1995 Chicago heat wave

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The July 1995 Chicago heat wave led to 739 heat-related deaths in Chicago over a period of five days. [1] Most of the victims of the heat wave were elderly poor residents of the city, who did not have air conditioning, or had air conditioning but could not afford to turn it on, and did not open windows or sleep outside for fear of crime. [2] The heat wave also heavily impacted the wider Midwestern region, with additional deaths in both St. Louis, Missouri [3] and Milwaukee, Wisconsin. [4]

Contents

Weather

High pressure up traps heat near the ground, forming a heat wave Heat Wave.jpg
High pressure up traps heat near the ground, forming a heat wave

The temperatures soared to record highs in July with the hottest weather occurring from July 12 to July 16. The high of 106 °F (41 °C) on July 13 was the second warmest July temperature (warmest being 110 °F (43 °C) set on July 23, 1934) since records began at Chicago Midway International Airport in 1928. Nighttime low temperatures were unusually high — in the upper 70s and lower 80s °F (about 26 °C).

Plotted observed temperatures from O'Hare International Airport. Red Lines are daily max temperatures, Blue Lines are daily minimum temperatures, and the Black Line is the July 1960-2016 mean temperature. 1995HeatWaveChicago.png
Plotted observed temperatures from O'Hare International Airport. Red Lines are daily max temperatures, Blue Lines are daily minimum temperatures, and the Black Line is the July 1960–2016 mean temperature.

The humidity made a large difference for the heat in this heat wave when compared to the majority of those of the 1930s, 1988, 1976–78 and 1954–56, which were powered by extremely hot, dry, bare soil and/or air masses which had originated in the desert Southwest. Each of the above-mentioned years' summers did have high-humidity heat waves as well, although 1988 was a possible exception in some areas. Moisture from previous rains and transpiration by plants drove up the humidity to record levels and the moist humid air mass originated over Iowa previous to and during the early stages of the heat wave. Numerous stations in Iowa, Wisconsin, Illinois and elsewhere reported record dew point temperatures above 80 °F (27 °C) with a peak at 90 °F (32 °C) with an air temperature of 104 °F (40 °C) making for a 153 °F (67 °C) heat index reported from at least one station in Wisconsin (Appleton) [5] at 5:00 pm local time on the afternoon of 14 July 1995, a probable record for the Western Hemisphere; this added to the heat to cause heat indices above 130 °F (54 °C) in Iowa and southern Wisconsin on several days of the heat wave as the sun bore down from a cloudless sky and evaporated even more water seven days in a row.

A few days after, the heat moved to the east, with temperatures in Pittsburgh, Pennsylvania reaching 100 °F (38 °C)[ citation needed ] and in Danbury, Connecticut, 106 °F (41 °C) which is Connecticut's highest recorded temperature. [6] North of the border, Toronto, Ontario reached 37 °C (99 °F), when coupled with record high humidity from the same airmass resulted in its highest ever humidex value of 50 C (122 F).[ citation needed ]

Dewpoint records are not as widely kept as those of temperature, however, the dew points during the heat wave were at or near national and continental records.[ citation needed ]

2-meter temperature (colors) and 500 hPa geopotential heights (contours) for the United States on 1995-07-13 20:00 UTC in the MERRA-2 reanalysis ERAI.png
2-meter temperature (colors) and 500 hPa geopotential heights (contours) for the United States on 1995-07-13 20:00 UTC in the MERRA-2 reanalysis

Analysis

The heat wave was caused by a large high pressure system that traversed across the midwest United States. This system was consistently producing maximum temperatures in the 90's °F (32-38 °C) during the day with minimum temperatures still remaining as high as the 80s °F (27-32 °C) at night, which is abnormal for midwest summer months. [7] The system also brought extremely low wind speeds, along with high humidity. In the MERRA-2 and the ERAI meteorological reanalyses, the system (see figure) moved eastward, becoming indistinguishable by July 18.

Victims

Eric Klinenberg, author of the 2002 book Heat Wave: A Social Autopsy of Disaster in Chicago, has noted that the map of heat-related deaths in Chicago mirrors the map of poverty. [2] [8] Most of the heat wave victims were the elderly poor living in the heart of the city, who either had no air conditioning, or had air conditioning but could not afford to turn it on. Many older citizens were also hesitant to open windows and doors at night for fear of crime. [9] Elderly women, who may have been more socially engaged, were less vulnerable than elderly men. By contrast, during the heat waves of the 1930s, many residents slept outside in the parks or along the shore of Lake Michigan. [2]

Because of the nature of the disaster, and the slow response of authorities to recognize it, no official "death toll" has been determined. However, figures show that 739 additional people died in that particular week above the usual weekly average. [10] Further epidemiologic analysis showed that Black residents were more likely to die than White residents, and that Hispanic residents had an unusually low death rate due to heat. At the time, many Black residents lived in areas of sub-standard housing and less cohesive neighborhoods, while Hispanic residents at the time lived in places with higher population density, and more social cohesion. [2]

