• Title/Summary/Keyword: CloudSat

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Study on the Development of Snowfall Retrieval Algorithm using CloudSat and Passive Microwave (CloudSat와 수동 마이크로파 자료를 결합한 강설 추정 알고리즘 개발에 관한 연구)

  • Park, Kyung-Won;Kim, Jong-Pil;Kim, Na-Ri;Kim, Young-Seup
    • Proceedings of the Korea Water Resources Association Conference
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    • 2012.05a
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    • pp.265-265
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    • 2012
  • 한반도 지역의 강설(snowfall)은 전체 연 강수량의 약 10% 이하로 매우 적은 양을 차지하고 있다. 하지만 강설은 대기질(air quality)을 개선하고 산불 발생률을 저감시키며, 특히 봄철 수자원의 제공과 가뭄피해 경감 등 수문학적으로도 중요한 기능을 가진다. 하지만 최근 기후변화로 인해 폭설 현상이 빈번하게 발생하여 사회 경제적 손실을 유발하고 있다. 따라서 강설로 인한 피해를 최소한으로 줄이기 위해서는 정확한 강설탐지 및 강설 추정 방법이 필요하다. 최근 해외의 수많은 연구들을 통하여 수동 마이크로파 센서 자료를 활용한 강설 추정의 가능성이 확인되고 있다. 하지만 수동 마이크로파 센서의 휘도온도를 이용한 추정 방법들은 대기의 연직 구조 파악에 어려움이 있기 때문에 정확한 강설량을 추정하는 데에 한계가 있다. 그러나 2006년 발사된 CloudSat의 Cloud Profiling Radar는 강설의 연직 프로파일에 대한 가치 있는 정보를 제공하기 때문에 수동 마이크로파 센서 자료와의 결합을 통해 보다 정확한 강설 추정 알고리즘을 제시할 수 있을 것으로 판단된다. 따라서 본 연구에서는 CloudSat의 Cloud Profiling Radar (CPR) 자료와 수동 마이크로파 센서인 NOAA의 Microwave Humidity Sounder (MHS) 센서 자료를 결합하여 한반도 강설 추정에 적합한 알고리즘을 개발하고자 한다.

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Development of Snowfall Retrieval Algorithm by Combining Measurements from CloudSat, AQUA and NOAA Satellites for the Korean Peninsula

  • Kim, Young-Seup;Kim, Na-Ri;Park, Kyung-Won
    • Korean Journal of Remote Sensing
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    • v.27 no.3
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    • pp.277-288
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    • 2011
  • Cloudsat satellite data is sensitive to snowfall and collected during each month beginning with Dec 2007 and ending Feb 2008. In this study, we attempt to develop a snowfall retrieval algorithm using a combination of radiometer and cloud radar data. We trained data from the relation between brightness temperature measurements from NOAA's Advanced Microwave Sounder Unit-B(AMSU-B) and the radar reflectivity of the 2B-GEOPROF product from W-band(94 GHz) cloud radar onboard Cloudsat and applied it to the Korea peninsula. We use a principal components analysis to quantify the variations that are the result of the radiometric signatures of snowfall from those of the surface. Finally, we quantify the correlation between the higher principal component (orthogonal to surface variability) of the microwave radiances and the precipitation-sensitive CloudSat radar reflectivities. This work summarizes the results of applying this approach to observations over the East Sea during Feb. 2008. The retrieved data show reasonable estimation for snowfall rate compared with Cloudsat vertical image.

Development of a Retrieval Algorithm for Adjustment of Satellite-viewed Cloudiness (위성관측운량 보정을 위한 알고리즘의 개발)

