Abstract

Superresolution mapping (SRM) is a method to produce a fine-spatial-resolution land cover map from coarse-spatial-resolution remotely sensed imagery. A popular approach for SRM is a two-step algorithm, which first increases the spatial resolution of coarse fraction images by interpolation and then determines class labels of fine-resolution pixels using the maximum a posteriori (MAP) principle. By constructing a new image formation process that establishes the relationship between the observed coarse-resolution fraction images and the latent fine-resolution land cover map, it is found that the MAP principle only matches with area-to-point interpolation algorithms and should be replaced by deconvolution if an area-to-area interpolation algorithm is to be applied. A novel iterative interpolation deconvolution (IID) SRM algorithm is proposed. The IID algorithm first interpolates coarse-resolution fraction images with an area-to-area interpolation algorithm and produces an initial fine-resolution land cover map by deconvolution. The fine-spatial-resolution land cover map is then updated by reconvolution, back-projection, and deconvolution iteratively until the final result is produced. The IID algorithm was evaluated with simulated shapes, simulated multispectral images, and degraded Landsat images, including comparison against three widely used SRM algorithms: pixel swapping, bilinear interpolation, and Hopfield neural network. Results show that the IID algorithm can reduce the impact of fraction errors and can preserve the patch continuity and the patch boundary smoothness simultaneously. Moreover, the IID algorithm produced fine-resolution land cover maps with higher accuracies than those produced by other SRM algorithms.

Highlights

  • Super-resolution mapping (SRM) is a method to predict the spatial distribution of land cover classes located within the geographical area represented by coarse spatial resolution pixels

  • Through analyzing the popular interpolation-based two-step SRM algorithms, we found that the maximum a posteriori (MAP) principle, which is used as the second step in existing algorithms, is suitable only when an area-to-point interpolation method is used

  • If a traditional areato-area interpolation method is used, the MAP process should be replaced by the de-convolution process, based on a new constructed conceptual image formation process that establishes the relationship between the observed coarse spatial resolution fraction images and the latent fine spatial resolution land cover map

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Summary

Introduction

Super-resolution mapping (SRM) is a method to predict the spatial distribution of land cover classes located within the geographical area represented by coarse spatial resolution pixels. Compared with hard classification that only produces a land cover map at the coarse spatial resolution pixel scale and spectral unmixing that only produces coarse spatial resolution fraction images without detailed land cover spatial pattern information, SRM can produce a more informative result. The input to a SRM analysis is typically a set of coarse spatial resolution fraction images, in which the image value represents the area percentage of one land cover class in one coarse spatial resolution pixel. The output of SRM is a fine spatial resolution land cover map, that is, a labeled image in which the label represents the land cover class that a fine spatial resolution pixel belongs to. Given that the input of SRM is continuous values (e.g. percentage class coverage) while the output is discrete values (e.g. hard class labels), and their spatial resolutions are different, SRM often needs perform two tasks: the increment of the spatial resolution of input fraction images and the transformation between continuous and discrete values

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