Mortality displacement refers to the deaths that occur during a heat wave that would have occurred anyway in a near future, but which were precipitated by the heat wave itself. In other words, people who are already very ill and close to death (expected to die, for instance, within days or a few weeks) might die sooner than they might have otherwise, because of the impact of the heat wave on their health. However, because their deaths have been hastened by the heat wave, in the months that follow the number of deaths becomes lower than average. This is also called a harvesting effect, in which part of the expected (future) mortality shifts forward a few weeks to the period of the heat wave. Initially some public officials suggested that the high death toll during the weeks of the heat wave was due to mortality displacement; an analysis of the data later found that mortality displacement during the heat wave was limited to about 26% of the estimated 692 excess deaths in the period between June 21 and August 10, 1995. Mortality risks affected Black residents disproportionally. Appropriately targeted interventions may have a tangible effect on life expectancy. [11]

In August, the remains of forty-one victims whose bodies had not been claimed were buried in a mass grave in Homewood, Illinois. [12]

Aggravating factors

Impacts in the Chicago urban center were exacerbated by an urban heat island that raised nocturnal temperatures by more than 2 °C (3.6 °F). [13] Urban heat islands are caused by the concentration of buildings and pavement in urban areas, which tend to absorb more heat in the day and radiate more of that heat at night into their immediate surroundings than comparable rural sites. Therefore, built-up areas get hotter and stay hotter.

Other aggravating factors were inadequate warnings, power failures, inadequate ambulance service and hospital facilities, and lack of preparation. [14] City officials did not release a heat emergency warning until the last day of the heat wave. Thus, such emergency measures as Chicago's five cooling centers were not fully utilized. The medical system of Chicago was severely taxed as thousands were taken to local hospitals with heat-related problems.

Another powerful factor in the heat wave was that a temperature inversion grew over the city, and air stagnated in this situation. Pollutants and humidity were confined to ground level, and the air was becalmed and devoid of wind. Without wind to stir the air, temperatures grew even hotter than could be expected with just an urban heat island, and without wind there was truly no relief. Without any way to relieve the heat, even the insides of homes became ovens, with indoor temperature exceeding 90 °F (32 °C) at night. This was especially noticeable in areas which experienced frequent power outages. At Northwestern University just north of Chicago, summer school students lived in dormitories without air conditioning. In order to ease the effects of the heat, some of the students slept at night with water-soaked towels as blankets.

The scale of the human tragedy sparked denial in some quarters, grief and blame elsewhere. [2] From the moment the local medical examiner began to report heat-related mortality figures, political leaders, journalists, and in turn the Chicago public have actively denied the disaster's significance. Although so many city residents died that the coroner had to call in seven refrigerated trucks to store the bodies, skepticism about the trauma continues today. In Chicago, people still debate whether the medical examiner exaggerated the numbers and wonder if the crisis was a "media event." [8] The American Journal of Public Health established that the medical examiner's numbers actually undercounted the mortality by about 250 since hundreds of bodies were buried before they could be autopsied. [10]

Environmental racism

Various aggravating factors in this context have informed discussions about environmental racism, environmental injustice within a racialized context.

In the context of the 1995 Chicago heat wave, principles of environmental racism have been used to better understand the hugely unequal death rates between various groups in the Chicago population. Out of the 739 heat related deaths attributed to the heat wave, it was found that Black citizens died at a much higher rate than their white peers. Further, this finding was statistically significant beyond the consideration of increased rate of death in impoverished areas. [15]

In 2018, filmmaker Judith Hefland created Cooked: Survival by Zip Code, a documentary exploring the unequal death rates observed during the 1995 heat wave. Cooked examines the factors that most directly contributed to these unequal death rates, and posits that such a crisis was not a one time catastrophe, but rather a dangerous trend occurring beyond Chicago.

This documentary examined the particularly devastating impact of various aggravating factors on Black communities. Most directly, the lack of adequate warning and failure to utilize pre-existing cooling centers disadvantaged impoverished groups, and caused particularly devastating effects in Chicago's poorest areas. Hefland warns that Chicago can serve as a model for the environmental racism present in many American cities.

Urban heat islands still exist throughout the United States and beyond, and impoverished, minority groups still disproportionately occupy these at risk neighborhoods. With the number of climate disasters increasing five fold [16] over the past 50 years, the risk to these groups increases as well, and social movements calling for environmental justice have grown in turn.

