Kinematics and Physics of Celestial Bodies最新文献

Longitudinal, latitudinal, and altitudinal features of the zonal wind in the Northern Hemisphere under the influence of 27-day variations of solar activity (SA) were studied. The research aims to improve the accuracy of weather forecasts and deepening our knowledge about dynamic processes of the interaction of atmospheric layers. Zonal wind data by 5° latitude from the website https://psn.noaa.gov at the longitudes of Europe and North America from 15 altitude levels (from 1000 to 10 hPa) and SA data from the website https://www-app3.gfz-potsdam.de were used. Twenty high-amplitude 27-day SA cycles during the decline phase of the 23rd 11-year solar cycle from 2002 to 2004 were studied. The average 27-day wind changes for each latitude and altitude are calculated by the superposed epoch analysis separately for the winter and summer seasons. For the first time, 27-day latitudinal and altitudinal variations of zonal wind with an amplitude of ~8 m/s, capable of influencing the weather in the extratropical atmosphere, were established. Despite the significant difference in the background wind field in winter and summer, the response of the wind field to SA influence is similar for both seasons. The maximum wind changes occur in the southern part of the polar atmospheric cell and the northern part of the Ferrell cell (50°–70° N) and gradually decrease in magnitude to the south and north. Wind changes are many times smaller in the tropical troposphere. At the boundaries of the global circulation cells, the direction of disturbed wind changes to the opposite. Changes in the position of jet streams by more than 1° in latitude and changes in the size of atmospheric circulation cells are also observed. In terms of height, the largest changes in the wind at all latitudes occur in the upper troposphere. There is a close relationship between the magnitude of the perturbed wind and changes in the tropopause height. The impact is realized through two-way dynamic stratospheric-tropospheric interaction, primarily in the area of the polar night jet and polar front jet stream. The presence of significant wind changes for the summer season indicates an important role not only of planetary-scale Rossby waves but also of shorter-wavelength waves. At the same time, their upward propagation can be ensured by nonlinear interaction between them.

This study examines the absorption lines of promethium, a radioactive element with a short half-life, in the spectra of the magnetic peculiar star HD 25 354, which belongs to the spectral class A0Vp. It also determines the promethium abundance in the star’s atmosphere. The analysis utilized an archival spectrum of HD 25 354 from the ELODIE database, obtained in 1996, covering the wavelength range of 400.0–680.0 nm, with a spectral resolution of R = 42 000 and a signal-to-noise ratio (S/N) of 100, recorded at the 1.93-m telescope at the Haute-Provence Observatory. Additionally, spectra collected by F. Musaev in 2006, using the 2-m telescope at Terskol Peak Observatory, were analyzed. These spectra covered the wavelength range of 370.0–940.0 nm, with S/N = 200 and R = 60 000. The previously determined atmospheric parameters of the star (T_eff = 12 800 K, log g = 4.15, V_micro = 0.23 km/s) and the chemical composition of its elements were used to calculate a synthetic spectrum over a wide range. This synthetic spectrum generally gave a satisfactory approximation of the observed spectrum. By comparing the synthetic spectrum of HD 25 354 with the observed data, 11 lines of promethium were identified, and its abundance was determined. The promethium abundance was found to be consistent with the abundance levels of other lanthanides, with a value of log N = 5.8–5.9 on the hydrogen scale, where log N(H) = 12. According to literature data, the promethium abundance in the atmosphere of HR 465 (log N = 5.05) is also within the range of lanthanide abundance.

The relevance of this study stems from the fact that, to date, there is no reliable and detailed explanation of the electromagnetic mechanism governing interactions between subsystems within the Earth (inner shells)–atmosphere–ionosphere–magnetosphere (EAIM) system. This mechanism can manifest itself under the action of high-energy sources of both natural and anthropogenic origins. Natural sources include weather fronts, thunderstorms, hurricanes (typhoons), volcanic eruptions, earthquakes, etc. All these natural processes may generate intense electromagnetic radiation in the VLF range (3–30 kHz). Such radiation is capable of interacting with the plasma in the lower ionosphere, triggering a series of secondary geophysical processes. This study presents the findings on the electromagnetic mechanism of subsystem interactions within the EAIM system, specifically focusing on the impact of intense electromagnetic radiation on the parameters of the lower ionosphere. A single lightning strike during the daytime can increase electron temperature by a factor of 60–44 at altitudes of 60–80 km, respectively. At night, a significant increase in electron temperature (by a factor of 60–50) can occur at altitudes of 80–95 km, respectively. This substantial electron heating results in the transparentization effect of the lower ionosphere plasma, leading to reduced electromagnetic radiation absorption at altitudes up to 80 km during the day. At night, however, the plasma exhibits a saturation effect at altitudes of 80–100 km, which is accompanied by an increase in electromagnetic radiation absorption. A single lightning strike does not cause a noticeable disturbance in electron density or the intensity of its fluctuations. However, it can produce minor (~0.01 nT) perturbations in the geomagnetic field and significant (~1 V/m) spikes in the vortex electric field. At a sufficiently high lightning frequency, noticeable disturbances in electron density and the intensity of its fluctuations may occur, potentially leading to the accumulation of disturbances N and (overline {Delta {{N}^{2}}} ). Significant perturbations in the parameters of the lower ionosphere can, in turn, generate secondary effects that propagate into the magnetosphere and magnetically conjugate regions.

