Siple VLF transmissions and their magnetospheric effects observed at Halley,Antarctica

Halley (75.5°S, 26.7°W, L = 4.3) is well placed for reception of subionospheric signals from the Siple transmitter. Occasionally a two-hop magnetospheric response to such signals can be observed. The data presented here are relevant to the problems of the radiation and propagation of VLF waves in the polar earth/ionosphere waveguide, duct stimulation and ducted wave amplification and the growth of triggered emissions. An upper sideband emission 20–40 Hz higher in frequency than the transmitted pulse was often received at a similar strength to, and simultaneously with the two-hop whistler mode echo.     

VLF line radiation observed at Halley and Siple

Power Line Harmonic Radiation and associated emissions observed at Siple [1, 2] are compared with line radiation activity observed at Halley, Antarctica [3]. We discuss the evidence for a Sunday decrease in magnetospheric VLF wave activity at the two stations. Other properties of line radiation relating to bandwidth, diurnal variation, wave echoing and frequency spacing are reviewed.     

Power line radiation in the magnetosphere

VLF radiation from electrical power transmission lines stimulates nonlinear wave-particle and wave-wave interactions in the magnetosphere, resulting in wave growth, triggering of emissions, and entrainment of other natural or manmade VLF waves. Examples of these effects will be reviewed using both ground-based and satellite data. In many instances, the interpretation of data is aided by Siple transmitter results that show similar spectral characteristics.     

A model of the rapid burster

A new burst mode of MXB 1730 - 335, the rapid burster, as discovered by Hakucho in August 1979, is characterized by a train of long X-ray bursts whose behaviour is dictated by the accretion rate. In this mode the burst luminosity reaches the Eddington limit, so that the X-ray pressure controls the accretion from a reservoir in the magnetopause and accretion columns in the polar regions explain general features of the rapid burster observed in August 1979.     

Optical bursts from X-ray irradiated accretion disk

A new burst mode of MXB 1730 - 335, the rapid burster, as discovered by Hakucho in August 1979, is characterized by a train of long X-ray bursts whose behaviour is dictated by the accretion rate. In this mode the burst luminosity reaches the Eddington limit, so that the X-ray pressure controls the accretion from a reservoir in the magnetopause and accretion columns in the polar regions explain general features of the rapid burster observed in August 1979.     

Electron precipitation near L=4: Longitudinal variation

Observations of penetrating electron precipitation at two L ∼ 4 stations in the southern hemisphere, Kerguelen and Siple Station, Antarctica, are summarized. The nearly complete absence of precipitation at Kerguelen and its frequent occurrence at Siple Station is explained in terms of their location with respect to the center of the South Atlantic geomagnetic anomaly at L ∼ 4. Conclusions which result from this explanation are discussed along with questions which remain concerning penetrating electron precipitation.     

VLF Emissions observed at the low latitude Indian station Varanasi

VLF emissions such as hiss, chorus, pulsing hiss, triggered emissions observed at Varanasi (geom. lat. = 14° 55′ N, long. = 153° 55′ E) are reported. An attempt has been made to explain the dynamic spectra in terms of the generation mechanism and propagation through the inhomogeneous magnetoplasma. It is noted that the reported events have propagated along different L-values in the magnetosphere, although they have been recorded at the same station. The ULF waves propagating along geomagnetic field lines modulate the growth rate of VLF waves, which results in the pulsation of VLF hiss intensity. The pulsating growth rate has been computed.     

ISEE-1 observations in the magnetosphere of VLF emissions triggered by nonducted coherent VLF waves during VLF waveinjection experiments

Recent data from the ISEE-1 spacecraft indicates that VLF emissions triggered by nonducted coherent VLF waves can differ in important aspects from VLF emissions triggered by ducted VLF waves.     

The rapid burster activity observed from tenma

The Japanese X-ray astronomy satellite Hakucho and Tenma observed the activity of the rapid burster MXB 1730-335 in 1979 and 1983. In the first observation from 8 to 22 August 1979, the activity began with rapidly repetitive type II bursts which are similar to those observed earlier. Then the energy per burst quickly increased and evolved to exhibit a long flat top or roughly trapezoidal shape. In the last phase, burst size became smaller and the activity returned to the short type II burst mode. In the second observation from 5 to 31 August 1983, the burster started to emit a train of bursts which aparently resemble to type I bursts with quasi-periodical occurrence of 74 ～ 90 minutes. In the second phase, there appeared long type II bursts of trapezoidal profiles and exotic long bursts. In the last phase, about 3000 rapidly repetitive short type II bursts were observed. The bursts with shortest intervals exhibited almost periodic features of 16 sec.The type II bursts in both observation evolved to the size E of ～ 6 × 10⁴⁰ erg that is one order larger than ever observed. They were long bursts (τ ≦ 600 s) of flat topped (trapezoidal) shape and those of exotic profiles. Those type II bursts exhibited some kinds of quasi-periodicities, which implies the vibrations or instabilities of the mass accretion onto the neutron stars. The type I bursts were often observed with/without type II bursts.     

