Impact of heatwave on a megacity: an observational analysis of New York City during July 2016

More than half of the world’s current population resides in urban areas, and cities account for roughly three-quarters of the total greenhouse gas emissions. Current and future trends in urbanization will have significant impacts on global climate. However, our collective understanding of the climat...

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Main Authors: Prathap Ramamurthy, Jorge González, Luis Ortiz, Mark Arend, Fred Moshary
Format: Article
Language:English
Published: IOP Publishing 2017-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aa6e59
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author Prathap Ramamurthy
Jorge González
Luis Ortiz
Mark Arend
Fred Moshary
author_facet Prathap Ramamurthy
Jorge González
Luis Ortiz
Mark Arend
Fred Moshary
author_sort Prathap Ramamurthy
collection DOAJ
description More than half of the world’s current population resides in urban areas, and cities account for roughly three-quarters of the total greenhouse gas emissions. Current and future trends in urbanization will have significant impacts on global climate. However, our collective understanding of the climate of urban areas remains deficient, which is mainly related to significant knowledge gaps in observations. The New York City Summer Heat Campaign was initiated to address some of these critical knowledge gaps. As part of the campaign the urban boundary layer over New York City was continuously monitored during July 2016, a period that witnessed three heatwave events. Surface weather stations and indoor sensors were also used to characterize the urban heat island intensity. Our results reveal that during the month, the urban heat island intensity was nearly twice compared to the decadal average. During the heatwave episodes, urban heat island intensities as high as 10 °C were observed. The thermal profiles indicate elevated temperatures in much of the boundary layer between 800–2500 m during the heatwave episodes. The profiles indicate a complex thermal structure and high intra-city variability. Thermal internal boundary layer was observed in neighborhoods populated by tall buildings. Overall the high-pressure system during the heatwave episodes acted as a thermal block and much of the heat generated in the urban surface layer remained within the boundary layer, thereby amplifying the near surface air temperature.
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spelling doaj.art-91529c6c55b94f47a4fc8e8cfaed56f92023-08-09T14:33:16ZengIOP PublishingEnvironmental Research Letters1748-93262017-01-0112505401110.1088/1748-9326/aa6e59Impact of heatwave on a megacity: an observational analysis of New York City during July 2016Prathap Ramamurthy0Jorge González1Luis Ortiz2Mark Arend3Fred Moshary4Department of Mechanical Engineering, City College of New York , New York, NY, United States of America; Author to whom any correspondence should be addressed.Department of Mechanical Engineering, City College of New York , New York, NY, United States of AmericaDepartment of Mechanical Engineering, City College of New York , New York, NY, United States of AmericaDepartment of Electrical Engineering, City College of New York , New York, NY, United States of AmericaDepartment of Electrical Engineering, City College of New York , New York, NY, United States of AmericaMore than half of the world’s current population resides in urban areas, and cities account for roughly three-quarters of the total greenhouse gas emissions. Current and future trends in urbanization will have significant impacts on global climate. However, our collective understanding of the climate of urban areas remains deficient, which is mainly related to significant knowledge gaps in observations. The New York City Summer Heat Campaign was initiated to address some of these critical knowledge gaps. As part of the campaign the urban boundary layer over New York City was continuously monitored during July 2016, a period that witnessed three heatwave events. Surface weather stations and indoor sensors were also used to characterize the urban heat island intensity. Our results reveal that during the month, the urban heat island intensity was nearly twice compared to the decadal average. During the heatwave episodes, urban heat island intensities as high as 10 °C were observed. The thermal profiles indicate elevated temperatures in much of the boundary layer between 800–2500 m during the heatwave episodes. The profiles indicate a complex thermal structure and high intra-city variability. Thermal internal boundary layer was observed in neighborhoods populated by tall buildings. Overall the high-pressure system during the heatwave episodes acted as a thermal block and much of the heat generated in the urban surface layer remained within the boundary layer, thereby amplifying the near surface air temperature.https://doi.org/10.1088/1748-9326/aa6e59heatwavesurban boundary layerurban heat island
spellingShingle Prathap Ramamurthy
Jorge González
Luis Ortiz
Mark Arend
Fred Moshary
Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
Environmental Research Letters
heatwaves
urban boundary layer
urban heat island
title Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
title_full Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
title_fullStr Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
title_full_unstemmed Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
title_short Impact of heatwave on a megacity: an observational analysis of New York City during July 2016
title_sort impact of heatwave on a megacity an observational analysis of new york city during july 2016
topic heatwaves
urban boundary layer
urban heat island
url https://doi.org/10.1088/1748-9326/aa6e59
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