1,721,047 research outputs found
The centenary of solar-terrestrial physics
No full textThe years 1900–1902 saw important scientific landmarks, namely Marconi's transatlantic radio experiment and theoretical ideas of Lodge and Fitzgerald about what are now known as the solar wind, magnetosphere and ionosphere. These advances built on previous ideas put forward by several European scientists. Taking the discovery of the electron in 1897 as a prerequisite for real physical understanding of solar-terrestrial phenomena, the present time is the centenary of solar-terrestrial physics. Concentrating on the years around 1900, this paper also selects landmarks from 1600 onwards that led up to that time, and some from subsequent decades
Patterns of F2-layer variability
No full textThe ionosphere displays variations on a wide range of time-scales, ranging from operational time-scales of hours and days up to solar cycles and longer. We use ionosonde data from thirteen stations to study the day-to-day variability of the peak F2-layer electron density, NmF2, which we use to define quantitative descriptions of variability versus local time, season and solar cycle. On average, for years of medium solar activity (solar decimetric flux approximately 140 units), the daily fluctuations of NmF2 have a standard deviation of 20% by day and 33% by night. We examine and discuss the patterns of behaviour of ionospheric and geomagnetic variability, in particular the equinoctial peaks. For further analysis we concentrate on one typical midlatitude station, Slough. We find that the standard deviations of day-to-day and night-to-night values of Slough NmF2 at first increase with increasing length of the dataset, become fairly constant at lengths of 10–20 days and then increase further (especially at equinox) because of seasonal changes. We found some evidence of two-day waves, but they do not appear to be a major feature of Slough's F2 layer. Putting together the geomagnetic and ionospheric data, and taking account of the day-to-day variability of solar and geomagnetic parameters, we find that a large part of F2-layer variability is linked to that of geomagnetic activity, and attribute the rest to ‘meteorological’ sources at lower levels in the atmosphere. We suggest that the greater variability at night is due to enhanced auroral energy input, and to the lack of the strong photochemical control of the F2-layer that exists by day
The 70th anniversary of ionospheric sounding
No full textRoutine sounding of the ionosphere is 70 years old. This article describes its origins, starting from the pioneering trans-Atlantic transmission of 1901, and its development from 1931 to the present day, together with some recent directions in research using ionosonde dat
The solar-terrestrial event of 23 February 1956
No full textThe solar flare of 23 February 1956 and the resulting geophysical disturbance ranks as one of the most remarkable solar-terrestrial events of the twentieth century. It sparked many papers and has seldom been equalled. Fifty years after the International Geophysical Year, it seems timely to review the observations of the event from today’s perspective, and to draw on the recollections of scientists who were active at the time
Dynamics of Titan's thermosphere
Full text linkWe estimate the wind speeds in Titan’s thermosphere by considering the various terms of the wind equation, without actually solving it, with a view to anticipating what might be observed by the Cassini spacecraft in 2004. The winds, which are driven by horizontal pressure gradients produced by solar heating, are controlled in the Earth’s thermosphere by ion-drag and coriolis force, but in Titan’s thermosphere they are mainly controlled by the nonlinear advection and curvature forces. Assuming a day–night temperature difference of 20 K, we find that Titan’s thermospheric wind speed is typically 60 m s-1. In contrast, the Earth’s thermospheric winds, of order 50 m s-1, do not equalize day and night temperatures. We speculate on other factors, such as the electrodynamics of Titan’s thermosphere and the tides due to Saturn
The equatorial F-layer: Progress and puzzles
No full textThis work reviews some aspects of the ionospheric F-layer in the vicinity of the geomagnetic equator. Starting with a historical introduction, brief summaries are given of the physics that makes the equatorial ionosphere so interesting, concentrating on the large-scale structure rather than the smaller-scale instability phenomena. Several individual topics are then discussed, including eclipse effects, the asymmetries of the 'equatorial trough', variations with longitude, the semiannual variation, the effects of the global thermospheric circulation, and finally the equatorial neutral thermosphere, including 'superrotation' and possible topographic influences
Day-by-day modelling of the ionospheric F2-layer for year 2002
No full textThe thermosphere–ionosphere–mesosphere-electrodynamics general circulation model (TIME-GCM) has been run for the year 2002. Its version 1.2 features include day-by-day input of solar irradiance, geomagnetic energy input parameterized by the 3-h Kp index, and global lower boundary conditions from the National Centres for Environmental Prediction (NCEP) data. In addition, it includes tidal forcing from the global-scale wave model (GSWM) and parameterized gravity waves from below. The computed day-by-day values of noon peak electron density NmF2 agree well with ionosonde data for five northern sites and two southern mid-latitude sites, and closely follow the day-by-day modelled concentration ratio of atomic oxygen to molecular nitrogen. Seasonal and hemispheric patterns appear in the model with some, though not full, success. The model's day-to-day patterns show an impressive degree of variability, with simulations of total variability both above and below those observed.<br/
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