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821.
Konrad Dennerl 《Space Science Reviews》2006,126(1-4):403-433
X-rays from Mars were first detected in July 2001 with the satellite Chandra. The main source of this radiation was fluorescent
scattering of solar X-rays in its upper atmosphere. In addition, the presence of an extended X-ray halo was indicated, probably
resulting from charge exchange interactions between highly charged heavy ions in the solar wind and neutrals in the Martian
exosphere. The statistical significance of the X-ray halo, however, was very low. In November 2003, Mars was observed again
in X-rays, this time with the satellite XMM-Newton. This observation, characterized by a considerably higher sensitivity,
confirmed the presence of the X-ray halo and proved that charge exchange is indeed the origin of the emission. This was the
first definite detection of charge exchange induced X-ray emission from the exosphere of another planet. Previously, this
kind of emission had been detected from comets (which are largely exospheres) and from the terrestrial exosphere. Because
charge exchange interactions between atmospheric constituents and solar wind ions are considered as an important nonthermal
escape mechanism, probably responsible for a significant loss of the Martian atmosphere, X-ray observations may lead to a
better understanding of the present state of the Martian atmosphere and its evolution. X-ray images of the Martian exosphere
in specific emission lines exhibited a highly anisotropic morphology, varying with individual ions and ionization states.
With its capability to trace the X-ray emission out to at least 8 Mars radii, XMM-Newton can explore exospheric regions far
beyond those that have been observationally explored to date. Thus, X-ray observations provide a novel method for studying
processes in the Martian exosphere on a global scale. 相似文献
822.
The Neutral Particle Detector (NPD) of the ASPERA-3 experiment (Analyser of Space Plasmas and Energetic Atoms) on board the
Mars Express (MEX) spacecraft observed an intense flux of H ENAs (energetic neutral atoms) with average energy of about 1.5
keV emitted anisotropically from the subsolar region of Mars. The NPD detected the ENA jet near the bow shock at radial distances
of about 1 R
M from the Martian surface as the spacecraft moved outbound, while the NPD continuously pointed towards the subsolar region.
The jet intensity shows oscillative behavior. These intensity variations occur on two clearly distinguishable time scales.
The majority of the identified events have an average oscillation period of about 50 sec. The second group consists of events
with long-scale variations with a time scale of approximately 300 sec. The fast oscillations of the first group exhibit a periodic structure and are detected in every orbit, while the slow variations of the second group are identified in ∼40% of orbits. The intensity of the fast oscillations have a peak-to-valley ratio about 20 to 30% of the peak intensity. One of the possible mechanisms to explain
fast oscillations is the formation of the low frequency ion waves at the subsolar region of Mars. Slow variations may be explained by either temporal variations in the ENA generation source or by a specific structure of the
ENA generation source, in which hair-like ENA subjets can be present. 相似文献
823.
Because of its chemical and radiative properties, atmospheric ozone constitutes a key element of the Earth’s climate system.
Absorption of sunlight by ozone in the ultraviolet wavelength range is responsible for stratospheric heating, and determines
the temperature structure of the middle atmosphere. Changes in middle atmospheric ozone concentrations result in an altered
radiative input to the troposphere and to the Earth’s surface, with implications on the energy balance and the chemical composition
of the lower atmosphere. Although a wide range of ground- and satellite-based measurements of its integrated content and of
its vertical distribution have been performed since several decades, a number of uncertainties still remain as to the response
of middle atmospheric ozone to changes in solar irradiance over decadal time scales. This paper presents an overview of achieved
findings, including a discussion of commonly applied data analysis methods and of their implication for the obtained results.
We suggest that because it does not imply least-squares fitting of prescribed periodic or proxy data functions into the considered
times series, time-domain analysis provides a more reliable method than multiple regression analysis for extracting decadal-scale
signals from observational ozone datasets. Applied to decadal ground-based observations, time-domain analysis indicates an
average middle atmospheric ozone increase of the order of 2% from solar minimum to solar maximum, which is in reasonable agreement
with model results. 相似文献
824.
Adaptive combining of experimentally obtained heterodyned pulse position modulated (PPM) signals with pulse-to-pulse coherence, in the presence of simulated spatial distortions resembling atmospheric turbulence, is demonstrated. The adaptively combined PPM signals are phased up via an least-mean-square algorithm suitably optimized to operate with PPM in the presence of additive shot noise. A convergence analysis of the algorithm is presented, and results with both computer simulated and experimentally obtained PPM signals are analyzed. 相似文献
825.
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
826.
