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Planetary upper atmospheres-coexisting thermospheres and ionospheres-form an important boundary between the planet itself
and interplanetary space. The solar wind and radiation from the Sun may react with the upper atmosphere directly, as in the
case of Venus. If the planet has a magnetic field, however, such interactions are mediated by the magnetosphere, as in the
case of the Earth. All of the Solar System’s giant planets have magnetic fields of various strengths, and interactions with
their space environments are thus mediated by their respective magnetospheres. This article concentrates on the consequences
of magnetosphere-atmosphere interactions for the physical conditions of the thermosphere and ionosphere. In particular, we
wish to highlight important new considerations concerning the energy balance in the upper atmosphere of Jupiter and Saturn,
and the role that coupling between the ionosphere and thermosphere may play in establishing and regulating energy flows and
temperatures there. This article also compares the auroral activity of Earth, Jupiter, Saturn and Uranus. The Earth’s behaviour
is controlled, externally, by the solar wind. But Jupiter’s is determined by the co-rotation or otherwise of the equatorial
plasmasheet, which is internal to the planet’s magnetosphere. Despite being rapid rotators, like Jupiter, Saturn and Uranus
appear to have auroral emissions that are mainly under solar (wind) control. For Jupiter and Saturn, it is shown that Joule
heating and “frictional” effects, due to ion-neutral coupling can produce large amounts of energy that may account for their
high exospheric temperatures. 相似文献
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The interaction of the solar wind with the Martian exosphere and ionosphere leads to significant loss of atmosphere from the
planet. Spacecraft data confirm that this is the case. However, the issue is how much is actually lost. Given that spacecraft
coverage is sparse, simulation is one of the few ways for these estimates to be made. In this paper the evolution of our attempts
to place bounds on this loss rate will be addressed. Using a hybrid particle code the loss rate with respect to solar EUV
flux is addressed as well as a variety of numerical and chemical issues. The progress made has been of an evolutionary nature,
with one approach tried and tested followed by another as the simulations are improved and better estimates are produced.
The results to be reported suggest that the ion loss rates are high enough to explain the loss of water from Mars during earlier
solar epochs. 相似文献
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E. Nielsen H. Zou D. A. Gurnett D. L. Kirchner D. D. Morgan R. Huff R. Orosei A. Safaeinili J. J. Plaut G. Picardi 《Space Science Reviews》2006,126(1-4):373-388
The Martian ionosphere has for the first time been probed by a low frequency topside radio wave sounder experiment (MARSIS)
(Gurnett et al., 2005). The density profiles in the Martian ionosphere have for the first time been observed for solar zenith angles less
than 48 degrees. The sounder spectrograms typically have a single trace of echoes, which are controlled by reflections from
the ionosphere in the direction of nadir. With the local density at the spacecraft derived from the sounder measurements and
using the lamination technique the spectrograms are inverted to electron density profiles. The measurements yield electron
density profiles from the sub-solar region to past the terminator. The maximum density varies in time with the solar rotation
period, indicating control of the densities by solar ionizing radiation. Electron density increases associated with solar
flares were observed. The maximum electron density varies with solar zenith angle as predicted by theory. The altitude profile
of electron densities between the maximum density and about 170m altitude is well approximated by a classic Chapman layer.
The neutral scale height is close to 10 to 13 km. At altitudes above 180 km the densities deviate from and are larger than
inferred by the Chapman layer. At altitudes above the exobase the density decrease was approximated by an exponential function
with scale heights between 24 and 65 km. The densities in the top side ionosphere above the exobase tends to be larger than
the densities extrapolated from the Chapman layer fitted to the measurements at lower altitudes, implying more efficient upward
diffusion above the collision dominated photo equilibrium region. 相似文献
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At present, the main problem faced by ground-based augment system (GBAS) is that though carder smoothing filter and local differential global positioning system (LDGPS) improve the accuracy of the pseudorange by reducing the noise in it and eliminating almost all the common errors between the user and the reference station, they also cause extra errors on account of the effects of the ionosphere temporal and spatial gradients. Based on the analysis of these errors as well as the smoothing noise, this article suggests a new algorithm to design the optimal Hatch filter, whose smoothing window width varies real-time with the satellite elevation, ionosphere variation, and distance from the user to the reference station. By conducting the positioning process in the GBAS emulation platform for several hours and after its comparison with the performances of traditional Hatch filters, it is found that the errors in the differential correction become smaller and the positioning accuracy gets heightened with this new method. 相似文献
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Michael W. Liemohn Yingjuan Ma Rudy A. Frahm Xiaohua Fang Janet U. Kozyra Andrew F. Nagy J. David Winningham James R. Sharber Stas Barabash Rickard Lundin 《Space Science Reviews》2006,126(1-4):63-76
Atmospheric photoelectrons have been observed well above the ionosphere of Mars by the ASPERA-3 ELS instrument on Mars Express.
