Abstract

Satellite images have been widely used for urban heat island (UHI) monitoring in recent studies, among which the summer UHI has attracted more attention. However, the studies based on high spatial resolution images have to use single-day land surface temperature (LST) to analyze the summer UHI, due to the low temporal resolution, which is not representative of the summer and leads to incomparability in the time series. The studies based on low spatial resolution images can generate a time series of representative LSTs for summer (e.g., summer mean LSTs), due to the high temporal resolution, but these LSTs lack sufficient spatial details for a refined analysis. To fill these gaps, we propose to integrate the respective advantages of the above approaches to generate a comparable and fine-scale LST time series with a high spatiotemporal resolution. By normalizing the LSTs between the different satellite images via robust fitting with Huber's M-estimator and moment matching, the comparability is ensured. Furthermore, the high-spatial resolution and high-temporal resolution are combined via the spatiotemporal fusion. Overall, we propose a procedure to produce a comparable time series of annual and fine-scale summer mean LSTs, which can serve as a basis for elaborate analysis of the thermal environment.

Highlights

  • U NDER the circumstance of global climate change [1]–[4], there is a need for us to establish the evolution of the thermal environment

  • The long-term coarse-scale images generated in this study were a moderate-resolution Imaging Spectroradiometer (MODIS)-like dataset, which included the MOD11A1 Land surface temperature (LST) after 2000 and the normalized advanced very high resolution radiometer (AVHRR) LSTs before 2000

  • Since the accuracy of the MODIS products has been tested to be reliable in previous research, the accuracy for the whole MODIS-like dataset depends on the temporal normalization between the AVHRR LSTs and MODIS LSTs

Read more

Summary

Introduction

U NDER the circumstance of global climate change [1]–[4], there is a need for us to establish the evolution of the thermal environment. If the history of the thermal environment can be interpreted, it may help us take action in the present day. Land surface temperature (LST), which is a result of surface-atmosphere interactions and energy budget considerations [5]–[7], is a key parameter for the monitoring of the thermal. To thoroughly establish both the past and the present of the thermal environment, a long-term and fine-scale series of summer LST is required for an elaborate analysis [11], [12]

Methods
Results
Conclusion
Full Text
Published version (Free)

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