Abstract
Increased urbanization and climate change have resulted in the intensification of the urban heat island (UHI) effect, particularly in tropical cities. One of the main causes of UHI is the man-made urban surfaces influencing the radiation budget by absorbing, reflecting, and emitting radiation at various wavelengths. The radiative budget of a city is directly influenced by the urban geometry, surface materials, direct solar radiation and incident angle, and atmospheric diffuse radiation. Vegetation cover, in contrast, can decrease UHI by intercepting radiation and through the process of photosynthesis. Better understanding the effect of urban vegetation on the radiative budget can thus contribute towards the mitigation of the UHI effect and ultimately the development of climate resilient urban spaces. To analyze the contribution of vegetation to the radiative budget of a city, a detailed simulation of the complex interaction between the built environment and the vegetation is required. This study proposes an approach for analyzing the 3-D structure of both vegetation and built environment to quantify the contribution of vegetation to the radiative budget of an urban landscape. In a first step, a detailed 3-D model of Singapore including buildings and vegetation was reconstructed using a combination of free and commercial Earth Observation data. Then, the 3-D Discrete Anisotropic Radiative Transfer (DART) model was repurposed to estimate the radiation absorbed by the urban surfaces accounting for the presence of vegetation cover with changing Leaf Area Density (LAD) conditions. The presence of trees in the scene accounted for a significant reduction of the absorbed radiation by buildings and ground. For example, in the case of a residential low-building neighborhood, although having low tree cover, the reduction of the absorbed radiation by buildings and ground was up to 15.5% for a LAD =1. The field validation shows good agreement (R2 = 0.9633, RMSE = 10.8830 and Bias = −1.3826) between the DART-simulated shortwave exitance and upwelling shortwave measurements obtained from a net radiometer mounted on a local flux tower in the urban area of Singapore, over the studied period. Our approach can be used for neighborhood-scale analysis, at any desired location of a city, to allow test scenarios with varying surface materials and vegetation properties.
Highlights
Tropical cities are experiencing more frequent temperature extremes due to climate change and the urban heat island (UHI) effect [1]
The results comprise the effect of varying Leaf Area Density (LAD) in the amount of shortwave radiation absorbed by ground and buildings and the absorbed photosynthetic active radiation (APAR)
A decrease in the rate Absorbed Photosynthetically Active Radiation (APAR) is observed toward higher LAD values
Summary
Tropical cities are experiencing more frequent temperature extremes due to climate change and the UHI effect [1]. Two of the key factors that contribute to the UHI effect are the radiative interaction between complex urban surfaces and the reduced vegetation cover [5]. The radiative budget is a key parameter in urban energy balance and climate models. It summarizes the interaction between radiation and the urban surfaces. The radiative budget is directly influenced by the urban geometry, surface materials, solar incident angle, and atmospheric diffuse radiation. Urban greenery, such as trees and other types of vegetation provide local cooling via shading, evapotranspiration and photosynthetic activity [8,9]. Examining the effect of urban vegetation on the radiative budget of a city is essential to guide the development of livable urban environments
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