排序方式: 共有27条查询结果,搜索用时 218 毫秒
11.
T. G. Slanger T. E. Cravens J. Crovisier S. Miller D. F. Strobel 《Space Science Reviews》2008,139(1-4):267-310
Much of what we know about the atmospheres of the planets and other bodies in the solar system comes from detection of photons over a wide wavelength range, from X-rays to radio waves. In this chapter, we present current information in various categories—measurements of the airglows of the terrestrial planets, the dayglows of the outer planets and satellites, aurora throughout the solar system, observations of cometary spectra, and the emission of X-rays from a variety of planetary bodies. 相似文献
12.
Y.-J. Ma K. Altwegg T. Breus M. R. Combi T. E. Cravens E. Kallio S. A. Ledvina J. G. Luhmann S. Miller A. F. Nagy A. J. Ridley D. F. Strobel 《Space Science Reviews》2008,139(1-4):311-353
Understanding the processes involved in the interaction of solar system bodies with plasma flows is fundamental to the entire field of space physics. The features of the interaction can be very different, depending upon the properties of the incident plasma as well as the nature of the obstacle. The properties of the atmosphere/ionosphere associated with the obstacle are of particular importance into understanding the plasma interaction process, especially for non-magnetized obstacle. This paper discusses in detail the roles of the atmosphere and ionosphere systems of plasma interaction around Venus, Mars, comets and some particular satellites. The coupling between magnetosphere and ionosphere is also discussed for Earth and Giant planets. 相似文献
13.
J. L. Burch R. Goldstein T. E. Cravens W. C. Gibson R. N. Lundin C. J. Pollock J. D. Winningham D. T. Young 《Space Science Reviews》2007,128(1-4):697-712
The ion and electron sensor (IES) is part of the Rosetta Plasma Consortium (RPC). The IES consists of two electrostatic plasma
analyzers, one each for ions and electrons, which share a common entrance aperture. Each analyzer covers an energy/charge
range from 1 eV/e to 22 keV/e with a resolution of 4%. Electrostatic deflection is used at the entrance aperture to achieve
a field of view of 90°× 360° (2.8π sr). Angular resolution is 5°× 22.5° for electrons and 5°× 45° for ions with the sector
containing the solar wind being further segmented to 5°× 5°. The three-dimensional plasma distributions obtained by IES will
be used to investigate the interaction of the solar wind with asteroids Steins and Lutetia and the coma and nucleus of comet
67P/Churyumov–Gerasimenko (CG). In addition, photoelectron spectra obtained at these bodies will help determine their composition. 相似文献
14.
H. E. Spence G. D. Reeves D. N. Baker J. B. Blake M. Bolton S. Bourdarie A. A. Chan S. G. Claudepierre J. H. Clemmons J. P. Cravens S. R. Elkington J. F. Fennell R. H. W. Friedel H. O. Funsten J. Goldstein J. C. Green A. Guthrie M. G. Henderson R. B. Horne M. K. Hudson J.-M. Jahn V. K. Jordanova S. G. Kanekal B. W. Klatt B. A. Larsen X. Li E. A. MacDonald I. R. Mann J. Niehof T. P. O’Brien T. G. Onsager D. Salvaggio R. M. Skoug S. S. Smith L. L. Suther M. F. Thomsen R. M. Thorne 《Space Science Reviews》2013,179(1-4):311-336
15.
O. Witasse T. Cravens M. Mendillo J. Moses A. Kliore A. F. Nagy T. Breus 《Space Science Reviews》2008,139(1-4):235-265
This article reviews our understanding of the ionospheres in the solar system. It provides some basic information on the sources and sinks of the ionospheric plasma, its dynamics, the energetics and the coupling to the neutral atmosphere. Ionospheres in the solar system are reviewed and comparative ionospheric topics are discussed. 相似文献
16.
Möbius E. Kistler L.M. Popecki M.A. Crocker K.N. Granoff M. Turco S. Anderson A. Demain P. Distelbrink J. Dors I. Dunphy P. Ellis S. Gaidos J. Googins J. Hayes R. Humphrey G. Kästle H. Lavasseur J. Lund E.J. Miller R. Sartori E. Shappirio M. Taylor S. Vachon P. Vosbury M. Ye V. Hovestadt D. Klecker B. Arbinger H. Künneth E. Pfeffermann E. Seidenschwang E. Gliem F. Reiche K.-U. Stöckner K. Wiewesiek W. Harasim A. Schimpfle J. Battell S. Cravens J. Murphy G. 《Space Science Reviews》1998,86(1-4):449-495
The Solar Energetic Particle Ionic Charge Analyzer (SEPICA) is the main instrument on the Advanced Composition Explorer (ACE)
to determine the ionic charge states of solar and interplanetary energetic particles in the energy range from ≈0.2 MeV nucl−1
to ≈5 MeV charge−1. The charge state of energetic ions contains key information to unravel source temperatures, acceleration,
fractionation and transport processes for these particle populations. SEPICA will have the ability to resolve individual charge
states and have a substantially larger geometric factor than its predecessor ULEZEQ on ISEE-1 and -3, on which SEPICA is based.
