Abstract

Surface Urban Heat Island (SUHI) is a phenomenon of high spatial and temporal variability. However, studies that investigate urban land surface temperature (LST) observed in different seasons frequently utilize a single satellite measurement and do not incorporate temporal composites. Temporally aggregated data increase clear sky coverage, which is important in many aspects of urban climatology. However, it is critical to account for possible errors and quality of the data that are utilized. The objective of this paper is to analyze the impact of MODIS Quality Control (QC) and the view angle on temporally aggregated urban surface temperature and long-term SUHI intensity. To achieve this, a weighted arithmetic mean was utilized whose weights were based on the view angle of satellite observation and the MODIS QC flags; namely, LST retrieval errors and emissivity errors. In order to investigate the impact of the MODIS QC on long-term LST composites, five exponential powers were applied to weights during the temporal aggregation process, resulting in five thresholds of best quality pixel promotion. It was found that there are significant differences between temporal composites that take into account the MODIS QC and the view angle and those that do not (obtained by means of a simple arithmetic mean with no weights applied), in terms of spatial distribution and density distribution of urban and rural LST. The differences were more distinctive in spring or daytime cases than in autumn or nighttime cases. The impact of the MODIS QC and the view angle on temporal composites was highest in the city center. Ten SUHI indicators were utilized. It was found that the impact on long-term SUHI intensity is weaker than on the spatial pattern of LST and that SUHI indicators are inconsistent.

Highlights

  • The urban heat island (UHI) is a direct consequence of anthropogenic land transformation [1].It is a phenomenon that describes a local perturbation in the three-dimensional (3D) temperature field of the atmosphere in the vicinity of urban agglomerations

  • probability density functions (PDFs) graphs were prepared for each raster constructed by means of the first type of composition

  • We found that the impact of MODIS Quality Control (QC) and view angle on long-term land surface temperature (LST) composites is weaker in the nighttime cases than in the daytime cases

Read more

Summary

Introduction

The urban heat island (UHI) is a direct consequence of anthropogenic land transformation [1]. It is a phenomenon that describes a local perturbation in the three-dimensional (3D) temperature field of the atmosphere in the vicinity of urban agglomerations. It is typically referred to as the difference between air temperatures observed in urban and rural areas. Air temperature is a parameter that is most apparent to the inhabitants. It is recorded with high frequency and accuracy by meteorological weather stations. In most cases, the density of the meteorological network is not sufficient to characterize the spatial pattern [2]. Satellite instruments are capable of instantaneous measurement of land surface temperature (LST) over vast areas, which represents their greatest advantage over other observational techniques

Objectives
Results
Conclusion

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.