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The 2006 New Orleans Mayoral Election: The Political Ramifications of a Large-Scale Natural Disaster

Published online by Cambridge University Press:  01 October 2008

James Vanderleeuw
Affiliation:
Lamar University
Baodong Liu
Affiliation:
University of Utah
Erica Williams
Affiliation:
University of Louisville
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Extract

On Monday, August 29, 2005, the Gulf Coast of the United States was hit by the sixth most destructive Atlantic hurricane on record, Hurricane Katrina. Katrina formed in the Bahamas on August 23 and entered the Gulf of Mexico two days later, on the twenty-fifth (Knabb 2005). Twelve hours after entering the gulf, Katrina grew from a Category 3 to a Category 5 storm on the Saffir-Simpson scale, with winds up to 160 miles per hour. Katrina made landfall on the twenty-ninth as a powerful Category 3 storm with winds up to 145 miles per hour. However, once Katrina made landfall she maintained a storm surge equivalent to a Category 5 storm. For the city of New Orleans, the greatest threat without question was to be from the storm surge. Lake Pontchartrain—which normally sits at one foot above sea level—was elevated to eight and a half feet above sea level. On Tuesday, August 30, the city's levees broke in three places—along the Industrial Canal, the 17th Street Canal, and the London Street Canal (Mihelich 2005). As a result, 80% of the city was flooded, in some places with water as high as 20 feet above sea level (Knabb 2005).

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Copyright © The American Political Science Association 2008
Figure 0

Figure 1.Black Voter Support for Ray Nagin in the 2002 and 2006 Mayoral RunoffsNote: Nagin's black support is estimated through King's (1997) EI method (see Liu 2006, 74, for a discussion of the method). The unit of analysis in this chart is the voting precinct. Each data point represents how blacks in a precinct voted in the 2002 runoff versus how they voted in the 2006 runoff in the same precinct. This chart reveals that blacks in most precincts provided less than 50% voting support for Nagin in the 2002 runoff (the horizontal axis). However, all the precincts provided more than 60% of the black vote for Nagin in the 2006 runoff (the vertical axis).

Figure 1

Figure 2.White Voter Support for Ray Nagin in the 2002 and 2006 Mayoral RunoffsNote: Nagin's white support is estimated through King's (1997) EI method. The unit of analysis in this chart is the voting precinct. Each data point represents how whites in a precinct voted in the 2002 runoff versus how they voted in the 2006 runoff in the same precinct. This chart reveals that whites in most precincts provided more than 60% voting support for Nagin in the 2002 runoff (the horizontal axis). However, all the precincts provided less than 60% of the white vote for Nagin in the 2006 runoff (the vertical axis).

Figure 2

Figure 3.2002 vs. 2006 Mayoral Runoffs—Turnout at the Precinct LevelNote: Each data point in this chart represents a precinct's turnout rate in the 2002 runoff versus the same precinct's turnout rate in the 2006 runoff. Turnout is calculated by dividing the total number of votes cast in a precinct by the total number of registered voters in that precinct. Most data points (precincts) show a greater turnout rate in the 2002 runoff (the horizontal axis) than in the 2006 runoff (the vertical axis).

Figure 3

Figure 4.2006 Mayoral Runoff Turnout in PrecinctsNote: The unit of analysis is precinct. The horizontal dimension reveals precincts' black proportion of registered voters (calculated by the total number of black registered voters divided by the total number of registered voters). The vertical dimension provides the true turnout rates in these precincts (calculated by the total number of votes cast divided by the total number of registered voters). This chart shows that as precincts' black proportion increases, the turnout rates tend to go down in the 2006 runoff.