To achieve these two requirements at the same time, SEPICA is composed of one high-charge resolution sensor section and two
low- charge resolution, but large geometric factor sections. The charge resolution is achieved by the focusing of the incoming
ions, through a multi-slit mechanical collimator, deflection in an electrostatic analyzer with a voltage up to 30 kV, and
measurement of the impact position in the detector system. To determine the nuclear charge (element) and energy of the incoming
ions, the combination of thin-window flow-through proportional counters with isobutane as counter gas and ion-implanted solid
state detectors provide for 3 independent ΔE (energy loss) versus E (residual energy) telescopes. The multi-wire proportional
counter simultaneously determines the energy loss ΔE and the impact position of the ions. Suppression of background from penetrating
cosmic radiation is provided by an anti-coincidence system with a CsI scintillator and Si-photodiodes. The data are compressed
and formatted in a data processing unit (S3DPU) that also handles the commanding and various automatted functions of the instrument.
The S3DPU is shared with the Solar Wind Ion Charge Spectrometer (SWICS) and the Solar Wind Ion Mass Spectrometer (SWIMS) and
thus provides the same services for three of the ACE instruments. It has evolved out of a long family of data processing units
for particle spectrometers.
This revised version was published online in June 2006 with corrections to the Cover Date. 相似文献
17.
L. A. Frank J. B. Sigwarth J. D. Craven J. P. Cravens J. S. Dolan M. R. Dvorsky P. K. Hardebeck J. D. Harvey D. W. Muller 《Space Science Reviews》1995,71(1-4):297-328
The Visible Imaging System (VIS) is a set of three low-light-level cameras to be flown on the POLAR spacecraft of the Global Geospace Science (GGS) program which is an element of the International Solar-Terrestrial Physics (ISTP) campaign. Two of these cameras share primary and some secondary optics and are designed to provide images of the nighttime auroral oval at visible wavelengths. A third camera is used to monitor the directions of the fields-of-view of these sensitive auroral cameras with respect to sunlit Earth. The auroral emissions of interest include those from N
2
+
at 391.4 nm, Oi at 557.7 and 630.0 nm, Hi at 656.3 nm, and Oii at 732.0 nm. The two auroral cameras have different spatial resolutions. These resolutions are about 10 and 20 km from a spacecraft altitude of 8R
e
. The time to acquire and telemeter a 256×256-pixel image is about 12 s. The primary scientific objectives of this imaging instrumentation, together with thein-situ observations from the ensemble of ISTP spacecraft, are (1) quantitative assessment of the dissipation of magnetospheric energy into the auroral ionosphere, (2) an instantaneous reference system for thein-situ measurements, (3) development of a substantial model for energy flow within the magnetosphere, (4) investigation of the topology of the magnetosphere, and (5) delineation of the responses of the magnetosphere to substorms and variable solar wind conditions. 相似文献
18.
D. T. Young J. E. Nordholt J. L. Burch D. J. McComas R. P. Bowman R. A. Abeyta J. Alexander J. Baldonado P. Barker R. K. Black T. L. Booker P. J. Casey L. Cope F. J. Crary J. P. Cravens H. O. Funsten R. Goldstein D. R. Guerrero S. F. Hahn J. J. Hanley B. P. Henneke E. F. Horton D. J. Lawrence K. P. McCabe D. Reisenfeld R. P. Salazar M. Shappirio S. A. Storms C. Urdiales J. H. Waite Jr. 《Space Science Reviews》2007,129(4):327-357
The Plasma Experiment for Planetary Exploration (PEPE) flown on Deep Space 1 combines an ion mass spectrometer and an electron
spectrometer in a single, low-resource instrument. Among its novel features PEPE incorporates an electrostatically swept field-of-view
and a linear electric field time-of-flight mass spectrometer. A significant amount of effort went into developing six novel
technologies that helped reduce instrument mass to 5.5 kg and average power to 9.6 W. PEPE’s performance was demonstrated
successfully by extensive measurements made in the solar wind and during the DS1 encounter with Comet 19P/Borrelly in September
2001.
P. Barker is deceased. 相似文献
19.
A simple model has been developed that demonstrates that heliospheric X-ray emission can account for about 25%–50% of observed
soft X-ray background intensities. Similar to cometary soft X-ray emission, these X-rays are thought to be produced in the
heliosphere due to charge transfer collisions between heavy solar wind ions and interstellar neutrals. A more complex model
has now been developed to take into account temporal and spatial variations of the solar wind and interstellar neutrals. Measured
time histories of the solar wind proton flux are used in the model and the results are compared with the ‘long-term enhancements’
in the soft X-ray background measured by ROSAT for the same time period.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
20.
A.F. Nagy T.E. Cravens 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》1985,5(9):135-143
Our understanding of the physical and chemical processes which control the behavior of the Venus ionosphere has advanced significantly during the last few years. These advances are the result of a still growing data base and a variety of evolving theoretical models. This review summarizes some of these recent studies, especially those concerning the dynamics of the ionosphere, the maintenance of the nightside ionosphere, the energetics of the nightside ionosphere, and the time evolution of magnetic fields in the dayside ionosphere. 相似文献