Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe
This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated i...
Ausführliche Beschreibung
Autor*in: |
Mushore, Terence Darlington [verfasserIn] Chimuti, Brandon [verfasserIn] Gwenzi, Juliet [verfasserIn] Manjowe, Moven [verfasserIn] Mutasa, Collen [verfasserIn] Mashonjowa, Emmanuel [verfasserIn] Mhizha, Tedious [verfasserIn] Muroyiwa, Godfrey [verfasserIn] Rousta, Iman [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2019 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Physics and chemistry of the earth - Amsterdam [u.a.] : Elsevier Science, 1956, 110, Seite 138-148 |
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Übergeordnetes Werk: |
volume:110 ; pages:138-148 |
DOI / URN: |
10.1016/j.pce.2019.01.010 |
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Katalog-ID: |
ELV002322528 |
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100 | 1 | |a Mushore, Terence Darlington |e verfasserin |0 (orcid)0000-0003-4279-8877 |4 aut | |
245 | 1 | 0 | |a Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe |
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520 | |a This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. | ||
650 | 4 | |a Thermal discomfort | |
650 | 4 | |a Temperature | |
650 | 4 | |a Humidity | |
650 | 4 | |a Temperature humidity index | |
650 | 4 | |a Heat stress | |
650 | 4 | |a Discomfort index | |
700 | 1 | |a Chimuti, Brandon |e verfasserin |4 aut | |
700 | 1 | |a Gwenzi, Juliet |e verfasserin |0 (orcid)0000-0001-6499-2393 |4 aut | |
700 | 1 | |a Manjowe, Moven |e verfasserin |4 aut | |
700 | 1 | |a Mutasa, Collen |e verfasserin |4 aut | |
700 | 1 | |a Mashonjowa, Emmanuel |e verfasserin |0 (orcid)0000-0002-8293-6632 |4 aut | |
700 | 1 | |a Mhizha, Tedious |e verfasserin |4 aut | |
700 | 1 | |a Muroyiwa, Godfrey |e verfasserin |4 aut | |
700 | 1 | |a Rousta, Iman |e verfasserin |0 (orcid)0000-0002-3694-6936 |4 aut | |
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2019 |
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10.1016/j.pce.2019.01.010 doi (DE-627)ELV002322528 (ELSEVIER)S1474-7065(18)30239-0 DE-627 ger DE-627 rda eng 550 DE-600 38.32 bkl 38.70 bkl Mushore, Terence Darlington verfasserin (orcid)0000-0003-4279-8877 aut Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index Chimuti, Brandon verfasserin aut Gwenzi, Juliet verfasserin (orcid)0000-0001-6499-2393 aut Manjowe, Moven verfasserin aut Mutasa, Collen verfasserin aut Mashonjowa, Emmanuel verfasserin (orcid)0000-0002-8293-6632 aut Mhizha, Tedious verfasserin aut Muroyiwa, Godfrey verfasserin aut Rousta, Iman verfasserin (orcid)0000-0002-3694-6936 aut Enthalten in Physics and chemistry of the earth Amsterdam [u.a.] : Elsevier Science, 1956 110, Seite 138-148 Online-Ressource (DE-627)306661349 (DE-600)1500664-5 (DE-576)081986912 1873-5193 nnns volume:110 pages:138-148 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie 38.70 Geophysik: Allgemeines AR 110 138-148 |
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10.1016/j.pce.2019.01.010 doi (DE-627)ELV002322528 (ELSEVIER)S1474-7065(18)30239-0 DE-627 ger DE-627 rda eng 550 DE-600 38.32 bkl 38.70 bkl Mushore, Terence Darlington verfasserin (orcid)0000-0003-4279-8877 aut Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index Chimuti, Brandon verfasserin aut Gwenzi, Juliet verfasserin (orcid)0000-0001-6499-2393 aut Manjowe, Moven verfasserin aut Mutasa, Collen verfasserin aut Mashonjowa, Emmanuel verfasserin (orcid)0000-0002-8293-6632 aut Mhizha, Tedious verfasserin aut Muroyiwa, Godfrey verfasserin aut Rousta, Iman verfasserin (orcid)0000-0002-3694-6936 aut Enthalten in Physics and chemistry of the earth Amsterdam [u.a.] : Elsevier Science, 1956 110, Seite 138-148 Online-Ressource (DE-627)306661349 (DE-600)1500664-5 (DE-576)081986912 1873-5193 nnns volume:110 pages:138-148 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie 38.70 Geophysik: Allgemeines AR 110 138-148 |
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10.1016/j.pce.2019.01.010 doi (DE-627)ELV002322528 (ELSEVIER)S1474-7065(18)30239-0 DE-627 ger DE-627 rda eng 550 DE-600 38.32 bkl 38.70 bkl Mushore, Terence Darlington verfasserin (orcid)0000-0003-4279-8877 aut Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index Chimuti, Brandon verfasserin aut Gwenzi, Juliet verfasserin (orcid)0000-0001-6499-2393 aut Manjowe, Moven verfasserin aut Mutasa, Collen verfasserin aut Mashonjowa, Emmanuel verfasserin (orcid)0000-0002-8293-6632 aut Mhizha, Tedious verfasserin aut Muroyiwa, Godfrey verfasserin aut Rousta, Iman verfasserin (orcid)0000-0002-3694-6936 aut Enthalten in Physics and chemistry of the earth Amsterdam [u.a.] : Elsevier Science, 1956 110, Seite 138-148 Online-Ressource (DE-627)306661349 (DE-600)1500664-5 (DE-576)081986912 1873-5193 nnns volume:110 pages:138-148 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie 38.70 Geophysik: Allgemeines AR 110 138-148 |
