|
Global Research, April 24, 2012 | |
The facts do not lie. Not when they are honestly presented. All copyrighted sources are quoted and used for comment and education in accord with the nonprofit provisions of: Title 17 U.S.C., Section 107. These sites are in accordance with Title 17 U.S.C., Section 107 and are protected under: The First Amendment Congress shall make no law respecting an establishment of religion, or prohibiting the free exercise thereof; or abridging the freedom of speech, ….
|
Global Research, April 24, 2012 | |
RQ-1 Predator is a long-endurance, medium-altitude unmanned aircraft system for surveillance and reconnaissance missions. Surveillance imagery from synthetic aperture radar, video cameras and a forward-looking infrared (FLIR) can be distributed in real-time both to the front line soldier and to the operational commander, or worldwide in real-time via satellite communication links. MQ-1, armed with AGM-114 Hellfire missiles, is the multi-role version which is used for armed reconnaissance and interdiction.
A contract was awarded to General Atomics Aeronautical Systems in January 1994 to execute the Tier II, medium-altitude endurance Predator programme. The Predator system first flew in 1994 and entered production in August 1997.
Predators are currently in production for the US Air Force and are operational with the USAF 11th and 15th Reconnaissance Squadrons. Over 125 Predators have been delivered to the USAF. 36 additional MQ-1B Predators (with Hellfire missile installation kits) were ordered in September 2007. Six Predator UAVs are in service with the Italian Air Force. Italian company Meteor was responsible for assembly of five of the six. The Italian system was deployed to Iraq in January 2005.
Predator UAVs have been operational in Bosnia since 1995 in support of Nato, UN and US operations and as part of Operation Enduring Freedom in Afghanistan and Operation Iraqi Freedom, flying over 500,000 flight hours on over 50,000 flights. The MQ-1 Predator achieved initial operating capability (IOC) in February 2005.
General Atomics is the prime contractor and the main subcontractors include: Versatron / Wescam for the electro-optical Skyball Gimbal; Northrop Grumman for the synthetic aperture radar; L3 Communication for the wideband satellite communications link; and Boeing for the intelligence workstation and mission planning system.
In February 2001, the Hellfire-C laser-guided missile was successfully fired from a Predator air vehicle in flight tests at Nellis air force base, Nevada. In November 2002 in Yemen, a Predator UAV was used to drop a Hellfire missile which destroyed a civilian vehicle carrying suspected terrorists. A Northrop Grumman Bat submunition was successfully dropped and a FINDER mini-UAV launched from a Predator UAV in August 2002.
In May 1998 General Atomics was awarded a block 1 upgrade contract to expand the capabilities of the Predator system. System upgrades include development of an improved relief-on-station (ROS) system which allows continuous coverage over areas of interest without any loss of time on station, secure air traffic control voice relay, Ku-band satellite tuning and implementation of an air force mission support system (AFMSS).
The upgrade also covers a more powerful turbocharged engine and wing de-icing systems to enable year-round operations. The upgraded Predator, the Predator B, has been operational in the Balkans since April 2001. In March 2005, the USAF awarded a further contract for the system design and development (SDD) of MQ-9 Reaper Hunter / Killer. 21 MQ-9 have been ordered and eight delivered to the USAF.
The first USAF MQ-9 squadron, the 42nd Attack Squadron, was formed in March 2007. It is based at Creech AFB in Nevada. A decision on full-rate production of the MQ-9 is expected in 2009.
The USAF first deployed the MQ-9 Reaper to Afghanistan in October 2007, where it is being used for precision strikes. The MQ-9 Reaper flew its first operational mission in Iraq in July 2008.
The MQ-9 Reaper has an operational ceiling of 50,000ft, a maximum internal payload of 800lb and external payload over 3,000lb. It can carry up to four Hellfire II anti-armour missiles and two laser-guided bombs (GBU-12 or EGBU-12) and 500lb GBU-38 JDAM (joint direct attack munition). In May 2008, a USAF Reaper successfully test dropped four Raytheon GBU-49 Enhanced Paveway II 500lb bombs, which have laser and GPS guidance.
The MQ-9 sensor payload can include the General Atomics Lynx SAR (synthetic aperture radar). Lynx also features ground moving target indicator technology. The Predator is to be flight tested with a L-3 communications tactical common datalink (TCDL).
In August 2005, a version of Predator B, called Sky Warrior, was chosen for the four-year system development and demonstration (SDD) phase of the US Army's extended range / multi-purpose (ER/MP) UAV programme – 11 Sky Warrior systems, each with 12 air vehicles and five ground control stations.
