20170309
Author :
Christopher W. Mackey, Xuhui Lee, Ronald B. Smith
Christopher W. Mackey, Xuhui Lee, Ronald B. Smith
Year :
2012
2012
Title :
Remotely sensing the cooling effects of city scale efforts to reduce urban heat island
Remotely sensing the cooling effects of city scale efforts to reduce urban heat island
Journal :
Building and Environment
Building and Environment
Comment :
Faced with urban heat island (UHI) effect, many urban planner or scientists are developing a number of possible cooling strategies and two have gained acceptance to the point that they are being implemented in a number of cities. These implemented strategies include one that seeks to increase urban albedo and another that seeks to increase urban vegetation. This study is an attempt to analyze a real large scale application by observing recent vegetated and reflective surfaces in LANDSAT images of Chicago (over the last 15 years). Results show that plots between albedo increase and corresponding LANDSAT temperature change have linear regressions with steeper slopes (-15.7) and stronger linear correlations (-0.33) than plots between NDVI increase and temperature change (-8.9 slope, -0.17 correlation). This indicates that the albedo increases produced greater LANDSAT cooling than the NDVI increases.
Faced with urban heat island (UHI) effect, many urban planner or scientists are developing a number of possible cooling strategies and two have gained acceptance to the point that they are being implemented in a number of cities. These implemented strategies include one that seeks to increase urban albedo and another that seeks to increase urban vegetation. This study is an attempt to analyze a real large scale application by observing recent vegetated and reflective surfaces in LANDSAT images of Chicago (over the last 15 years). Results show that plots between albedo increase and corresponding LANDSAT temperature change have linear regressions with steeper slopes (-15.7) and stronger linear correlations (-0.33) than plots between NDVI increase and temperature change (-8.9 slope, -0.17 correlation). This indicates that the albedo increases produced greater LANDSAT cooling than the NDVI increases.
댓글
댓글 쓰기