Subpixel Mapping of Surface Water in the Tibetan Plateau with MODIS Data

Chenzhou Liu,Xiuying Liu,Jiancheng Shi,Ji Zhu,Zhaoyong Shi

doi:10.3390/rs12071154

Abstract

This article presents a comprehensive subpixel water mapping algorithm to automatically produce routinely open water fraction maps in the Tibetan Plateau (TP) with the Moderate Resolution Imaging Spectroradiometer (MODIS). A multi-index threshold endmember extraction method was applied to select the endmembers from MODIS images. To incorporate endmember variability, an endmember selection strategy, called the combined use of typical and neighboring endmembers, was adopted in multiple endmember spectral mixture analysis (MESMA), which can assure a robust subpixel water fractions estimation. The accuracy of the algorithm was assessed at both the local scale and regional scale. At the local scale, a comparison using the eight pairs of MODIS/Landsat 8 Operational Land Imager (OLI) water maps demonstrated that subpixels water fractions were well retrieved with a root mean square error (RMSE) of 7.86% and determination coefficient (R2) of 0.98. At the regional scale, the MODIS water fraction map in October 2014 matches well with the TP lake data set and the Global Lake and Wetland Database (GLWD) in both latitudinal and longitudinal distribution. The lake area estimation is more consistent with the reference TP lake data set (difference of −3.15%) than the MODIS Land Water Mask (MOD44W) (difference of −6.39%).

Highlights

The Tibetan Plateau (TP) is known as the earth’s third pole [1,2] and the water tower of Asia, and is an important factor greatly affecting the earth’s climate system [3,4]
The water map of the Tibetan Plateau was compared with four public data sets: the TP lake data set, the Global Lake and Wetland Database (GLWD), the European Space Agency (ESA) surface water data, and MOD44W
This study presents a method that is very suitable for mountain areas to map open water in the TP

Summary

Introduction

The Tibetan Plateau (TP) is known as the earth’s third pole [1,2] and the water tower of Asia, and is an important factor greatly affecting the earth’s climate system [3,4]. As the headwater area of ten major rivers in Asia, the TP supplies water resources to the billions of inhabitants in the plateau and surrounding regions [5]. Surface water such as lakes, rivers, and artificial reservoirs in the TP, which have been greatly affected by climate change [6] and human disturbance [7,8], are playing an essential role in climate balance, hydrological cycle, and ecosystem balance [9,10]. Digitization through visualization with prior knowledge can ensure relatively high accuracy of water boundary extraction and provide databases with strict quality control [13,14].

Methods

Results

Discussion

Conclusion