• Journal of information and communication convergence engineering
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• 제3권3호
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• pp.146-151
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• 2005

This paper represents an attempt to bring together and analyses the measurement data measured by the Satellite Signal Monitoring Center in Korea and the Korea Meteorological Administration/Korea Meteorological Research Institute in close cooperation with this study team. This paper presents the signal characteristic of GEO satellite operating in frequency range 1 to 20GHz associated with Asian Sand Dust (the so-called Yellow Sand Dust). The downlink signal power (dBm) for L-, S-, C-, Ku-, and Ka-band frequencies from GEO satellites were measured in a clear weather and in Asian Sand Dust weather by the Satellite Signal Monitoring Center. The measured signal power(dBm) were compared to the total number concentration and size distribution of Sand Dust that were measured by the Korea Meteorological Administration/Korea Meteorological Research Institute and the possible correlation between these sets data were analyzed. The results demonstrate that the downlink signal level (dBm) of GEO satellite is attenuated by Asian Sand Dust. Hitherto, merger information has been reported as to the influence of sand dust on satellite communications operating in regions affected by sand dust.

• 대한원격탐사학회지
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• 제16권2호
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• pp.117-133
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• 2000

We studied the sea level variations at Kerguelen island in the South Indian Ocean with ARGOS data and meteorological data during about 1 year(May 1993~April 1994) through using filter, spectral analysis, coherency and phase, and found characteristics for the two oceanic signal levels(detided oceanic signal level, h$_{detided}$ and seasonal oceanic level, h$_{corr.ib}$). The forms of atmospheric pressure variations are good agreed to between ARGOS data and meteorological data in the observed periods. This Kerguelen area shows the inflow of an air temperature(gain of a radiant heat) into the sea water and the stagnation of high atmospheric pressure bands in summer, and the outflow of a sea water temperature(loss of sensible and latent heat) toward the atmosphere and the stagnation of low atmospheric pressure bands in winter. The seasonal difference of sea level between summer and winter is about 1.6cm. Both the detided oceanic signal level(h$_{detided}$) variation and the inverted barometer level(h$_{ib}$) variation have a strong correlation for T>1day period bands. The characteristics of h$_{detided}$ variation are not decided by the influence of any meteorological distributions (atmospheric pressure), but the influence of other factors(bottom water temperature) for T>2days periods bands. h$_{corr.ib}$ plays a very important role of sea level variation in the observed periods (especially T>about 180days period bands).

• Journal of Astronomy and Space Sciences
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• 제25권3호
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• pp.267-282
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• 2008

대류층의 중성 대기는 전자가파의 신호 지연을 일으키기 때문에, GNSS(Global Navigation Satel-lite System)를 이용한 정밀측위의 가장 큰 오차요인으로 작용한다. 대류층 지연오차는 대류층의 굴절률과 연관 있으며, 대류층의 굴절률은 경험적으로 압력, 온도 및 수증기 분압으로 표현된다. 따라서 GNSS 안테나 위치의 기상 정보를 알고 있다면, 대류층 지연오차는 경험적 법칙에 의해 산출될 수 있다. 이 연구에서는 임의의 장소와 시간에 대한 대류층 지연오차를 생성하기 위한 기상정보 생성에 대하여 연구하였다. 한국천문연구원이 운영하는 9개의 상시 관측소에 설치된 디지털 기상 센서의 관측값을 가지고 범용 크리깅 (Ordinary Kriging)을 적용하여 기상 정보를 생성하였고, 상시 관측소의 데이터 공백을 메우기 위해 각 상시관측소의 기상 데이터를 분석하여 수치 모델을 만들어 보완하였다.

• 대기
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• 제17권1호
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• pp.27-44
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• 2007

The purpose of this study is to investigate predictability of the seasonal simulation by the METRI (Meteorological Research Institute) AGCM (Atmospheric General Circulation Model), which is a long-term prediction model for the METRI 3-month prediction system. We examine the performance skill of climate simulation and predictability by the analysis of variance of the METRI AGCM, focusing on the precipitation, 850 hPa temperature, and 500 hPa geopotential height. According to the result, the METRI AGCM shows systematic errors with seasonal march, and represents large errors over the equatorial region, compared to the observation. Also, the response of the METRI AGCM by the variation of the sea surface temperature is obvious for the wintertime and springtime. However, the METRI AGCM does not show the significant ENSO-related signal in autumn. In case of prediction over the east Asian region, errors between the prediction results and the observation are not quite large with the lead-time. However, in the predictability assessment using the analysis of variance method, longer lead-time makes the prediction better, and the predictability becomes better in the springtime.

• 대기
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• 제16권3호
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• pp.215-223
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• 2006

Among observational, local-environmental, and large-scale factors causing significant changes in climate records, the site relocations and the replacement of the instruments are well-known nonclimatic factors for the analysis of climatic trends, climatic variability, and for the detection of anthropogenic climate change such as heat-island effect and global warming. Using dataset that were contaminated by these nonclimatic factors can affect seriously the assessment of climatic trends and variability, and the detection of the climatic change signal. In this paper, the inhomogeneities, which have been caused by relocation of the observation site, in the climate data of Korea Meteorological Administration (KMA) were examined using two-phase regression model. The observations of pan evaporation and wind speed are more sensitive to site relocations than those of other meteorological elements, such as daily mean, maximum and minimum temperatures, with regardless to region.

