Kallio Kari, Attila Jenni, Härmä Pekka, Koponen Sampsa, Pulliainen Jouni, Hyytiäinen Ulla-Maija, Pyhälahti Timo
Finnish Environment Institute, P.O. Box 140, Helsinki, 00251, Finland.
Environ Manage. 2008 Sep;42(3):511-22. doi: 10.1007/s00267-008-9146-y. Epub 2008 May 29.
We investigated the use of Landsat ETM+ images in the monitoring of turbidity, colored dissolved organic matter (CDOM), and Secchi disk transparency (Z(SD)) in lakes of two river basins located in southern Finland. The ETM+ images were acquired in May, June, and September 2002 and were corrected for atmospheric disturbance using the simplified method of atmospheric correction (SMAC) model. The in situ measurements consisted of water sampling in the largest lake of the region, routine monitoring results for the whole study area, and Z(SD) observations made by volunteers. The ranges of the water quality variables in the dataset were as follows: turbidity, 0.6-25 FNU; absorption coefficient of CDOM at 400 nm, 1.0-12.2 m(-1); Z(SD), 0.5-5.5 m; and chlorophyll a concentration, 2.4-80 microg L(-1). The estimation accuracies of the image-specific empirical algorithms expressed as relative errors were 23.0% for turbidity, 17.4% for CDOM, and 21.1% for Z(SD). If concurrent in situ measurements had not been used for algorithm training, the average error would have been about 37%. The atmospheric correction improved the estimation accuracy only slightly compared with the use of top-of-atmospheric reflectances. The accuracy of the water quality estimates without concurrent in situ measurements could have been improved if in-image atmospheric parameters had been available. The underwater reflectance simulations of the ETM+ channel wavelengths using water quality typical for Finnish lakes (data from 1113 lakes) indicated that region-specific algorithms may be needed in other parts of the country, particularly in the case of Z(SD). Despite the limitations in the spectral and radiometric resolutions, ETM+ imagery can be an effective aid, particularly in the monitoring and management of small lakes (<1 km(2)), which are often not included in routine monitoring programs.
我们研究了利用陆地卫星增强型专题制图仪(ETM+)影像监测芬兰南部两个流域湖泊中的浊度、有色可溶性有机物(CDOM)和塞氏盘透明度(Z(SD))。ETM+影像于2002年5月、6月和9月获取,并使用简化大气校正(SMAC)模型对大气干扰进行了校正。现场测量包括在该地区最大湖泊进行水样采集、整个研究区域的常规监测结果以及志愿者进行的Z(SD)观测。数据集中水质变量的范围如下:浊度为0.6 - 25福尔马肼浊度单位(FNU);CDOM在400纳米处的吸收系数为1.0 - 12.2米⁻¹;Z(SD)为0.5 - 5.5米;叶绿素a浓度为2.4 - 80微克/升。以相对误差表示的特定影像经验算法的估计精度为:浊度23.0%、CDOM 17.4%、Z(SD) 21.1%。如果未使用同步现场测量进行算法训练,平均误差将约为37%。与使用大气层顶反射率相比,大气校正仅略微提高了估计精度。如果影像中的大气参数可用,未进行同步现场测量时水质估计的精度本可提高。利用芬兰湖泊典型水质(来自1113个湖泊的数据)对ETM+通道波长进行的水下反射率模拟表明,该国其他地区可能需要特定区域算法,特别是对于Z(SD)。尽管在光谱和辐射分辨率方面存在局限性,但ETM+影像仍可成为一种有效的辅助手段,尤其是在小型湖泊(<1平方千米)的监测和管理方面,这些小型湖泊通常未纳入常规监测计划。