Initial operating capability is planned for 2009. Two block 0 Sky Warrior UAVs were deployed to Iraq in April 2008.
Also in August 2005, the US Department of Homeland Security / Customs and Border Protection (DHS/CBP) ordered two Predator B systems for monitoring of the USA's south-west border. The first was delivered in late 2005, the second in September 2006. Two further systems were ordered in October 2006, for monitoring operations on the border with Canada.
In September 2006, the UK requested the foreign military sale (FMS) of two MQ-9 Reaper systems with Lynx SAR, multi-spectral targeting systems and one ground station. Deliveries began in mid-2007 and the RAF deployed the system in Afghanistan in November 2007. In January 2008, the UK requested the sale of an additional ten MQ-9 systems.
In August 2008, Italy requested the sale of four MQ-9 Reaper systems with three ground stations.
A typical Predator system configuration would include four aircraft, one ground control system and one Trojan Spirit II data distribution terminal. The Predator air vehicle is 27ft in length and has a 49ft wingspan. The system operates at an altitude of 25,000ft and at a range of 400nm.
The endurance of the air vehicle is more than 40 hours and the cruise speed is over 70kt. The air vehicle is equipped with UHF and VHF radio relay links, a C-band line-of-sight data link which has a range of 150nm and UHF and Ku-band satellite data links.
The surveillance and reconnaissance payload capacity is 450lb and the vehicle carries electro-optical and infrared cameras and a synthetic aperture radar. The two-colour DLTV television is equipped with a variable zoom and 955mm Spotter. The high resolution FLIR has six fields of view, 19mm to 560mm.
The Raytheon multi-spectral targeting system (MTS-A) is fitted on the MQ-1/9 Predator. The MTS-A provides real-time imagery selectable between infrared and day TV as well as a laser designation capability. MQ-1 can employ two laser-guided Hellfire anti-armour missiles with the MTS.
The Northrop Grumman TESAR synthetic aperture radar is fitted on the MQ-1 and provides all-weather surveillance capability, has a resolution of 1ft. Other payload options, which can be selected to meet mission requirements, include a laser designator and rangefinder, electronic support and countermeasures and a moving target indicator (MTI).
The USAF plans to equip a number of MQ-1 and MQ-9 Predators with a version of the Northrop Grumman airborne signals intelligence payload (ASIP) from 2010. Northrop Grumman was awarded a contract for the development and flight testing of the system on an MQ-1 in April 2008. ASIP is being tested on the U-2 reconnaissance aircraft and will also be fitted on the RQ-4 Global Hawk.
The UAV ground control station is built into a single 30ft trailer, containing pilot and payload operator consoles, three Boeing data exploitation and mission planning consoles and two synthetic aperture radar workstations together with satellite and line-of-sight ground data terminals.
The ground control station can send imagery data via a landline to the operational users or to the Trojan Spirit data distribution system which is equipped with a 5.5m dish for Ku-band ground data terminal and a 2.4m dish for data dissemination.
Predator follows a conventional launch sequence from a semi-prepared surface under direct line-of-sight control. The take-off and landing length is typically 2,000ft. The mission can be controlled through line-of-site data links or through Ku-band satellite links to produce continuous video.
Video signals received in the ground control station are passed to the Trojan Spirit van for worldwide intelligence distribution or directly to operational users via a commercial global broadcast system. Command users are able to task the payload operator in real-time for images or video on demand.
Arcturus T-20 Unmanned Aerial Vehicle
T-20 is a medium range tactical unmanned aerial vehicle (UAV) system...
Maveric Small Unmanned Aerial System
The Maveric is a mini unmanned aerial system (UAS) developed by...
Penguin B Unmanned Aerial Vehicle
Penguin B is a multirole small unmanned aerial vehicle designed...
DRDO Lakshya Unmanned Aerial Vehicle
Lakshya is a remotely piloted aerial vehicle designed and built...
RQ-170 Sentinel Unmanned Aerial Vehicle
The RQ-170 Sentinel is a high altitude and long endurance unmanned ...
I have heard much speculation that HAARP caused the earthquake in China in May, 2008. Does the real science back this speculation?
This is the website for HAARP
http://www.haarp.alaska.edu/
This speculation seems to be unjustified.
