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A new soil moisture index driven from an adapted long-term temperature-vegetation scatter plot using MODIS data

机译:一种新的土壤湿度指数,从改进的长期温度 - 植被散点图驱动的土壤湿度指数驱动

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摘要

The estimation of soil moisture content on the global scale is a key research issue in the field of remote sensing and, to date, a range of methods have been developed to achieve this. The temperature-vegetation (T-V) technique, which is perhaps one of the most common and successful, suffers from being inaccurate in some cases, especially when the daily T-V scatter plots are not able to define the wet and dry edges in a reliable way. A further challenge is the scale inconsistency between the results obtained on different days, which is a serious concern when monitoring soil moisture changes over periods of time. To address these restrictions, this paper introduces a new soil moisture index, called SMiSEE, driven by a new long-term T-V scatter plot that is established from data covering a 1-year period. The normalized NDVI is set as the horizontal axis and three different temperature factors are suggested as the vertical axis in the proposed 1-year scatter plot. From these three temperature factors, the results proved that "LSTday-Ta-day (10:30 am)" is the most appropriate choice. In contrast to most linear co-distance indexes reported in the literature, the proposed SMiSEE is a novel non-linear soil moisture index that defines the locus of co-moisture points in the scatter plot as unequal distance curves. To investigate the proposed method, two different soil moisture observation networks with different climate and vegetation conditions, namely, SMAPVEX12 in Canada and REMEDHUS in Spain, were applied. The results demonstrated that the efficiency of the proposed 1-year scatter plot, which was even applicable to, and improved upon, other indexes in the literature. In addition, SMiSEE outperformed SEE, iTVDI and phi as the most recent similar indexes, achieving correlation coefficients of 0.65 and 0.74 for the SMAPVEX12 and REMEDHUS networks, respectively. These results appear to be promising, especially for the vegetated area in the SMAPVEX12 network.
机译:估算土壤水分含量在全球范围内是遥感领域的关键研究问题,迄今为止,已经开发了一系列方法来实现这一目标。在某些情况下,温度 - 植被(T-V)技术可能是最常见和最成功的,遭受不准确的,特别是当日常T-V散射图不能以可靠的方式定义湿和干燥的边缘时。进一步的挑战是在不同日期获得的结果之间的规模不一致,这是在监测土壤水分的时间内发生严重问题。为解决这些限制,本文介绍了一种新的土壤湿度指数,称为Smisee,由新的长期T-V散散地图驱动,该图是从覆盖1年期间的数据建立的。标准化的NDVI被设定为水平轴,并且在提出的1年散点图中建议了三种不同的温度因子作为垂直轴。从这三种温度因素,结果证明“LSTDAY-TA-DAY(上午10:30)”是最合适的选择。与文献中报告的大多数线性共距指标相反,所提出的Smisee是一种新型非线性土壤湿度指数,其定义了散点图中的共湿度点作为不等距离曲线的基因座。为了研究提出的方法,应用了不同气候和植被条件的两种不同的土壤水分观察网络,即加拿大和西班牙的雷姆斯的Smapvex12。结果表明,提出的1年散点图的效率,甚至适用于文献中的其他指标。此外,SMISEE优于SEN,ITVDI和PHI作为最近类似的索引,分别实现了SMAPVEX12和Remedhus网络的相关系数0.65和0.74。这些结果似乎很有希望,特别是对于Smapvex12网络中的植被区域。

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