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10.1016/j.pce.2019.01.010 doi (DE-627)ELV002322528 (ELSEVIER)S1474-7065(18)30239-0 DE-627 ger DE-627 rda eng 550 DE-600 38.32 bkl 38.70 bkl Mushore, Terence Darlington verfasserin (orcid)0000-0003-4279-8877 aut Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index Chimuti, Brandon verfasserin aut Gwenzi, Juliet verfasserin (orcid)0000-0001-6499-2393 aut Manjowe, Moven verfasserin aut Mutasa, Collen verfasserin aut Mashonjowa, Emmanuel verfasserin (orcid)0000-0002-8293-6632 aut Mhizha, Tedious verfasserin aut Muroyiwa, Godfrey verfasserin aut Rousta, Iman verfasserin (orcid)0000-0002-3694-6936 aut Enthalten in Physics and chemistry of the earth Amsterdam [u.a.] : Elsevier Science, 1956 110, Seite 138-148 Online-Ressource (DE-627)306661349 (DE-600)1500664-5 (DE-576)081986912 1873-5193 nnns volume:110 pages:138-148 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie 38.70 Geophysik: Allgemeines AR 110 138-148 |
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10.1016/j.pce.2019.01.010 doi (DE-627)ELV002322528 (ELSEVIER)S1474-7065(18)30239-0 DE-627 ger DE-627 rda eng 550 DE-600 38.32 bkl 38.70 bkl Mushore, Terence Darlington verfasserin (orcid)0000-0003-4279-8877 aut Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index Chimuti, Brandon verfasserin aut Gwenzi, Juliet verfasserin (orcid)0000-0001-6499-2393 aut Manjowe, Moven verfasserin aut Mutasa, Collen verfasserin aut Mashonjowa, Emmanuel verfasserin (orcid)0000-0002-8293-6632 aut Mhizha, Tedious verfasserin aut Muroyiwa, Godfrey verfasserin aut Rousta, Iman verfasserin (orcid)0000-0002-3694-6936 aut Enthalten in Physics and chemistry of the earth Amsterdam [u.a.] : Elsevier Science, 1956 110, Seite 138-148 Online-Ressource (DE-627)306661349 (DE-600)1500664-5 (DE-576)081986912 1873-5193 nnns volume:110 pages:138-148 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_20 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.32 Geochemie 38.70 Geophysik: Allgemeines AR 110 138-148 |
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550 DE-600 38.32 bkl 38.70 bkl Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe Thermal discomfort Temperature Humidity Temperature humidity index Heat stress Discomfort index |
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Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe |
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Mushore, Terence Darlington Chimuti, Brandon Gwenzi, Juliet Manjowe, Moven Mutasa, Collen Mashonjowa, Emmanuel Mhizha, Tedious Muroyiwa, Godfrey Rousta, Iman |
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localised human thermal discomfort assessment using high temporal resolution meteorological data: a case of university of zimbabwe |
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Localised human thermal discomfort assessment using high temporal resolution meteorological data: A case of University of Zimbabwe |
abstract |
This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. |
abstractGer |
This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. |
abstract_unstemmed |
This study investigated the thermal discomfort patterns at the University of Zimbabwe in Harare, Zimbabwe; paying attention to the outdoor and indoor seasonal and diurnal variations. Temperature and relative humidity data from an automatic weather station located in the study area was incorporated into the temperature humidity index to retrieve outdoor human thermal discomfort patterns. Based on data availability, air temperature and humidity hourly data for the period 2014 to 2018 was used. The indoor human thermal discomfort patterns were then obtained using the linear relationship between outdoor temperatures and indoor comfort. The results show that there were only an average of 31 days per year of indoor thermal discomfort days in the hot and rainy seasons. There were on average 303 days in which at least half of the subjects felt thermally comfortable outdoors yearly. Throughout the whole year there were no heat stresses, 62 days of cold stress outdoors, and 334 days of cold stress indoors. The hot season was found to be the most thermally comfortable with 25% and 33% of thermally comfortable hours per day indoors and outdoors, respectively. It was concluded that subjects were mostly comfortable in the afternoon both indoors and outdoors. The study recommended that as more data is collected, future researchers should consider a longer period for analysis. The findings of this study are important for understanding, modelling and monitoring human thermal comfort/discomfort at learning institutions, work places and other environments. Such information can be used for making building guidelines on including systems like air conditioning units in response to climate change and increased variability. |
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