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9th International Conference on Urban Climate 12th Symposium on the Urban Environment An automatic GIS procedure to calculate urban densities to use in Urban Climatic Maps Ezequiel Correia 1 ,António Lopes 1 ; David Marques 1 1 Center of Geographical Studies, Institute of Geography and Spatial Planning, Universidade de Lisboa, Portugal e-mail: [email protected] Urban Climatic Maps (UCMaps), are important and recognized tools to attain a reliable urban management. Among several features included in UCMaps, urban density is one of the most important variables to consider, due to its effect of urban volumes on radiative and energy balances and on natural ventilation. However, this key factor to urban climate analysis is very often unavailable or not suitable for urban climate studies and its determination becomes a very time consuming task and difficult to carry out. In order to get urban density maps, a methodology developed with a GIS environment is presented, applied to Lisbon. Buildings geometry and volumetric parameters have been automatically computed as indicators of urban density and morphology. With a GIS, the urban area is divided into cells. For the densities calculation, each cell will take into account the height of buildings, the surface area and volume, the width of the streets and the area exposed to the prevailing wind (it is also possible to consider other directions). The aerodynamic roughness (z0) inside each cell will be also considered in the automation process. POSTER 12: GD – Local Climates Zones and urban databases UCMAPS - DATA AND METHODOLOGY Homogeneous climate- response units (climatopes) Urban morphology and other urban features Ventilation classes Terrain (relief) units Aerodinamic Roughness (z 0 ) Land cover maps Municipal information (3D buildings, streets, parks, other) DTM URBAN DENSITY Clustering Urban roughness Volumetric index H/W factor GIS PROCEDURES AND SQL STATEMENTS I – URBAN ROUGHNESS A – FACADE PARAMETERS MORPHOMETRIC METHOD Roughness length (z 0 ) = 0.5h x s/S (Lettau, 1969) A.1 – BUILD REGULAR BLOCK BUILDINGS Buildings Block buildings Regular block buildings # 54924 vector-based buildings database # 15357 vector-based block buildings database 20 m parallel lines perpendicular to the prevailing wind = Buildings windward cross section A.2 – CALCULATE BUILDINGS WINDWARD CROSS SECTION IN EACH CELL For each cross section: csh – block height (average of buildings height) csl – length of cross section MINIMUM BOUND GEOMETRY GENERALIZATION Data: Shapefiles with: Buildings (height; footprint area; volume) Streets (width) Resources: ArcGis™, MSAccess®, Excel®, SPSS® Sources: Municipality of Lisbon European Environmental Agency - Urban Atlas B – CALCULATE: SQL _(database) : ALONG each line, SUM cross section length FOR each cell, SELECT the greatest cross section sum Parameters obtained along select line: h – mean buildings height lf – sum of facade length S – cell area s – frontal area Validation Cell size effect Applied in Cascais municipality Lopes & Correia (2012) z 0 = 0.5h x s/S WINDWARD FRONTAL AREA URBAN ROUGHNESS Lisbon urban roughness II – VOLUMETRIC INDEX … but this concept doesn’t include the real volume of the Urban Boundary Layer Volumetric coefficient (VC) = Vc / Ac Vc – Cell volume Ac – Cell area Volumetric index (VI) = Vc / BVc Vc – Cell volume BVc – Average buildings volume Lisbon volumetric index our proposal III – H/W FACTOR Buildings heights Roads width + 4m (walkways) H V = URBAN DENSITY CLUSTER ANALYSIS - K-MEANS This methodology will allow us to speed up the process of creating bioclimatic indicators that can be use in applied urban climate studies. References: Alcoforado, M-J., H. Andrade, A. Lopes, J. Vasconcelos (2009) Application of Climatic Guidelines to Urban Planning. The Example of Lisbon (Portugal). Landscape and Urban Planning, 90:56-65. Alcoforado, M.J., H. Andrade, A. Lopes (2012) - Urban Climate Maps in Lisbon, Portugal. in C. Ren e Y-y Ng (ed.) – Urban Climatic Map – An Information Tool for Sustainable Urban Planning, Hong Kong. (chinese version). Alcoforado MJ, A. Lopes, H. Andrade (2015) Chapter 16. Urban Climatic Map Studies in Portugal: Lisbon. In Ng E, Ren C, The Urban Climatic Map. A Methodology for Sustainable Urban Planning. Routledge. (in press) Lopes A., E. Correia (2012) A Proposal to Enhance Urban Climate Maps with the Assessment of the Wind Power Potential. The Case of Cascais Municipality (Portugal). in Lenka Hájková et al Ed., Conference Proceedings, International Scientific Conference “Bioclimate 2012 Bioclimatology of Ecosystems, Ústí nad Labem, Rép. Checa: 68-69 Prata-Shimomura A, A. Lopes, E. Correia (2015) Chapter 17. Urban Climatic Map Studies in Brazil: Campinas In Ng E, Ren C, The Urban Climatic Map. A Methodology for Sustainable Urban Planning. Routledge. (in press) Most commonly used K Z0 IV HW N % Z0 IV HW Density 1 0.2 0.5 0.6 3029 51.2 -- +/- +/- Low 2 5.1 0.7 2.4 102 1.7 ++ + ++ High 3 0.6 2.9 0.9 623 10.5 +/- ++ + Medium 4 18.5 0.3 1.5 1 0.0 ++ - ++ High 5 0.7 0.9 1.4 1542 26.1 + + ++ Medium 6 2.1 0.8 1.8 617 10.4 ++ + ++ High

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Page 1: An automatic GIS procedure to calculate urban densities to ... · An automatic GIS procedure to calculate urban densities to use in Urban Climatic Maps Ezequiel Correia1,António

9th International Conference on Urban Climate12th Symposium on the Urban Environment

An automatic GIS procedure to calculate urban densities to use in Urban Climatic Maps

Ezequiel Correia1,António Lopes1; David Marques1

1 Center of Geographical Studies, Institute of Geography and Spatial Planning, Universidade de Lisboa, Portugale-mail: [email protected]

Urban Climatic Maps (UCMaps), are important and recognized tools to attain a reliable urbanmanagement. Among several features included in UCMaps, urban density is one of the mostimportant variables to consider, due to its effect of urban volumes on radiative and energy balancesand on natural ventilation. However, this key factor to urban climate analysis is very oftenunavailable or not suitable for urban climate studies and its determination becomes a very timeconsuming task and difficult to carry out.

