Measures to Mitigate Urban Heat Islands
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Challenge of Urban Heat Exposure Under Climate Change: an Analysis of Cities in the Sustainable Healthy Urban Environments (SHUE) Database
climate Article The Challenge of Urban Heat Exposure under Climate Change: An Analysis of Cities in the Sustainable Healthy Urban Environments (SHUE) Database James Milner 1,*, Colin Harpham 2, Jonathon Taylor 3 ID , Mike Davies 3, Corinne Le Quéré 4, Andy Haines 1 ID and Paul Wilkinson 1,† 1 Department of Social & Environmental Health Research, London School of Hygiene & Tropical Medicine, 15-17 Tavistock Place, London WC1H 9SH, UK; [email protected] (A.H.); [email protected] (P.W.) 2 Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK; [email protected] 3 UCL Institute for Environmental Design & Engineering, University College London, Central House, 14 Upper Woburn Place, London WC1H 0NN, UK; [email protected] (J.T.); [email protected] (M.D.) 4 Tyndall Centre for Climate Change Research, School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich NR4 7TJ, UK; [email protected] * Correspondence: [email protected]; Tel.: +44-020-7927-2510 † On behalf of the SHUE project partners. Received: 31 July 2017; Accepted: 8 December 2017; Published: 13 December 2017 Abstract: The so far largely unabated emissions of greenhouse gases (GHGs) are expected to increase global temperatures substantially over this century. We quantify the patterns of increases for 246 globally-representative cities in the Sustainable Healthy Urban Environments (SHUE) database. We used an ensemble of 18 global climate models (GCMs) run under a low (RCP2.6) and high (RCP8.5) emissions scenario to estimate the increase in monthly mean temperatures by 2050 and 2100 based on 30-year averages. -
The Relationship Between Land Cover and the Urban Heat Island in Northeastern Puerto Rico
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 31: 1222–1239 (2011) Published online 19 April 2010 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/joc.2145 The relationship between land cover and the urban heat island in northeastern Puerto Rico David J. Murphy,a* Myrna H. Hall,a Charles A. S. Hall,a Gordon M. Heisler,b† Stephen V. Stehmana and Carlos Anselmi-Molinac a 301 Illick Hall, SUNY – College of Environmental Science and Forestry, Syracuse, NY, 13210, USA b U.S. Forest Service, 5 Moon Library, SUNY-ESF, Syracuse, NY, 13210, USA c Physics Building, Marine Science Department, University of Puerto Rico Mayaguez, Puerto Rico, 00681-9000 ABSTRACT: Throughout the tropics, population movements, urban growth, and industrialization are causing conditions that result in elevated temperatures within urban areas when compared with that in surrounding rural areas, a phenomenon known as the urban heat island (UHI). One such example is the city of San Juan, Puerto Rico. Our objective in this study was to quantify the UHI created by the San Juan Metropolitan Area over space and time using temperature data collected by mobile- and fixed-station measurements. We also used the fixed-station measurements to examine the relationship between average temperature at a given location and the density of remotely sensed vegetation located upwind. We then regressed temperatures against regional upwind land cover to predict future temperature with projected urbanization. Our data from the fixed stations show that the average nighttime UHI calculated between the urban reference and rural stations ° ° (TCBD – rural) was 2.15 C during the usually wet season and 1.78 C during the usually dry season. -
ALBEDO ENHANCEMENT by STRATOSPHERIC SULFUR INJECTIONS: a CONTRIBUTION to RESOLVE a POLICY DILEMMA? an Editorial Essay
