URBAN CLIMATE RESEARCH IN NOVI SAD (SERBIA) Erasmus+ lecture at the Department of Geography, Masaryk University (Brno, Czech Republic) March, 27-31, 2017 dr Stevan Savić, associate professor Climatology and Hydrology Researcher Centre, Faculty of Sciences, University of Novi Sad, Serbia stevan.savic@dgt.uns.ac.rs internet portal: clihyd.com Brno, Czech Republic, 2017 Built-up and UHI patterns in Novi Sad Local Climate Zones (LCZ) The advantages of LCZ system are that it is a global classification scheme, with limited number of classes and the classes are separated by the main thermal characteristic of the urban surface. Table of LCZ classification made by Stewart and Oke 2012 (Bull. Am. Meteorol. Soc., 93, 1879-1900) Built types Land cover types Variable land cover properties LCZ 1 – Compact high-rise LCZ 2 – Compact midrise LCZ 3 – Compact low-rise LCZ 4 – Open high-rise LCZ 5 – Open midrise LCZ 6 – Open low-rise LCZ 7 – Lightweight low-rise LCZ 8 – Large low-rise LCZ 9 – Sparsely built LCZ 10 – Heavy industry LCZ A – Dense trees LCZ B – Scattered trees LCZ C – Bush, scrub LCZ D – Low plants LCZ E – Bare rock / paved LCZ F – Bare soil / sand LCZ G – Water b – bare trees s – snow cover d – dry ground w – wet ground LCZs and station sites definition methodology Definition of LCZs spatial pattern Building databases 47.000 building (Novi Sad) vector format (shape files) – footprint, height Aerial photographs high resolution, 3-4 spectral band Topographic maps Novi Sad – 1:25.000 Road databases all roads and streets Definition of LCZs spatial pattern Corine Land Cover (CLC) database major land-use types Satellite images RapidEye, 5m resolution, atmospheric correction Definition of LCZs spatial pattern Sky View Factor (SVF) describe the radiation balance of the surface and the speed of the cooling at night Building height Definition of LCZs spatial pattern 0.1 0.15 0.2 0.25 0.3 0.35 0.4 0.45 0.5 0.55 0.6 0.65 0.7 0.75 0.8 0.85 0.9 0.95 Surface albedo describes the short wave radiation reflectance of the surface Definition of LCZs spatial pattern Lot area polygon (a building block and the area belonging to it) aggregation of lot area polygons Definition of LCZs spatial pattern by Stewart and Oke 2012 (Bull. Am. Meteorol. Soc., 93, 1897-1900) Definition of LCZs spatial pattern World Urban Database and Access Portal Tools – WUDAPT using: Google Earth Landsat 7 GIS Saga software Temperature outcomes in Novi Sad Milošević, D., Savić, S., Unger, J., Gál, T. 2015. Urban climate monitoring system suitability for intraurban thermal comfort observations in Novi Sad (Serbia) – with 2014 examples. ICUC9 – 9th International Conference on Urban Climate jointly with 12th Symposium on the Urban Environment, 20th-24th July 2015, Toulouse, France, Extended Abstracts: 6 pp. Lelovics, E., Unger, J., Savić, S., Gál, T., Milošević, D., Gulyás, Á., Marković, V., Arsenović, D., Gál, CV. 2016. Intra-urban temperature observations in two Central European cities: a summer study. Idojaras, 120, 3: 283-300. Temperature outcomes in Novi Sad Milošević, D., Savić, S., Unger, J., Gál, T. 2015. Urban climate monitoring system suitability for intraurban thermal comfort observations in Novi Sad (Serbia) – with 2014 examples. ICUC9 – 9th International Conference on Urban Climate jointly with 12th Symposium on the Urban Environment, 20th-24th July 2015, Toulouse, France, Extended Abstracts: 6 pp. Lelovics, E., Unger, J., Savić, S., Gál, T., Milošević, D., Gulyás, Á., Marković, V., Arsenović, D., Gál, CV. 2016. Intra-urban temperature observations in two Central European cities: a summer study. Idojaras, 120, 3: 283-300. T threshold: 90th perc.  ≥ 24.9°C (01.07.2014-30.06.2015) 26,40 26,60 26,80 27,00 27,20 27,40 27,60 27,80 28,00 28,20 28,40 28,60 LCZ2 LCZ3 LCZ5 LCZ6 LCZ9 LCZ8 A D T threshold: 10th perc.  ≤ 2.3°C (01.07.2014-30.06.2015) -3,00 -2,50 -2,00 -1,50 -1,00 -0,50 0,00 LCZ2 LCZ3 LCZ5 LCZ6 LCZ9 LCZ8 A D www.clihyd.com