Note:
There was a Chinese video of the sky before the May 2008 earthquake. I addressed this phenomenon on this post:
http://heavenawaits.wordpress.com/signs-in-the-sky-%E2%80%93-natural-or-unnatural-end-times/
-
-
Reasons:
(1) Earthquakes have happened before HAARP even existed.
Earthquakes have happened before in China, in 1927 (7.9), in 1932,(7.6), and 1976 (7.5), all before HAARP was established in 1990. So, just because another earthquake happened in China, does not mean it is correlated with HAARP. See history map below.
-
-
(2)The earth is shifting in plates. The earth may be affected by electromagnetic activity of the sun, or other artificial devices, but it has its own electromagnetic and mechanical activity as well.
The Schumann resonances (SR) are a set of spectrum peaks in the extremely low frequency (ELF) portion of the Earth’s electromagnetic field spectrum. Schumann resonances are global electromagnetic resonances, excited by lightning discharges in the cavity formed by the Earth surface and the ionosphere. Schumann resonance occurs because the space between the surface of the Earth and the conductive ionosphere acts as a waveguide.
Since the early days of radio, in the age of Nikolai Tesla,it has been known the earth has a natural electromagnetic resonance of its own. If you take your receiver and tune below the Schumann Resonance down to about 0.9 or 1 Hz you will hear static from yet another resonant source. This is the Alfven Resonance. there are primarily three schools of thought about the source of the Alfven Resonance. These are: (1) magnetospheric, (2) ionospheric and (3) lithospheric interactions with radio waves. The Alfven Resonance may not be due to radio waves in the air, but is actually coming from the earth due to random seismic activity around the planet.
-
-
The magnetosphere is there to protect the earth from the solar winds.
-
-
The lithosphere (geosphere) is the “solid” part of Earth. It has two parts, the crust and the upper mantle.The crust is Earth’s outermost layer. The crust varies from 5 to 70 kilometers in thickness. The crust includes rocks, minerals, and soil. There are two kinds of crust: continental and oceanic. Yes, there is even crust under the ocean!
The crust is constantly moving, which is why continents move and earthquakes happen. The science that studies how the parts of the crust move is called “Plate Tectonics.”
Earth’s oceanic crust is a thin layer of dense rock about 5 kilometers thick. The continental crust is less dense, with lighter-colored rock, that varies from 30 to 70 kilometers thick. The continental crust is older and thicker than the oceanic crust.
-
-
The ionosphere is the uppermost part of the atmosphere, distinguished because it is ionized by solar radiation. It plays an important part in atmospheric electricity and forms the inner edge of the magnetosphere. It has practical importance because, among other functions, it influences radio propagation to distant places on the Earth. It is located in the Thermosphere.
The lowest part of the Earth’s atmosphere is called the troposphere and it extends from the surface up to about 10 km (6 miles). The atmosphere above 10 km is called the stratosphere, followed by the mesosphere. It is in the stratosphere that incoming solar radiation creates the ozone layer. At heights of above 80 km (50 miles), in the thermosphere, the atmosphere is so thin that free electrons can exist for short periods of time before they are captured by a nearby positive ion. The number of these free electrons is sufficient to affect radio propagation. This portion of the atmosphere is ionizedand contains a plasma which is referred to as the ionosphere.
The ionization depends primarily on the Sun and its activity. Thus there is a diurnal (time of day) effect and a seasonal effect. The local winter hemisphere is tipped away from the Sun, thus there is less received solar radiation. The activity of the sun is associated with the sunspot cycle, with more radiation occurring with more sunspots. Radiation received also varies with geographical location (polar, auroral zones, mid-latitudes, and equatorial regions). There are also mechanisms that disturb the ionosphere and decrease the ionization. There are disturbances such as solar flares and the associated release of charged particles into the solar wind which reaches the Earth and interacts with its geomagnetic field.
-
-
(3) It has historically been more evident that earthquakes affected the ionosphere (area of HAARP activity) rather than the ionosphere affecting the earthquakes.
References:
(a) Ultra-low-frequency electromagnetic waves in the Earth’s crust and magnetosphere
A V Guglielmi 2007 Phys.-Usp. 50 1197-1216
Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russian Federation
Abstract. Research on natural intra- and extra terrestrially produced electromagnetic waves with periods ranging from 0.2 to 600 s is reviewed. The way in which the energy of rock movements transforms into the energy of an alternating magnetic field is analyzed. Methods for detecting seismomagnetic signals against a strong background are described. In discussing the physics of ultra-low-frequency waves in the magnetosphere, the 11-year activity modulation of 1-Hz waves andponderomotive forces affecting plasma distribution are emphasized.