Low-level circulation during the 1979 Indian summer monsoon

The GARP Monsoon Experiment (MONEX) provided a unique set of observations during the months May, June, July and August 1979, to study the Indian summer monsoon. Data sets from different platforms were collected during this period. In this paper, these platforms are reviewed and their data are presented with a special emphasis on the non-conventional ones : geostationary satellite (GOES), constant-level balloons (BALSAMINE Experiment) and instrumented aircrafts. Some results on the low-level circulation over the Arabian Sea as deduced from these observations are given. In 1979, the onset of the monsoon was very late and took place around mid-June. It was characterized by the formation of a vortex off the western coast of India and its later westward displacement over the Arabian Sea.     

The extreme and far ultraviolet environment at shuttle altitudes

The astronomical data obtained by the Far Ultraviolet Space Telescope (FAUST) and the Very Wide Field Camera (VWFC) on board the Spacelab I mission have triggered questions on the natural and induced Extreme and Far Ultraviolet (EUV and FUV) environment of the space shuttle. Moreover, the recent discovery of ∼1k Rayleighs N₂ Lyman Birge Hopfield (LBH) nightglow emissions by the U. S. Air Force's S3-4 satellite, and subsequent confirmation by the Imaging Spectrometric Observatory (ISO) experiment on the Spacelab I mission have serious implications for the astronomical observations from the shuttle. Since both ISO and S3-4 experiments were conducted from shuttle altitudes, the implied EUV and FUV environment for astronomical observations can be severe. In order to address the question of the suitability of the shuttle as an astronomical platform, we have examined data from FAUST and other experiments. We conclude that the FAUST background is most likely due to the observation of tropical UV arcs, a natural airglow phenomenon. Strategies for future shuttle experiments to overcome this and other natural emissions are discussed.     

VLF emissions at frequencies above the LHR in the plasmasphere as observed on low-orbiting intercosmos satellites

In a number of VLF experiments with low-orbiting Intercosmos satellites, high-intensity, discrete VLF emissions at frequencies above the local LHR were observed predominantly between L = 2.3 and 4.0. The frequency of their intensity maximum varies continuously with geomagnetic latitude, and approximately parallels the value of a quarter of the equatorial electron gyrofrequency. This kind of emissions has not yet been found on the records of ground stations. Their occurrence on satellite records shows very good correlation with the simultaneously measued electron temperature enhancements. The origin and mode of propagation of the emissions are discussed.     

Recent observations of the very low frequency interplanetary radio emission

Observations of radio emissions in the frequency range of 2 to 3 kHz have been made in the distant heliosphere by the Voyager 1 and 2 plasma wave instruments. Based primarily on wideband observations made periodically throughout the cruise phases of the missions the radio emission, first observed in 1982, appears to have been present almost continuously since 1983. The spectrum is complex, usually showing two peaks, one near 2 and another near 3 kHz. Occasionally, only one of the peaks is observed. A possible source for the radio emissions is the terminal shock in the outer heliosphere.     

哈雷彗星的JHK光度和1.3—2.6微米分光观测结果及分析

本文给出哈雷彗星在1986年3月25日至4月2日之间JHK波段测光和1.3—2.6微米分光观测结果。测光结果表明,3月22日彗星爆发在近红外波段也造成了明显的光变,但恢复正常光度的时间要滞后一些,且光变较之可见光波段要平缓.并指出在爆发期间,彗星除光变外尚有色变。分光观测到彗星在1.4、1.9微米的水发射线和位于2.6微米之外的可能的OH发射线。      

CME影响下L1点附近等离子体及共生微波爆发的射电辐射机制研究

CME在产生和发展过程中与日冕和行星际介质相互作用并发出不同波长的射电辐射．在研究了无CME时空间等离子体的各种辐射机制基础上,统计分析了1999年2月至1999年8月期间有较大的CME发生情况下,在CME影响下L1拉格朗日点附近等离子体参数发生变化后的射电辐射机制．分析结果表明,其射电辐射机制主要是轫致辐射、微量的回旋辐射和更加微弱的复合辐射．此外,分析讨论了1999年2月至1999年8月期间与CME共生的太阳微波爆发．分析结果表明,与CME共生的是微波逐渐型爆发、尖峰爆发,其辐射机制主要是轫致辐射、回旋共振辐射、等离子体辐射及电子回旋脉泽辐射．     