This paper studies the response of the middle atmosphere to the 11-year solar cycle. The study is based on numerical simulations
with the Hamburg Model of the Neutral and Ionized Atmosphere (HAMMONIA), a chemistry climate model that resolves the atmosphere
from the Earth’s surface up to about 250 km. Results presented here are obtained in two multi-year time-slice runs for solar
maximum and minimum conditions, respectively. The magnitude of the simulated annual and zonal mean stratospheric response
in temperature and ozone corresponds well to observations. The dynamical model response is studied for northern hemisphere
winter. Here, the zonal mean wind change differs substantially from observations. The statistical significance of the model’s
dynamical response is, however, poor for most regions of the atmosphere. Finally, we discuss several issues that render the
evaluation of model results with available analyses of observational data of the stratosphere and mesosphere difficult. This
includes the possibility that the atmospheric response to solar variability may depend strongly on longitude. 相似文献
827.
Satellite Measurements of Middle Atmospheric Impacts by Solar Proton Events in Solar Cycle 23 总被引:1,自引:0,他引:1
C. H. Jackman M. T. Deland G. J. Labow E. L. Fleming M. López-Puertas 《Space Science Reviews》2006,125(1-4):381-391
Solar cycle 23 was extremely active with seven of the largest twelve solar proton events (SPEs) in the past forty years recorded.
These events caused significant polar middle atmospheric changes that were observed by a number of satellites. The highly
energetic protons produced ionizations, excitations, dissociations, and dissociative ionizations of the background constituents
in the polar cap regions (>60 degrees geomagnetic latitude), which led to the production of HOx (H, OH, HO2) and NOy (N, NO, NO2, NO3, N2O5, HNO3, HO2NO2, BrONO2, ClONO2). The HOx increases led to short-lived ozone decreases in the polar mesosphere and upper stratosphere due to the short lifetimes of
the HOx constituents. Polar middle mesospheric ozone decreases greater than 50 % were observed and computed to last for hours to
days due to the enhanced HOx. The NOy increases led to long-lived polar stratospheric ozone changes because of the long lifetime of the NOy family in this region. Upper stratospheric ozone decreases of >10 % were computed to last for several months past the solar
events in the winter polar regions because of the enhanced NOy. 相似文献
828.
Our current understanding of the acceleration of solar-energetic particles is reviewed. The emphasis in this paper is on analytic
theory and numerical modeling of the physics of diffusive shock acceleration. This mechanism naturally produces an energy
spectrum that is a power law over a given energy interval that is below a characteristic energy where the spectrum has a break,
or a rollover. This power law is a common feature in the observations of all types of solar-energetic particles, and not necessarily just those associated with shock waves (e.g. events associated with
impulsive solar flares which are often described in terms of resonant stochastic acceleration). Moreover, the spectral index
is observed to have remarkably little variability from one event to the next (about 50%). Any successful acceleration mechanism
must be able to produce this feature naturally and have a resulting power-law index that does not depend on physical parameters
that are expected to vary considerably. Currently, only diffusive shock acceleration does this. 相似文献
829.
J. Büchner 《Space Science Reviews》2006,124(1-4):345-360
Reconnection is a major commonality of solar and magnetospheric physics. It was conjectured by Giovanelli in 1946 to explain
particle acceleration in solar flares near magnetic neutral points. Since than it has been broadly applied in space physics
including magnetospheric physics. In a special way this is due to Harry Petschek, who in 1994 published his ground breaking
solution for a 2D magnetized plasma flow in regions containing singularities of vanishing magnetic field. Petschek’s reconnection
theory was questioned in endless disputes and arguments, but his work stimulated the further investigation of this phenomenon
like no other. However, there are questions left open. We consider two of them – “anomalous” resistivity in collisionless
space plasma and the nature of reconnection in three dimensions. The CLUSTER and SOHO missions address these two aspects of
reconnection in a complementary way -- the resistivity problem in situ in the magnetosphere and the 3D aspect by remote sensing of the Sun. We demonstrate that the search for answers to both questions
leads beyond the applicability of analytical theories and that appropriate numerical approaches are necessary to investigate
the essentially nonlinear and nonlocal processes involved. Necessary are both micro-physical, kinetic Vlasov-equation based
methods of investigation as well as large scale (MHD) simulations to obtain the geometry and topology of the acting fields
and flows. 相似文献
830.
Chemical and physical processes in the outer solar nebula are reviewed. It is argued that the outer nebula was a chemically
active environment with UV photochemistry and ion-molecule chemistry in its low density regions and grain-catalyzed chemistry
in Jovian protoplanetary subnebulae. Presolar material was altered to greater or lesser extent by these spatially and temporally
variable processes, which mimic many features of interstellar chemistry. Experiments, models, and observations are recommended
to address the questions of presolar versus nebular dominance in the outer solar nebula and of how to distinguish interstellar
and nebular sources of cometary volatiles.
This revised version was published online in June 2006 with corrections to the Cover Date. 相似文献