  • Son, Jiyoung;Lee, Yoon-Kyoung;Choi, Yong-Sang;Ok, Jung;Kim, Hye-Sil
    • Korean Journal of Remote Sensing
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    • v.35 no.3
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    • pp.415-431
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    • 2019
  • The satellite-viewed cloudiness, a ratio of cloudy pixels to total pixels ($C_{sat,\;prev}$), inevitably differs from the "ground-viewed" cloudiness ($C_{grd}$) due to different viewpoints. Here we develop an algorithm to retrieve the satellite-viewed, but adjusted cloudiness to $C_{grd} (C_{sat,\;adj})$. The key process of the algorithm is to convert the cloudiness projected on the plane surface into the cloudiness on the celestial hemisphere from the observer. For this conversion, the supplementary satellite retrievals such as cloud detection and cloud top pressure are used as they provide locations of cloudy pixels and cloud base height information, respectively. The algorithm is tested for Himawari-8 level 1B data. The $C_{sat,\;adj}$ and $C_{sat,\;prev}$ are retrieved and validated with $C_{grd}$ of SYNOP station over Korea (22 stations) and China (724 stations) during only daytime for the first seven days of every month from July 2016 to June 2017. As results, the mean error of $C_{sat,\;adj}$ (0.61) is less that than that of $C_{sat,\;prev}$ (1.01). The percent of detection for 'Cloudy' scenario of $C_{sat,\;adj}$ (73%) is higher than that of $C_{sat,\;prev}$ (60%) The percent of correction, the accuracy, of $C_{sat,\;adj}$ is 61%, while that of $C_{sat,\;prev}$ is 55% for all seasons. For the December-January-February period when cloudy pixels are readily overestimated, the proportion of correction of $C_{sat,\;adj$ is 60%, while that of $C_{sat,\;prev}$ is 56%. Therefore, we conclude that the present algorithm can effectively get the satellite cloudiness near to the ground-viewed cloudiness.

Critical Design of MIMAN CubeSat for Aerosol Monitoring Mission (미세먼지 관측 임무를 위한 MIMAN 큐브위성 상세 설계)

  • Jin, Sungmin;Kang, Dae-Eun;Kim, Geuk-Nam;Kim, Naeun;Kim, Young-Eon;Kim, Pureum;An, Seungmin;Ryu, Han-Gyeol;Park, Sang-Young
    • Journal of the Korean Society for Aeronautical & Space Sciences
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    • v.49 no.12
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    • pp.1027-1035
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    • 2021
  • We presents a design of 3U cubesat MIMAN (Monochrome imaging for monitoring aerosol by nano-satellite) for aerosol monitoring mission with high spatial resolution. The main objective of MIMAN mission is to take images of aerosols around Korea and to provide auxiliary data for GK 2B cloud masking. For this mission, we derived mission requirements and constraints for the MIMAN mission. We designed the mission architecture and concept of operations. To reduce risk factors in space operation, we considered the safety of the communication. In every operation modes, UHF communication is available so that the cubesat can operate based on the ground commands. So, we can handle every problem at the ground station during mission operations. Based on the mission and concept of operations, we confirmed that the system design satisfied the system requirements. We designed the system interface considering data flow of each hardware, and evaluated the safety of the system with system budget analysis.

An Analysis of Aerosol Optical Properties around Korea using AERONET (지상원격관측(AERONET)을 통한 한반도 주변 에어로솔 광학특성 분석)

  • Kim, Byung-Gon;Kim, You-Joon;Eun, Seung-Hee
    • Journal of Korean Society for Atmospheric Environment
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    • v.24 no.6
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    • pp.629-640
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    • 2008
  • This study investigates long-term trends and characteristics of aerosol optical depth ($\tau_a$) and Angstrom exponent (${\AA}$) around Korea in order to understand aerosol effects on the regional climate change. The analysis period is mainly from 1999 to 2006, and the analysis sites are Anmyun and Gosan, the background monitoring sites in Korea, and two other sites of Xianghe in China and Shirahama in Japan. The annual variations of $\tau_a$ at Anmyun and Gosan have slightly systematic increasing and decreasing trends, respectively. $\tau_a$ at Anmyun shows more substantial variation, probably because of it's being closer and vulnerable to anthropogenic influence from China and/or domestic sources than Gosan. Both values at Gosan and Anmyun are approximately 1.5 times greater than those at Shirahama. The monthly variation of $\tau_a$ exhibits the highest values at late Spring and the lowest at late-Summer, which are thought to be associated with the accumulation of fine aerosol formed through the photochemical reaction before the Jangma period and the scavenging effect after the Jangma period, respectively. Meanwhile, the episode-average $\tau_a$ for the Yellow dust period increases 2 times greater than that for the non-Yellow dust period. A significant decrease in ${\AA}$ for the Yellow dust period is attributable to an increase in the loading of especially the coarse particles. Also we found no weekly periodicity of $\tau_a$'s, but distinct weekly cycle of $PM_{10}$ concentrations, such as an increase on weekdays and a decrease on weekends at Anmyun and Gosan. We expect these findings would help to initiate a study on aerosol-cloud interactions through the combination of surface aerosol and satellite remote sensing (MODIS, Calipso and CloudSat) in East Asia.

