| Unit
1: What Are Environmental Hazards?
Background Information |
| Introduction to Environmental Hazards and this Module |
The purpose of this module is to understand the nature, distribution, and impacts of hazards and disasters worldwide and to examine how global changes will affect human vulnerability to such events. To do so, we address this complex subject through the following five questions (see also Cutter 1996):
In this unit, we lay the groundwork to address these
questions. We begin by taking a critical look at people’s perception of
hazards and the implications of different perceptions on the measurement
of hazard trends and on the individual, communal, and societal responses
to hazards. Building upon that critical awareness, we then examine some
commonly used terms and concepts in order to have a common language with
which to speak about past and future hazards trends and the ways in which
we attempt to lessen the dangers of living in an ever-changing world. In
this module, we use focus issues to highlight problematic aspects
of being confronted with hazards. You may want to discuss the questions
that accompany each focus issue with your classmates.
| When is Something a Hazard? |
The second argument challenging the notion that certain
phenomena are inherently hazardous is a little less obvious but even more
important than the first: what is a hazard to you may not be a hazard for
me. Here are a few examples.
| It is floodtime in Bulozi
There is the floodplain clothed in the water garment Everywhere there is water! there is brightness! there are some sparkles! Waves marry with the sun’s glory Birds fly over the floods slowly, they are drunken with cold air they watch a scene which comes but once a year floods are tasty (nice, beautiful) Bulozi is the floods’ place of abode every year the floods pay us a visit. |
A Lozi does not beg for floods
We do not turn the herbs to have floods We do not practice witchcraft whatsoever They are floodwaters indeed! The floods know their home area. Floods are ours the floods themselves they (floods) know their own route they know their home area they know where they’re needed they know where they are cared for And when we ourselves see them we are inflated with happiness our hearts become lighter we do not fear floods ... |
We should inject a note of caution. To say that a hazard to some may be a completely different experience for another is a heavily subjectivist position, meaning that reality is simply what we say or think it is; it’s all in our minds and there is no "external" foundation for whatever we perceive. To be sure, there are some thinkers who maintain such a position, but we do not adopt it in this module. Whether or not you perceive driving without a seat belt as hazardous, it does kill people; whether or not you perceive smoking as a hazard, countless studies show that your health is negatively affected by smoking. By analogy, to take a purely objectivist position and say that hazard perception is irrelevant because there is only one external reality and that’s all we need to worry about is insensitive to the reality of human beings and their experiences. Although in this module we repeatedly emphasize the importance of hazard perception, it is no longer the hottest or most pressing aspect of hazard studies.
Our perceptions of a hazard are influenced by factors such as personal experience with a hazard, varying knowledge of a hazard, different outlooks on the world (God, nature, technology, society, government, self, etc.), culture, gender, wealth, age, the personal and professional roles we have taken on, and adjustments and adaptations to the hazard we have managed. When we ask big questions like "Are things getting better or worse?" or "Is the world becoming more disastrous?" there can be no straightforward answer. We have to question the point of view from which someone would answer these questions, and we have to be aware of the context in which a statement is being made. For example, the answers to such questions are likely to differ between an insurer, an insured home owner, and someone who just lost insurance -- even though they may all speak about property losses from floods.
Similarly, responses to hazards will differ depending on people’s hazard perception and personal circumstances. If you are 10 years old and a major blizzard keeps you at home because schools are closed, you might celebrate the day by building a snowman or hanging out with friends. If you are a parent who is expected to be at work and can’t afford the loss of pay or a babysitter, that blizzard is not a source of joy!
The same caution about perceptions and responses applies to hazards associated with global environmental change. Scientists say that the effects of global climate change, for example, are likely to benefit some regions of the world while harming others. Superimposed on this unevenness in the effects of global change are differing perceptions of such changes, i.e., what we do and don’t perceive, and how we judge these changes.
