Temporal-spatial Changes of Urban Various Plant Communities on Cooling and Humidifying Effects at Small Scal
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Temporal-spatial Changes of Urban Various Plant Communities on Cooling and Humidifying Effects at Small Scal
Bulletin of Soiland Water ConservationVol. 32, Issue 4, Pages: 307-311(2013)
作者机构:
1. 江西财经大学鄱阳湖生态经济研究院,江西,南昌,330032
2. 云南财经大学国土资源与持续发展研究所,云南,昆明,650221
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Published:2013
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HUANG He-ping, ZOU Jin-lang. Temporal-spatial Changes of Urban Various Plant Communities on Cooling and Humidifying Effects at Small Scal[J]. Bulletin of Soiland Water Conservation, 2013, 32(4): 307-311.
DOI:
HUANG He-ping, ZOU Jin-lang. Temporal-spatial Changes of Urban Various Plant Communities on Cooling and Humidifying Effects at Small Scal[J]. Bulletin of Soiland Water Conservation, 2013, 32(4): 307-311.DOI:
Temporal-spatial Changes of Urban Various Plant Communities on Cooling and Humidifying Effects at Small Scal
The cooling and humidifying effect of the urban plant community plays an important role in alleviating the"urban heat island effect".To study the effect of vegetation in regulating urban microclimate at a small scale
arboreal forest
shrubs and lawns were chosen in Mailu campus of Jiangxi Finance and Economics University.The results showed that:(1)The most significant cooling effect of arboreal forest occurred at 20:00(-4.00 ℃)
while the weakest effect occurred at 10:00(-1.68 ℃).The most significant cooling effect of shrubs occurred at 8:00(-2.95℃)
while the least effect occurred at 12:00(-0.27 ℃).The most significant cooling effect of lawns occurred at 20:00(-2.31 ℃)
while the least effect occurred at 10:00(0.38℃).(2)In morning
the cooling and humidifying effects of shrubs were great
and the humidifying effects of lawns were significant.In afternoon
the cooling effect of lawns and the humidifying effect of arboreal forest varied greatly.(3)The cooling and humidifying effects of arboreal forest
shrubs and lawns decreased as the distance increased.The changes in temperature difference were consistent with the variation in relative humidity difference at the horizontal and vertical direction.