4.7 Article

Expansion of major urban areas in the US Great Plains from 2000 to 2009 using satellite scatterometer data

Journal

REMOTE SENSING OF ENVIRONMENT
Volume 204, Issue -, Pages 524-533

Publisher

ELSEVIER SCIENCE INC
DOI: 10.1016/j.rse.2017.10.004

Keywords

Urbanization; QuikSCAT; Dense Sampling Method; Impervious surface; LandScan

Funding

  1. NASA [NNX12AM89G, NNX14AJ32G]
  2. NASA Land-Cover and Land-Use Change (LCLUC)
  3. NASA [NNX12AM89G, 69725] Funding Source: Federal RePORTER

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A consistent dataset delineating and characterizing changes in urban environments will be valuable for socio-economic and environmental research and for sustainable urban development. Remotely sensed data have been long used to map urban extent and infrastructure at various spatial and spectral resolutions. Although many datasets and approaches have been tried, there is not yet a universal way to map urban extents across the world. Here we combined a microwave scatterometer (QuikSCAT) dataset at similar to 1 km posting with percent impervious surface area (%ISA) data from the National Land Cover Dataset (NLCD) that was generated from Landsat data, and ambient population data from the LandScan product to characterize and quantify growth in nine major urban areas in the US Great Plains from 2000 to 2009. Nonparametric Mann-Kendall trend tests on backscatter time series from urban areas show significant expanding trends in eight of nine urban areas with p-values ranging 0.032 to 0.001. The sole exception is Houston, which has a substantial non-urban backscatter at the northeastern edge of the urban core. Strong power law scaling relationships between ambient population and either urban area or backscatter power (r(2) of 0.96 in either model) with sub-linear exponents (beta of 0.911 and 0.866, respectively) indicate urban areas become more compact with more vertical built-up structure than lateral expansion to accommodate the increased population. Increases in backscatter and %ISA datasets between 2001 and 2006 show agreement in both magnitude and direction for all urban areas except Minneapolis-St. Paul (MSP), likely due to the presence of many lakes and ponds throughout the MSP metropolitan area. We conclude discussing complexities in the backscatter data caused by large metal structures and rainfall.

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