When we look at hazard trends, these differing hazard perceptions put us in a quandary. On the one hand we would like to appreciate differences in perceptions; on the other hand, in order to discern trends, we need measures of frequency or occurrence, and these measures need to be based on the same definition of a hazard over time to ensure comparability. In the next section we provide some common definitions of hazard-related terminology to allow us to look at trends from a common viewpoint and to connect with the scientific hazard literature. We will continue to point out, however, in the text and in the activities, how differences in perception of and responses to hazards and environmental change affect the discussion of trends and responses to hazards.
| Establishing a Common Language: Some Definitions |
| Types of Hazards |
Other hazards originate in social systems and include
terrorism (domestic bombing such as the Oklahoma City incident as well
as international acts of terrorism), warfare, epidemics
(such as the Ebola virus), and civil disorder or ethnic violence (such
as in Bosnia and Rwanda). The interaction of society, technology, and natural
systems produces another type of hazard often called technological
hazards. Nuclear power plant accidents such as the one at Chernobyl,
industrial accidents like the one in Bhopal, oil spills, and hazardous
materials spills all fall under in this category. Finally, there is a group
of hazards that do not stem from one event but rather arise from more chronic
conditions, including famine,
resource degradation,
pollution, and
large-scale toxic contamination. These chronic
hazards are the type that will be most affected by changes in the
global environment. A broader term like human-induced hazards is necessary
to encompass the last two categories of hazards (technological and chronic
types of dangers) and the above-mentioned hazards like warfare, terrorism,
and epidemics.
| I. Extreme Natural Events | |
| Meteorological | |
| Hydrologic | drought, flash floods, conventional floods |
| Atmospheric | hurricanes, cyclones, tropical storms, tornadoes |
| Geophysical | |
| Seismic | earthquakes, tsunamis, volcanoes |
| Geomorphic | mass movements, landslides |
| II. Common Natural Events | |
| Meteorological | wind and dust storms, temperature extremes (heat waves, frost), severe summer storms (lightning, hail), winter storms, coastal erosion, drought |
| Geophysical | avalanches, soil subsidence, coastal erosion |
| Other | wildfires |
| III. Biologic Agents | |
| Epidemics | AIDS, influenza, cholera, Ebola |
| Infestations | rabbits, termites, locusts, grasshoppers, bees |
| Other | recombinant DNA, bioengineering |
| IV. Social Disruptions | |
| Civil disorders | ethnic violence, riots, urban fires due to arson |
| Terrorism | local terrorism, global terrorism, bombings |
| Warfare | conventional war, chemical/biological weapons |
| V. Technological Hazards | |
| Extreme failures | nuclear accidents, industrial accidents, dam breaks |
| Common occurrences | power failures, radon, hazardous materials spills, oil spills, hazardous materials, transportation accidents |
| VI. Chronic/Globally Catastrophic Hazards | |
| Multiple types | pollution, environmental degradation, poverty, climate change, nuclear war, famine |
| Hazard Characteristics |
Magnitude describes the strength or force of an event. In order to assess the magnitude, one must first have a base line for comparison. In the case of floods for example, magnitude is often described as the maximum height of flood waters above average sea level, flood stage, or simply above ground. For seismic events, magnitude is measured on the Richter scale which is an estimate of the amount of energy released by an earthquake (see Table 2). But the strength of an event can also be measured by more than its physical characteristics. Intensity provides a useful measure of the severity of an event based on the subjective human experience of it. For example, the Modified Mercalli scale (see Table 3) measures the intensity of earthquakes based on damage to structures and the human experience of the event. For hurricanes, the Saffir-Simpson scale is a measure of both intensity and magnitude. It evaluates hurricane strength and impact based on a five-point scale with Category 5 hurricanes listed as the most severe and destructive (Table 4).
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| *The signals of seismic waves from which
energy release is calculated can vary in strength by factors of 100 million.
To accommodate this range, the Richter scale is logarithmic, i.e., the
magnitude of an earthquake increases tenfold from one Richter number to
the next (Skinner and Porter 1992, 413).
