Needless to say this is a task best left to the experts.
Green roof actual evapotranspiration.
Actual evapotranspiration can be achieved by multiplying eto by ks.
Green roofs on campus.
Even though the green roofs might be a quite simple system consisting of several layers all the processes within each layer must be controlled dynamically.
Abstract previous research has shown that most of the green roof benefits are related to the cooling effect.
One truly cannot design a green roof without fully understanding the annual water balance and evapotranspiration rates of the plant palette in the making of green roof design.
Simpler equations have been applied to green roof such as the thornthwaite mather version neglecting the rooting depth and moisture stress or the soil moisture extraction function smef that further removes the restriction of wilting point 59 74 93 97.
In the literature available however it is still not clear how and how much the evapotranspiration affects the performance of a green roof.
If it s hot and windy the roof dries faster than if it s cool and still.
Considering that the sun can account for about 95 of the excess heat coming in through a roof evapotranspiration alone would lower the temperature of a typical extensive green roof by only a few degrees and leave us with a bunch of fried sedum.
Green roof is one of the emerging lid technologies used for retaining rainfall volume and attenuating storm runoff peak flows.
Green roofs reduce storm water runoff through soil moisture retention and evapotranspiration berndtsson et al.
The plants in a green roof absorb water through their roots and then use surrounding heat from the air to evaporate the water while some roofs can reach temperatures of up to 90 f in the summertime these two features can allow green roofs to actually be cooler than the surrounding air temperature.
She pang 2010.
Evaporation is the loss of water from any old surface such as leaves and stems soil particles or debris.
Evapotranspiration drives water requirements and hence irrigation scheduling and is the driver of retention.
After irrigation there was a substantial increase in latent heat flux for both green roof and bare soil.
2013 the higher latent heat flux on soil with maximum value about 280 w m 2 compared to green roof with maximum value about 210 w m 2 suggested that wet soil freely evaporated while evapotranspiration from the green roof was limited by the lower surface temperatures and water uptake by vegetation.
Wind speed matters as it stirs up the so called boundary layer allowing water molecules to leave the surface as vapor.
On a green roof it s the same.
