top of page
Wendy Yu

HAARP(HIGH FREQUENCY ACTIVE AURORAL RESEARCH PROGRAM) Project

The HAARP (HIGH FREQUENCY ACTIVE AURORAL RESEARCH PROGRAM) program was initiated as an ionospheric research, but was also used as a kind of meteorological weapon. Through artificial control and changing the physical field of the earth, it can achieve the effect of controlling the wind, rain, and can even cause droughts, floods and earthquakes. In war, HAARP can be used to destroy the ozone layer above the target area, expose the enemy to strong cosmic rays, and destroy all the enemy's biological forces.


Origin of the HAARP program: HAARP is a joint deployment project of the US Air Force, Navy, and Department of Defense. Construction began in 1993 and settled in Gakona, Alaska Peninsula, USA, covering an area of ​​33 acres, about 13 hectares. The Ionospheric Research Instrument (IRI) consists of 180 phased antenna arrays, 12x15 units. At present, most people believe that the original developer of the HAARP technology was Dr. Bernard Eastlund, an American physicist, when helping Arko Petroleum to find an economical and applicable method to extract their 30 trillion cubic meters of natural gas underground in Alaska. He wanted to develop a super-large radio transmitter, powered by natural gas from Alaska, and let this super-large radio transmitter emit electromagnetic waves over a designated area, thereby changing the ionosphere structure to achieve the purpose of controlling the weather.

Dr. Eastlund said that his invention is based on an extension of Tesla's technology in the 1930s. Tesla is most famous for his Tesla coil and artificial lightning. Therefore, Tesla is also known as the "father of artificial lightning." Nevertheless, his research on earthquakes is also very deep. In his middle age, Tesla devoted himself to the study of non-linear problems, that is, the study of disproportionate input and output. Tesla once said: "If the vibration frequency of the object and the resonant frequency of the earth are properly combined, within a few weeks, the ground will shake and the ground will rise and fall." In 1898, Tesla was in New York. An extraordinary experiment was conducted in the Manhattan laboratory. He installed a small oscillator like an alarm clock on an iron railing, adjusted the vibration frequency precisely, and then the things in the laboratory resonated one by one. The vibration produced by the oscillator, as the iron railings passed down, the surrounding houses shook. Everyone thought there was an earthquake and rushed out of the house. Knowing this, Tesla realized that something was wrong, so he immediately stopped the experiment and everything returned to calm. Later, scientists estimated that if Tesla’s oscillator lasts for an hour, the Brooklyn Bridge in New York might be shattered. In the 1930s, Tesla also did another experiment. He drilled a deep well in the laboratory, buried several steel sleeves in the well, and then sealed the well. He inputs the shocks of different vibration frequencies into the well, and when it is adjusted to a specific frequency, the surrounding ground will vibrate.

The IRI is used to temporarily energize a small portion of the ionosphere, during which the transmitter system delivers a generated signal to the antenna array, then transmitted to 70 – 350 kilometers above sea level. Over the IRI, only a small volume of signal was absorbed. The intensity of the HF signal in the ionosphere is less than 3 µW/cm², though thousands of times weaker than the Sun’s electromagnetic radiation and its ultraviolet energy, can prove processes of solar – terrestrial interactions.

The antennae all have crossed dipoles with both an O-mode for linear polarization, and X-mode for transmission and reception. An inefficient antenna pattern and a high antenna loss results in a low operating frequency from effective radiated power.

When the IRI is transmitting signals at a bandwidth of 100kHz or less with continuous waves in 10 microseconds, the ionosphere can be modified. The modification and the decay results can be measured.


The Ionosphere

From the earth's surface upwards, the atmosphere can be divided into troposphere,

stratosphere and ionosphere. Above the atmosphere, there are magnetosphere and plasma layers. The troposphere, which is closely related to human life, directly affects our climate and living environment. The ionosphere at a distance of 60 to 1,000 kilometers from the ground is also critical. All kinds of rays radiated from the sun and the depths of the universe to the earth are all reflected and absorbed by the ozone layer in the ionosphere and stratosphere. Otherwise, all life on the earth would cease to exist. The earth sphere as a whole, the ionosphere is like a thin layer of foam wrapped around it. If the ionosphere is destroyed, it will inevitably affect the stratosphere and troposphere, and even affect changes in atmospheric circulation, causing climate disasters. At the same time, the free electrons and ions in the ionosphere play an important role in human long-distance radio communication. The ionosphere is also called "a mirror that reflects electric waves." Radio waves propagate forward through multiple reflections between the ground and the ionosphere, realizing long-distance radio communication. If we can selectively interfere with a part of the charged particles in the ionosphere, we can theoretically easily enhance or block long-range radio signals. This is vital both in war and in business.



Phased Array

An ordinary radar emits electromagnetic waves into the atmosphere through an antenna, forming a forward beam in a very narrow direction. After the electromagnetic wave encounters the target object in the beam, a part of the electromagnetic wave energy is reflected back to form the radar echo signal. By processing the signal, we can know the distance, direction and moving speed of the target object. But traditional radar has a congenital flaw, that is, it can only scan in one direction. If you want to scan in all directions, you need to rotate the radar antenna mechanically. But phased array radar makes up for this shortcoming. There are multiple elements in its antenna array, and each element can be understood as a small radar. The electromagnetic waves generated by each element will interfere with each other. By controlling the current phase of each element, the scanning direction of electromagnetic waves can be changed quickly and accurately. Unlike the traditional radar antenna having to rotate, the phased array radar can scan quickly without rotating. HAARP technology uses the principle of phased array antennas. The main body of HAARP is like a huge transmitting front of more than ten hectares. By adjusting the phase of electromagnetic waves emitted by each antenna, it destroys the structure of the ionosphere over the designated area. Its launch device can focus the powerful radio waves into a strong wave with more energy than a nuclear explosion, and shoot it to a certain point of the ionosphere accurately and powerfully, and even tear the ionosphere away, bringing devastating effects into the atmosphere.

Potential Threats of HAARP



1. If the ozone layer above the target area is destroyed, all kinds of cosmic harmful rays will drive straight in, causing huge damage to the human body, and may even destroy all living things in the target area.

2. It can control the wind and rain, and even cause earthquakes. Looking at the Earth’s surface as a whole, if the ionosphere is destroyed, the troposphere and stratosphere will also be affected, thereby disturbs the atmospheric circulation. There is also evidence that HAARP can interfere with enemy communications by changing the ionospheric structure during war. In a HBO documentary about HAARP, it was mentioned that in order to ensure the flight safety of surrounding aircraft, the HAARP base has also set up an early warning radar. If an aircraft enters the designated flight area, the HAARP system will automatically shut down. This proves the interference of HAARP on the ionosphere and its possible impact on the aircraft.

Comentarios


bottom of page