1997
DOI: 10.1016/s1350-4495(97)00020-0
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A heat balance model for partially vegetated surfaces

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Cited by 15 publications
(3 citation statements)
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“…The ozone in the atmosphere is mainly concentrated at an altitude of 20-50 km, and the content of methane is low. Therefore, water vapor and carbon dioxide are dominant in the absorption of infrared radiation in the troposphere [26]. Generally, the amount of water vapor in the atmosphere is expressed by the amount of precipitation.…”
Section: Absorption Of H2o Moleculesmentioning
confidence: 99%
“…The ozone in the atmosphere is mainly concentrated at an altitude of 20-50 km, and the content of methane is low. Therefore, water vapor and carbon dioxide are dominant in the absorption of infrared radiation in the troposphere [26]. Generally, the amount of water vapor in the atmosphere is expressed by the amount of precipitation.…”
Section: Absorption Of H2o Moleculesmentioning
confidence: 99%
“…where the term in the right is the energy stored in the green façade (leaves and branches), usually neglected (Zhang et al, 1997), L f is the latent heat (estimated in the next section), and qrad is the infrared net flux between the green façade and the surrounding surfaces given by:…”
Section: Energy Balance Of a Green Wallmentioning
confidence: 99%
“…Several mathematical models of ground vegetation canopy were developed in the field of climatology (Deardorff, 1978;Zhang, 1997) and were later adapted to simulate the thermal effects of plants in green roofs (Alexandri, 2007;Djedjig, 2012;Sailor, 2008). Such models should be able to dynamically simulate the effect of plants on the facade thermal performance for variable plant characteristics, facade properties, building orientations, and weather conditions.…”
Section: Building Energy Savings With Vegetated Facadesmentioning
confidence: 99%