Tagungsband - Fachvereinigung Bauwerksbegrünung eV

6. FBB-Symposium Fassadenbegrünung 2013 in Frankfurt a.M. am 19.09.2013
Heß, D., 2008: Pflanzenphysiologie. Grundlagen der Physiologie und Biotechnologie der Pflanzen.
11. Aufl., Ulmer: Stuttgart, 415 S.
Imhoff, M.L., Zhang, P., Wolfe, R.E. & L. Bounoua, 2010: Remote sensing of the urban heat island
effect across biomes in the continental USA. Remote Sensing of Environment 114 (3): 504–513.
Lindroth, A., Čermák, J., Kučera, J., Cienciala, E. & H. Eckersten, 1995: Sap flow by the heatbalance
method applied to small-size salix trees in a short rotation forest. Biomass and Bioenergy
8: 7-15.
Lougeay, R., Brazel, A. & M. Hubble, 1996: Monitoring intra-urban temperature patterns and
associated land cover in Phoenix, Arizona using landsat thermal data. Geocarto International 11
(4): 79-90.
Montávez, J.P., González-Rouco, J.F. & F. Valero, 2008: A simple model for estimating the
maximum intensity of nocturnal urban heat island. International Journal of Climatology 28: 235-242.
Mayer H. & P. Höppe, 1987: Thermal comfort of man in different urban environments. Theoretical
and Applied Climatology 38 (1): 43-49.
Pérez, G., Rincón, L., Vila, A., González, J.M. & L.F. Cabeza, 2011: Green vertical systems for
buildings as passive systems for energy savings. Applied Energy 88: 4854-4859.
Sham, J.F.C., Lo, T.Y. & S.A. Memon, 2012: Verification and application of continuous surface
temperature monitoring technique for investigation of nocturnal sensible heat release
characteristics by building fabrics. Energy and Buildings 53: 108-116.
Takebayashi, H. & M. Moriyama, 2007: Surface heat budget on green roof and high reflection roof
for mitigation of urban heat island. Building and Environment 42: 2971–2979.
Wang, L. & H.-Q. Xu, 2008: Study on the information extraction of evapotranspiration and its
relation with the urban heat island and urban expansion in Fuzhou City with its surrounding areas
of SE China. 2008 International Workshop on Earth Observation and Remote Sensing Applications
(EORSA): 6 S.
Abbildungen
0,50
Kumulative Wägung (l/m²
Blattfläche)
0,40
0,30
0,20
0,10
1:1 Linie
0,00
0,00 0,10 0,20 0,30
Kumulativer Saftfluss (l/m² Blattfläche)
Abb.1 Mittlerer kumulativer Tagesgang über 14 Tage von Saftfluss und Wägung im Vergleich.
12