ALBEDO ENHANCEMENT BY STRATOSPHERIC SULFUR INJECTIONS: A CONTRIBUTION TO RESOLVE A POLICY DILEMMA? An Editorial Essay Fossil fuel burning releases about 25 Pg of CO2 per year into the atmosphere, which leads to global warming (Prentice et al., 2001). However, it also emits 55 Tg S as SO2 per year (Stern, 2005), about half of which is converted to sub-micrometer size sulfate particles, the remainder being dry deposited. Recent research has shown that the warming of earth by the increasing concentrations of CO2 and other greenhouse gases is partially countered by some backscattering to space of solar radiation by the sulfate particles, which act as cloud condensation nuclei and thereby influ- ence the micro-physical and optical properties of clouds, affecting regional precip- itation patterns, and increasing cloud albedo (e.g., Rosenfeld, 2000; Ramanathan et al., 2001; Ramaswamy et al., 2001). Anthropogenically enhanced sulfate particle concentrations thus cool the planet, offsetting an uncertain fraction of the anthro- pogenic increase in greenhouse gas warming. However, this fortunate coincidence is “bought” at a substantial price. According to the World Health Organization, the pollution particles affect health and lead to more than 500,000 premature deaths per year worldwide (Nel, 2005). Through acid precipitation and deposition, SO2 and sulfates also cause various kinds of ecological damage. This creates a dilemma for environmental policy makers, because the required emission reductions of SO2, and also anthropogenic organics (except black carbon), as dictated by health and ecological considerations, add to global warming and associated negative conse- quences, such as sea level rise, caused by the greenhouse gases. -
Fact Sheet on the Kyoto Protocol
The U.S. View FACT SHEET ON THE KYOTO PROTOCOL t a conference held December 1–11, 1997, in Kyoto, Japan, the Parties to A the UN Framework Convention on Climate Change agreed to an historic Protocol to reduce greenhouse gas emissions by harnessing the forces of the global marketplace to protect the environment. Key aspects of the Kyoto Protocol include weather, either of which could spike emissions targets, timetables for industrial- emissions in a particular year. ized nations, and market-based measures for meeting those targets. The Protocol • The first budget period will be makes a down payment on the meaning- 2008–2012. The parties rejected bud- ful participation of developing countries, get periods beginning as early as but more needs to be done in this area. 2003, as neither realistic nor achiev- Securing meaningful developing country able. Having a full decade before the participation remains a core U.S. goal. start of the binding period will allow more time for companies to make the transition to greater energy efficiency Emissions Targets and/or lower carbon technologies. A central feature of the Kyoto Protocol is a set of binding emissions targets for • The emissions targets include all six developed nations. The specific limits major greenhouse gases: carbon diox- vary from country to country, though ide, methane, nitrous oxide, and three those for the key industrial powers of the synthetic substitutes for ozone-deplet- European Union, Japan, and the United ing CFCs that are highly potent and States are similar—8 percent below 1990 long-lasting in the atmosphere. emissions levels for the European Union, 7 percent for the United States, and 6 • Activities that absorb carbon, such as percent for Japan. -
Emissions Gap Report 2018 © 2018 United Nations Environment Programme November 2018
Emissions Gap Report 2018 © 2018 United Nations Environment Programme November 2018 ISBN: 978-92-807-3726-4 Job number: DEW/2210/NA This publication may be reproduced in whole or in part and in any form for educational or non-profit services without special permission from the copyright holder, provided acknowledgement of the source is made. UN Environment would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or any other commercial purpose whatsoever without prior permission in writing from UN Environment. Applications for such permission, with a statement of the purpose and extent of the reproduction, should be addressed to the Director, Communication Division, UN Environment, P. O. Box 30552, Nairobi 00100, Kenya. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of United Nations Environment Programme concerning the legal status of any country, territory or city or its authorities, or concerning the delimitation of its frontiers or boundaries. For general guidance on matters relating to the use of maps in publications please go to http://www.un.org/Depts/Cartographic/english/htmain.htm Disclaimers Mention of a commercial company or product in this document does not imply endorsement by UN Environment or the authors. The use of information from this document for publicity or advertising is not permitted. Trademark names and symbols are used in an editorial fashion with no intention on infringement of trademark or copyright laws. -
