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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Identification and quantification of diffuse fresh submarine groundwater discharge via airborne thermal infrared remote sensing
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Identification and quantification of diffuse fresh submarine groundwater discharge via airborne thermal infrared remote sensing

机译:机载热红外遥感对扩散性新鲜海底地下水排放的识别和定量

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Airborne thermal infrared (TIR) overflights were combined with shoreline radionuclide surveys to investigate submarine groundwater discharge (SGD) along the north shore of Long Island, NY between June 2013 and September 2014. Regression equations developed for three distinct geomorphological environments suggest a positive linear relationship between the rate of diffuse SGD and the spatial extent of the observed coastal TIR anomalies; such a relationship provides quantitative evidence of the ability to use TIR remote sensing as a tool to remotely identify and measure SGD. Landsat TIR scenes were unable to resolve any of the 18 TIR anomalies identified during the various airborne overflights. Two locations were studied in greater detail via Rn-222 time series and manual seepage meters in order to understand why specific shoreline segments did not exhibit a TIR anomaly. SGD at the first site, located within a large, diffuse TIR anomaly, was composed of a mixture of fresh groundwater and circulated seawater with elevated levels of nitrate. In contrast, SGD at the second site, where no coastal TIR anomaly was observed, was composed of circulated seawater with negligible nitrate. Despite the compositional differences in seepage, both sites were similar in discharge magnitude, with average time series Rn-222 derived SGD rates equal to 18 and 8 cm d(-1) for the TIR site and non-TIR site, respectively. Results suggest that TIR remote sensing has the ability to identify locations of a mixture between diffuse fresh and circulated seawater SGD. If TIR anomalies can be demonstrated to represent a mixture between fresh and circulated seawater SGD, then the cumulative area of the TIR anomalies may be used to estimate the fresh fraction of SGD relative to the cumulative area of the seepage face, and thus allows for improved SGD derived nutrient flux calculations on a regional scale. (C) 2015 Elsevier Inc. All rights reserved.
机译:机载热红外(TIR)飞越飞行与海岸线放射性核素测量相结合,以调查2013年6月至2014年9月之间纽约长岛北岸的海底地下水排放(SGD)。针对三种不同地貌环境开发的回归方程表明存在正线性关系SGD扩散率与观测到的沿海TIR异常的空间范围之间的关系;这种关系为使用TIR遥感作为远程识别和测量SGD的工具提供了定量证据。 Landsat TIR场景无法解决各种机载飞越过程中发现的18个TIR异常。通过Rn-222时间序列和手动渗流计对两个位置进行了更详细的研究,以了解为什么特定的海岸线段未显示TIR异常。位于第一个站点的SGD位于较大的,分散的TIR异常内,由新鲜地下水和循环海水以及硝酸盐含量升高的混合物组成。相反,在第二个站点(未观察到沿海TIR异常)的SGD由循环海水和硝酸盐可忽略不计组成。尽管渗流的成分有所不同,但两个站点的排放量都相似,Rn-222的平均时间序列得出的TGD站点和非TIR站点的SGD速率分别等于18和8 cm d(-1)。结果表明,TIR遥感具有识别淡水和循环海水SGD之间混合物位置的能力。如果可以证明TIR异常代表淡水和循环海水SGD之间的混合物,则TIR异常的累积面积可用于估计相对于渗流面累积面积的SGD的新鲜分数。 SGD在区域范围内得出的养分通量计算。 (C)2015 Elsevier Inc.保留所有权利。

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