MITIGATING NEW YORK CITY’S HEAT ISLAND: Integrating Stakeholder Perspectives and Scientific Evaluation

This study of New York City, New York's, heat island and its potential mitigation was structured around research questions developed by project stakeholders working with a multidisciplinary team of researchers. Meteorological, remotely-sensed, and spatial data on the urban environment were brou...

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Veröffentlicht in:Bulletin of the American Meteorological Society 2009-09, Vol.90 (9), p.1297-1312
Hauptverfasser: Rosenzweig, Cynthia, Solecki, William D., Parshall, Lily, Lynn, Barry, Cox, Jennifer, Goldberg, Richard, Hodges, Sara, Gaffin, Stuart, Slosberg, Ronald B., Savio, Peter, Dunstan, Frank, Watson, Mark
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container_end_page 1312
container_issue 9
container_start_page 1297
container_title Bulletin of the American Meteorological Society
container_volume 90
creator Rosenzweig, Cynthia
Solecki, William D.
Parshall, Lily
Lynn, Barry
Cox, Jennifer
Goldberg, Richard
Hodges, Sara
Gaffin, Stuart
Slosberg, Ronald B.
Savio, Peter
Dunstan, Frank
Watson, Mark
description This study of New York City, New York's, heat island and its potential mitigation was structured around research questions developed by project stakeholders working with a multidisciplinary team of researchers. Meteorological, remotely-sensed, and spatial data on the urban environment were brought together to understand multiple dimensions of New York City's heat island and the feasibility of mitigation strategies, including urban forestry, green roofs, and high-albedo surfaces. Heat island mitigation was simulated with the fifth-generation Pennsylvania State University–NCAR Mesoscale Model (MM5). Results compare the possible effectiveness of mitigation strategies at reducing urban air temperature in six New York City neighborhoods and for New York City as a whole. Throughout the city, the most effective temperature-reduction strategy is to maximize the amount of vegetation, with a combination of tree planting and green roofs. This lowered simulated citywide surface urban air temperature by 0.4°C on average, and 0.7°C at 1500 Eastern Standard Time (EST), when the greatest temperature reductions tend to occur. Decreases of up to 1.1°C at 1500 EST occurred in some neighborhoods in Manhattan and Brooklyn, where there is more available area for implementing vegetation planting. New York City agencies are using project results to guide ongoing urban greening initiatives, particularly tree-planting programs.
doi_str_mv 10.1175/2009bams2308.1
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source Jstor Complete Legacy; American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals
subjects Albedo
Bgi / Prodig
Climate change
Climate models
Climatology
Electricity
Energy research
Green roofs
Heat islands
Land cover
Load distribution
Local climates and microclimates
Outdoor air quality
Parks & recreation areas
Physical geography
Planting
R&D
Research & development
Street trees
Surface temperature
Temperature
Trees
Urban heat islands
Vegetation
title MITIGATING NEW YORK CITY’S HEAT ISLAND: Integrating Stakeholder Perspectives and Scientific Evaluation
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