Evaluating Distribution Trends of Classification Accuracy by Triangular Training Operator in SAR/VIR FCC : A Case Study of Songkhla Lake Basin in Thailand (SAR/VIR FCC에서 삼각 트레이닝 도구에 의한 분류정확도 분포추세 평가: 태국의 송클라 호수 유역을 사례로)

  • Jung Sup Um
    • Journal of the Korean Geographical Society
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    • v.38 no.3
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    • pp.375-388
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    • 2003
  • This study mainly focuses on evaluating how the triangular training operator could improve classification accuracy in SAR(Synthetic Aperture Radar) and VIR FCC(Visible Infra-red, False Colour Composite). The techniques for the determination of the most informative SAR/VIR combinations in the triangular space diagram, as developed tv the author of the paper, are given and the results obtained are presented. The SAR alone, VIR alone and SAR/VIR FCC classification showed trends for gradual improvement of accuracy. Accuracy distribution pattern for individual classes could be explained closely related to SAR/VIR signature components in the process of the triangular synergistic training. Due to contribution of SAR signature in training samples, it was possible to isolate major terrain features such as cloud cover area and roughness target with acceptable spatial precision. It is anticipated that this research output could be used as a valuable reference for distribution trends of classification accuracy obtained by triangular channel space based training in synergistic application.

Detection of Arctic Summer Melt Ponds Using ICESat-2 Altimetry Data (ICESat-2 고도계 자료를 활용한 여름철 북극 융빙호 탐지)

  • Han, Daehyeon;Kim, Young Jun;Jung, Sihun;Sim, Seongmun;Kim, Woohyeok;Jang, Eunna;Im, Jungho;Kim, Hyun-Cheol
    • Korean Journal of Remote Sensing
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    • v.37 no.5_1
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    • pp.1177-1186
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    • 2021
  • As the Arctic melt ponds play an important role in determining the interannual variation of the sea ice extent and changes in the Arctic environment, it is crucial to monitor the Arctic melt ponds with high accuracy. Ice, Cloud, and Land Elevation Satellite-2 (ICESat-2), which is the NASA's latest altimeter satellite based on the green laser (532 nm), observes the global surface elevation. When compared to the CryoSat-2 altimetry satellite whose along-track resolution is 250 m, ICESat-2 is highly expected to provide much more detailed information about Arctic melt ponds thanks to its high along-track resolution of 70 cm. The basic products of ICESat-2 are the surface height and the number of reflected photons. To aggregate the neighboring information of a specific ICESat-2 photon, the segments of photons with 10 m length were used. The standard deviation of the height and the total number of photons were calculated for each segment. As the melt ponds have the smoother surface than the sea ice, the lower variation of the height over melt ponds can make the melt ponds distinguished from the sea ice. When the melt ponds were extracted, the number of photons per segment was used to classify the melt ponds covered with open-water and specular ice. As photons are much more absorbed in the water-covered melt pondsthan the melt ponds with the specular ice, the number of photons persegment can distinguish the water- and ice-covered ponds. As a result, the suggested melt pond detection method was able to classify the sea ice, water-covered melt ponds, and ice-covered melt ponds. A qualitative analysis was conducted using the Sentinel-2 optical imagery. The suggested method successfully classified the water- and ice-covered ponds which were difficult to distinguish with Sentinel-2 optical images. Lastly, the pros and cons of the melt pond detection using satellite altimetry and optical images were discussed.