater called EISCAT near Tromsø, Norway. There, they pioneered exploration of the ionosphere by perturbing it with radio waves in the 2-10 MHz range, and studying how the ionosphere reacts. HAARP performs the same functions but with more power, and a more flexible and agile HF beam.

Some of the main scientific findings from HAARP include:

1. Generation of very low frequency radio waves by modulated heating of the auroral electrojet, useful because generating VLF waves ordinarily requires gigantic antennas
2. Production of weak luminous glow (below what you can see with your eye, but measurable) from absorption of HAARP's signal
3. Production of ultra low frequency waves in the 0.1 Hz range, which are next to impossible to produce any other way
4. Generation of whistler-mode VLF signals which enter the magnetosphere, and propagate to the other hemisphere, interacting with Van Allen radiation belt particles along the way
5. VLF remote sensing of the heated ionosphere

Research at the HAARP includes:

1. Ionospheric heating
2. Plasma line observations
3. Stimulated electron emission observations
4. Gyro-frequency heating research
5. Spread F observations
6. Airglow observations
7. Heating induced scintillation observations
8. VLF and ELF generation observations
9. Radio observations of meteors
10. Polar mesospheric summer echoes: Polar mesospheric summer echoes (PMSE) have been studied using the IRI as a powerful radar, as well as with the 28 MHz radar, and the two VHF radars at 49 MHz and 139 MHz. The presence of multiple radars spanning both HF and VHF bands allows scientists to make comparative measurements that may someday lead to an understanding of the processes that form these elusive phenomena.
11. Research on extraterrestrial HF radar echos: the Lunar Echo experiment (2008).
12. Testing of SS-Spread Spectrum Transmitters 2009

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Jesse Ventura, former wrestler and Minnesota governor, is hosting a new TV show about conspiracy theories.

In its premier telecast on December 2, “Conspiracy Theory with Jesse Ventura” investigated the High Frequency Active Auroral Research Program (HAARP) project in Gakona, Alaska.

For many years, the HAARP has been a favorite of the conspiracy set. It is about mind control, weather control, and other insidious plans by the federal government, the program’s opponents say.

On the other hand, it is about researching the physical and electrical properties of the ionosphere, not creating a new weapon, and it does not have the power to control minds or weather, supporters say.

The High Frequency Active Auroral Research Program (HAARP) is an investigation project jointly funded by the US Air Force, the US Navy, the University of Alaska, and the Defense Advanced Research Projects Agency (DARPA).Its purpose is to investigate the ionosphere and establish whether some of its properties can be used for communication or surveillance purposes. Started in 1993, the project is proposed to last for a period of twenty years. The system was designed and built by Advanced Power Technologies[citation needed] (APTI) and since 2003, by BAE Advanced Technologies.

The facility currently operates a VHF and UHF radar, a fluxgate magnetometer, a digisonde, and an induction magnetometer alongside the transmitter facilities.

HAARP's main goal is basic science research of the uppermost portion of the atmosphere, known as the ionosphere. Essentially a transition between the atmosphere and the magnetosphere, the ionosphere is where the atmosphere is thin enough that the sun's x-rays and UV rays can reach it, but thick enough that there are still enough molecules present to absorb those rays. Consequently, the ionosphere consists of a rapid increase in density of free electrons, beginning at ~70 km, reaching a peak at ~300 km, and then falling off again as the atmosphere disappears entirely by ~1000 km. Various aspects of HAARP can study all of the main layers of the ionosphere.

The profile of the ionosphere, however, is highly variable, showing minute-to-minute changes, diurnal changes, seasonal changes, and year-to-year changes. This becomes particularly complicated near the Earth's poles, where a host of physical processes (like auroral lights) are unlocked by the fact that the alignment of the Earth's magnetic field is nearly vertical.

On the other hand, the ionosphere is traditionally very difficult to measure. Balloons cannot reach it because the air is too thin, but satellites cannot orbit there because the air is still too thick. Hence, most experiments on the ionosphere give only small pieces of information. HAARP approaches the study of the ionosphere by following in the footsteps of an ionospheric heater called EISCAT near Tromsø, Norway. There, they pioneered exploration of the ionosphere by perturbing it with radio waves in the 2-10 MHz range, and studying how the ionosphere reacts. HAARP performs the same functions but with more power, and a more flexible and agile HF beam.

Some of the main scientific findings from HAARP include:

1. Generation of very low frequency radio waves by modulated heating of the auroral electrojet, useful because generating VLF waves ordinarily requires gigantic antennas
2. Production of weak luminous glow (below what you can see with your eye, but measurable) from absorption of HAARP's signal
3. Production of ultra low frequency waves in the 0.1 Hz range, which are next to impossible to produce any other way
4. Generation of whistler-mode VLF signals which enter the magnetosphere, and propagate to the other hemisphere, interacting with Van Allen radiation belt particles along the way
5. VLF remote sensing of the heated ionosphere

Research at the HAARP includes:

1. Ionospheric heating
2. Plasma line observations
3. Stimulated electron emission observations
4. Gyro-frequency heating research
5. Spread F observations
6. Airglow observations
7. Heating induced scintillation observations
8. VLF and ELF generation observations
9. Radio observations of meteors
10. Polar mesospheric summer echoes: Polar mesospheric summer echoes (PMSE) have been studied using the IRI as a powerful radar, as well as with the 28 MHz radar, and the two VHF radars at 49 MHz and 139 MHz. The presence of multiple radars spanning both HF and VHF bands allows scientists to make comparative measurements that may someday lead to an understanding of the processes that form these elusive phenomena.
11. Research on extraterrestrial HF radar echos: the Lunar Echo experiment (2008).
12. Testing of SS-Spread Spectrum Transmitters 2009

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