4.7 Article

The influence of different data and method on estimating the surface urban heat island intensity

期刊

ECOLOGICAL INDICATORS
卷 89, 期 -, 页码 45-55

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.ecolind.2018.01.044

关键词

Surface urban heat island; Different data and method; Spatiotemporal characteristics; China

资金

  1. National Natural Science Foundation of China [41601044]
  2. Special Fund for Basic Scientific Research of Central Colleges, China University of Geosciences, Wuhan [CUG150631, CUGL170401]
  3. Opening Foundation of Key Laboratory for National Geograophy State Monitoring (National Administration of Surveying, Mapping and Geoinformation)
  4. Key Laboratory of Middle Atmosphere and Global environment Observation (LAGEO)
  5. State Key of Laboratory of Atmospheric Boundary Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences

向作者/读者索取更多资源

Few studies have examined the influence of different data and method on estimating the SUHIs. This study aims at analyzing the impact of different method (to define rural area) and different data (MODIS Terra and Aqua satellite data) on estimating the SUHI intensity (SUHII, LST in urban minus rural reference) in 31 cities of China. The major findings include: (1) For SUHII, ignoring the influence of elevation and water body will overestimate the SUHII by 1.68 degrees C (averaged for 31 cities, hereafter) and 0.28 degrees C, respectively, in summer days (SDs). Using nearby suburban area as reference will underestimate the SUHII by 1.48 degrees C in SDs. Different data and method have smaller impact on estimating the SUHII in summer nights (SNs) than in SDs. (2) For spatial variation of SUHII, ignoring the influence of elevation will influence the spatial variation of SUHII in SDs (r = 0.3, p >.05), but other methods have little impact on estimating the spatial variation of SUHII. (3) For interannual variation of SUHII, using nearby suburban area will underestimate the increasing rate of SUHII (SD: 0.106 degrees C/year, SN: 0.012 degrees C/year), whereas ignoring the influence of elevation and water body have little influence on the changing rate of SUHII. The changing rates of SUHII in SDs monitored by Terra satellite were 0.025 degrees C/year lower than Aqua satellite. In all, the present study can enhance our understanding of the influence of different data and method on estimating the SUHII, and provide a useful reference to study the SUHII.

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