Assessing Urban Heat Island Mitigation Using Green Roofs: a Hardware Scale Modeling Approach
ASSESSING URBAN HEAT ISLAND MITIGATION USING GREEN ROOFS: A HARDWARE SCALE MODELING APPROACH By William C. Pompeii II A Thesis Submitted to the Department of Geography and Earth Science and the Graduate Council in partial fulfillment of the requirements for the degree of Master of Science in Geoenvironmental Studies SHIPPENSBURG UNIVERSITY Shippensburg, Pennsylvania May, 2010 DEPARTMENT OF GEOGRAPHY AND EARTH SCIENCE SHIPPENSBURG UNIVESITY Upon the recommendation of the chairperson of the department of Geography and Earth Science this thesis is hereby accepted in partial fulfillment of the requirements for the degree of Master of Science in Geoenvironmental Studies Thesis Committee __________________________________________________ ________________ Committee Chairperson Date Dr. Timothy W. Hawkins __________________________________________________ ________________ Committee Member Date Dr. Claire Jantz __________________________________________________ ________________ Committee Member Date Dr. George Pomeroy Table of Contents List of Figures iii List of Tables v ABSTRACT vi Chapter 1: Introduction 1 1.1 Statement of Problem 1 Chapter 2: Review of Literature 3 2.1 Background 3 2.1.1 Urban Heat Island 3 2.2 Green Roofs 6 2.2.1 Origin and Types 6 2.2.2 Benefits of Green Roofs 7 2.3 Chicago-A Case Study City 9 2.3.1 Green Roof Case Study-Chicago City Hall Building 13 2.4 Methods of Study the Urban Heat Island and Benefits of Green Roof Mitigation 15 2.4.1. Urban Heat Island Methods-Dataloggers 15 2.4.2 Green Roof effects on Urban Heat Island -
Urban Surface Temperatures and the Urban Heat Island Effects
NASA Climate Change Research Initiative Applied Research STEM Curriculum Portfolio CCRI Unit Plan NASA Science Mission Directorate | Earth Sciences Division NASA Goddard Institute for Space Studies NASA Goddard Space Flight Center | Office of STEM Engagement Unit Title: Urban Surface Temperatures and the Urban Heat Island Effects Overarching Investigative Research Question: How does Urban Heat Island contributes to climate change? NASA STEM Educator / Associate Researcher: Alejandro Mundo NASA PI /Mentor: Dr. Christian Braneon NASA Goddard Institute for Space Studies | Climate Change Research Initiative (CCRI)) 1 Matthew Pearce | Education Program Specialist | GSFC Office of STEM Engagement I. Executive Summary Cities that are growing at a fast pace are notable entities of innovation and city development. As population keeps growing in urban settings, the need to understand urban climates has awakened much interest and discussion among our society. Due to urbanization, land surface temperatures are intensifying with much warmer temperatures than surrounding areas, making cities experience the Urban Heat Island phenomenon. This unit plan called “Urban Surface Temperatures and the Urban Heat Island Effects“ has the purpose to educate students how climate is changing in urban settings and produce mitigation solutions for city environmental concerns through the use of groundbreaking technology and authentic science learning experiences. Students are exposed to real-world scientific experiences like the exploration of climate simulation models, global temperature profiles and climate change evidence analysis during the first lesson. Later, they learn about remote sensing and investigate instruments on climate satellites. Students are exposed to remote sensing imagery analysis and dive into the Urban Heat Island effects on the third lesson. -
Radiative Cooling New Opportunities & Enabling Technologies
