Ningaloo Skies A Journey Through Space and Time - Astroimaging by Al Brockman |
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Establishment and Operation The Observatory was established by agreement between the Australian and United States Governments in October 1977 and operations commenced in April 1979. Located on North West Cape, Western Australia (22.2 S, 114.1 E), the site overlooks Exmouth Gulf to the east and Cape Range to the west. It is part of a network of solar The Observatory is staffed seven days per week, from sunrise to sunset. Staff include analysts to monitor and interpret observations, maintenance technicians, Learmonth Observatory operates optical and radio telescopes to monitor the Sun. In collaboration with Geophysics Australia, magnetometers are operated to sense
Data Collection, Distribution and Use Information collected at Learmonth is reported directly to forecast centres in both Australia and the USA. The IPS Australian Space Forecast Centre in Sydney
Monitoring The Space Environment The Sun is the primary source of variations in the space environment through which the Earth moves. In a sense, the Earth is immersed in the Sun's outer atmosphere which consists of the solar wind that is constantly flowing from the Sun. It not only emits large quantities of light and heat, but other electromagnetic radiation such as radio waves, ultraviolet light and X-rays. Huge eruptions occurring on the Sun (Coronal Mass Ejections) can eject large clouds of plasma into space. These, preceded by shock waves may impinge on the Earth's magnetic field and inject plasma particles, creating a geomagnetic storm. The Learmonth optical telescope monitors solar surface features. These include susnpots, plage, filaments, fibrils, prominences and magnetic fields. These features change constantly and may appear and disappear on time scales from minutes to months. One of the most spectacular events to be viewed on the Sun is a flare, an explosive release of incredible amounts of constrained magnetic energy. The optical telescope, includes many subsystems to monitor all the above phenomena for any potential impact that they might have on, or around, the Earth. The radio telescopes monitor emissions from the Sun that complements information gained from the optical systems. Different radio frequencies indicate different potential effects on the Earth. Mid-microwave frequencies indicate the emission of X-rays from the Sun. This affects the Earth's ionosphere which supports high frequency (HF) radio communication. Variations in X-ray emissions control the range of frequenciesHF radio communicators may use. The radio telescopes can also track ejected material as it travels up through the Sun's atmosphere which can assist in predicting those events likely to have an impact on Earth. Magnetometers, another instrument at LSO monitor very small changes in the Earth's magnetic field, detect interplanetary shock waves and monitor the course of geomagnetic storms. An ionosonde is a vertically directed HF radar providing information on the ionosphere. This data is useful to support radio communications and navigation, both ground and satellite based.
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Design and production 2009 byAl Brockman
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