klimatanpassad urban design Erik Johansson Boende och Bostadsutveckling



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Urbant Uba klimat at& klimatanpassad urban design Erik Johansson Boende och Bostadsutveckling

Urbant klimat & klimatanpassad urban design Urbant klimat Temperatur Vind Exempel Fez (Marocko) Colombo (Sri Lanka) Inverkan av urbana normer

Global, regional and local climate phenomena

Urban climate Source: Boundary Layer Climates by T R Oke

Urban microclimate

Characteristics of the urban climate Mean air temperature Pollution Cloudiness Solar radiation Mean wind speed Turbulence 1-3 C warmer (occasionally up to 12 C) 10-25% higher concentrations 5-10% more 5-25% less 20 50% of rural wind speed 10 50% greater

Värmeön (the Urban Heat Island) Source: Boundary Layer Climates by TROk Oke

Värmeön (the Urban Heat Island) Source: Boundary Layer Climates by T R Oke

Temperaturvariationer för stad och landsbygd Fuente: Boundary Layer Climates por T R Oke

Maximum heat island effect 3 5 hours after sunset Calm weather Cloudless skies

Causes of the urban heat island Geometry of the built environment Thermal properties of building materials Heat from traffic, buildings etc Lack of vegetation Air pollution

Radiation balance day Urban

Radiation balance night

H/W ratio sky view factor Sky View Factor (SVF) = cos

Heat island as a function of H/W Source: Boundary Layer Climates by T R Oke

Surface material properties Reflection Thermal capacity (MJ/m3 C) Dry soil 0.4 1.3 Humid soil 0.05 3.0 Grass 015025 0.15-0.25 -- Asphalt 0.05 0.20 1.9 Concrete 0.10 0.35 2.1

Andra orsaker till värmeön Värme från trafik, byggnader Brist på vegetation Luftföroreningar

Effect of water bodies Large water bodies (seas, big lakes and rivers) may cause cooling through the sea breeze effect Smaller water bodies may cause cooling through evaporation

Parker och grönområden Lägre temperatur på grund av skuggning och evapotranspiration Större parker kan vara 1 4ºC svalare än omgivande bebyggelseb Fler träd ger större effekt Parkens klimat på- verkar angränsande bebyggda områden 21

Fördelar med vegetation Ger skugga Evapotranspiration medför temperatursänkning Absorberar regnvatten Vindskydd (viktigt under kalla årstider) Filtrerar luftföroreningar Biologisk mångfald Estetiskt tilltalande Motverkar stress 22

Effect of shading trees Protection against direct solar radiation Less reflected radiation Lower surface temperatures

Permeable surfaces Increased infiltration Increased evaporation (cooling) 27 jan-10 Erik Johansson, HDM 24

Wind in urban areas

Wind data Urban winds 25-50% of rural wind speeds 27 jan-10 Erik Johansson, HDM 26

Urban wind more turbulent

Wind in urban areas Source: Boundary Layer Climates by T R Oke

Wind: effect of highrise h i buildings Source: Boundary Layer Climates by T R Oke

Point Hyllie, Malmö (30 våningar)

Scandinavian Tower, Hyllie (17 våningar) Hotell, Västra Hamnen, Malmö (85 m)

Exempel på problem i kallt klimat Vindproblem vid höga byggnader Raka gator

Ways to reduce wind speeds near high-rise buildings Use of podium

Increased wind speeds between buildings funnel effect High Higher Highest

Urban climate field studies Fez Colombo Fez, Morocco: Colombo, Sri Lanka: 1 million inhab. 1.4 million inhab.

Methods 1. Microclimate measurements and calculation of thermal comfort 2. Simulations of how urban design influences microclimate and comfort 3. Analysis of urban regulations and interviews with urban planners and designers

Climate measurements in street canyons Air and surface temperatures Humidity Wind speed H W

Calculation of outdoor thermal comfort Air temperature Physiologically i ll Mean radiant Equivalent temperature Temperature (PET) Humidity Wind Assumed upper comfort limit: PET = 33 C Assumed lower comfort limit: PET = 18 C

Climate of Fez, Morocco 40 Temp. ( C) Max. temp. Min. temp 30 20 10 0 J F M A M J J A S O N D Month Relative humidity: 40 70%

Measurement sites Fez

Plot coverage of the neighbourhoods Compact, traditional Dispersed, modern (deep canyon) (shallow canyon)

Measured air temperature in Fez Summer C 38 36 34 32 30 28 26 24 22 20 18 Old city New city Rural Height/Width ratio: Old city 10 New City 0.6 16 00:00 06:00 12:00 18:00 24:00

Measured air temperature in Fez Winter C 18 Old city 16 New city 14 Rural Height/Width ratio: Old city 10 12 10 8 New City 0.6 6 4 00:00 03:0000 06:0000 09:0000 12:00 15:00 18:00 21:00 24:00

PET fysiologiskt ekvivalenta temperaturen PET inkluderar kyleffekt från vinden och värmetillskott från solstrålning. Temp. Solförhållanden Vindförhållanden d PET 20 C molnigt vindstilla 20 C 20 C soligt vindstilla 30 C 20 C molnigt blåsigt 10 C

Comfort comparison Summer (PET) C 50 45 Old city New city 40 35 30 25 20 15 00:00 06:00 12:00 18:00 00:00

Comfort comparison Winter (PET) C 25 20 Deep Shallow 15 10 5 0 00:00 06:00 12:00 18:00 00:00

Conclusion from measurements in Fez Urban areas were found to be both warmer (heat island) and cooler (cool island) than the rural surroundings There are big variations in thermal comfort within the city, both in summer and winter

Climate of Colombo Temp. ( C) 40 Temp. max Temp. min 30 20 10 0 J F M A M J J A S O N D Month Relative humidity: 75 90%

Measurement sites: Colombo

C Day 38 36 34 32 30 Measured air temperature, Colombo 28 26 24 07:00 10:00 13:00 16:00 19:00 C Night 32 30 28 26 24 20:00 23:00 02:00 05:00 C 38CBD - high rise 36 34Old city (dense) 32 30Centre - big avenue 28 26Suburb (inland) 24 07:00 10:00 13:00 16:00 19:00 Rural

Sea breeze Sunny afternoons Erik Johansson, HDM 52

Results from measurements in Colombo Large climate variations within the city Max. PET decreases with increasing height-to-width (H/W) ratio of urban canyons Lower PET near the coast due to the sea- breeze Lower PET under colonnades and shading trees

Results from interviews Climate is rarely considered in urban planning and ddesign Lack of knowledge about climate-conscious design Lack of tools and guidelines

Current urban codes in Fez and Colombo Introduced during the colonial time Based on principles from western countries low density to encourage solar access and fresh air as well as daylight in buildings

Lack of shade for pedestrians Wide streets Low buildings No shade trees, arcades or other overhead shading

How to promote a climate- conscious urban design Improvements of urban codes: Allow higher H/W ratios Allow ventilation around buildings (hot humid) Prescriptions for shading Development of design guidelines Training of urban planners/designers in climate-conscious design Development of design tools