• Current Optics and Photonics
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• 제2권1호
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• pp.7-14
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• 2018

As a sophisticated detection technology, LIDAR has been widely employed to probe low-altitude windshear. Due to the drawbacks of the traditional ramp algorithm, the alarm accuracy of the LIDAR has not been satisfactory. Aiming at settling this matter, a novel method is proposed on the basis of improved signal smoothing and second windshear detection, which essentially acts as a combination of ramp algorithm and segmentation approach, involving the human factor as well as signal fluctuations. Experiments on the real and artificial signals verify our approach.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2000년도 춘계 학술대회 논문집 통권 3호 Proceedings of the 2000 KSRS Spring Meeting
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• pp.13-18
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• 2000

We observed sea level variation of the long time at Kerguelen island in the South Indian Ocean with ARGOS data and meteorological data during about 1 year(May 1993~March 1994) through using filter, spectral analysis, coherency and phase, and found characteristics for the two oceanic signal levels(detided oceanic signal level, h$_{detided}$ and seasonal oceanic level, h$_{corr.ib}$). The forms of variations are very well agreed to between ARGOS data and meteorological data for atmospheric pressure in the observed periods. The seasonal difference of sea level between Summer and Winter is about 1.6cm. Both the detided oceanic signal level(h$_{detided}$) variation and the inverted barometer level(h$_{ib}$) variation have a strong correlation for T>1day period bands. Characteristics of h$_{detided}$ variation are decided not by the influence of any meteorological distributions (pressure, winds, etc), but the influence of another factors(temperature, salinity, etc.) for T>2days periods bands. h$_{corr.ib}$ plays an very important role of sea level variation of the long time term(especially T>about 180days period bands).

• 대기
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• 제34권1호
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• pp.55-67
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• 2024

This paper aims to provide a detailed introduction to the concept of the Ratio of Predictable Component (RPC) and the Signal-to-Noise Paradox. Then, we derive insights from them by exploring the paradoxical features by conducting a seasonal and regional analysis through ensemble expansion in KMA's climate prediction system (GloSea). We also provide an explanation of the ensemble generation method, with a specific focus on stochastic physics. Through this study, we can provide the predictability limits of our forecasting system, and find way to enhance it. On a global scale, RPC reaches a value of 1 when the ensemble is expanded to a maximum of 56 members, underlining the significance of ensemble expansion in the climate prediction system. The feature indicating RPC paradoxically exceeding 1 becomes particularly evident in the winter North Atlantic and the summer North Pacific. In the Siberian Continent, predictability is notably low, persisting even as the ensemble size increases. This region, characterized by a low RPC, is considered challenging for making reliable predictions, highlighting the need for further improvement in the model and initialization processes related to land processes. In contrast, the tropical ocean demonstrates robust predictability while maintaining an RPC of 1. Through this study, we have brought to attention the limitations of potential predictability within the climate prediction system, emphasizing the necessity of leveraging predictable signals with high RPC values. We also underscore the importance of continuous efforts aimed at improving models and initializations to overcome these limitations.

• 한국위성정보통신학회논문지
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• 제5권2호
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• pp.19-24
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• 2010

통신해양기상위성(COMS)은 통신, 해양, 기상 탑재체를 장착하고 3개의 임무를 수행하는 복합 정지궤도 위성이다. COMS는 기상탑재체 MI와 해양 탑재체 GOCI가 관측 후 전송하는 원시 데이터를 지상국에 전송하고 지상국에서 처리된 기상 데이터를 최종 사용자국에 중계하는 기능을 갖는 기상해양자료송수신계(MODCS)가 있다. 여기서 시스템 관점에서 관측 데이터 SD 신호와 중계 신호를 전송하는 L-대역 송신 안테나는 MI 탑재체와 기상탑재체와 함께 COMS 위성의 지구패널에 장착시 안테나 합성 이득을 예측하도록 요구되어진다. 우선 주어진 요구 사항에 대해 L-대역 송신 안테나 설계 및 해석이 수행된다. 설계된 안테나를 지구패널에 장착 후 3가지 다른 해석 방법을 사용하여 합성이득 해석이 수행된다. 얻어진 안테나 이득들은 3가지 다른 해석 방법 사이에 매우 유사한 결과를 제공하는 것을 확인하였으며 최종적으로 0.5 dB 이하의 안테나 이득 열화가 추정되어진다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 춘계학술대회 논문집
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• pp.377-380
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• 2006

본 논문에서는 통신해양기상위성의 지상국에 구축된 고 출력증폭기에 대한 특성 모델링 및 이에 따른 입력신호에 따른 출력 신호의 상호 간섭에 대한 결과가 정리되어 있다. 고 출력증폭기는 지상국에서 위성으로 신호를 전송할 때 필요한 장비로써 비선형 특성으로 인해 입력된 신호에 대한 다양한 하모닉 성분이 발생된다. 특히 통신해양 기상위성의 지상국의 경우에는 하나의 고 출력증폭기에 대해 두개의 서로 다른 주파수의 신호를 입력해야 하는 것을 고려해야 하기 때문에 이에 대한 영향은 사전에 반드시 분석되어야 한다. 본 논문에서는 고출력증폭기의 P1dB 특성곡선에 의해 특성 모델링을 수행한 결과 및 이러한 모델을 검증하기 위해 이미 정의된 두 신호에 대한 간섭의 양을 확인하였다. 특히 고 출력 증폭기의 전단에 속하는 상향 주파수 변환기의 특성을 고려한 신호를 사용하여 실제의 통신해양기상위성으로 데이터를 전송할 때의 결과를 얻는데 중점을 두었다. 그 결과 상호간의 간섭에 의해 발생되는 신호는 실제 보내고자 하는 신호의 대역과 매우 가깝게 있으며 그 크기는 보내고자 하는 신호의 특성에 따라 달라지는 것을 확인 할 수 있었다.