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What have we learned?
What have we learned?

... • Mars’s primordial atmosphere may have been thicker and warmer than the present-day atmosphere • It is unclear whether it contained enough carbon dioxide and water vapor to support a greenhouse effect that would permit liquid water to exist on the planet’s surface • The present Martian atmosphere i ...
Studies on post-flare loop prominence of 1981 April 27
Studies on post-flare loop prominence of 1981 April 27

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... At various times in the past the orientation has been reversed. A rock crystallizing at this time would have a magnetism pointed toward the south magnetic pole. The magnetic time scale below provides a record of when the Earth’s magnetic field was either normal (black bars) or reversed (white bars). ...
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Section_38_Dynamos_0..

... physics: How to explain the structure, dynamics, and maintenance of magnetic fields in the universe. “Dynamo action” will be defined precisely later in this Section. For now, we say that a dynamo is a process that can generate and amplify magnetic fields in the presence of resistive diffusion. Altho ...
Different Alfvén wave acceleration processes of electrons - HAL-Insu
Different Alfvén wave acceleration processes of electrons - HAL-Insu

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... C). Jack and Jessie: through a mixture of B and E forces. D). Jack: though only E forces. Jessie: through a mixture of B and E forces. ...
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... moving in an external magnetic field so that its velocity is perpendicular to the field The force is always directed toward the center of the circular path The magnetic force causes a centripetal acceleration, changing the direction of the velocity of the particle ...
Chapter 19
Chapter 19

Chapter 19
Chapter 19

... moving in an external magnetic field so that its velocity is perpendicular to the field The force is always directed toward the center of the circular path The magnetic force causes a centripetal acceleration, changing the direction of the velocity of the particle ...
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... the other way round or that the magnet would need to be put the other way round. However some answers were so poorly expressed that it was impossible to be ...
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CIII 97.7 nm - Astronomy at Swarthmore College

Physics 2 for Electrical Engineering Ben Gurion University of the Negev , www.bgu.ac.il/atomchip
Physics 2 for Electrical Engineering Ben Gurion University of the Negev , www.bgu.ac.il/atomchip

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... According to the theory of plate tectonics, (from the Greek, tekto, “builder”), the Earth’s crust is broken into many slowly moving plates. Sea floor spreading occurs at the mid-ocean ridge where two plates are moving away from each other. Here, magma rises up from below as the sea floor spreads out ...
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... lines and other electric facilities, the configuration of the lines, and the amount of electric current carried by those lines at any given time, which will increase or decrease as customer demand for energy increases or decreases. Configuration of the transmission lines can be a factor as magnetic ...
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... • Currently, Earth’s south magnetic pole is located in northern Canada about 1,500 km from the geographic north pole. • Earth’s magnetic poles move slowly with time. • Sometimes Earth’s magnetic poles switch places so that Earth’s south magnetic pole is the southern hemisphere near the geographic so ...
causes of solar activity - The National Academies of Sciences
causes of solar activity - The National Academies of Sciences

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... What the observation of CR anisotropies might suggest  there are sources nearby.  the galactic magnetic field is not what we think (only if the effect is due to charged cosmic rays):  the role of the Solar wind as well as the magnetic field in the solar system may be non-negligible.  there migh ...
PHYS 1443 – Section 501 Lecture #1
PHYS 1443 – Section 501 Lecture #1

... • The more they get cut, the more magnets are made ...
Rocket observation of energetic electrons in the low-altitude auroral
Rocket observation of energetic electrons in the low-altitude auroral

... dashed curves show energy spectra of the downward (7085◦ ) and the upward (95–110◦ ) pitch angles, respectively. Thin dotted lines denote one count levels (the lowest level for detection) during the integrated time. Here, A (104– 113 s, 113 km) and C (130–139 s, 129 km) represent the points inside t ...
Plate Tectonics II
Plate Tectonics II

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Circuit Theory I: goals and underlaying assumptions
Circuit Theory I: goals and underlaying assumptions

... other words the current entering into terminal x is the same as the current exiting from terminal y (i.e. there is no net charge accumulated inside the limped element) ...
Directed Reading
Directed Reading

... c. The solar wind bends around Earth. d. The solar wind changes as it gets farther from the sun. ______ 36. Where on Earth are auroras usually seen? a. near Earth’s equator b. everywhere in Earth’s atmosphere c. close to Earth’s magnetic poles d. only in Earth’s northern hemisphere ______ 37. Why ar ...
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Aurora



An aurora is a natural light display in the sky, predominantly seen in the high latitude (Arctic and Antarctic) regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere (thermosphere/exosphere), where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes. Different aspects of an aurora are elaborated in various sections below.
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