Direct magnetic field measurements in sunspots by many spectral lines are important for elucidating the true magnitude and structure of the magnetic field at different levels of the solar atmosphere. Currently, magnetographic measurements are the most widespread, but such measurements mainly represent the longitudinal component of the magnetic field. In the sunspot umbra, such measurements give unreliable information and do not allow for determining the actual value of the module (absolute value) of the magnetic field. Such data can be obtained from spectral-polarization observations, thanks to which the magnetic field can be determined directly from Zeeman splitting, rather than as calibrated polarization in line profiles. The presented work presents the results of the study into the magnetic field in the sunspot on July 17, 2023, which was observed on the Echelle spectrograph of the horizontal solar telescope of the Astronomical Observatory of Taras Shevchenko National University of Kyiv. The I ± V profiles of ten photospheric lines of Fe I, Fe II, Ti I, and Ti II were analyzed in detail. The strongest magnetic field measured by the Fe I lines reaches 2600 G, and the difference in the measured intensities by these lines is sometimes at the level of 50–80%. The umbral lines of Ti I show, in general, the same magnetic fields as Fe I lines, while the lines of Fe II and Ti II show significantly weaker fields. Although the lateral field profile in the spot by most of the Fe I lines is smooth, quasi-Gaussian, one of the lines, namely Fe I λ 629.10 nm, shows a “dip” at 400–600 G in the sunspot umbra, which, most likely, is real. The obtained data probably indicate a combination of at least two effects: the dependence of measurements on the height of line formation in the solar atmosphere and the manifestation of Zeeman “saturation” in lines with different Lande factors. It also turned out that the umbral line of Ti I λ 630.38 nm shows somewhat stronger magnetic fields compared to non-umbral lines. The obtained data are planned to be used to clarify the general picture of the magnetic field in the spot by means of simulation.

Magnetic storm, ionospheric storm, atmospheric storm, and electrical storm are the components of a geospace storm resulting from a solar storm. In the literature, the main attention is paid to the analysis of severe and extreme geospace storms. It is these storms that have the greatest impact on the Earth–atmosphere–ionosphere–magnetosphere system. They are most dangerous for space-based and ground-based technological systems. Such storms have a significant impact on human well-being and health. Minor and moderate storms are much less studied than severe and extreme ones. There are good reasons to believe that such storms can have some impact on the systems and people. It is important that the frequency of occurrence of moderate storms is much greater than the frequency of occurrence of severe storms. All this determined the relevance of this work, which consists in the study of magnetic disturbances that arise during moderate geospace storms, which receive undeservedly little attention. The purpose of this paper is to analyze on a global scale the temporal variations of geomagnetic field components during moderate magnetic storms on April 28–29 and May 1–2, 2023. The latitudinal dependence of the geomagnetic field components temporal variations during two moderate magnetic storms in April–May 2023 and on reference days was analyzed on a global scale using the data of the global network of Intermagnet stations. The limits of fluctuations in the level of the geomagnetic field under quiet conditions and during moderate storms were estimated. The range of variations in the geomagnetic field level under quiet conditions decreased from 200–260 to 30–50 nT with decreasing geographic latitude. During the storms, these limits increased 1.3–2.1 times. The variations in the level of components at stations equidistant from the equator were close. This is true for both the Western and Eastern Hemispheres. The fluctuations of the geomagnetic field level at the stations operating approximately at the same latitude but in different hemispheres were also close.

Based on observations conducted at the Ernest Gurtovenko Horizontal Solar Telescope, the height of the polar chromosphere of the Sun was determined for the period 2012–2023. The measurement was calculated as the difference between the positions of the maximum radial brightness gradients in the continuum and at the core of the H_α line. The results indicate that the height of the polar chromosphere is lower near the maximum of the solar cycle (approximately 4500 km, or 6.3″) and higher near the minimum of the cycle (approximately 5000 km, or 6.9″). The chromosphere’s height at the southern pole in 2012–2013 and, particularly, 2016–2017 was higher than at the northern pole. This north–south asymmetry is likely related to differences in the dynamics and magnitude of the polar magnetic fields during Solar Cycle 24. The findings demonstrate that the time changes in the chromosphere’s height closely correlate with sunspot numbers, the strength of the polar magnetic field, and chromospheric indices of solar activity. The correlation coefficient between the average annual height of the chromosphere and the smoothed relative sunspot number is –0.64 for the northern hemisphere and –0.75 for the southern hemisphere. The correlation coefficient between the average annual height of the chromosphere and the smoothed values of the polar magnetic field strength (based on data from the Wilcox Solar Observatory) is 0.86 for the northern hemisphere and 0.53 for the southern hemisphere (the latter value increases to 0.77). The correlation coefficient between the average annual height of the chromosphere and the chromospheric index I_K2 reaches the highest values, 0.91, for the northern pole and 0.80 for the southern pole.

