Unterschiede
Hier werden die Unterschiede zwischen zwei Versionen angezeigt.
| Beide Seiten der vorigen Revision Vorhergehende Überarbeitung | Letzte ÜberarbeitungBeide Seiten der Revision | ||
| thesis:etvar [2016/01/26 21:01] – m.koelbing | thesis:etvar [2016/01/27 07:19] – schuetz | ||
|---|---|---|---|
| Zeile 2: | Zeile 2: | ||
| == Problem == | == Problem == | ||
| - | The heterogeneity of urban surfaces including buildings and vegetation causes high variability of micrometeorological variables on small spatial scales which makes it hard to observe or even predict climate conditions and in particular evapotranspiration with high resolution on the scale of entire cities. Regarding future climate changes and their impacts on urban climate and hydrology, the predictability of these small scale variations becomes more and more relevant for e.g. urban planners to improve the development of appropriate mitigation strategies. Therefore, new transfer functions for meteorological variables are needed, which consider the structural variability in urban areas and its impacts on the energy balance (shading effects, ventilation, | + | The heterogeneity of urban surfaces including buildings and vegetation causes high variability of micrometeorological variables on small spatial scales which makes it hard to observe or even predict climate conditions and in particular evapotranspiration with high resolution on the scale of entire cities. Regarding future climate changes and their impacts on urban climate and hydrology, the predictability of these small scale variations becomes more and more relevant for e.g. urban planners to improve the development of appropriate mitigation strategies. Therefore, new transfer functions for meteorological variables are needed, which consider the structural variability in urban areas and its impacts on the energy balance (shading effects, ventilation, |
| == Goal of the thesis | == Goal of the thesis | ||