[guide.chat] 4 haarp

  • From: "Vanessa" <qwerty1234567a@xxxxxxxxxxxxxx>
  • To: "GuideChat" <guide.chat@xxxxxxxxxxxxx>
  • Date: Mon, 22 Aug 2011 09:44:40 +0100

The High Frequency Active Auroral Research Program (HAARP) is an  ionospheric.  
research program jointly funded by the  US Air Force. , the  US Navy. , the  
University of Alaska.  and the  Defense Advanced Research Projects Agency.  
(DARPA). [1]. 
Built by  BAE Advanced Technologies (BAEAT). , its purpose is to analyze the 
ionosphere and investigate the potential for developing ionospheric enhancement 
technology for radio communications and surveillance purposes. [2].  The HAARP 
program operates a major Arctic facility, known as the HAARP Research Station, 
on an Air Force owned site near  Gakona, Alaska. .
The most prominent instrument at the HAARP Station is the Ionospheric Research 
Instrument (IRI), a high power  radio frequency.   transmitter.  facility 
operating in the  high frequency.  (HF) band. The IRI is used to temporarily 
excite a limited area of the ionosphere. Other instruments, such as a  VHF.  
and a  UHF.   radar. , a  fluxgate.   magnetometer. , a  digisonde.  and an 
induction magnetometer, are used to study the physical processes that occur in 
the excited region.
Work on the HAARP Station began in 1993. The current working IRI was completed 
in 2007, and its prime contractor was  BAE Systems Advanced Technologies. . 
[1]. 
As of 2008, HAARP had incurred around $250 million in tax-funded construction 
and operating costs. HAARP has also been blamed by  conspiracy theorists.  for 
a range of events, including numerous  natural disasters. .
Contents.  [ hide. ]
1 Objectives.  
2 Research.  
3 Instrumentation and operation.  
4 Site.  
5 Related facilities.  
6 Conspiracy theories.  
7 In popular culture.  
8 See also.  
9 References.  
10 Further reading.  
11 External links.   Objectives. 
HAARP antenna array
The HAARP project directs a 3.6  MW.  signal, in the 2.8-10  MHz.  region of 
the HF [High Frequency] band, into the ionosphere. The signal may be pulsed or 
continuous. Then, effects of the transmission and any recovery period can be 
examined using associated instrumentation, including VHF and UHF radars, HF 
receivers, and optical cameras. According to the HAARP team, this will advance 
the study of basic natural processes that occur in the ionosphere under the 
natural but much stronger influence of solar interaction, as well as how the 
natural ionosphere affects radio signals.
This will enable scientists to develop techniques to mitigate these effects in 
order to improve the reliability and/or performance of communication and 
navigation systems, which would have a wide range of applications in both the 
civilian and military sectors, such as an increased accuracy of GPS navigation, 
and advancements in underwater and underground research and applications. This 
may lead to improved methods for submarine communication and the ability to 
remotely sense the mineral content of the terrestrial subsurface, among other 
things. One application would be to map out the underground complexes of 
countries. The current facility lacks the range to reach these countries, but 
the research could be used to develop a mobile platform. [3]. 
The HAARP program began in 1990. The project is funded by the  Office of Naval 
Research.  and jointly managed by the ONR and  Air Force Research Laboratory. , 
with the principal involvement of the University of Alaska. Many other 
universities and educational institutions have been involved in the development 
of the project and its instruments, namely the University of Alaska 
(Fairbanks),  Stanford University. ,  Penn State University.  (ARL),  Boston 
College. ,  UCLA. ,  Clemson University. ,  Dartmouth College. ,  Cornell 
University. ,  Johns Hopkins University. ,  University of Maryland, College 
Park. ,  University of Massachusetts. ,  MIT. ,  Polytechnic Institute of New 
York University. , and the  University of Tulsa. . The project's specifications 
were developed by the universities, which are continuing to play a major role 
in the design of future research efforts.
According to HAARP's management, the project strives for openness and all 
activities are logged and publicly available. Scientists without security 
clearances, even foreign nationals, are routinely allowed on site. The HAARP 
facility regularly (once a year on most years according to the HAARP home page) 
hosts open houses, during which time any civilian may tour the entire facility. 
In addition, scientific results obtained with HAARP are routinely published in 
major research journals (such as  Geophysical Research Letters. , or  Journal 
of Geophysical Research. ), written both by university scientists (American and 
foreign) or by  US Department of Defense.  research lab scientists. Each 
summer, the HAARP holds a summer-school for visiting students, including 
foreign nationals, giving them an opportunity to do research with one of the 
world's foremost research instruments.Research. 
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 is highly variable, showing minute-to-minute 
changes, daily changes, seasonal changes, and year-to-year changes. This 
profile becomes particularly complicated near the Earth's magnetic poles, where 
the nearly vertical alignment and intensity of the Earth's magnetic field can 
cause physical effects like  aurorae. .
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, scientists 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:
