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      혼합 최저고도각 반사도 자료를 이용한 레이더 강우추정 정확도 향상 = Improvement of Radar Rainfall Estimation Using Radar Reflectivity Data from the Hybrid Lowest Elevation Angles

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      https://www.riss.kr/link?id=A104624597

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      국문 초록 (Abstract)

      레이더 반사도를 이용한 강수추정의 개선을 위해 새로운 접근 방식인 경북대학교에서 개발한 하이브리드 고도면을 이용한 강수량 추정기법(Hybrid Surface Rainfall, KNU-HSR)을 사용하였다. KNU-HSR기...

      레이더 반사도를 이용한 강수추정의 개선을 위해 새로운 접근 방식인 경북대학교에서 개발한 하이브리드 고도면을 이용한 강수량 추정기법(Hybrid Surface Rainfall, KNU-HSR)을 사용하였다. KNU-HSR기법은 지형에코와 레이더 빔차폐의 영향을 받지 않는 2차원 하이브리드 고도면에서의 반사도를 이용하여 강수량을 추정한다. 본 연구에서는 정적 HSR 및 동적 HSR기법이 사용되었으며 비교·검증되었다. 정적 HSR은 빔차폐지도와 지형에코지도를 사용하며, 동적 HSR은 정적 HSR에 추가적으로 실시간 퍼지로직 품질관리를 통한 품질지수지도를 사용한다. 검증을 위해 상관계수(correlation coefficient), 총비율(total ratio), 평균편의(mean bias), 정규화된 표준편차(normalized standard deviation), 평균상대오차(mean relative error)를 사용하였으며, 10개 강우사례의 지상우량계 강우자료를 이용하여 두 HSR의 강우추정 성능을 평가하였다. 모든 검증지수에서 동적 HSR은 반사도 보정을 하지 않은 정적 HSR에 비해 더 우수한 성능을 보였다. 동적 HSR은 레이더로부터 근거리에서는 과대추정하였으며 원거리에서는 빔 폭 확장 및 빔 고도증가로 인해 과소추정하였다. 동적 HSR의 정규화된 표준편차와 평균상대오차는 레이더로부터의 거리에 관계없이 가장 좋은 결과를 보였다. 정적 HSR은 약한 강우강도에서 상당히 과대추정하였으나 동적 HSR은 모든 강우강도에서 1.0에 총비율을 보였다. 반사도의 시스템오차 보정 후, 동적 HSR의 정규화된 표준편차와 평균상대오차는 각각 약 20%와 15%로 개선되었다.

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      다국어 초록 (Multilingual Abstract)

      A novel approach, hybrid surface rainfall (KNU-HSR) technique developed by Kyungpook Natinal University, was utilized for improving the radar rainfall estimation. The KNU-HSR technique estimates radar rainfall at a 2D hybrid surface consistings of the...

      A novel approach, hybrid surface rainfall (KNU-HSR) technique developed by Kyungpook Natinal University, was utilized for improving the radar rainfall estimation. The KNU-HSR technique estimates radar rainfall at a 2D hybrid surface consistings of the lowest radar bins that is immune to ground clutter contaminations and significant beam blockage. Two HSR techniques, static and dynamic HSRs, were compared and evaluated in this study. Static HSR technique utilizes beam blockage map and ground clutter map to yield the hybrid surface whereas dynamic HSR technique additionally applies quality index map that are derived from the fuzzy logic algorithm for a quality control in real time. The performances of two HSRs were evaluated by correlation coefficient (CORR), total ratio (RATIO), mean bias (BIAS), normalized standard deviation (NSD), and mean relative error (MRE) for ten rain cases. Dynamic HSR (CORR=0.88, BIAS=-0.24mmhr-1, NSD=0.41, MRE=37.6%) shows better performances than static HSR without correction of reflectivity calibration bias (CORR=0.87, BIAS=-2.94mmhr-1, NSD=0.76, MRE=58.4%) for all skill scores. Dynamic HSR technique overestimates surface rainfall at near range whereas it underestimates rainfall at far ranges due to the effects of beam broadening and increasing the radar beam height. In terms of NSD and MRE, dynamic HSR shows the best results regardless of the distance from radar. Static HSR significantly overestimates a surface rainfall at weaker rainfall intensity. However, RATIO of dynamic HSR remains almost 1.0 for all ranges of rainfall intensity. After correcting system bias of reflectivity, NSD and MRE of dynamic HSR are improved by about 20% and 15%, respectively.

