Abstract

The mixed pixel problem is common in remote sensing. A soft classification can generate land cover class fraction images that illustrate the areal proportions of the various land cover classes within pixels. The spatial distribution of land cover classes within each mixed pixel is, however, not represented. Super-resolution land cover mapping (SRM) is a technique to predict the spatial distribution of land cover classes within the mixed pixel using fraction images as input. Spatial–temporal SRM (STSRM) extends the basic SRM to include a temporal dimension by using a finer-spatial resolution land cover map that pre- or postdates the image acquisition time as ancillary data. Traditional STSRM methods often use one land cover map as the constraint, but neglect the majority of available land cover maps acquired at different dates and of the same scene in reconstructing a full state trajectory of land cover changes when applying STSRM to time-series data. In addition, the STSRM methods define the temporal dependence globally, and neglect the spatial variation of land cover temporal dependence intensity within images. A novel local STSRM (LSTSRM) is proposed in this paper. LSTSRM incorporates more than one available land cover map to constrain the solution, and develops a local temporal dependence model, in which the temporal dependence intensity may vary spatially. The results show that LSTSRM can eliminate speckle-like artifacts and reconstruct the spatial patterns of land cover patches in the resulting maps, and increase the overall accuracy compared with other STSRM methods.

Highlights

  • IntroductionUnderstanding the distribution and dynamics of land cover is essential to better understand the Earth’s processes

  • LAND cover and its dynamic play a major role in global change

  • Several popular super-resolution mapping (SRM) algorithms were used for comparison including the pixel swapping algorithm based SRM (PSA) [20], the Kriging interpolation based SRM (KI) [41, 46, 47], the Hopfield neural network based SRM (HNN) [25], the spatial-temporal pixel swapping algorithm (STPSA) [17], the subpixel land cover change mapping algorithm (SLCCM) [5], and the SRM based on spatial–temporal dependence from a former map (SRM_STD) [34]

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Summary

Introduction

Understanding the distribution and dynamics of land cover is essential to better understand the Earth’s processes. Sensed images are the main data source in mapping land cover and monitoring land cover changes at different spatial resolutions. Soft classification can generate land cover class fraction images that represent the areal proportions of different land cover classes within a pixel. The output of a soft classification is a number of fraction images equal to the number of land cover classes. SRM can be viewed as the post processing of soft classification that predicts the spatial distribution of land cover classes at the sub-pixel scale. The fraction images output from a soft classification are inputted to an SRM to produce a land cover map with a finer spatial resolution than the original remotely sensed image

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