Human thermal comfort in Local climate zones of Berlin
- 1Ines Langer, Freie Universität Berlin, Institute of Meteorology, Berlin, Germany (ines.langer@met.fu-berlin.de)
- 2Alexander Pasternack, Freie Universität Berlin, Institute of Meteorology, Berlin, Germany (Alexander.Pasternack@met.fu-berlin.de)
- 3Uwe Ulbrich, Freie Universität Berlin, Institute of Meteorology, Berlin, Germany (ulbrich@met.fu-berlin.de)
Urban areas show higher nocturnal temperature comparing to rural areas, which is denoted by urban heat island. This effect can intensify the impact of global warming in urban areas especially during heat waves, that leads to higher energy demand for cooling the building and higher thermal stress for residents.
The aim of this study is to identify the Urban Heat Island (UHI) effect during the heat spell 2018 and 2019 in order to calculated human thermal comfort for Berlin. Berlin, the capital city of Germany covers an area of 892km2 and its population is growing, therefore more residential areas will be planned in future through higher building. The methodology of this research is to divide Berlin into Local Climate Zones (LCZ's) regarding the concept of Stewart & Oke (2012). Then to evaluate the accuracy of this concept using 30 microclimate stations. Estimating the magnitude of urban heat island and its seasonal changes in combination with human thermal perception in different LCZ during summer time is another objective of this research.
Ten LCZ's for Berlin were selected, as class 1 (compact high rise), class 3 (compact low rise), class 7 (lightweight low-rise), class C (bush, scrub), class E (bare rock or paved) and class F (bare soil or sand) don't exist in Berlin. Class A (dense trees) is with a fraction of 18.6% in a good agreement with the percentage of dense trees reported from the city administration of Berlin (18.4%), class G (water) has a coverage of 5.1% through our classification instead of 6.7% reported by the city administration. In summary, the LCZ 1-10 cover 59.3% (more than half) of the city area.
Regarding temperature measurements, which represent a hot summer day with calm wind and clear sky the difference of Local Climate Zones will be calculated and the temperature variability in every LCZ's regarding sky view factor values show the hot spot of the city.
The vulnerability of LCZ's to heat stress will be ranked and discussed regarding ventilation and other factors.
Literature
Matzarakis, A. Mayer, H., Iziomon, M. (1999) Applications of a universal thermal index: Physiological equivalent temperature: Intern. J. of Biomet 43 (2), 76-84.
Stewart, I.D., Oke, T.R. (2012) Local climate zones for urban temperature studies. Bull. Amer. Meteor. Soc. 93 1879-1900. DOI: 10.1175/BAMS-D-11-00019.1.
How to cite: Langer, I., Pasternack, A., and Ulbrich, U.: Human thermal comfort in Local climate zones of Berlin, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7741, https://doi.org/10.5194/egusphere-egu2020-7741, 2020