**The energy release from one Richter magnitude to the next increases roughly 30 times (31.6 to be exact), thus the energy release from an earthquake with Richter magnitude 3 is 31.6 x 31.6 x 31.6 = ~1000 times bigger than the energy release of an earthquake with Richter magnitude 1, hence the multiplication factors in this column. |
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| Class |
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| I | Not felt except by a very few under exceptionally favorable circumstances. |
| II | Felt only by a few persons at rest, especially on upper floors of buildings. Delicately suspended objects may swing. |
| III | Felt quite noticeably indoors, especially on upper floors of buildings, but many people do not recognize it as an earthquake. Standing automobiles may rock slightly. Vibration like passing truck. Duration estimated. |
| IV | During day felt indoors by many, outdoors by few. At night some awakened.
Dishes, windows, doors disturbed; walls make creaking sound. Sensation
like heavy truck striking building. Standing automobiles
rocked noticeably. |
| V | Felt by nearly everyone, many awakened. Some dishes, windows and soon broken; cracked plaster in a few places; unstable objects overturned. Disturbance of trees, poles and other tall objects sometimes noticed. Pendulum clocks may stop. |
| VI | Felt by all, many frightened and run outdoors. Some heavy furniture moved; a few instances of fallen plaster and damaged chimneys. Damage slight. |
| VII | Everybody runs outdoors. Damage negligible in buildings of good design and construction; damage slight to moderate in well-built ordinary structures; some chimneys broken. Noticed by persons driving cars. |
| VIII | Damage slight in specially designed structures, considerable in ordinary substantial buildings with partial collapse, great in poorly built structures. Panel walls thrown out of frame structures. Fall of chimneys, factory stacks, columns, walls, and monuments. |
| IX | Damage considerable in specially designed structures; well-designed
frame structures thrown out of plumb; damage great in substantial buildings,
with partial collapse. Buildings shifted off foundations. Ground cracked
conspicuously. Underground pipes broken. |
| X | Some well-built wooden structures destroyed; most masonry and frame
structures destroyed with foundations; ground badly cracked. Rails bent.
Landslides considerable from river banks and steep slopes. Shifted sand
and mud. Water splashed, slopped over banks. |
| XI | Few, if any (masonry) structures remain standing. Bridges destroyed. Broad fissures in ground. Underground pipelines completely out of service. Earth slumps and land slips in soft ground. Rails bent greatly. |
| XII | Damage total. Waves seen on ground surface. Lines of sight and level distorted. Objects thrown into the air. |
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Description |
| One | Winds 74-95 MPH. Storm surge 4-5 feet above normal. Minimal damage to buildings. Damage to trees, shrubs, and unanchored mobile homes. Minor pier damage, some coastal road flooding. |
| Two | Winds 96-110 MPH. Storm surge 6-8 feet above normal. Some roof, door, and window damage to buildings. Damage to vegetation, mobile homes, and piers. Boats break loose from moorings. Coastal escape routes are flooded. |
| Three | Winds 111-130 MPH. Storm surge 9-12 feet above normal. Structural damage to homes and utility buildings. Mobile homes destroyed. Coastal flooding destroys small structures; floating debris damages large structures. Land lower than 5 feet ASL (above sea level) may be flooded inland 8 miles or more. |
| Four | Winds 131-155 MPH. Storm surge 13-18 feet above normal. Extensive infrastructural damage to homes and buildings. Roofs collapse or are blown off. Major erosion of beaches. Major damage to lower levels of structures near the coast. Land lower than 10 feet ASL is flooded. Massive evacuation of residents 6 miles inland. |
| Five | Winds greater than 155 MPH. Storm surge greater than 18 feet above normal. Complete roof failure on industrial buildings and homes. Some buildings completely collapsed. Major damage to lower floors of all structures less than 15 feet ASL. Massive evacuation of residential areas on low ground within 10 miles of the shoreline. |
| *This scale is used to give estimates of property damage and potential flood levels along the coast in the event of a hurricane. | |
Speed or rate of onset refers to the length of time between the first appearance of the event and its peak. We can think of rapid onset events such as tornadoes and nuclear power plant accidents or slow onset hazards such as soil erosion, pollution, or drought. The speed of onset is a characteristic of a hazard that is crucial in our efforts to avoid some of the worst impacts of hazards. In other words, much of modern hazard management effort is geared toward improving our ability to detect signs of an impending hazard event as early as possible so as to expand the time between signal detection and the peak of the event for warning and possibly evacuating vulnerable populations.