Generation of  very low frequency.  radio waves by modulated heating of the 
auroral  electrojet. , useful because generating VLF waves ordinarily requires 
gigantic antennas 
Production of weak luminous glow (below what can be seen with the naked eye, 
but measurable) from absorption of HAARP's signal 
Production of  extremely low frequency.  waves in the 0.1 Hz range. These are 
next to impossible to produce any other way, because the length of a transmit 
antenna is dictated by the wavelength of the signal it is designed to produce. 
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 
VLF remote sensing of the heated ionosphere 
Research.  at the HAARP includes:
Ionospheric.  super heating 
Plasma.  line observations 
Stimulated  electron emission.  observations 
Gyro frequency.  heating research 
Spread F observations 
High velocity trace runs 
Airglow.  observations 
Heating induced  scintillation.  observations 
VLF.  and  ELF.  generation observations [4].  
Radio.  observations of  meteors.  
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. 
Research on  extraterrestrial.  HF radar echos: the Lunar Echo experiment 
(2008). [5].  [6].  
Testing of  Spread Spectrum.  Transmitters (2009) 
Meteor shower impacts on the ionosphere 
Response and recovery of the ionosphere from solar flares and geomagnetic 
storms 
The effect of ionospheric disturbances on GPS satellite signal quality 
Instrumentation and operation. 
The main instrument at HAARP Station is the Ionospheric Research Instrument 
(IRI). This is a high power, high-frequency  phased array.  radio  transmitter. 
 with a set of 180  antennas. , disposed in an array of 12x15 units that occupy 
a rectangle of about 33 acres (13 hectares). The IRI is used to temporarily 
energize a small portion of the  ionosphere. . The study of these disturbed 
volumes yields important information for understanding natural ionospheric 
processes.
During active ionospheric research, the signal generated by the transmitter 
system is delivered to the  antenna array.  and transmitted in an upward 
direction. At an altitude between 70 km (43 mi) to 350 km (217 mi) (depending 
on operating frequency), the signal is partially absorbed in a small volume 
several tens of kilometers in diameter and a few meters thick over the IRI. The 
intensity of the  HF.  signal in the ionosphere is less than 3 µW/cm², tens of 
thousands of times less than the Sun's natural electromagnetic radiation 
reaching the earth and hundreds of times less than even the normal random 
variations in intensity of the Sun's natural  ultraviolet.  (UV) energy which 
creates the ionosphere. The small effects that are produced, however, can be 
observed with the sensitive scientific instruments installed at the HAARP 
Station, and these observations can provide information about the dynamics of  
plasmas.  and insight into the processes of solar-terrestrial interactions. 
[7]. 
Each antenna element consists of a crossed  dipole.  that can be polarized for 
linear,  ordinary mode.  (O-mode), or  extraordinary mode.  (X-mode) 
transmission and reception. [8].  [9].  Each part of the two section crossed 
dipoles are individually fed from a custom built transmitter, that has been 
specially designed with very low distortion. The  Effective Radiated Power.  
(ERP) of the IRI is limited by more than a factor of 10 at its lower operating 
frequencies. Much of this is due to higher antenna losses and a less efficient 
antenna pattern.
The IRI can transmit between 2.7 and 10 MHz, a frequency range that lies above 
the AM radio broadcast band and well below Citizens' Band frequency 
allocations. The HAARP Station is licensed to transmit only in certain segments 
of this frequency range, however. When the IRI is transmitting, the bandwidth 
of the transmitted signal is 100 kHz or less. The IRI can transmit in 
continuous waves (CW) or in pulses as short as 10 microseconds (µs). CW 
transmission is generally used for ionospheric modification, while transmission 
in short pulses frequently repeated is used as a radar system. Researchers can 
run experiments that use both modes of transmission, first modifying the 
ionosphere for a predetermined amount of time, then measuring the decay of 
modification effects with pulsed transmissions.
There are other geophysical instruments for research at the Station. Some of 
them are:
A  fluxgate.   magnetometer.  built by the University of Alaska Fairbanks  
Geophysical Institute. , available to chart variations in the Earth's magnetic 
field. Rapid and sharp changes of it may indicate a  geomagnetic storm. . 
A  digisonde.  that provides ionospheric profiles, allowing scientists to 
choose appropriate frequencies for IRI operation. The HAARP makes current and 
historic digisonde information available online. 
An induction magnetometer, provided by the  University of Tokyo. , that 
measures the changing geomagnetic field in the  Ultra Low Frequency.  (ULF) 
range of 0-5 Hz. Site. 
The project site ( 62°23'30?N 145°09'03?W? / ?62.39167°N 145.15083°W? / 
62.39167; -145.15083. ) is north of  Gakona. ,  Alaska.  just west of  
Wrangell-Saint Elias National Park. . An  environmental impact statement.  led 
to permission for an array of up to 180  antennas.  to be erected. [10].  The 
HAARP has been constructed at the previous site of an  over-the-horizon radar.  
(OTH) installation. A large structure, built to house the OTH now houses the 
