Heat Islands: Understanding and Mitigating Heat in Urban by Lisa Gartland

By Lisa Gartland

City warmth islands are metropolitan components which are considerably hotter than their atmosphere. the most reasons are amendment of the land floor through city improvement and waste warmth generated by means of strength utilization. warmth island difficulties have gotten extra urgent as towns keep growing and sprawl.This entire publication brings jointly the most recent information regarding warmth islands and their mitigation. warmth island formation and the issues they reason, mitigation applied sciences and their advantages and guidelines, and activities for cooling groups are defined in complete. the writer contains sections on roof cooling and funky paving and explains their advantages intimately, delivering sensible instructions for his or her choice and install. The ebook additionally comprises potent methodologies for utilizing bushes and crops for cooling, corresponding to eco-friendly roofs. during this groundbreaking booklet, Lisa Gartland deals a entire resource of data for turning warmth islands into cool groups.

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Extra resources for Heat Islands: Understanding and Mitigating Heat in Urban Areas

Sample text

A. Spronken-Smith, E. Jauregui and C. S. B. Grimmond (1999) ‘The energy balance of central Mexico City during the dry season’. ,A. Bitan and P. Berliner (1999) ‘Microclimate analysis of “compact” urban canyons in an arid zone’. Atmospheric Environment 33: 4143–4150 Taha, H. (1997) ‘Urban climates and heat islands: Albedo, evapotranspiration and anthropogenic heat’. ,A. Stan-Sion,A. Lupu, C. Soci and C. Oprea (1999) ‘Influences of the city of Bucharest on weather and climate parameters’. A. and T.

Further study over the past century has determined that urban surfaces are hotter than rural surfaces for two main reasons. First, man-made surfaces are generally composed of dark materials that readily absorb and store the sun’s heat. Exacerbating this high solar absorptance, buildings and pavements form canyons that tend to trap reflected heat. Second, most building materials are watertight, so rainwater runs away and cannot dissipate heat by evaporation (or evapotranspiration, when plants are involved).

Hanaki (1999) ‘Impact of anthropogenic heat on urban climate in Tokyo’. Atmospheric Environment 33: 3897–3909 Jauregui, E. and E. Luyando (1999) ‘Global radiation attenuation by air pollution and its effects on the thermal climate in Mexico City’. International Journal of Climatology 19: 683–694 Khan, S. M. W. Simpson (2001) ‘Effect of a heat island on the meteorology of a complex urban airshed’. Boundary Layer Meteorology 100: 487–506 Landsberg, H. E. (1981) The Urban Climate. New York, NY,Academic Press Mills, G.

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