Enumerating and Modelling the Seasonal alterations of Surface Urban Heat and Cool Island: A Case Study over Indian Cities

Author:

Bhanage Vinayak12ORCID,Kulkarni Sneha3,Sharma Rajat4ORCID,Lee Han25ORCID,Gedam Shirishkumar1

Affiliation:

1. Centre of Studies in Resources Engineering, IIT Bombay, Powai, Mumbai 400076, India

2. Transdisciplinary Science and Engineering Program, Graduate School of Advanced Science and Engineering, Hiroshima University, Hiroshima 739-8529, Japan

3. Institute of Engineering Innovation, School of Engineering, The University of Tokyo, Tokyo 113-8656, Japan

4. School of Energy & Environment, Thapar Institute of Engineering & Technology, Patiala 147004, India

5. Centre for Planetary Health and Innovation Science, The IDEC Institute, Hiroshima University, Hiroshima 739-8529, Japan

Abstract

The present study has been carried out to analyze the seasonal variation of the Urban Heat and Cool Island over the nine developing cities of India. The magnitude of urban heat/cool island and vegetation gradient (∆NDVI) were measured from the daytime satellite datasets. Results of this study show that during the pre-monsoon (March to May) season, the maximum magnitude of the Surface Urban Heat Island (SUHI) was experienced over Kolhapur city, whereas, in the winter, the highest intensity of SUHI was noticed over Pune city. Subsequently, outcomes also depict that the changes in ∆NDVI restrain the pre-monsoon means and the seasonal alterations in SUHI magnitude. However, during the winter (November to February) season, it is controlled by the temperature–vegetation conditions of the rural areas. For pre-monsoon and seasonal changes in SUHI, with the aid of ∆NDVI and the surface temperature of the urban area, regression equations were fitted for pre-monsoon and seasonal changes in SUHI, which explains nearly 90% of SUHI variation. Similarly, the variation of SUHI has been modeled for winter, which elucidates up to 84% of SUHI discrepancy. The study reveals that, on a seasonal scale, a decrement of 0.1 in seasonal ∆NDVI leads to an increase in the seasonal intensity of SUHI by 1.74 °C, which is quite a significant augmentation.

Funder

DST-INSPIRE program

Publisher

MDPI AG

Subject

General Medicine

Reference35 articles.

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4. The dimensions of global urban expansion: Estimates and projections for all countries, 2000–2050;Angel;Prog. Plann.,2011

5. City size and the urban heat island;Oke;Atmos. Environ. Pergamon Press,1973

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