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Academic literature on the topic 'Geomagnetically quiet'

Author: Grafiati
Published: 6 September 2023

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Journal articles on the topic "Geomagnetically quiet"

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Unnikrishnan, K. "A comparative study on chaoticity of equatorial/low latitude ionosphere over Indian subcontinent during geomagnetically quiet and disturbed periods." Nonlinear Processes in Geophysics 17, no. 6 (December 15, 2010): 765–76. http://dx.doi.org/10.5194/npg-17-765-2010.

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Abstract. In the present study, the latitudinal aspect of chaotic behaviour of ionosphere during quiet and storm periods are analyzed and compared by using GPS TEC time series measured at equatorial trough, crest and outside crest stations over Indian subcontinent, by employing the chaotic quantifiers like Lyapunov exponent (LE), correlation dimension (CD), entropy and nonlinear prediction error (NPE). It is observed that the values of LE are low for storm periods compared to those of quiet periods for all the stations considered here. The lowest value of LE is observed at the trough station, Agatti (2.38° N, Geomagnetically), and highest at crest station, Mumbai (10.09° N, Geomagnetically) for both quiet and storm periods. The values of correlation dimension computed for TEC time series are in the range 2.23–2.74 for quiet period, which indicate that equatorial ionosphere may be described with three variables during quiet period. But the crest station Mumbai shows a higher value of CD (3.373) during storm time, which asserts that four variables are necessary to describe the system during storm period. The values of non linear prediction error (NPE) are lower for Agatti (2.38° N, Geomagnetically) and Jodhpur (18.3° N, Geomagnetically), during storm period, compared to those of quiet period, mainly because of the predominance of non linear aspects during storm periods The surrogate data test is carried out and on the basis of the significance of difference of the original data and surrogates for various aspects, the surrogate data test rejects the null hypothesis that the time series of TEC during storm and quiet times represent a linear stochastic process. It is also observed that using state space model, detrended TEC can be predicted, which reasonably reproduces the observed data. Based on the values of the above quantifiers, the features of chaotic behaviour of equatorial trough crest and outside the crest regions of ionosphere during geomagnetically quiet and disturbed periods are briefly discussed.
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SHEN, Changshou, Minyun ZI, Jingsong WANG, and Jiyao XU. "Structure Distribution ofNmF2 during a Geomagnetically Quiet Period." Chinese Journal of Geophysics 46, no. 6 (November 2003): 1050–57. http://dx.doi.org/10.1002/cjg2.425.

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Kane, T. A., R. A. Makarevich, and J. C. Devlin. "HF radar observations of ionospheric backscatter during geomagnetically quiet periods." Annales Geophysicae 30, no. 1 (January 18, 2012): 221–33. http://dx.doi.org/10.5194/angeo-30-221-2012.

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Abstract. The quiet-time coherent backscatter from the F-region observed by the Tasman International Geospace Environment Radar (TIGER) Bruny Island HF radar is analysed statistically in order to determine typical trends and controlling factors in the ionospheric echo occurrence. A comparison of the F-region peak density values from the IRI-2007 model and ionosonde measurements in the vicinity of the radar's footprint shows a very good agreement, particularly at subauroral and auroral latitudes, and model densities within the radar's footprint are used in the following analyses. The occurrence of F-region backscatter is shown to exhibit distinct diurnal, seasonal and solar cycle variations and these are compared with model trends in the F-region peak electron density and Pedersen conductance of the underlying ionosphere. The solar cycle effects in occurrence are demonstrated to be strong and more complex than a simple proportionality on a year-to-year basis. The diurnal and seasonal effects are strongly coupled to each other, with diurnal trends exhibiting a systematic gradual variation from month to month that can be explained when both electron density and conductance trends are considered. During the night, the echo occurrence is suggested to be controlled directly by the density conditions, with a direct proportionality observed between the occurrence and peak electron density. During the day, the echo occurrence appears to be controlled by both conductance and propagation conditions. It is shown that the range of echo occurrence values is smaller for larger conductances and that the electron density determines what value the echo occurrence takes in that range. These results suggest that the irregularity production rates are significantly reduced by the highly conducting E layer during the day while F-region density effects dominate during the night.
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Kitamura, N., K. Seki, Y. Nishimura, N. Terada, T. Ono, T. Hori, and R. J. Strangeway. "Photoelectron flows in the polar wind during geomagnetically quiet periods." Journal of Geophysical Research: Space Physics 117, A7 (July 2012): n/a. http://dx.doi.org/10.1029/2011ja017459.

