2021
DOI: 10.3390/su13020868
|View full text |Cite
|
Sign up to set email alerts
|

Canopy-scale Built-environment Characteristics and Urban Heat Island Effect in a Tropical Medium-sized City

Abstract: Previous studies have found that built-environment characteristics in large cities produce important effects of the urban heat island (UHI) and know the horizontal space affected by the urban canopy microclimate ranges from about 30–200 m, but there are few studies in medium-sized cities. Therefore, this study investigates canopy-scale built-environment characteristics and their correlation with urban heat island (UHI) effects in Chiayi city, a tropical, medium-sized city. Under a 100 m buffer size, 2D and 3D … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(1 citation statement)
references
References 28 publications
0
1
0
Order By: Relevance
“…According to recent research, there are four different types of UHI: the surface heat island at the ground level, the canopy heat island that reaches up to the tallest buildings, the ground heat island that occurs within the soil [3], and the boundary layer heat island that occurs above the buildings and reaches the atmosphere [4,5]. There are two common ways to gather meteorological data on the UHI of the canopy layer: fixed measuring points through weather stations [6] and movable transects employing vehicles [7,8]. The main difficulty lies in balancing cost-effectiveness and spatial and temporal resolution, as each approach has distinct benefits and drawbacks [9].…”
Section: Introductionmentioning
confidence: 99%
“…According to recent research, there are four different types of UHI: the surface heat island at the ground level, the canopy heat island that reaches up to the tallest buildings, the ground heat island that occurs within the soil [3], and the boundary layer heat island that occurs above the buildings and reaches the atmosphere [4,5]. There are two common ways to gather meteorological data on the UHI of the canopy layer: fixed measuring points through weather stations [6] and movable transects employing vehicles [7,8]. The main difficulty lies in balancing cost-effectiveness and spatial and temporal resolution, as each approach has distinct benefits and drawbacks [9].…”
Section: Introductionmentioning
confidence: 99%