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Tree canopy and summer surface temperature
1 Introduction
Urban surface temperatures vary sharply over short distances, and tree canopy is one of the few factors a city can change.
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Each ten-point increase in canopy cover is associated with a 1.3 °C drop in afternoon surface temperature. The effect is strongest in dense districts and weakens where more than half the ground is already unpaved.
树冠覆盖率每提高十个百分点,午后地表温度约下降 1.3 °C。这一效应在建筑密集的街区最为明显,而在一半以上地面尚未硬化的地方则有所减弱。
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We combine satellite thermal imagery with street-level canopy surveys across 214 neighbourhoods over six summers. Each ten-point increase in canopy cover is associated with a 1.3 °C drop in afternoon surface temperature. Because the design is observational, we cannot rule out that cooler neighbourhoods were simply easier to plant.
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that paper saying trees cool dense areas the most
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The effect is strongest in dense districts and weakens where more than half the ground is already unpaved.
Tree canopy and summer surface temperature
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Canopy cools streets by about 1.3 °C per ten points of cover.
The authors do not claim the trees cause the cooling.
Source · sentence 3
Each ten-point increase in canopy cover is associated with a 1.3 °C drop in afternoon surface temperature.
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Canopy and cooling
Slope is about −1.3 °C per ten points of cover. Stronger in dense districts, so check it against Street width before using it in Chapter 3 draft.
From · Tree canopy and summer surface temperature
Each ten-point increase in canopy cover is associated with a 1.3 °C drop in afternoon surface temperature.
Linked from 2 notes
- Urban heat: what actually works
- Open questions for the methods section
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\section{Results} Canopy cover is associated with lower afternoon surface temperature~\cite{canopy2025}, with a slope of $-1.3\,^{\circ}\mathrm{C}$ per ten points of cover.
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2 Results
Canopy cover is associated with lower afternoon surface temperature [1], with a slope of −1.3 °C per ten points of cover.
[1] Tree canopy and summer surface temperature.
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