Radiative Cooling New Opportunities & Enabling Technologies Aaswath P. Raman, Ph.D. [email protected] Research Associate, Fan Group, Ginzton Laboratory ARPA-E Alternative Power Plant Cooling Workshop, May 12, 2014 1 An opportunity to tap an underutilized resource Use the cold of outer space to cold outer space! (-80°C ! -270°C)! radiatively pump heat from the ground through sky access New: Possible at all hours of the day through photonic design of thermally emissive layers Heat Atmosphere Thermal Meaningful cooling power that EM Waves scales with area: analogies to PV Radiative Cooling Surface! 2 I. INTRODUCTION Radiative cooling is a technique that exploits a natural transparency window for electro- magnetic waves in the Earths atmosphere to transport heat from terrestrial objects into cold space. As a result, objects with the appropriate radiative properties can passively cool them- selves down to temperatures well below the ambient. The atmospheric transparency window is found in the 8-13µm wavelength range, as shown in Fig. 1, and fortuitously overlaps with the blackbody spectralAtmospheric radiance corresponding to typical terrestrialtransmittance temperatures (0-50C), thus enabling objects at these temperatures to emit more power than they absorb. 1 Atmospheric Transmission Radiative cooling is enabled by 0◦C blackbody 50◦C blackbody an atmospheric transparency 0.5 window between 8 – 13 μm 0 7 9 11 13 15 Blackbody spectrum of typical λ [µm] Earth temperature objects overlap with window FIG. 1. Atmopheric Transmissioncold in the outer zenith space direction! vs. wavelength; normalized blackbody spectral radiance of a 0◦C and a(upper 50◦C blackbody atmosphere) emitter ! Varies with cloud cover, Prior work in radiative cooling has almost entirely focused on nighttime cooling,geographic where location and one aims to maximize emission in the atmospheric transparency window, without having to contend with solar radiation. -
Spatiotemporal Variability of Urban Heat Island: Influence of Urbanization on Seasonal Pattern of Land Surface Temperature in the Metropolitan Region of Belém, Brazil
Scientific Article doi: 10.1590/2175-3369.013.e20200260 Spatiotemporal variability of urban heat 3369 island: Influence of urbanization on - seasonal pattern of land surface temperature in the Metropolitan Region ISSN 2175 of Belém, Brazil Variabilidade espaço-temporal das ilhas de calor urbano: Influência da urbanização no padrão sazonal da temperatura da superfície terrestre na Região Metropolitana de Belém, Brasil Licenciadosob uma Licença Creative Commons Jefferson Inayan de Oliveira Souto [a] , Julia Clarinda Paiva Cohen [a] [a] Universidade Federal do Pará, Instituto de Geociências, Belém, PA, Brasil How to cite: Souto, J. I. O., & Cohen, J. C. P. (2021). Spatiotemporal variability of urban heat island: Influence of urbanization on seasonal pattern of land surface temperature in the Metropolitan Region of Belém, Brazil. urbe. Revista Brasileira de Gestão Urbana, v. 13, e20200260. https://doi.org/10.1590/2175-3369.013.e20200260 Abstract Cities experience the extensive urban heat island effect (UHI), which continue to pose challenges for humanity's increasingly urban population, where tropical cities have experienced a continued and rapid urbanization process in the past few decades. We present the evolution of surface UHI and its controlling factors in the Metropolitan Region of Belém, over the last 16 years (2003–2018), which has experienced unique consolidated economic growth and urban transformation under wet equatorial climate. We incorporate MODIS and Landsat satellite data and evaluate statistical techniques for estimates the variation in the land surface temperature (LST) during two seasons: wet season and dry season. Our result revealed that the regions of fast urbanization resulted in a decrease of normalized difference vegetation index and increase of LST. -
Global Climate Coalition Primer on Climate Change Science
~ ~ Chairman F.SOHWAB Poraohe TECH-96-29 1st Viae C".lrrn.n C. MAZZA 1/18/96 Hyundal 2nd Vic. Ohalrrnan C. SMITH Toyota P S_cret.ry C. HELFMAN TO: AIAM Technical Committee BMW Treasurer .,J.AMESTOY Mazda FROM: Gregory J. Dana Vice President and Technical Director BMW c ••woo Flat RE: GLOBAL CLIMATE COALITION-(GCC)· Primer on Honda Hyundal Climate Change Science· Final Draft lauzu Kia , Land Rover Enclosed is a primer on global climate change science developed by the Mazda Mlt8ublehl GCC. If any members have any comments on this or other GCC NIB.an documents that are mailed out, please provide me with your comments to Peugeot forward to the GCC. Poreche