THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO

Alteration of climatic conditions and the urban heat island effect (UHI) are consequences of increased human population and activities in urban zones. Determining the magnitude of the UHI is important to improve urban planning in medium-size cities like Querétaro. Increase and conservation of vegeta...

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Authors: Colunga, Maria L.; Cambrón-Sandoval, Víctor Hugo; Suzán-Azpiri, Humberto; Guevara-Escobar, Aurelio; Luna-Soria, Hugo
Format: Article
Status:Published version
Publication date:2015
Country:México
Institution:UNAM
Repository:Atmósfera
Language:English
OAI Identifier:oai:ojs.pkp.sfu.ca:article/43365
Online Access:https://www.revistascca.unam.mx/atm/index.php/atm/article/view/ATM.2015.28.03.05
Access Level:Open access
Keyword:Climate change
urban heat island effect
urban planning
Querétaro
vegetation.
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author Colunga, Maria L.
author2 Cambrón-Sandoval, Víctor Hugo
Suzán-Azpiri, Humberto
Guevara-Escobar, Aurelio
Luna-Soria, Hugo
author2_role author
author
author
author
author_browse Cambrón-Sandoval, Víctor Hugo
Colunga, Maria L.
Guevara-Escobar, Aurelio
Luna-Soria, Hugo
Suzán-Azpiri, Humberto
author_facet Colunga, Maria L.
Cambrón-Sandoval, Víctor Hugo
Suzán-Azpiri, Humberto
Guevara-Escobar, Aurelio
Luna-Soria, Hugo
author_role author
collection Atmósfera
description Alteration of climatic conditions and the urban heat island effect (UHI) are consequences of increased human population and activities in urban zones. Determining the magnitude of the UHI is important to improve urban planning in medium-size cities like Querétaro. Increase and conservation of vegetated areas is a mitigation option for UHI. Here we characterized both the UHI and the role of vegetation cover over temperature regularization in urban zones. Four local climatic zones were defined: three urban and one rural, each with two plots with low and high canopy cover defined by their average leaf area index (0.5 and 2.0, respectively). Air temperature and relative humidity were measured with data loggers at a 30 min time step from June 2012 to May 2013. Climatic data from six weather stations was also analyzed. Daily mean temperature increased at a rate of 0.75 ºC per decade (r2 = 0.38, P < 0.0001), and this was related to population dynamics (r2 = 0.52, P < 0.0001). Patterns of air temperature defined a cold and a warm season: July to March and April to June for maximum temperature, and November to March and April to October for minimum temperature. The difference between cold and warm seasons was 5 ºC (P < 0.0001). The minimum temperature was similar between canopy cover levels. However, relative humidity was higher in high canopy cover plots. The relationship between UHI and the pervious surface fraction of the city was inversely proportional. The UHI ranged from 0.1 to 5 ºC and this magnitude was similar between the warm and cold seasons. Vegetation with high canopy cover had lower temperature at 17:00 LT and higher at 9:00 to 10:00 LT during the warm season. Increasing the urban zone canopy cover by 50% would reduce the UHI by 2.05 ºC. In conclusion, vegetation with higher canopy cover improved environmental conditions in terms of relative humidity and regularization of extreme temperatures during the warm season. 
eu_rights_str_mv openAccess
format article
id MX_b734db01115e0b53e8e338019bc6a708
identifier_str_mv 10.20937/ATM.2015.28.03.05
institution UNAM
instname_str UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
language eng
network_acronym_str MX
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oai_identifier_str oai:ojs.pkp.sfu.ca:article/43365
publishDate 2015
publishDateSort 2015
publisher Instituto de Ciencias de la Atmósfera y Cambio Climático, Universidad Nacional Autónoma de México
publisherStr Instituto de Ciencias de la Atmósfera y Cambio Climático, Universidad Nacional Autónoma de México
reponame_str Atmósfera
spelling THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO Colunga, Maria L. Cambrón-Sandoval, Víctor Hugo Suzán-Azpiri, Humberto Guevara-Escobar, Aurelio Luna-Soria, Hugo Climate change urban heat island effect urban planning Querétaro vegetation. Alteration of climatic conditions and the urban heat island effect (UHI) are consequences of increased human population and activities in urban zones. Determining the magnitude of the UHI is important to improve urban planning in medium-size cities like Querétaro. Increase and conservation of vegetated areas is a mitigation option for UHI. Here we characterized both the UHI and the role of vegetation cover over temperature regularization in urban zones. Four local climatic zones were defined: three urban and one rural, each with two plots with low and high canopy cover defined by their average leaf area index (0.5 and 2.0, respectively). Air temperature and relative humidity were measured with data loggers at a 30 min time step from June 2012 to May 2013. Climatic data from six weather stations was also analyzed. Daily mean temperature increased at a rate of 0.75 ºC per decade (r2 = 0.38, P < 0.0001), and this was related to population dynamics (r2 = 0.52, P < 0.0001). Patterns of air temperature defined a cold and a warm season: July to March and April to June for maximum temperature, and November to March and April to October for minimum temperature. The difference between cold and warm seasons was 5 ºC (P < 0.0001). The minimum temperature was similar between canopy cover levels. However, relative humidity was higher in high canopy cover plots. The relationship between UHI and the pervious surface fraction of the city was inversely proportional. The UHI ranged from 0.1 to 5 ºC and this magnitude was similar between the warm and cold seasons. Vegetation with high canopy cover had lower temperature at 17:00 LT and higher at 9:00 to 10:00 LT during the warm season. Increasing the urban zone canopy cover by 50% would reduce the UHI by 2.05 ºC. In conclusion, vegetation with higher canopy cover improved environmental conditions in terms of relative humidity and regularization of extreme temperatures during the warm season.  Instituto de Ciencias de la Atmósfera y Cambio Climático, Universidad Nacional Autónoma de México https://www.revistascca.unam.mx/atm/index.php/atm/article/view/ATM.2015.28.03.05 10.20937/ATM.2015.28.03.05
spellingShingle THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
Colunga, Maria L.
Climate change
urban heat island effect
urban planning
Querétaro
vegetation.
status_str publishedVersion
title THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
title_full THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
title_fullStr THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
title_full_unstemmed THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
title_short THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
title_sort THE ROLE OF URBAN VEGETATION IN TEMPERATURE AND HEAT ISLAND EFFECTS IN QUERÉTARO CITY, MEXICO
topic Climate change
urban heat island effect
urban planning
Querétaro
vegetation.
topic_facet Climate change
urban heat island effect
urban planning
Querétaro
vegetation.
url https://www.revistascca.unam.mx/atm/index.php/atm/article/view/ATM.2015.28.03.05