• Title/Summary/Keyword: Atmospheric propagation

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Evaluating Laser Beam Parameters for Ground-to-space Propagation through Atmospheric Turbulence at the Geochang SLR Observatory

  • Ji Hyun Pak;Ji Yong Joo;Jun Ho Lee;Ji In Kim;Soo Hyung Cho;Ki Soo Park;Eui Seung Son
    • Current Optics and Photonics
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    • v.8 no.4
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    • pp.382-390
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    • 2024
  • Laser propagation through atmospheric disturbances is vital for applications such as laser optical communication, satellite laser ranging (SLR), laser guide stars (LGS) for adaptive optics (AO), and laser energy transmission systems. Beam degradation, including energy loss and pointing errors caused by atmospheric turbulence, requires thorough numerical analysis. This paper investigates the impact of laser beam parameters on ground-to-space laser propagation up to an altitude of 100 km using vertical atmospheric disturbance profiles from the Geochang SLR Observatory in South Korea. The analysis is confined to 100 km since sodium LGS forms at this altitude, and beyond this point, beam propagation can be considered free space due to the absence of optical disturbances. Focusing on a 100-watt class laser, this study examines parameters such as laser wavelengths, beam size (diameter), beam jitter, and beam quality (M2). Findings reveal that jitter, with an influence exceeding 70%, is the most critical parameter for long-exposure radius and pointing error. Conversely, M2, with an influence over 45%, is most significant for short-exposure radius and scintillation.

Analysis of Propagation Characteristics by Statistical Analysis in Domestic Atmospheric Environments (국내 대기 환경의 통계적 특성 분석을 통한 전파 특성 분석)

  • Choi, Moon-Young;Lee, Gil-Jae;Kim, Hyun-Soo;Pack, Jeong-Ki
    • The Journal of Korean Institute of Electromagnetic Engineering and Science
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    • v.19 no.6
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    • pp.698-705
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    • 2008
  • When electromagnetic waves propagate through atmosphere, waves are affected by various factors. Atmosphere normally consists of different molecular species, water vapours, rain, fog, snow and small suspended particles called aerosols. The distributions of atmosphere molecules, water vapours, rain rate, snowfall and aerosol are dependent on geometrical regions or environment. In order to predict propagation characteristics in atmospheric environment, statistical analysis of the relevant parameters such as temperature, humidity, atmospheric pressure, wind speed, areosol and rainfall is crucial. In this paper, we performed a long-term statistical analysis for the atmospheric parameters in domestic environments and analyzed the propagation characteristics through atmosphere based on that.

The Role of the Background Meridional Moisture Gradient on the Propagation of the MJO over the Maritime Continent

  • Daehyun Kang;Daehyun Kim;Min-Seop Ahn;Soon-Il An
    • Journal of Climate Change Research
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    • v.34 no.16
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    • pp.6565-6581
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    • 2021
  • This study investigates the role of the background meridional moisture gradient (MMG) on the propagation of the Madden-Julian oscillation (MJO) across the Maritime Continent (MC) region. It is found that the interannual variability of the seasonal mean MMG over the southern MC area is associated with the meridional expansion and contraction of the moist area in the vicinity of the MC. Sea surface temperature anomalies associated with relatively high and low seasonal mean MMG exhibit patterns that resemble those of El Niño-Southern Oscillation. By contrasting the years with anomalously low and high MMG, we show that MJO propagation through the MC is enhanced (suppressed) in years with higher (lower) seasonal mean MMG, although the effect is less robust when MMG anomalies are weak. Column-integrated moisture budget analysis further shows that sufficiently large MMG anomalies affect MJO activity by modulating the meridional advection of the mean moisture via MJO wind anomalies. Our results suggest that the background moisture distribution has a strong control over the propagation characteristics of the MJO in the MC region.

Optimized Station to Estimate Atmospheric Integrated Water Vapor Levels Using GNSS Signals and Meteorology Parameters

  • Beldjilali, Bilal;Benadda, Belkacem
    • ETRI Journal
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    • v.38 no.6
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    • pp.1172-1178
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    • 2016
  • The atmospheric meteorology parameters of the earth, such as temperature, pressure, and humidity, strongly influence the propagation of signals in Global Navigation Satellite Systems (GNSSs). The propagation delays associated with GNSS signals can be modeled and explained based on the atmospheric temperature, pressure, and humidity, as well as the locations of the satellites and receivers. In this paper, we propose an optimized and simplified low cost GNSS base weather station that can be used to provide a global estimate of the integrated water vapor value. Our algorithm can be used to measure the zenith tropospheric delay based on the measured propagation delays in the received signals. We also present the results of the data measurements performed at our station located in the Tlemcen region of Algeria.

