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A Modeling-Based Approach for Soil Frost Detection in the Northern Boreal Forest Region With C-Band SAR

机译:基于模型的C波段SAR北部北方森林土壤霜冻检测方法

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This paper presents a new approach for monitoring soil frost in the northern boreal forest region using co-polarized C-band synthetic aperture radar (SAR) data. Due to the high sensitivity of the C-band signal to vegetation, estimating the soil freeze/thaw (F/T) state directly from the measured backscatter is not feasible over dense vegetation, such as boreal forests. The presented method is based on applying a simple zeroth-order model to estimate the contribution of the ground and the forest canopy on the observed total backscatter. The retrieved ground and canopy backscatter values were compared with in situ information on soil F/T state. By using a linear least sum of square errors classification algorithm, the retrieved ground and canopy backscatter values representing frozen and thawed ground were successfully separated. The method was tested for various soil types and incidence angles. For soil types with higher water holding capacities and lower infiltration rates such as fine Haplic Podzol and Umbric Gleysol, the estimation accuracy of the F/T state was over 97%, whereas for drier, well-drained soil types such as Haplic Arenosol and Coarse Haplic Podzol it was over 94%. Estimation accuracy slightly increased with higher incidence angle. The method is not feasible in rocky terrain due to very low water content, or in wet snow conditions due to lack of penetration of the C-band SAR signal through wet snow. With low ancillary data and computational requirements, the proposed method is applicable for continuous near real-time monitoring of soil F/T state.
机译:本文提出了一种使用同极化C波段合成孔径雷达(SAR)数据监测北部北方森林地区土壤霜冻的新方法。由于C波段信号对植被具有很高的敏感性,因此在密集的植被(如北方森林)上,直接从测得的反向散射来估算土壤的冻融(F / T)状态是不可行的。提出的方法是基于应用简单的零阶模型来估计地面和森林冠层对观测到的总反向散射的贡献。将获取的地面和冠层反向散射值与有关土壤F / T状态的原位信息进行比较。通过使用线性最小均方误差分类算法,检索到的代表冻结和解冻地面的地面和冠层反向散射值已成功分离。测试了该方法的各种土壤类型和入射角。对于具有较高持水能力和较低渗透率的土壤类型(例如细Haplic Podzol和Umbric Gleysol),F / T状态的估计准确性超过97%,而对于较干燥的,排水良好的土壤类型(Haplic Arenosol和Coarse) Haplic Podzol超过94%。随着入射角的增加,估计精度略有提高。由于含水量非常低,该方法在岩石地形中不可行,或者由于缺乏C波段SAR信号穿过湿雪而在湿雪条件下,该方法不可行。该方法在辅助数据少,计算量少的情况下,适用于土壤F / T状态的连续近实时监测。

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