Spatiotemporal analysis of extreme heat events in Indianapolis and Philadelphia for the years 2010 and 2011

dc.contributor.advisorJohnson, Daniel P. (Daniel Patrick), 1971-
dc.contributor.authorBeerval Ravichandra, Kavya Urs
dc.contributor.otherWilson, Jeffrey S. (Jeffrey Scott), 1967-
dc.contributor.otherBein, Frederick L. (Frederick Louis), 1943-
dc.date.accessioned2014-03-12T14:48:01Z
dc.date.available2014-03-12T14:48:01Z
dc.date.issued2014-03-12
dc.degree.date2013en_US
dc.degree.disciplineDepartment of Geographyen
dc.degree.grantorIndiana Universityen_US
dc.degree.levelM.S.en_US
dc.descriptionIndiana University-Purdue University Indianapolis (IUPUI)en_US
dc.description.abstractOver the past two decades, northern parts of the United States have experienced extreme heat conditions. Some of the notable heat wave impacts have occurred in Chicago in 1995 with over 600 reported deaths and in Philadelphia in 1993 with over 180 reported deaths. The distribution of extreme heat events in Indianapolis has varied since the year 2000. The Urban Heat Island effect has caused the temperatures to rise unusually high during the summer months. Although the number of reported deaths in Indianapolis is smaller when compared to Chicago and Philadelphia, the heat wave in the year 2010 affected primarily the vulnerable population comprised of the elderly and the lower socio-economic groups. Studying the spatial distribution of high temperatures in the vulnerable areas helps determine not only the extent of the heat affected areas, but also to devise strategies and methods to plan, mitigate, and tackle extreme heat. In addition, examining spatial patterns of vulnerability can aid in development of a heat warning system to alert the populations at risk during extreme heat events. This study focuses on the qualitative and quantitative methods used to measure extreme heat events. Land surface temperatures obtained from the Landsat TM images provide useful means by which the spatial distribution of temperatures can be studied in relation to the temporal changes and socioeconomic vulnerability. The percentile method used, helps to determine the vulnerable areas and their extents. The maximum temperatures measured using LST conversion of the original digital number values of the Landsat TM images is reliable in terms of identifying the heat-affected regions.en_US
dc.identifier.urihttps://hdl.handle.net/1805/4083
dc.identifier.urihttp://dx.doi.org/10.7912/C2/778
dc.language.isoen_USen_US
dc.subjectExtreme Heat Eventsen_US
dc.subjectSpatiotemporal analysis of extreme heat eventsen_US
dc.subjectLand Surface Temperaturesen_US
dc.subjectGeographic Information Scienceen_US
dc.subjectRemote Sensingen_US
dc.subjectLandsat TMen_US
dc.subjectPercentile values for studying heat events- Indianapolis, Philadelphiaen_US
dc.subject.lcshHeat waves (Meteorology)en_US
dc.subject.lcshUrban climatology -- Research -- United States -- Methodologyen_US
dc.subject.lcshUrban climatology -- Research -- Indiana -- Indianapolis -- Methodologyen_US
dc.subject.lcshUrban climatology -- Research -- Pennsylvania -- Philadelphia -- Methodologyen_US
dc.subject.lcshThermal analysis in earth sciencesen_US
dc.subject.lcshArtificial satellites in remote sensingen_US
dc.subject.lcshSpatial analysis (Statistics)en_US
dc.subject.lcshLandsat satellites -- Research -- Analysisen_US
dc.subject.lcshApplied ecology -- Researchen_US
dc.subject.lcshGeospatial data -- Analysis -- Measurementen_US
dc.subject.lcshGeographic information systems -- Research -- Measurement -- Evaluationen_US
dc.subject.lcshClimatic changes -- Mathematical modelsen_US
dc.subject.lcshEarth sciences -- Remote sensingen_US
dc.subject.lcshEnvironmental monitoringen_US
dc.subject.lcshClimatic changes -- Health aspectsen_US
dc.subject.lcshHeat -- Radiation and absorptionen_US
dc.subject.lcshImage processingen_US
dc.titleSpatiotemporal analysis of extreme heat events in Indianapolis and Philadelphia for the years 2010 and 2011en_US
dc.typeThesisen
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