Advanced Dual-Satellite Method for Detection of Low Stratus and Fog near Japan at Dawn from FY-4A and Himawari-8
- 주제(키워드) fog , low stratus , dual satellite method , Himawari-8 , Fengyun-4A
- 주제(기타) Environmental Sciences
- 주제(기타) Geosciences, Multidisciplinary
- 주제(기타) Remote Sensing
- 주제(기타) Imaging Science & Photographic Technology
- 설명문(일반) [Yang, Jung-Hyun; Choi, Yong-Sang] Ewha Womans Univ, Dept Atmospher Sci & Engn, Seoul 120750, South Korea; [Yoo, Jung-Moon] Ewha Womans Univ, Dept Sci Educ, Seoul 120750, South Korea
- 관리정보기술 faculty
- 등재 SCIE, SCOPUS
- 발행기관 MDPI
- 발행년도 2021
- URI http://www.dcollection.net/handler/ewha/000000181444
- 본문언어 영어
- Published As http://dx.doi.org/10.3390/rs13051042
초록/요약
The detection of low stratus and fog (LSF) at dawn remains limited because of their optical features and weak solar radiation. LSF could be better identified by simultaneous observations of two geostationary satellites from different viewing angles. The present study developed an advanced dual-satellite method (DSM) using FY-4A and Himawari-8 for LSF detection at dawn in terms of probability indices. Optimal thresholds for identifying the LSF from the spectral tests in DSM were determined by the comparison with ground observations of fog and clear sky in/around Japan between April to November of 2018. Then the validation of these thresholds was carried out for the same months of 2019. The DSM essentially used two traditional single-satellite tests for daytime such as the 0.65-mu m reflectance (R-0.65), and the brightness temperature difference between 3.7 mu m and 11 mu m (BTD3.7-11); in addition to four more tests such as Himawari-8 R-0.65 and BTD13.5-8.5, the dual-satellite stereoscopic difference in BTD3.7-11 (Delta BTD3.7-11), and that in the Normalized Difference Snow Index (Delta NDSI). The four were found to show very high skill scores (POD: 0.82 +/- 0.04; FAR, 0.10 +/- 0.04). The radiative transfer simulation supported optical characteristics of LSF in observations. The LSF probability indices (average POD: 0.83, FAR: 0.10) were constructed by a statistical combination of the four to derive the five-class probability values of LSF occurrence in a grid. The indices provided more details and useful results in LSF spatial distribution, compared to the single satellite observations (i.e., R-0.65 and/or BTD3.7-11) of either LSF or no LSF. The present DSM could apply for remote sensing of environmental phenomena if the stereoscopic viewing angle between two satellites is appropriate.
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