4.7 Article

A simple method for determination of fine resolution urban form patterns with distinct thermal properties using class-level landscape metrics

Journal

LANDSCAPE ECOLOGY
Volume 36, Issue 7, Pages 1863-1876

Publisher

SPRINGER
DOI: 10.1007/s10980-020-01156-9

Keywords

Land surface temperature; Urban land cover classification; Fragstats; Class-level landscape metrics; K-means clustering

Funding

  1. Fragments, Functions and Flows in Urban Ecosystem Services (F3UES) project as part of the larger Biodiversity and Ecosystem Service Sustainability (BESS) framework [NE/J015067/1]
  2. UK Natural Environment Research Council (NERC)
  3. Biotechnology and Biological Sciences Research Council (BBSRC)
  4. NERC
  5. BESS programme
  6. NERC [NE/J015067/1, nceo020007] Funding Source: UKRI

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This study aimed to sub-divide a high-resolution land cover map into patches with distinct spatial and thermal properties for urban LST research at micro-scales. The two-tiered unsupervised k-means clustering analysis successfully produced spatially distinct groups of patches with different thermal properties and spatial configurations for major land cover classes.
Context Relationships between land surface temperature (LST) and spatial configuration of urban form described by landscape metrics so far have been investigated with coarse resolution LST imagery within artificially superimposed land divisions. Citywide micro-scale observations are needed to better inform urban design and help mitigate urban heat island effects in warming climates. Objectives The primary objective was to sub-divide an existing high-resolution land cover (LC) map into groups of patches with distinct spatial and thermal properties suitable for urban LST studies relevant to micro-scales. The secondary objective was to provide insights into the optimal analytical unit size to calculate class-level landscape metrics strongly correlated with LST at 2 m spatial resolution. Methods A two-tiered unsupervised k-means clustering analysis was deployed to derive spatially distinct groups of patches of each major LC class followed by further subdivisions into hottest, coldest and intermediary sub-classes, making use of high resolution class-level landscape metrics strongly correlated with LST. Results Aggregation class-level landscape metrics were consistently correlated with LST for green and grey LC classes and the optimal search window size for their calculations was 100 m for LST at 2 m resolution. ANOVA indicated that all Tier 1 and most of Tier 2 subdivisions were thermally and spatially different. Conclusions The two-tiered k-means clustering approach was successful at depicting subdivisions of major LC classes with distinct spatial configuration and thermal properties, especially at a broader Tier 1 level. Further research into spatial configuration of LC patches with similar spatial but different thermal properties is required.

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