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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Evaluating simple proxy measures for estimating depth of the similar to 1900 nm water absorption feature from hyperspectral data acquired under natural illumination
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Evaluating simple proxy measures for estimating depth of the similar to 1900 nm water absorption feature from hyperspectral data acquired under natural illumination

机译:评估简单的代理度量以从自然光照下获取的高光谱数据中估算与1900 nm吸水特征相似的深度

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Direct measurement of depth of the similar to 1900 nm feature (F-1900) caused by molecular water is not possible from hyperspectral data acquired under natural illumination. Proxy measures for depth were evaluated to estimate the true depth of F-1900 from such data. Suitable proxy measures were identified using data acquired by a high-resolution spectrometer (under artificial and natural illumination) and by a hyperspectral imaging sensor (under artificial illumination), with different amounts of simulated atmospheric noise. The best performing proxy measures were used to estimate depth from hyperspectral imagery acquired in the field under natural illumination. Proxy measures comprised a ratio of reflectance, continuum-removed depth at a single wavelength and continuum-removed depth integrated over several wavelengths. For high resolution spectra, a ratio of reflectance at 2017 nm and 1967 nm (Ratio(2017/1967)) and the continuum-removed depth at 1967 nm (CRD1967) were strongly correlated with depth R-2 = 0.98-0.99 and R-2 = 0.95-0.96, respectively. For hyperspectral imagery acquired in the laboratory, Ratio(2017/1967) and CRD1967 were strongly correlated with depth across all levels of atmospheric noise (R-2 = 0.94-0.98 and 0.94-0.97, respectively). Proxy measures using integrated depth performed relatively poorly (R-2 = 0.65-0.86). In independent tests, depth of F-1900 was consistently overestimated by CRD1967 but not by Ratio(2017/1967). Validation of field imagery was done by comparing depth predicted by the proxy measures with depth measured from laboratory imagery of collocated samples from the field. Ratio(2017/1967) derived from a polynomial fit to the data between 1961 and 2134 nm (Ratio(2017/1967)) most closely approximated measured depth. Ratio(2017/1967), derived from the original data either under or overestimated depth. Measures of continuum-removed depth generated from the original data (CRD1967) and from a polynomial fit to the original data (CRDP1967) overestimated the depth of F-1900. This study showed that the depth of F-1900 can be predicted from data acquired under natural illumination however, the choice of proxy measure can have a significant impact upon quantitative estimates. (C) 2015 The Author. Published by Elsevier Inc.
机译:由分子水引起的类似于1900 nm特征(F-1900)的深度的直接测量是不可能的,这是根据在自然光照下获取的高光谱数据得出的。评估了深度的替代措施,以便根据此类数据估算F-1900的真实深度。使用高分辨率光谱仪(在人工和自然照明下)和高光谱成像传感器(在人工照明下)采集的数据,并以不同数量的模拟大气噪声,确定合适的替代措施。表现最佳的代理度量用于从自然照明下在现场获取的高光谱图像估计深度。替代指标包括反射率,单个波长处的连续光谱去除深度和多个波长处的连续光谱去除深度之比。对于高分辨率光谱,在2017 nm和1967 nm处的反射率之比(Ratio(2017/1967))和在1967 nm处连续去除的深度(CRD1967)与深度R-2 = 0.98-0.99和R- 2 = 0.95-0.96。对于在实验室获得的高光谱图像,Ratio(2017/1967)和CRD1967与所有级别的大气噪声深度都高度相关(分别为R-2 = 0.94-0.98和0.94-0.97)。使用综合深度的替代指标表现相对较差(R-2 = 0.65-0.86)。在独立测试中,CRD1967始终高估了F-1900的深度,但比率(2017/1967)却没有高估它。实地图像的验证是通过将代理指标预测的深度与从实地并置样本的实验室图像中测得的深度进行比较来完成的。由多项式拟合得出的比率(2017/1967),最接近于所测量的深度,该数据是1961年至2134 nm之间的数据(比率(2017/1967))。比率(2017/1967),是根据原始数据得出的,低于或高估的深度。根据原始数据(CRD1967)和多项式拟合原始数据(CRDP1967)产生的连续体去除深度的度量高估了F-1900的深度。这项研究表明,F-1900的深度可以根据在自然光照下获得的数据进行预测,但是,替代度量的选择可能会对定量估计产生重大影响。 (C)2015作者。由Elsevier Inc.发布

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