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Maeda, Sawako, Hitoshi Fujiwara, and Satonori Nozawa. "Momentum balance of daysideEregion neutral winds during geomagnetically quiet summer days." Journal of Geophysical Research: Space Physics 104, A9 (September 1, 1999): 19871–79. http://dx.doi.org/10.1029/1999ja900224.

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Liu, Z. ‐Y, Q. ‐G Zong, H. Zou, Y. F. Wang, and B. Wang. "Drifting Electron Holes Occurring During Geomagnetically Quiet Times: BD‐IES Observations." Journal of Geophysical Research: Space Physics 124, no. 11 (November 2019): 8695–706. http://dx.doi.org/10.1029/2019ja027194.

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7

Edward, Uluma, Ndinya Boniface, and Omondi George. "SCINDA-GPS derived TEC depletions and amplitude scintillations over Kisumu, Kenya during selected quiet and storm days of 2013 and 2014." International Journal of Advanced Astronomy 8, no. 1 (May 15, 2020): 1. http://dx.doi.org/10.14419/ijaa.v8i1.30232.

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Total Electron Content (TEC) depletion and amplitude scintillation (S4) can be derived from, SCINDA-GPS receivers situated in various parts of the equatorial region. In this paper we present results of characterization of TEC depletions and amplitude scintillations over Kisumu, Kenya (Geomagnetic coordinates: 9.64o S, 108.59o E; Geographic coordinates: 0.02o S, 34.6o E) for both selected geomagnetically quiet and geomagnetically disturbed conditions between 1st January 2013 and 31st December 2014 using data derived from the Kisumu NovAtel GSV4004B SCINDA-GPS receiver situated at Maseno University. TEC depletions and amplitude scintillations affect Global Positioning System (GPS) signals in the ionosphere as they propagate from the satellite to the receiver. This study aims to investigate day to day variability of TEC depletions and amplitude scintillations over Kisumu, Kenya during both geomagnetically quiet and geomagnetically disturbed days of 2013 and 2014 which was a high solar activity period for Solar Cycle 24. Seasonal variability of TEC depletions and S4 index is also presented. The Receiver Independent Exchange (RINEX) data for the years 2013 and 2014 was retrieved from the Kisumu SCINDA-GPS receiver, processed to obtain Vertical Total Electron Content (VTEC), S4 and Universal Time (UT) and fed into MATLAB to generate VTEC and S4 plots against UT for each selected quiet and storm day within the 2013 and 2014 period. The obtained results showed a diurnal variation of TEC where TEC was minimum at pre-sunrise, maximum during daytime and minimum during nighttime. The minimum TEC during pre-sunrise and nighttime was attributed to reduced solar intensity while maximum TEC during daytime is attributed to increased solar intensity. Most of the selected quiet and storm days of the years 2013 and 2014 showed TEC depletions and TEC enhancements corresponding with enhanced amplitude scintillations between 1800UT and 20:00UT. This might be attributed to the rapid rise of the F-layer and the increase in the vertical E x B plasma drift due to the Pre-reversal Enhancement (PRE) of the eastward electric field. Post-midnight TEC depletions and amplitude scintillations were observed for some days and this was attributed to the effect of zonal winds which brought post-midnight enhancement of the E x B drift. The percentage occurrence of amplitude scintillations for the selected quiet and storm days exhibited a seasonal dependence with equinoctial months having higher occurrences than the solstitial months. The higher average S4 index during equinoctial months might be attributed to increased solar intensity resulting from the close alignment of the solar terminator and the geomagnetic meridian.
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Bounhir, Aziza, Zouhair Benkhaldoun, Jonathan J. Makela, Mohamed Kaab, Brian Harding, Daniel J. Fisher, Amine Lagheryeb, et al. "Thermospheric Dynamics in Quiet and Disturbed Conditions." Proceedings of the International Astronomical Union 13, S335 (July 2017): 151–58. http://dx.doi.org/10.1017/s174392131700919x.