HAARP control room, kitchen, and offices. Several other small structures house 
various instruments.
The HAARP site has been constructed in three distinct phases: [11]. 
The Developmental Prototype (DP) had 18 antenna elements, organized in three 
columns by six rows. It was fed with a total of 360 kilowatts (kW) combined 
transmitter output power. The DP transmitted just enough power for the most 
basic of ionospheric testing. 
The Filled Developmental Prototype (FDP) had 48 antenna units arrayed in six 
columns by eight rows, with 960 kW of transmitter power. It was fairly 
comparable to other  ionospheric heating facilities. . This was used for a 
number of successful scientific experiments and ionospheric exploration 
campaigns over the years. 
The Final IRI (FIRI) is the final build of the IRI. It has 180 antenna units, 
organized in 15 columns by 12 rows, yielding a theoretical maximum gain of 31  
dB. . A total of 3.6 MW of transmitter power will feed it, but the power is 
focused in the upward direction by the geometry of the large  phased array.  of 
antennas which allow the antennas to work together in controlling the 
direction. As of March 2007 [update]. , all the antennas were in place, the 
final phase was completed and the  antenna array.  was undergoing testing aimed 
at fine-tuning its performance to comply with safety requirements required by 
regulatory agencies. The facility officially began full operations in its final 
3.6 MW transmitter power completed status in the summer of 2007, yielding an 
effective radiated power (ERP) of 5.1  Gigawatts.  or 97.1  dBW.  at maximum 
output. However, the site typically operates at a fraction of that value due to 
the lower  antenna gain.  exhibited at standard operational frequencies. [12].  
Related facilities. 
In America, there are two related  ionospheric heating.  facilities: the  
HIPAS. , near  Fairbanks, Alaska. , which was dismantled in 2009, and 
(currently offline for reconstruction) one at the  Arecibo Observatory.   Link 
text.  in  Puerto Rico. . The  European Incoherent Scatter Scientific 
Association.  (EISCAT) operates an ionospheric heating facility, capable of 
transmitting over 1 GW  effective radiated power.  (ERP), near  Tromsø. ,  
Norway. . [13].   Russia.  has the  Sura Ionospheric Heating Facility. , in  
Vasilsursk.  near  Nizhniy Novgorod. , capable of transmitting 190 MW 
ERP.Conspiracy theories. 
See also:  List of conspiracy theories: Development of weapons technology. 
HAARP is the subject of numerous  conspiracy theories. , with individuals 
ascribing various hidden motives and capabilities to the project. Journalist  
Sharon Weinberger.  called HAARP "the  Moby Dick.  of conspiracy theories" and 
said the popularity of conspiracy theories often overshadows the benefits HAARP 
may provide to the scientific community. [14].  [15]. 
The alleged dangers of HAARP were dramatized in popular culture by  Marvel 
Comics. , author  Tom Clancy. , and  The X-Files. . A Russian military journal 
wrote that ionospheric testing would "trigger a cascade of electrons that could 
flip Earth's magnetic poles." The  European Parliament.  and the  Alaska.  
state legislature held hearings about HAARP, the former citing "environmental 
concerns." Author of the self-published Angels Don't Play This HAARP, Nick 
Begich has told lecture audiences that HAARP could trigger earthquakes and turn 
the upper atmosphere into a giant lens so that "the sky would literally appear 
to burn." [16].  [17]. 
A 2009 episode of  The History Channel.  series  That's Impossible.  speculated 
that ionospheric heating from HAARP could theoretically cause localised 
atmospheric upcurrents that disrupt or "bend" the jet stream and influence 
regional weather patterns, prompting conspiracy theorists to connect changed 
weather patterns in the Atlantic Ocean during the 1980s as well as subsequent  
El Nino.  events with HAARP.  [18]. 
Conspiracy theorists have linked HAARP to numerous earthquakes. An opinion 
piece on a  Venezuelan.  state-run television channel's website named HAARP as 
a cause of the  2010 Haiti earthquake. . [19].  [20].  [21]. 
Skeptic computer scientist David Naiditch called HAARP "a magnet for conspiracy 
theorists", saying the project has been blamed for triggering catastrophes such 
as  floods. ,  droughts. ,  hurricanes. ,  thunderstorms. , and devastating  
earthquakes.  in  Pakistan.  and the  Philippines.  aimed to shake up 
"terrorists." Naiditch says HAARP has been blamed for diverse events including 
major  power outages. , the downing of  TWA Flight 800. ,  Gulf War syndrome. , 
and  chronic fatigue syndrome. . Conspiracy theorists have also suggested links 
between HAARP and the work of  Nikola Tesla.  (particularly potential 
combinations of HAARP energy with Tesla's work on  pneumatic small-scale 
earthquake generation. ) and physicist  Bernard Eastlund. . According to 
Naiditch, HAARP is an attractive target for conspiracy theorists because "its 
purpose seems deeply mysterious to the scientifically uninformed". [22]. In 
popular culture. 
A fictionalized HAARP was the setting for a stage in the  X-Men Legends.  game. 
[23].  HAARP was also featured in the animated series  G.I. Joe: Resolute.  and 
in the first episode of  Conspiracy Theory with Jesse Ventura. . Another 
fictionalized HAARP-like system called DESTINI was featured in the 2003 sci-fi 
film  The Core. 

Vanessa the Google Girl
My Skype name is rainbowstar123

Other related posts:

  • » [guide.chat] 4 haarp - Vanessa