(b) The quaking ionosphere – earthquake disturbs ionosphere
Science News, Oct 19, 1985
On April 12, 1978, something strange happened to the ionosphere above Chatanika, Alaska. Scientists routinely monitoring the flow of ionospheric particles detected very large verticle oscillations corresponding at times to ion velocities of up to 100 meters per second. Normally, ionospheric winds travel almost exclusively in the horizontal direction. And any verticle motions –rarely larger than 2 m/sec — are usually associated with changes in the magnetic field, but no such variations were recorded that day.
The mystery was solved when Michael Kelley at Cornell University in Ithaca, N.Y., and Robert Livingston and Mary McCready at SRI International in Menlo Park, Calif., linked the nine-hour-long ionospheric disturbance to an earthquake that had occurred 1,000 kilometers from the radar site just before the oscillations began. As discussed in the September GEOPHYSICAL RESEARCH LETTERS, the researchers found that their data compared well with a theory developed 18 years ago, which predicts that a nuclear explosion or earthquake will excite atmospheric motion near the event much like that created when a pebble falls in water.
In order to fit the data to the model, however, they had to assume that the ionosphere was hotter than normal, suggesting that the earthquake had heated the upper atmosphere. According to Kelley, energy from earthquakes, tornadoes and weather in the lower atmosphere may play a much more important role in warming the upper atmosphere than has usually been assumed.
(c). GPS detection of total electron content variations over Indonesia and Thailand following the 26 December 2004 earthquake
We report the response of the ionosphere to the large earthquake that occurred in West Sumatra, Indonesia, at 0058 UT on December 26, 2004. We have analyzed Global Positioning System (GPS) data obtained at two sites in Sumatra and at three sites in Thailand to investigate total electron content (TEC) variations. Between 14 and 40 min after the earthquake, TEC enhancements of 1.6-6.9 TEC units (TECU) were observed at subionospheric points located 360-2000 km north of the epicenter. From the time delays of the observed TEC enhancements, we find that the TEC enhancements propagated northward from the epicenter. The time delays between the earthquake and rapid increases in TEC, which occurred near the epicenter, are consistent with the idea that acoustic waves generated by the earthquake propagated into the ionosphere at the speed of sound to cause the TEC variations. A small TEC enhancement of 0.6 TECU was observed south of the epicenter, while no TEC enhancements were seen east of the epicenter. From a model calculation, we find that this directivity of the TEC variations with respect to the azimuth from the epicenter could be caused partially by the directivity in the response of the electron density variation to the acoustic waves in the neutral atmosphere.
(d) Ionospheric post-seismic perturbations following the Tokachi-Oki earthquake from high rate GPS Japanese data : wave source and propagation Ionospheric perturbations
Crespon, F. (1,2) ; Occhipinti, G. (1); Garcia, R. (1);Lognonné, P. (1) and Murakami, M. (3)(1) Institutde Physique duGlobe de Paris, Départementde Géophysique Spatialeet Planétaire, 4 avenue de Neptune, 94107, St Maurdes Fossés, France (2) Noveltis, Parc Technologique duCanal, 2 rue de l’Europe, 31520, Ramonville, France(3) Geographical Survey Institute, Geography and CrustalDynamics Research Center, Kitasato-1, Tsukuba, 305-0811
Ionospheric perturbations following the Tokachi-Oki earthquake (East of Hokkaido island) have been sensed by the high rate continuous GPS Network of Japan. Thestrong motions have produced infrasonic waves propagating into the ionosphere and generating electronic density perturbations. The electronic content along GPS satellite to GPS receiver rays is extracted from the raw data. The attenuation of infrasonic waves by the atmosphere is demonstrated on these signals. Then, the GPS data have been inverted to reconstruct 3D tomographic images of the electronic density perturbations. The ionospheric waves far from the source are propagating horizontally at the speed of seismic surface waves and vertically at the speed of sound in the atmosphere. Close to the source, the signal has been analyzed and modeled in order to constraint the source location and the source mechanism. These studies demonstrate the interest of post-seismic ionospheric perturbations to retrieve the long period strong motions that are notable inland due to the saturation of seismometers, and in the ocean due to the low number of ocean bottom seismometers.
Conclusion:
I doubt that HAARP activity caused the China earthquake.It is more likely that the pre- and post- earthquake conditions affected the atmosphere, rather than the atmosphere affected the earthquake.