Stratospheric flights with large polyethylene baloons from equatorial latitudes

Starting with average 50% success for stratospheric balloon flights during 1959–1969 and attaining 100% success during 1972–1973, the success record dropped to 50% during 1974–1979. Through a critical analysis of 59 flights made from Hyderabad and 21 flights made from other equatorial bases, revised design criteria were proposed for balloons to be flown from equatorial latitudes, which were accepted by M/s Winzen International, Inc. (WII), U.S.A. and have again raised the success record to 93% for 15 flights made since April 1980. A revised analysis for 71 flights made from 1965 to 1984 has been presented. Stratospheric circulation over Hyderabad indicating predominance of easterlies with mesospheric westerlies descending occasionally into stratosphere has been discussed.     

Vertical density and temperature structure over Northern Europe

During the Energy Budget Campaign, several profiles of the density and temperature of the upper atmosphere were obtained. The measurements were made using rocket-borne instrumentation launched from ESRANGE, Sweden and Andoya Rocket Range, Norway during November and December, 1980. The techniques included meteorological temperature sondes, passive falling spheres, accelerometer instrumented falling spheres, density gauges, mass spectrometers and infrared emission experiments. The instruments provided data within the altitude range from 20 km to 150 km. The measurements were made during periods which have been grouped into three categories by level of geomagnetic activity. Analysis has been made to compare the results and to examine the oscillations and fluctuations in the vertical profiles for scales ranging between hundreds of meters and tens of kilometers. Most of the features observed fit qualitatively within the range expected for internal gravity waves. The geomagnetic storm conditions may be associated with enhanced wave activity and heating observed in the lower thermosphere.     

Validation of aerosol measurements by the satellite sensors SAM II and SAGE

The satellite sensors SAM II and SAGE have been developing a global data base on stratospheric aerosols since they were launched in October 1978 and February 1979, respectively. The validity of this data base has been tested by numerous comparisons with other measurements made by lidars, balloon-borne particle counters, and aircraft-borne impactors and filters. Because the satellite sensors measure extinction and the correlative sensors measure other properties (e.g., backscatter, number, mass), special techniques are required to convert each measured property to other properties and to quantify conversion uncertainties and measurement uncertainties. Use of these techniques in two major comparative experiments shows that the SAM II and SAGE extinction measurements agree with each other and with values derived from dustsonde, lidar, and filter measurements. In addition, the comparative experiments have highlighted the uncertainties of each type of sensor and stimulated further efforts to reduce these uncertainties.     

Field and wave measurements aboard the Aureol-3 spacecraft

In the Soviet-French Arcad-3 project, 3 experiments TBF-ONCH, TRAC and ISOPROBE are carried out on board the Aureol-3 satellite to measure the AC and DC electric and magnetic fields and waves. Several modes of telemetry, real time and memory regimes are available for data transmission. TBF-ONCH is devoted to the measurement of 3 components of the DC electric field, 2 electric and 3 magnetic components of the waves. In one mode of the real time telemetry these 5 components are transmitted simultaneously in the frequency range 10 Hz-1.5 kHz in order to be able to determine the wave normal directions of natural emissions and to localize their sources. In the second mode, morphological studies of saucers, chorus, hiss and triggered emissions can be undertaken using the wide band transmission (70 Hz-16 kHz) of any one of these 5 components with the possibility of periodically changing the transmitted component every 4 seconds or keeping the same one during all the pass. TRAC makes use of the on board 3 axis flux gate magnetometer to perform a fine measurement of the magnetic effects of the currents flowing in the vicinity of the spacecraft either in the ionosphere or along the magnetic field lines, with a resolution of ～ 12 nT and in the frequency range from DC to ～ 20 Hz. One component of the HF electric field (0.1–10 Mhz) is measured by ISOPROBE (see companion paper). Examples of inflight measurements from the above instruments and their presentation on microfiches are shown. Some new phenomena are emphasized and briefly discussed.     

A skeptic's view of PLR effects in the magnetosphere

A critical appraisal is made of the hypothesis that power-line harmonic radiation can influence the Earth's radiation belts by triggering intense magnetospheric emissions which in turn resonantly scatter trapped electrons into the atmospheric loss cone. While such triggering may indeed occur, a combination of theoretical arguments supplemented by an indepth analysis of OGO-5 satellite data is employed to show that triggered waves comprise at best a small fraction of the total magnetospheric wave population. Previous claims to the contrary have been either based on erroneous statistical arguments or biased by the limited sample of ducted waves detectable by ground based receivers. The totality of satellite data is consistent with a predominantly natural origin for the two classes of electromagnetic waves (chorus and plasmaspheric hiss) which are known to interact strongly with energetic radiation belt electrons.