A Study on the Meteorological Threshold of the Meteo-Tsunami Occurrence in the Yellow Sea, Korea (기상해일사례분석을 통한 기상해일발생 임계조건 도출)

  • Choi, Yo-Hwan;Kim, Hyunsu;Woo, Seung-Buhm;Kim, Myung-Seok;Kim, Yoo-Keun
    • Journal of Environmental Science International
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    • v.27 no.1
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    • pp.11-25
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    • 2018
  • Both the propagation velocity and the direction of atmospheric waves are important factors for analyzing and forecasting meteo-tsunami. In this study, a total of 14 events of meteo-tsunami over 11 years (2006-2016) are selected through analyzing sea-level data observed from tidal stations along the west coast of the Korean peninsula. The propagation velocity and direction are calculated by tracing the atmospheric disturbance of each meteo-tsunami event predicted by the WRF model. Then, the Froude number is calculated using the propagation velocity of atmospheric waves and oceanic long waves from bathymetry data. To derive the critical condition for the occurrence of meteo-tsunami, supervised learning using a logistic regression algorithm is conducted. It is concluded that the threshold distance of meteo-tsunami occurrence, from a propagation direction, can be calculated by the amplitude of air-pressure tendency and the resonance factor, which are found using the Froude number. According to the critical condition, the distance increases logarithmically with the ratio of the amplitude of air-pressure tendency and the square of the resonance factor, and meteo-tsunami do not occur when the ratio is less than 5.11 hPa/10 min.

Deep Water Wave Model for the East Sea (東海에서의 파랑추산을 위한 심해파랑모형에 대한 연구)

  • Yoon, Jong-Tae
    • Journal of Ocean Engineering and Technology
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    • v.13 no.2 s.32
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    • pp.116-128
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    • 1999
  • A deep water wave prediction model applicable to the East Sea is presnted. This model incorporates rediative transter of energy specrum, atmospheric input form the wind, nonlinear interaction, and energy dissipation by white capping. The propagation scheme by Gadd shows satisfactory results and the characteristics of the nonlinear interaction is simulated well by discrete interaction approximatiion. The application of the model to the sea around the Korean Peninsula shows reasonable agreement with the observation.

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Number of Phase Screens Required for Simulation of a High-energy Laser Beam's Propagation Experiencing Atmospheric Turbulence and Thermal Blooming (대기 난류와 열적 블루밍을 겪는 고출력 레이저 빔의 대기 전파 시뮬레이션에 필요한 위상판 개수 분석)

  • Seokyoung Yoon;Woohyeon Moon;Hoon Kim
    • Korean Journal of Optics and Photonics
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    • v.35 no.2
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    • pp.49-60
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    • 2024
  • We analyze the number of phase screens required for the simulation of a high-energy laser beam's propagation over an atmospheric channel. For high-energy lasers exceeding tens of kilowatts (kW) in power, the laser beam is mainly affected by atmospheric turbulence and thermal blooming. When using the split-step method to implement losses due to atmospheric absorption and scattering and distortion of the beam due to turbulence and thermal blooming, the number of phase screens is a critical factor in determining the accuracy and time required for the simulation. By comparing simulation results obtained using a large number of phase screens (e.g., 150 screens) under a wide range of atmospheric turbulence conditions, we provide new guidelines for the number of phase screens required for simulating the beam propagation of a high-power laser below 2.5×106 W/m2 (e.g., a 500-kW laser beam having a 50-cm diameter).

Influence of HAPS and GEO Satellite under SANDU Layering and Gas Attenuations

  • Harb, Kamal
    • International Journal of Computer Science & Network Security
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    • v.21 no.12
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    • pp.93-100
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    • 2021
  • Satellite communication for high altitude platform stations (HAPS) and geostationary orbit (GEO) systems suffers from sand and dust (SANDU) storms in desert and arid regions. The focus of this paper is to propose common relations between HAPS and GEO for the atmospheric impairments affecting the satellite communication networks operating above Ku-band crossing the propagation path. A double phase three-dimensional relationship for HAPS and GEO systems is then presented. The comparison model present the analysis of atmospheric attenuation with specific focus on sand and dust based on particular size, visibility, adding gas effects for different frequency, and propagation angle to provide systems' operations with a predicted vision of satellite parameters' values. Thus, the proposed system provides wide range of selecting applicable parameters, under different weather conditions, in order to achieve better SNR for satellite communication.

ESTIMATION OF THE SGP4 DRAG TERM FROM TWO OSCULATING ORBIT STATES

  • Lee, Byoung-Sun;Park, Jae-Woo
    • Journal of Astronomy and Space Sciences
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    • v.20 no.1
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    • pp.11-20
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    • 2003
  • A method for estimating the NORAD SGP4 atmospheric drag term from minimum osculating orbit states, i.e., two osculating orbits, is developed. The first osculating orbit state is converted into the NORAD TLE-type mean orbit state by iterative procedure. Then the converted TLE is propagated to the second orbit state using the SGP4 model with the incremental SGP4 drag term. The iterative orbit propagation procedure is finished when the difference of the two osculating semi-major axes between the propagated orbit and the given second orbit is minimized. In order to minimize the effect of the short-term variations of the osculating semi-major axis, the osculating argument of latitude of the second orbit is propagated to the same argument of latitude of the first orbit. The method is applied to the estimation of the NORAD-type TLE for the KOMPSAT-1 spacecraft. The SGP4 drag terms are estimated from both NORAD SGP4 orbit propagation and the numerical orbit propagation results. Variations of the estimated drag terms are analyzed for the KOMPSAT-1 satellite orbit determination results.