In order to get urban density maps, a methodology developed with a GIS environment is presented,applied to Lisbon.

Buildings geometry and volumetric parameters have been automatically computed as indicators ofurban density and morphology. With a GIS, the urban area is divided into cells. For the densitiescalculation, each cell will take into account the height of buildings, the surface area and volume,the width of the streets and the area exposed to the prevailing wind (it is also possible to considerother directions). The aerodynamic roughness (z0) inside each cell will be also considered in theautomation process.

POSTER 12: GD – Local Climates Zones and urban databases

UCMAPS - DATA AND METHODOLOGY

Homogeneous climate-response units (climatopes)

Urban morphology and other urban features

Ventilation classes

Terrain (relief) units

AerodinamicRoughness (z0)

Land cover maps Municipal information

(3D buildings, streets, parks, other)

DTM

URBAN DENSITY Clustering

Urban roughness

Volumetric index

H/W factor

GIS P

RO

CED

UR

ES AN

D SQ

L STATEM

ENTS

I – URBAN ROUGHNESS

A – FACADE PARAMETERS

MORPHOMETRIC METHODRoughness length (z0) = 0.5h x s/S (Lettau, 1969)

A.1 – BUILD REGULAR BLOCK BUILDINGS

Buildings Block buildings Regular block buildings

# 54924 vector-basedbuildings database

# 15357 vector-basedblock buildings database

20 m parallel lines perpendicular to the prevailing wind

=

Buildings windward cross section

A.2 – CALCULATE BUILDINGS WINDWARD CROSS SECTION IN EACH CELL

For each cross section:csh – block height (average of buildings height)csl – length of cross section

MINIMUM BOUND GEOMETRYGENERALIZATION

Data:Shapefiles with:Buildings (height; footprint area; volume)Streets (width)

Resources: ArcGis™, MSAccess®, Excel®, SPSS®Sources:

Municipality of LisbonEuropean Environmental Agency - Urban Atlas

B – CALCULATE:

SQL _(database) : • ALONG each line, SUM cross section length• FOR each cell, SELECT the greatest cross section

sum

Parameters obtained along select line:h – mean buildings heightlf – sum of facade length

S – cell area

s – frontal area

Validation

Cell size effect

Applied in Cascais municipalityLopes & Correia (2012)

z0= 0.5h x s/S

• WINDWARD FRONTAL AREA• URBAN ROUGHNESS

Lisbon urban roughness

II – VOLUMETRIC INDEX

… but this conceptdoesn’t include the real

volume of the Urban Boundary Layer

Volumetric coefficient (VC) = Vc / AcVc – Cell volumeAc – Cell area

Volumetric index (VI) = Vc / BVcVc – Cell volumeBVc – Average buildings volume Lisbon volumetric index

our proposal

III – H/W FACTOR

Buildings heights

Roads width + 4m (walkways)

H

V

=

URBAN DENSITY

CLUSTER ANALYSIS - K-MEANS

This methodology will allow usto speed up the process ofcreating bioclimatic indicatorsthat can be use in appliedurban climate studies.

References:Alcoforado, M-J., H. Andrade, A. Lopes, J. Vasconcelos (2009) Application of Climatic Guidelines to Urban Planning. The Example of Lisbon (Portugal). Landscape and Urban Planning, 90:56-65.Alcoforado, M.J., H. Andrade, A. Lopes (2012) - Urban Climate Maps in Lisbon, Portugal. in C. Ren e Y-y Ng (ed.) –Urban Climatic Map – An Information Tool for Sustainable Urban Planning, Hong Kong. (chinese version).Alcoforado MJ, A. Lopes, H. Andrade (2015) Chapter 16. Urban Climatic Map Studies in Portugal: Lisbon. In Ng E, RenC, The Urban Climatic Map. A Methodology for Sustainable Urban Planning. Routledge. (in press)Lopes A., E. Correia (2012) A Proposal to Enhance Urban Climate Maps with the Assessment of the WindPower Potential. The Case of Cascais Municipality (Portugal). in Lenka Hájková et al Ed., Conference Proceedings, International Scientific Conference “Bioclimate 2012 – Bioclimatology of Ecosystems, Ústí nadLabem, Rép. Checa: 68-69Prata-Shimomura A, A. Lopes, E. Correia (2015) Chapter 17. Urban Climatic Map Studies in Brazil: Campinas In Ng E, Ren C, The Urban Climatic Map. A Methodology for Sustainable Urban Planning. Routledge. (in press)

Most commonly used

K Z0 IV HW N % Z0 IV HW Density

1 0.2 0.5 0.6 3029 51.2 -- +/- +/- Low

2 5.1 0.7 2.4 102 1.7 ++ + ++ High

3 0.6 2.9 0.9 623 10.5 +/- ++ + Medium

4 18.5 0.3 1.5 1 0.0 ++ - ++ High

5 0.7 0.9 1.4 1542 26.1 + + ++ Medium

6 2.1 0.8 1.8 617 10.4 ++ + ++ High