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      50 Grades of Shade

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          Abstract

          Cities increasingly recognize the importance of shade to reduce heat stress and adopt urban forestry plans with ambitious canopy goals. Yet, the implementation of tree and shade plans often faces maintenance, water use, and infrastructure challenges. Understanding the performance of natural and non-natural shade is critical to support active shade management in the built environment. We conducted hourly transects in Tempe, Arizona with the mobile human-biometeorological station MaRTy on hot summer days to quantify the efficacy of various shade types. We sampled sun-exposed reference locations and shade types grouped by urban form, lightweight/engineered shade, and tree species over multiple ground surfaces. We investigated shade performance during the day, at peak incoming solar, peak air temperature, and after sunset using three thermal metrics: the difference between a shaded and sun-exposed location in air temperature ( ΔT a ), surface temperature ( ΔT s ), and mean radiant temperature ( ΔT MRT ). ΔT a did not vary significantly between shade groups, but ΔT MRT spanned a 50°C range across observations. At daytime, shade from urban form most effectively reduced T s and T MRT , followed by trees and lightweight structures. Shade from urban form performed differently with changing orientation. Tree shade performance varied widely; native and palm trees were least effective, while non-native trees were most effective. All shade types exhibited heat retention (positive ΔT MRT ) after sunset. Based on the observations, we developed characteristic shade performance curves that will inform the City of Tempe’s design guidelines towards using “the right shade in the right place” and form the basis for the development of microclimate zones (MCSz).

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          Local Climate Zones for Urban Temperature Studies

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            Urban greening to cool towns and cities: A systematic review of the empirical evidence

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              More intense, more frequent, and longer lasting heat waves in the 21st century.

              A global coupled climate model shows that there is a distinct geographic pattern to future changes in heat waves. Model results for areas of Europe and North America, associated with the severe heat waves in Chicago in 1995 and Paris in 2003, show that future heat waves in these areas will become more intense, more frequent, and longer lasting in the second half of the 21st century. Observations and the model show that present-day heat waves over Europe and North America coincide with a specific atmospheric circulation pattern that is intensified by ongoing increases in greenhouse gases, indicating that it will produce more severe heat waves in those regions in the future.
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                Author and article information

                Journal
                Bulletin of the American Meteorological Society
                American Meteorological Society
                0003-0007
                1520-0477
                May 07 2021
                May 07 2021
                : 1-35
                Affiliations
                [1 ]School of Arts, Media and Engineering (AME), School of Computing, Informatics, and Decision Systems Engineering (CIDSE), Arizona State University, 950 S. Forest Mall, Stauffer B, Tempe, AZ 85281, ariane.middel@asu.edu
                [2 ]College of Architecture, Kuwait University, saud.alkhaled@ku.edu.kw
                [3 ]School of Sustainability, Arizona State University, florian.schneider@asu.edu
                [4 ]School of Sustainability, Arizona State University, bjoern.hagen@asu.edu
                [5 ]The Design School, Arizona State University, paul.coseo@asu.edu
                Article
                10.1175/BAMS-D-20-0193.1
                34446943
                b3a76ef6-49c6-48db-b4df-d8721392a471
                © 2021
                History

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