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dc.contributor.authorOrosa, José A.
dc.contributor.authorCosta, Ángel M.
dc.contributor.authorGhanghermeh, Abdolazim
dc.contributor.authorRoshan, Gholamreza
dc.date.accessioned2024-05-20T18:43:22Z
dc.date.available2024-05-20T18:43:22Z
dc.date.issued2019
dc.identifier.citationGhanghermeh, A.; Roshan, G.; Orosa, J.A.; Costa, Á.M. Analysis and Comparison of Spatial–Temporal Entropy Variability of Tehran City Microclimate Based on Climate Change Scenarios. Entropy 2019, 21(1), 13. https://doi.org/10.3390/e21010013es_ES
dc.identifier.urihttp://hdl.handle.net/2183/36543
dc.description.abstract[Abstract] Urban microclimate patterns can play a great role for the allocation and management of cooling and heating energy sources, urban design and architecture, and urban heat island control. Therefore, the present study intends to investigate the variability of spatial and temporal entropy of the Effective Temperature index (ET) for the two basic periods (1971–2010) and the future (2011–2050) in Tehran to determine how the variability degree of the entropy values of the abovementioned bioclimatic would be, based on global warming and future climate change. ArcGIS software and geostatistical methods were used to show the Spatial and Temporal variations of the microclimate pattern in Tehran. However, due to global warming the temperature difference between the different areas of the study has declined, which is believed to reduce the abnormalities and more orderly between the data spatially and over time. It is observed that the lowest values of the Shannon entropy occurred in the last two decades, from 2030 to 2040, and the other in 2040–2050. Because, based on global warming, dominant areas have increased temperature, and the difference in temperature is reduced daily and the temperature difference between the zones of different areas is lower. The resultsof this study show a decrease in the coefficient of the Shannon entropy of effective temperature for future decades in Tehran. This can be due to the reduction of temperature differences between different regions. However, based on the urban-climate perspective, there is no positive view of this process. Because reducing the urban temperature difference means reducing the local pressure difference as well as reducing local winds. This is a factor that can effective, though limited, in the movement of stagnant urban air and reduction of thermal budget and thermal stress of the city.es_ES
dc.description.sponsorshipThis research was funded by The University of A Coruña (Grant No. 64900). The authors wish to express their deepest gratitude to the Sustainability Specialization Campus of the University of A Coruña for the administrative and technical support.es_ES
dc.description.sponsorshipUniversidade da Coruña ; 64900es_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.relation.urihttps://doi.org/10.3390/e21010013es_ES
dc.rightsCreative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).es_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectGlobal warminges_ES
dc.subjectClimatic modelinges_ES
dc.subjectSpatial analysises_ES
dc.subjectUrban sprawles_ES
dc.subjectShannon entropyes_ES
dc.titleAnalysis and Comparison of Spatial–Temporal Entropy Variability of Tehran City Microclimate Based on Climate Change Scenarioses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccesses_ES
UDC.journalTitleEntropyes_ES
UDC.volume21es_ES
UDC.issue1es_ES
UDC.startPage13es_ES
dc.identifier.doi10.3390/e21010013


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