Statistics

Chicago's daily low and high temperatures in 1995:

Statistics about the averaged July monthly average temperatures from 1960–2016 give us a mean of 74 degrees F and a standard deviation of 2.7. [17]

During the week of the heat wave, there were 11% more hospital admissions than average for comparison weeks and 35% more than expected among patients aged 65 years and older. The majority of this excess (59%) were treatments for dehydration, heat stroke, and heat exhaustion. [18]

Wet-bulb temperatures

Wet-bulb temperatures during the heat wave reached 85 °F (29 °C) in some places. [19] A wet-bulb temperature of 95 °F (35 °C) may be fatal to healthy young humans if experienced over six hours or more for children one month of age as well as the elderly 70 and over. [20]

Related Research Articles

<span class="mw-page-title-main">Humidity</span> Concentration of water vapour in the air

Humidity is the concentration of water vapor present in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew, or fog to be present.

<span class="mw-page-title-main">Dew point</span> Temperature at which air becomes saturated with water vapour during a cooling process

The dew point of a given body of air is the temperature to which it must be cooled to become saturated with water vapor. This temperature depends on the pressure and water content of the air. When the air is cooled below the dew point, its moisture capacity is reduced and airborne water vapor will condense to form liquid water known as dew. When this occurs through the air's contact with a colder surface, dew will form on that surface.

<span class="mw-page-title-main">Extreme weather</span> Unusual, severe or unseasonal weather

Extreme weather includes unexpected, unusual, severe, or unseasonal weather; weather at the extremes of the historical distribution—the range that has been seen in the past. Extreme events are based on a location's recorded weather history. They are defined as lying in the most unusual ten percent. The main types of extreme weather include heat waves, cold waves and heavy precipitation or storm events, such as tropical cyclones. The effects of extreme weather events are economic costs, loss of human lives, droughts, floods, landslides. Severe weather is a particular type of extreme weather which poses risks to life and property.

<span class="mw-page-title-main">Hyperthermia</span> Elevated body temperature due to failed thermoregulation

Hyperthermia, also known simply as overheating, is a condition in which an individual's body temperature is elevated beyond normal due to failed thermoregulation. The person's body produces or absorbs more heat than it dissipates. When extreme temperature elevation occurs, it becomes a medical emergency requiring immediate treatment to prevent disability or death. Almost half a million deaths are recorded every year from hyperthermia.

<span class="mw-page-title-main">Heat index</span> Temperature index that accounts for the effects of humidity

The heat index (HI) is an index that combines air temperature and relative humidity, in shaded areas, to posit a human-perceived equivalent temperature, as how hot it would feel if the humidity were some other value in the shade. For example, when the temperature is 32 °C (90 °F) with 70% relative humidity, the heat index is 41 °C (106 °F). The heat index is meant to describe experienced temperatures in the shade, but it does not take into account heating from direct sunlight, physical activity or cooling from wind.

<span class="mw-page-title-main">Heat wave</span> Prolonged period of excessively hot weather

A heat wave, sometimes known as extreme heat, is a period of abnormally hot weather. High humidity often accompanies heat waves. This is especially the case in oceanic climate countries. Definitions vary but are similar. A heat wave is usually measured relative to the usual climate in the area and to normal temperatures for the season. Temperatures that people from a hotter climate consider normal can be called a heat wave in a cooler area. This would be the case if the warm temperatures are outside the normal climate pattern for that area. Heat waves have become more frequent, and more intense over land, across almost every area on Earth since the 1950s. This is due to climate change.

The 1980 United States heat wave was a period of intense heat and drought that wreaked havoc on much of the Midwestern United States and Southern Plains throughout the summer of 1980. It was among the most destructive and deadliest natural disasters in U.S. history, claiming at least 1,700 lives. Because of the massive drought, agricultural damage reached US$20 billion. It is among the billion-dollar weather disasters listed by the National Oceanic and Atmospheric Administration.

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<span class="mw-page-title-main">Wet-bulb temperature</span> Temperature read by a thermometer covered in water-soaked cloth

The wet-bulb temperature (WBT) is the temperature read by a thermometer covered in water-soaked cloth over which air is passed. At 100% relative humidity, the wet-bulb temperature is equal to the air temperature ; at lower humidity the wet-bulb temperature is lower than dry-bulb temperature because of evaporative cooling.

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<span class="mw-page-title-main">Air conditioning</span> Cooling of air in an enclosed space

Air conditioning, often abbreviated as A/C (US) or air con (UK), is the process of removing heat from an enclosed space to achieve a more comfortable interior environment and in some cases also strictly controlling the humidity of internal air. Air conditioning can be achieved using a mechanical 'air conditioner' or by other methods, including passive cooling and ventilative cooling. Air conditioning is a member of a family of systems and techniques that provide heating, ventilation, and air conditioning (HVAC). Heat pumps are similar in many ways to air conditioners, but use a reversing valve to allow them both to heat and to cool an enclosed space.

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<span class="mw-page-title-main">Eric Klinenberg</span> American sociologist

Eric M. Klinenberg is an American sociologist and a scholar of urban studies, culture, and media. He is currently Helen Gould Shepard Professor in Social Science and Director of the Institute for Public Knowledge at New York University. Klinenberg is best known for his contributions as a public sociologist.

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References

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