南京大学学报(自然科学版)
南京大學學報(自然科學版)
남경대학학보(자연과학판)
Journal of Nanjing University (Natural Sciences)
2015年
5期
944-954
,共11页
蒋璐媛%肖鹏峰%冯学智%耶楠%贺广均%张学良
蔣璐媛%肖鵬峰%馮學智%耶楠%賀廣均%張學良
장로원%초붕봉%풍학지%야남%하엄균%장학량
雪面反射率%各向异性校正%地形校正%GF-1%玛纳斯河流域
雪麵反射率%各嚮異性校正%地形校正%GF-1%瑪納斯河流域
설면반사솔%각향이성교정%지형교정%GF-1%마납사하류역
snow reflectance%anisotropy correction%topographic correction%GF-1%Manasi River Basin
针对山区遥感影像计算雪面反射率的难点,采用各向异性校正与地形校正相结合的方法,将研究区不同坡面方向的雪面反射率归一化至平坦地表垂直观测方向上的雪面反射率,以消除地形影响。其中,各向异性校正采用二向反射分布函数(Bidirectional Reflectance Distribution Function,BRDF)模型;地形校正采用山地辐射传输模型。遥感影像选用新疆玛纳斯河流域的高分一号卫星(GF-1)宽幅相机数据。利用同步观测的积雪光谱数据对此方法的校正能力进行验证,结果表明此方法能够消除大部分地形和大气的影响;计算的雪面反射率在非阴影区与阴影区均与实测数据相一致;该方法可为山区积雪的光学遥感研究提供技术支撑。
針對山區遙感影像計算雪麵反射率的難點,採用各嚮異性校正與地形校正相結閤的方法,將研究區不同坡麵方嚮的雪麵反射率歸一化至平坦地錶垂直觀測方嚮上的雪麵反射率,以消除地形影響。其中,各嚮異性校正採用二嚮反射分佈函數(Bidirectional Reflectance Distribution Function,BRDF)模型;地形校正採用山地輻射傳輸模型。遙感影像選用新疆瑪納斯河流域的高分一號衛星(GF-1)寬幅相機數據。利用同步觀測的積雪光譜數據對此方法的校正能力進行驗證,結果錶明此方法能夠消除大部分地形和大氣的影響;計算的雪麵反射率在非陰影區與陰影區均與實測數據相一緻;該方法可為山區積雪的光學遙感研究提供技術支撐。
침대산구요감영상계산설면반사솔적난점,채용각향이성교정여지형교정상결합적방법,장연구구불동파면방향적설면반사솔귀일화지평탄지표수직관측방향상적설면반사솔,이소제지형영향。기중,각향이성교정채용이향반사분포함수(Bidirectional Reflectance Distribution Function,BRDF)모형;지형교정채용산지복사전수모형。요감영상선용신강마납사하류역적고분일호위성(GF-1)관폭상궤수거。이용동보관측적적설광보수거대차방법적교정능력진행험증,결과표명차방법능구소제대부분지형화대기적영향;계산적설면반사솔재비음영구여음영구균여실측수거상일치;해방법가위산구적설적광학요감연구제공기술지탱。
Aiming at the difficulty in calculating snow reflectance from high spatial resolution image in mountain areas,a method combined with anisotropy correction and topographic correction was proposed to covert the snow re-flectance in different slope to the nadir direction on the flat surface.In the process of anisotropy correction and topo-graphic correction,BRDF model and mountain radiation transmission model were applied to eliminate topographic effects respectively.The GF-1 WFV image of Manasi River Basin,Xinjiang Province was chosen as research data and snow spectral data achieved by synchronous observation was employed to evaluate the this method.The results show that this method could generally eliminate the influence caused by rugged terrain and atmosphere,and the snow re-flectance calculated by this method was in agreement with field observations in both non-shadow area and shadow area.This method can support the research on optical remote sensing of snow in mountain areas.