Wave disturbances from the solar terminator in the morning and evening hours were investigated using a ground-based network of very low frequency (VLF) radio stations. The data of measurements of the amplitudes of VLF radio signals on the GQD–A118 radio path with a transmitter in Great Britain (GQD, f = 22.1 kHz) and a receiving point in France (A118) were used. Amplitudes of radio signals change as a result of the propagation of atmospheric waves at the altitudes of localization of the upper wall of the Earth-ionosphere VLF waveguide. This makes it possible to use a network of VLF radio stations to monitor wave activity in the mesosphere (lower ionosphere). Based on the analysis of experimental data, it was established that pronounced periodic fluctuations in the amplitudes of radio signals are observed in the evening and in the morning for several hours after the passage of the solar terminator. Histograms of the distribution of these fluctuation periods for several months were constructed. The predominance of periods of radio signal fluctuations of 20–25 min was revealed both in the evening and in the morning hours. For the evening terminator, this result is consistent with our previous studies. The predominance of approximately the same wave periods in the morning was established for the first time. It is assumed that the observed fluctuations are caused by the propagation of acoustic-gravity waves (AGWs) from the solar terminator. The existence of a dominant period probably indicates that these perturbations represent a fundamental wave mode moving synchronously with the solar terminator.

The study of MHD waves in coronal structures is of great importance in coronal seismology. The study of these waves makes it possible to reveal the physical structure and heating mechanism of the solar corona. It is of great interest to calculate the line profile in the emission spectrum of a magneto-sonic wave for various physical parameters, calculate the energy flux and compare them with observations. In this paper, the profiles of the FeIX λ171Å line in the emission spectrum of slow magneto-acoustic waves propagating in coronal loops are calculated for cases of an optically thin layer and the change in density. The line profiles were calculated for the following parameter values: wave velocity amplitude ({{upsilon }_{0}}) = 10 km/s, coronal loop width 2000 and 5000 km, wavelength Λ = 20 000 and 50 000 km, Doppler width Δλ_d = 0.01 Å, and at values of the angle of the line of sight and at different phases of the wave. The energy flux density is 622.5 erg/(cm² s). The calculated values of the energy flux density strongly depend on the angle of the line of sight and on the phase of the wave and range from zero at large values of θ to ~4 × 10³ erg/(cm² s), the values of Doppler velocities ({{upsilon }_{{text{d}}}}) and velocities of non-thermal movements ({{upsilon }_{{{text{nt}}}}}) at small values of θ have a maximum value of ~13 km/s and decrease almost to zero at large values of θ. At different values of the angle of the line of sight, the asymmetry is almost not noticeable. An interesting result is that the values of the calculated (observed) energy flux can be both much less and much more than the true value: from almost zero at small values of θ. These values depend not only on the angle of the line of sight, but also on the width of the coronal loop and the wavelength.

Nonlinear equations called the Stenflo equations are usually used for the analytical description of the propagation of internal gravity waves in the Earth’s upper atmosphere. Solutions in the form of dipole vortices, tripole vortices, and vortex chains are previously obtained by these equations. The Stenflo equations also describe rogue waves, breathers, and dark solitons. If disturbances cease to be small, then their profiles are usually deformed, and, presumably, they cannot be considered plane waves. This study shows that this is not always the case for internal gravity waves and that these waves can propagate as plane waves even with large amplitudes. An exact solution of the system of nonlinear Stenflo equations for internal gravity waves that contain nonlinear terms in the form of Poisson brackets is given. The solution is obtained in the form of plane waves with arbitrary amplitude. To find a solution, the original system of equations is transformed. It is split into equations for the stream and vorticity functions as well as equations for the perturbed density. To solve the obtained equations, the procedure of the successive zeroing of Poisson brackets is applied. As a result, linear equations that allow one to find the accurate analytical solutions for internal gravity waves in the form of plane waves with arbitrary amplitude are obtained. By solving these linear equations in two different ways, we have analytically found expressions for the perturbed quantities and the dispersion equation. The nonlinear equations obtained for the current, vorticity, and perturbed density functions can be used to find other nonlinear solutions. The given solutions in the form of plane waves with arbitrary amplitude may be of interest for the analysis of the propagation of internal gravity waves in the Earth’s atmosphere and the interpretation of experimental data.