Abstract

Land surface characteristics, including soil type, terrain slope, and antecedent soil moisture, have significant impacts on surface runoff during heavy precipitation in highly urbanized areas. In this study, a Linear Spectral Mixture Analysis (LSMA) method is modified to extract high-precision impervious surface, vegetation, and soil fractions. In the modified LSMA method, the representative endmembers are first selected by combining a high-resolution image from Google Earth; the unmixing results of the LSMA are then post-processed to reduce errors of misclassification with Normalized Difference Built-up Index (NDBI) and Normalized Difference Vegetation Index (NDVI). The modified LSMA is applied to the Landsat 8 Operational Land Imager (OLI) image from 18 October 2015 of the main urban area of Guangzhou city. The experimental result indicates that the modified LSMA shows improved extraction performance compared with the conventional LSMA, as it can significantly reduce the bias and root-mean-square error (RMSE). The improved impervious surface, vegetation, and soil fractions are used to calculate the composite curve number (CN) for each pixel according to the Soil Conservation Service curve number (SCS-CN) model. The composite CN is then adjusted with regional data of the terrain slope and total 5-day antecedent precipitation. Finally, the surface runoff is simulated with the SCS-CN model by combining the adjusted CN and real precipitation data at 1 p.m., 4 May 2015.

Highlights

  • With the rapid process of urbanization, the portion of impervious area has significantly increased and the urban pervious surface including forest, green land, bare soil, and wetland has decreased, which may lead to a high risk of urban rainstorm waterlogging [1]

  • This study presented a method for extracting the impervious surface, vegetation, and soil

  • This study presented a method for extracting the impervious surface, vegetation, and soil fractions

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Summary

Introduction

With the rapid process of urbanization, the portion of impervious area has significantly increased and the urban pervious surface including forest, green land, bare soil, and wetland has decreased, which may lead to a high risk of urban rainstorm waterlogging [1]. It is very important to quantitatively model the relationship between rainfall-runoff and different land use conditions [2]. This has significant importance and has fundamental influence on urban planning, urban management, exploitation, and utilization of water resources [3]. The Soil Conservation Service curve number (SCS-CN) was developed by the United States The SCS-CN model has been integrated into many widely used hydrological models to simulate surface runoff, including the Soil and Water

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