Renault RolI&-Aoyoe S ••b GJD:ljf ""al'"u .z.ukl Toyota VOlkswagen Volvo President P. HUTOHINSON ASSOCIATION OF INTERNATIONAL AUTOMOBILE MANUFACTURERS. INC. 1001 19TH ST. NORTH. SUITE 1200 • ARLINGTON, VA 22209. TELEPHONE 703.525.7788. FAX 703.525.8817 AIAM-050771 Mobil Oil Corporation ENVIRONMENTAL HEALTH AND SAFETY DEPARTh4ENT P.O. BOX1031 PRINCETON, NEW JERSEY 08543-1031 December 21, 1995 'To; Members ofGCC-STAC Attached is what I hope is the final draft ofthe primer onglobal climate change science we have been working on for the past few months. It has been revised to more directly address recent statements from IPCC Working Group I and to reflect comments from John Kinsman and Howard Feldman. We will be discussing this draft at the January 18th STAC meeting. Ifyou are coming to that meeting, please bring any additional comments on the draft with you. Ifyou have comments but are unable to attend the meeting, please fax them to Eric Holdsworth at the GeC office. -
Ocean Acidification
Ocean acidification: Obligations under international and regional treaty law Candidate number: 8023 Submission deadline: 1 December 2018 Number of words: 17.996 Table of contents 1 INTRODUCTION - THE PROBLEM OF OCEAN ACIDIFICATION .................. 1 1.1 Methodology, structure and legal sources used ................................................................ 2 1.2 The science behind ocean acidification and the problems repercussions ......................... 3 1.2.1 Scientific background of ocean acidification ...................................................... 3 1.2.2 Artificial contribution to ocean acidification ...................................................... 4 1.2.3 Consequences of ocean acidification for the ocean as an ecosystem .................. 4 1.2.4 Consequences of ocean acidification on particularly sensitive areas .................. 5 1.2.5 The problem of inconsistent results .................................................................... 6 1.2.6 The effects of ocean acidification on human life ................................................ 6 1.2.7 Implications ......................................................................................................... 7 2 ANALYSIS OF THE OBLIGATIONS UNDER INTERNATIONAL TREATY LAW IN REGARD TO OCEAN ACIDIFICATION .................................................. 9 2.1 Ocean acidification under the International Climate Change Regime ............................. 9 2.1.1 The United Nations Framework Convention on Climate Change (UNFCCC) ... 9 2.1.2 Kyoto -
Concentrated Radiative Cooling Arxiv:2010.02426V1 [Physics.App
Concentrated Radiative Cooling Joseph Peoples,1 Yu-Wei Hung,2 Xiangyu Li,1 Daniel Gallagher,1 Nathan Fruehe,1 Anil Yuksel,3 James Braun,1 Travis Horton,2 Xiulin Ruan1∗ 1School of Mechanical Engineering, Purdue University, West Lafayette, IN 47907, USA, 2School of Civil Engineering, Purdue University, West Lafayette, IN 47907, USA, 3IBM Corporation, Austin, TX, 78758, USA ∗To whom correspondence should be addressed; E-mail: [email protected]. A fundamental limit of current radiative cooling systems is that only the top surface facing deep-space can provide the radiative cooling effect, while the bottom surface cannot. Here, we propose and experimentally demonstrate a concept of \concentrated radia- tive cooling" by nesting a radiative cooling system in a mid-infrared reflective trough, so that the lower surface, which does not con- tribute to radiative cooling in previous systems, can radiate heat to deep-space via the reflective trough. Field experiments show that the temperature drop of a radiative cooling pipe with the trough arXiv:2010.02426v1 [physics.app-ph] 6 Oct 2020 is more than double that of the standalone radiative cooling pipe. Furthermore, by integrating the concentrated radiative cooling sys- tem as a preconditioner in an air conditioning system, we predict electricity savings of > 75% in Phoenix, AZ, and > 80% in Reno, NV, for a single-story commercial building. 1 Introduction In 2018, 9.3% of the total generated electricity in the United States went to space cooling and refrigeration of commercial buildings, equating to 164.7 million metric tons of carbon dioxide emission, just for commercial cooling (1).