O desconforto térmico estival em Lisboa - uma abordagem bioclimática

THE SUMMER THERMAL STRESS IN LISBOA; A BIOCLIMATIC APPROACH. The summer frequency of hot days was studied, in Lisboa/Portela, with daily data from the period 1981/97. We used the Physiological Equivalent Temperature, an index of thermal confort based on the human energy balance, and calculated with...

Full description

Bibliographic Details
Main Author: Henrique Andrade
Format: Article
Language:English
Published: CEG 1998-12-01
Series:Finisterra - Revista Portuguesa de Geografia
Subjects:
Online Access:http://www.ceg.ul.pt/finisterra/numeros/1998-66/66_03.pdf
id doaj-67be25ff947b4e028683393fe5e8d705
record_format Article
spelling doaj-67be25ff947b4e028683393fe5e8d7052021-08-02T18:18:10ZengCEGFinisterra - Revista Portuguesa de Geografia0430-50271998-12-01XXXIII664158O desconforto térmico estival em Lisboa - uma abordagem bioclimáticaHenrique AndradeTHE SUMMER THERMAL STRESS IN LISBOA; A BIOCLIMATIC APPROACH. The summer frequency of hot days was studied, in Lisboa/Portela, with daily data from the period 1981/97. We used the Physiological Equivalent Temperature, an index of thermal confort based on the human energy balance, and calculated with air temperature, vapour pressure, wind speed and mean radiant temperature. It was assumed that mean radiant temperature was equal to air temperature, which is acceptable in the shade. The days were classifiend in two groups: hot days and very hot days, according to the thresholds of PET of 29ºC and 35ºC; 10% of the days had warm stress, with a maximum of frequency in July and a great interanual variability. The relation between the thermal discomfort and the wind regime was analysed. Most of the unconfortable days had breeze conditions, with the wind blowing from the East (from the estuary) during the morning; in the afternoon, the barometric gradient between the Ocean and the Iberian Peninsula increases, the breeze is replaced by a week northerly wind. The frequent occurence of strong northerly winds in summer is an important factor of reduction of the warm stress in Lisbonhttp://www.ceg.ul.pt/finisterra/numeros/1998-66/66_03.pdfLisbonthermal conforthuman energy balancePhysiological Equivalent Temperaturebreezenortherly wind
collection DOAJ
language English
format Article
sources DOAJ
author Henrique Andrade
spellingShingle Henrique Andrade
O desconforto térmico estival em Lisboa - uma abordagem bioclimática
Finisterra - Revista Portuguesa de Geografia
Lisbon
thermal confort
human energy balance
Physiological Equivalent Temperature
breeze
northerly wind
author_facet Henrique Andrade
author_sort Henrique Andrade
title O desconforto térmico estival em Lisboa - uma abordagem bioclimática
title_short O desconforto térmico estival em Lisboa - uma abordagem bioclimática
title_full O desconforto térmico estival em Lisboa - uma abordagem bioclimática
title_fullStr O desconforto térmico estival em Lisboa - uma abordagem bioclimática
title_full_unstemmed O desconforto térmico estival em Lisboa - uma abordagem bioclimática
title_sort o desconforto térmico estival em lisboa - uma abordagem bioclimática
publisher CEG
series Finisterra - Revista Portuguesa de Geografia
issn 0430-5027
publishDate 1998-12-01
description THE SUMMER THERMAL STRESS IN LISBOA; A BIOCLIMATIC APPROACH. The summer frequency of hot days was studied, in Lisboa/Portela, with daily data from the period 1981/97. We used the Physiological Equivalent Temperature, an index of thermal confort based on the human energy balance, and calculated with air temperature, vapour pressure, wind speed and mean radiant temperature. It was assumed that mean radiant temperature was equal to air temperature, which is acceptable in the shade. The days were classifiend in two groups: hot days and very hot days, according to the thresholds of PET of 29ºC and 35ºC; 10% of the days had warm stress, with a maximum of frequency in July and a great interanual variability. The relation between the thermal discomfort and the wind regime was analysed. Most of the unconfortable days had breeze conditions, with the wind blowing from the East (from the estuary) during the morning; in the afternoon, the barometric gradient between the Ocean and the Iberian Peninsula increases, the breeze is replaced by a week northerly wind. The frequent occurence of strong northerly winds in summer is an important factor of reduction of the warm stress in Lisbon
topic Lisbon
thermal confort
human energy balance
Physiological Equivalent Temperature
breeze
northerly wind
url http://www.ceg.ul.pt/finisterra/numeros/1998-66/66_03.pdf
work_keys_str_mv AT henriqueandrade odesconfortotermicoestivalemlisboaumaabordagembioclimatica
_version_ 1721228439790288896