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AbstractThis paper presents the thermospheric winds and temperature properties measured with a Fabry-Pérot interferometer (FPI) over Oukaimeden observatory (31.2°N, 7.8°W, 22.8°N magnetic) in Morocco. After Three years of successful functioning from 2014 to 2017, we can address the seasonal behavior of the temperature and the winds (vertical, zonal and meridional). The dependence of the thermospheric winds and temperature on the solar cycle is also presented. The day-to-day variations of the quiet time wind pattern exhibits the importance of other type of waves superposed to the main diurnal tides. The storm time wind and temperature exhibits also a variety of ways to react to the storm. However, there is seasonal effect to the storm that will be illustrated in this paper. The signature of the MTM phenomenon is also present in the winds and temperature in geomagnetically quiet and disturbed nights. The occurrence of this phenomenon over the studied area is also addressed.
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Mendes, Odim, Margarete Oliveira Domingues, Ezequiel Echer, Rajkumar Hajra, and Varlei Everton Menconi. "Characterization of high-intensity, long-duration continuous auroral activity (HILDCAA) events using recurrence quantification analysis." Nonlinear Processes in Geophysics 24, no. 3 (August 1, 2017): 407–17. http://dx.doi.org/10.5194/npg-24-407-2017.

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Abstract. Considering the magnetic reconnection and the viscous interaction as the fundamental mechanisms for transfer particles and energy into the magnetosphere, we study the dynamical characteristics of auroral electrojet (AE) index during high-intensity, long-duration continuous auroral activity (HILDCAA) events, using a long-term geomagnetic database (1975–2012), and other distinct interplanetary conditions (geomagnetically quiet intervals, co-rotating interaction regions (CIRs)/high-speed streams (HSSs) not followed by HILDCAAs, and events of AE comprised in global intense geomagnetic disturbances). It is worth noting that we also study active but non-HILDCAA intervals. Examining the geomagnetic AE index, we apply a dynamics analysis composed of the phase space, the recurrence plot (RP), and the recurrence quantification analysis (RQA) methods. As a result, the quantification finds two distinct clusterings of the dynamical behaviours occurring in the interplanetary medium: one regarding a geomagnetically quiet condition regime and the other regarding an interplanetary activity regime. Furthermore, the HILDCAAs seem unique events regarding a visible, intense manifestations of interplanetary Alfvénic waves; however, they are similar to the other kinds of conditions regarding a dynamical signature (based on RQA), because it is involved in the same complex mechanism of generating geomagnetic disturbances. Also, by characterizing the proper conditions of transitions from quiescent conditions to weaker geomagnetic disturbances inside the magnetosphere and ionosphere system, the RQA method indicates clearly the two fundamental dynamics (geomagnetically quiet intervals and HILDCAA events) to be evaluated with magneto-hydrodynamics simulations to understand better the critical processes related to energy and particle transfer into the magnetosphere–ionosphere system. Finally, with this work, we have also reinforced the potential applicability of the RQA method for characterizing nonlinear geomagnetic processes related to the magnetic reconnection and the viscous interaction affecting the magnetosphere.
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Mendoza, B., and J. Ramírez. "A straightforward estimation of the maximum sunspot number for cycle 23." Annales Geophysicae 17, no. 5 (May 31, 1999): 639–41. http://dx.doi.org/10.1007/s00585-999-0639-7.

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Abstract. Using the annual number of geomagnetically quiet days (aa < 20 γ) for the year after the solar minimum, this precursor method predicts that the maximum sunspot number for cycle 23 will be 140 ± 32, indicating that cycle 23 will be similar to cycles 21 and 22.Key words. Solar physics · astrophysics and astronomy (magnetic fields; general)
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Book chapters on the topic "Geomagnetically quiet"

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Hasebe, N., A. Ryowa, M. Kobayashi, K. Kondoh, J. Hamada, Y. Mishima, K. Nagata, K. Kohno, J. Kikuchi, and T. Doke. "Global Distributions of Trapped He Fluxes from OHZORA Satellite During the Geomagnetically Quiet Period of 1984-1987." In Radiation Belts: Models and Standards, 255–58. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm097p0255.

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Conference papers on the topic "Geomagnetically quiet"

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Eltrass, A., W. A. Scales, A. Mahmoudian, S. de Larquier, J. M. Ruohoniemi, J. B. H. Baker, R. A. Greenwald, and P. J. Erickson. "Investigation of the generation source of decameter-scale sub-auroral ionospheric irregularities during geomagnetically quiet periods." In 2014 XXXIth URSI General Assembly and Scientific Symposium (URSI GASS). IEEE, 2014. http://dx.doi.org/10.1109/ursigass.2014.6929950.

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