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      참고문헌 (Reference)

      1 Hubbert, C. J., "Weather radar ground clutter. Part I : Identification, modeling, and simulation" 26 : 1165-1180, 2009

      2 Maddox, R. A., "Weather radar coverage over the contiguous United States" 17 : 927-934, 2002

      3 O'Bannon, T., "Using a terrain-based hybrid scan to improve WSR-88D precipitation estimates" American Meteorological Society 506-507, 1997

      4 Steiner, M., "Use of threedimensional reflectivity structure for automated detection and removal of nonprecipitating echoes in radar data" 19 : 673-686, 2002

      5 Creutin, J. D., "Use of a weather radar for the hydrology of a mountainous area. Part II : Radar measurement validation" 193 : 26-44, 1997

      6 Andrieu, H., "Use of a weather radar for the hydrology of a mountainous area. Part I : Radar measurement interpretation" 193 : 1-25, 1997

      7 Kruger, A., "Two-dimensional video disdrometer : A description" 19 : 602-617, 2002

      8 Bech, J., "The sensitivity of single polarization weather radar beam blockage correction to variability in the vertical refractivity gradient" 20 : 845-855, 2003

      9 Fulton, R. A., "The WSR-88D rainfall algorithm" 13 : 377-395, 1998

      10 Ministry of Land, Infrastructure and Transport, "Study on the optimization of scan strategy of Mt. Bisl rain radar"

      1 Hubbert, C. J., "Weather radar ground clutter. Part I : Identification, modeling, and simulation" 26 : 1165-1180, 2009

      2 Maddox, R. A., "Weather radar coverage over the contiguous United States" 17 : 927-934, 2002

      3 O'Bannon, T., "Using a terrain-based hybrid scan to improve WSR-88D precipitation estimates" American Meteorological Society 506-507, 1997

      4 Steiner, M., "Use of threedimensional reflectivity structure for automated detection and removal of nonprecipitating echoes in radar data" 19 : 673-686, 2002

      5 Creutin, J. D., "Use of a weather radar for the hydrology of a mountainous area. Part II : Radar measurement validation" 193 : 26-44, 1997

      6 Andrieu, H., "Use of a weather radar for the hydrology of a mountainous area. Part I : Radar measurement interpretation" 193 : 1-25, 1997

      7 Kruger, A., "Two-dimensional video disdrometer : A description" 19 : 602-617, 2002

      8 Bech, J., "The sensitivity of single polarization weather radar beam blockage correction to variability in the vertical refractivity gradient" 20 : 845-855, 2003

      9 Fulton, R. A., "The WSR-88D rainfall algorithm" 13 : 377-395, 1998

      10 Ministry of Land, Infrastructure and Transport, "Study on the optimization of scan strategy of Mt. Bisl rain radar"

      11 Delrieu, G., "Simulation of radar mountain returns using a digitized terrain model" 12 : 1038-1049, 1995

      12 Jung, S. H., "Simulation of radar beam propagation using digital elevation model" 346-347, 2007

      13 Shedd, R. C., "Sectorized hybrid scan strategy of the NEXRAD precipitation processing system" University of Salford 9-, 1989

      14 Vivekanandan, J., "Rigorous approach to polarimetric radar modeling of hydrometeor orientation distributions" 30 : 1053-1063, 1991

      15 Kwon, S., "Rainfall estimation from an operational Sband dual-polarization radar : Effect of radar calibration and uncertainty in dual-polarimetric parameters" Kyungpook National University 2012

