H21J-1531
Advantages of a Vertical High-Resolution Distributed-Temperature-Sensing System Used to Evaluate the Thermal Behavior of Green Roofs

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Francisco I Suarez1, Jose Antonio Cousiño1,2, Mark B Hausner2,3, Felipe Victorero1, Carlos A Bonilla4, Jorge A Gironas1, Sergio Vera2, Waldo Bustamante2, Victoria Rojas5, Eduardo Leiva1,2 and Pablo Pasten6, (1)Pontifical Catholic University of Chile, Santiago, Chile, (2)CEDEUS, Santiago, Chile, (3)Desert Research Institute Las Vegas, Las Vegas, NV, United States, (4)Pontificia Universidad Catolica de Chile, Santiago, Chile, (5)VR+ARQ, Santiago, Chile, (6)Centro de Desarrollo Urbano Sustentable, Santiago, Chile
Abstract:
Technological innovations used for sustainable urban development, green roofs offer a range of benefits, including reduced heat island effect, rooftop runoff, roof surface temperatures, energy consumption, and noise levels inside buildings, as well as increased urban biodiversity. Green roofs feature layered construction, with the most important layers being the vegetation and the substrate layers located above the traditional roof. These layers provide both insulation and warm season cooling by latent heat flux, reducing the thermal load to the building. To understand and improve the processes driving this thermal energy reduction, it is important to observe the thermal dynamics of a green roof at the appropriate spatial and temporal scales.

Traditionally, to observe the thermal behavior of green roofs, a series of thermocouples have been installed at discrete depths within the layers of the roof. Here, we present a vertical high-resolution distributed-temperature-sensing (DTS) system installed in different green roof modules of the Laboratory of Vegetated Infrastructure for Buildings (LIVE –its acronym in Spanish) of the Pontifical Catholic University of Chile. This DTS system allows near-continuous measurement of the thermal profile at spatial and temporal resolutions of approximately 1 cm and 30 s, respectively. In this investigation, the temperature observations from the DTS system are compared with the measurements of a series of thermocouples installed in the green roofs. This comparison makes it possible to assess the value of thermal observations at better spatial and temporal resolutions. We show that the errors associated with lower resolution observations (i.e., from the thermocouples) are propagated in the calculations of the heat fluxes through the different layers of the green roof. Our results highlight the value of having a vertical high-resolution DTS system to observe the thermal dynamics in green roofs.