To systematically interpret these observations, field lines from two global MHD simulations were analyzed for connectivity
to the dayside ionosphere (allowing photoelectron escape). It is found that there is a hollow cylinder behind the planet from
1–2 R
M away from the Mars-Sun line that has a high probability of containing magnetic field lines with connectivity to the dayside
ionosphere. These results are in complete agreement with the ELS statistics. It is concluded that the high-altitude photoelectrons
are the result of direct magnetic connectivity to the dayside at the moment of the measurement, and no extra trapping or bouncing
mechanisms are needed to explain the data. 相似文献
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Kamide Y. Kihn E.A. Ridley A.J. Cliver E.W. Kadowaki Y. 《Space Science Reviews》2003,107(1-2):307-316
We report the recent progress in our joint program of real-time mapping of ionospheric electric fields and currents and field-aligned
currents through the Geospace Environment Data Analysis System (GEDAS) at the Solar-Terrestrial Environment Laboratory and
similar computer systems in the world. Data from individual ground magnetometers as well as from the solar wind are collected
by these systems and are used as input for the KRM and AMIE magnetogram-inversion algorithms, which calculate the two-dimensional
distribution of the ionospheric parameters. One of the goals of this program is to specify the solar-terrestrial environment
in terms of ionospheric processes, providing the scientific community with more than what geomagnetic activity indices and
statistical models provide.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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We discuss quasi-static and dynamic models of the magnetotail response to perturbations imposed by the solar wind, focusing
particularly on the formation of thin current sheets, their structure and breakup. 相似文献
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本文给出了一个使滞后的相似组合大系统镇定的分散鲁棒控制器的设计方法。不确定性是时变的,是以不确定参数出现在每个子系统中,而存在于互联项中的不确定性假设可能知道它的边界,当系统具有某种特征时,简化了一般控制器的设计。 相似文献
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系统科学与民航安全文化建设 总被引:2,自引:0,他引:2
用现代系统理论观战,审视了中国民航安全文化建设的历史经验,得出了有益于安全文化建设的指导思想。首先,通过对安全文化与民航系统的协同问题的分析,探讨了对”安全第一“原则的深层次理解及在实际工作中的把握;其次,研究了系统的运动与安全文化发展的内在关系,提出了保证安全文化建设健康发展的思路。 相似文献
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航空发动机燃油与控制系统的研究与展望 总被引:3,自引:0,他引:3
归纳和分析了国内外军用航空发动机燃油与控制系统的研制现状和今后的发展方向 ,简要介绍和评述了主燃油控制、加力燃油控制、尾喷口控制、防喘控制、发动机状态监视 ,特别是FADEC系统的技术特点、方案选择和研究动向。从中可以看出 ,这些方面的技术进步推动了航空发动机的发展 相似文献
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I. I. Alexeev 《Space Science Reviews》2006,122(1-4):55-68
A dependence of the polar cap magnetic flux on the interplanetary magnetic field and on the solar wind dynamic pressure is
studied. The model calculations of the polar cap and auroral oval magnetic fluxes at the ionospheric level are presented.
The obtained functions are based on the paraboloid magnetospheric model calculations. The scaling law for the polar cap diameter
changing for different subsolar distances is demonstrated. Quiet conditions are used to compare theoretical results with the
UV images of the Earth’s polar region obtained onboard the Polar and IMAGE spacecrafts. The model calculations enable finding
not only the average polar cap magnetic flux but also the extreme values of the polar cap and auroral oval magnetic fluxes.
These values can be attained in the course of the severe magnetic storm. Spectacular aurora often can be seen at midlatitude
during severe magnetic storm. In particularly, the Bastille Day storm of July 15–16, 2000, was a severe magnetic storm when
auroral displays were reported at midlatitudes. Enhancement of global magnetospheric current systems (ring current and tail
current) and corresponding reconstruction of the magnetospheric structure is a reason for the equatorward displacement of
the auroral zone. But at the start of the studied event the contracted polar cap and auroral oval were observed. In this case,
the sudden solar wind pressure pulse was associated with a simultaneous northward IMF turning. Such IMF and solar wind pressure
behavior is a cause of the observed aurora dynamics. 相似文献
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In seeking to understand the formation of the giant planets and the origin of their atmospheres, the heavy element abundance
in well-mixed atmosphere is key. However, clouds come in the way. Thus, composition and condensation are intimately intertwined
with the mystery of planetary formation and atmospheric origin. Clouds also provide important clues to dynamical processes
in the atmosphere. In this chapter we discuss the thermochemical processes that determine the composition, structure, and
characteristics of the Jovian clouds. We also discuss the significance of clouds in the big picture of the formation of giant
planets and their atmospheres. We recommend multiprobes at all four giant planets in order to break new ground. 相似文献
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用矩量法求解闭合导体目标的电场积分方程或磁场积分方程将得到不正确的表面电流。提出了一种确定正确表面电流的有效方法,即正确的表面电流由非谐振模电流和归一化的谐振模电流与一未知复因子的乘积组成,通过令闭合导体内给定点的总电场为零可得该未知复因子。计算了一无限长理想导体圆柱谐振时的表面电流,所得结果与解析解一致,进而证明了本方法的有效性和准确性。 相似文献
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华丹宏 《中国民航学院学报》1998,16(4):44-48
介绍了A340导航系统:大气数据惯性基准系统、电子飞行仪表系统、ATC/S模式应答机及机载防撞系统等。分析了机载导航系统的现状及发展方向,为同类飞机的雏护和培训提供参考。 相似文献
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高温下直流电位法测量裂纹长度的应用 总被引:1,自引:0,他引:1
介绍了直流电位法测量疲劳裂纹长度方法的基本原理、实现方法、及所需配置的仪器,并对有关影响因素作了分析.该测量系统主要用于在高温下测量各种材料在恒幅载荷下的疲劳裂纹扩展和门槛值试验中的疲劳裂纹长度,可以提高测量疲劳裂纹长度的自动化水平. 相似文献
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牟德一 《中国民航学院学报》2001,19(5):23-27
从哲学视角论述了现代系统科学的产生与发展,探讨其与马克思主义辩证只唯物史观的内在联系,并且从博大精深的古老中华文化里探究系统观念之渊源。 相似文献