      16 Kwon, S., "Rainfall estimation from an operational S-band dual-polarization radar: Effect of radar calibration" 93 : 2015

      17 Lee, G. W., "Radar calibration by gage, disdrometer, and polarimetry : Theoretical limit caused by the variability of drop size distribution and application to fast scanning operational radar data" 328 : 83-97, 2006

      18 Kucera, P. A., "Radar beam occultation studies using GIS and DEM technology : An example study of Guam" 21 : 995-1006, 2004

      19 Kabeche, F., "Quantitative precipitation estimation(QPE)in the French Alps with a dense network of polarimetric Xband radars" American Meteorological Society

      20 Ye, B. -Y., "Quality control of radar moment data by combining moment-based fuzzy logic algorithm and radar signal processing" Kyungpook National University 2013

      21 Zhang, P., "Partial beam blockage correction using polarimetric radar measurements" 30 : 861-872, 2013

      22 Lang, T. J., "On the correction of partial beam blockage in polarimetric radar data" 26 : 943-957, 2009

      23 Zhang, J., "National mosaic and multi-sensor QPE(NMQ). system : Description, results, and future plans" 92 : 1321-1338, 2011

      24 Cho, Y. H., "Identification and removal of ground echoes and anomalous propagation using the characteristics of radar echoes" 23 : 1206-1222, 2006

      25 Shedd, R. C., "Hydrological Applications of Weather Radar" Ellis Horwood 151-159, 1991

      26 Kwon, S., "Evaluation Radar and KNU QPE Algorithm" 2012

      27 Thurai, M., "Drop shapes, model comparisons, and calculations of polarimetric radar parameters in rain" 24 : 1019-1032, 2007

      28 Atlas, D., "Doppler radar characteristics of precipitation at vertical incidence" 11 : 1-35, 1973

      29 Doviak, R. J., "Doppler radar and weather observations" Academic Press 562-, 1993

      30 Korea Air Force, "Development of tracking technique of convective cell around an air base using three dimensional radar mosaic" 73rd weather group 82-, 2012

      31 Grecu, M., "Detection of anomalous propagation echoes in weather radar data using neural networks" 37 : 287-296, 1999

      32 Park, S. -G., "Correction of radar reflectivity and differential reflectivity for rain attenuation at Xband. Part II : Evaluation and application" 22 : 1633-1655, 2005

      33 Park, S. -G., "Correction of radar reflectivity and differential reflectivity for rain attenuation at X band. Part I : Theoretical and empirical basis" 22 : 1621-1632, 2005

      34 Rico-Ramirez, M. A., "Classification of ground clutter and anomalous propagation using dual-polarization weather radar" 46 : 1892-1904, 2008

      35 Giangrande, S. E., "Calibration of dualpolarization radar in the presence of partial beam blockage" 22 : 1156-1166, 2005

      36 S.-G. Park, "Calibration of Radar Reflectivity Measurements from the KMA Operational Radar Network" 한국기상학회 46 (46): 243-259, 2010

      37 Bringi, V., "An examination of propagation effects in rainfall on radar measurements at microwave frequencies" 7 : 829-840, 1990

      38 Berenguer, M., "A fuzzy logic technique for identifying nonprecipitating echoes in radar scans" 23 : 1157-1180, 2006

      39 Bellon, A., "A 9-year summary of radar characteristics of mesocyclonic storms and of deep convection in Southern Quebec" 41 : 99-120, 2003

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      2027 평가예정 재인증평가 신청대상 (재인증)
      2021-01-01 평가 등재학술지 유지 (재인증) KCI등재
      2018-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2015-01-01 평가 등재학술지 유지 (등재유지) KCI등재
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      2008-02-19 학회명변경 영문명 : 미등록 -> The Korean Earth Science Society KCI등재
      2007-01-01 평가 등재 1차 FAIL (등재유지) KCI등재
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.47 0.47 0.49
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
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