Temporal spacing describes the sequencing and seasonality of events. Some hazards are quite random in their timing (industrial accidents, volcanic eruptions), whereas other hazards have a seasonal or regular periodicity (tornadoes, hurricanes). The implications of temporal spacing for hazard management are quite clear; if you can expect certain hazards to be more likely in certain seasons or at relatively regular intervals, you can be ready to communicate the risk to potentially affected populations in a timely manner, and mount the necessary efforts to allow you to respond more quickly and effectively to an emergency. Hurricane Bertha in July 1996 serves as a good example. After much criticism of the delayed federal response to Hurricane Andrew, the federal government issued a Presidential statement before Bertha’s landfall that the emergency response teams were in place and ready for whatever may come (National Public Radio, July 12, 1996). Randomly occurring hazards are much more challenging to emergency response agencies because they require a low level of preparedness at all times for the rare case that requires quick, efficient, and effective responses.
The next two characteristics of a hazard allow us to examine its geographic extent. Areal extent is a measure of the space covered by an event. Some hazards like a tornado or a small gasoline spill may have a small areal extent; others such as droughts or major nuclear accidents (like the one at Chernobyl in 1986), affect large geographic regions. Spatial dispersion refers to the distribution of hazards over the space in which they can occur. Spatial dispersion is a useful measure of the geography of hazards because it differentiates between hazards that occur within a particular region and those that are more widespread. For example, although tornadoes can occur just about anywhere in the US, they primarily occur in the "tornado belt" of the Central Plains from Texas to Nebraska.
A final hazard characteristic refers to the nature of exposure, which is an important concern in reducing risk and mitigating the impact of hazards. For example, is exposure voluntary or involuntary? With many environmental hazards, we have little control over whether or not we are exposed to them; we can neither control the weather nor stop earthquakes. On the other hand, we do have some degree of choice (voluntariness) about where we live (e.g., floodplains, coastal regions), what kind of food we eat (e.g., organically or commercially grown produce), or what types of activities we engage in (e.g., scuba diving, using drugs, or smoking) that directly affect our vulnerability to some hazards. Parts 1 and 2 of Focus Issue 1 highlight issues of frequency, magnitude, and the nature of exposure for flood hazards and provide a concrete example from South Africa.
| Focus Issue 1 -- Part 1: Living on the Edge:
Why on Earth in the Floodplain?
Very few places on earth are not vulnerable to floods, except for the highest mountain tops and under present climate conditions, huge expanses of deserts such as the Gobi or the Sahara. The areal extent of flooding events is often vast and some places experience prolonged durations that result in a heavy toll. An example of a flood that brought large financial losses is the 1993 flood in the Midwestern US; disastrous losses of life are periodically seen in China and other Southeast Asian countries. Flooding accounts for 40% of all natural disasters with more than one hundred deaths per event (Burton, Kates, and White 1993). This enormous toll is due to the extent and frequency of flooding, the fact that people live and work in areas prone to flooding, and inadequate warning of the approaching dangers. Given these facts, why do people continue to live in riverain and coastal areas bound to be flooded? Floodplains are areas defined as most at risk from flooding, both riverain and coastal. The areal extent of the flood varies with the magnitude of storms, the rapidness of snowmelt, the height of the storm surge, and other geographic factors. Yet floodplains are also among the most attractive areas for human occupance; they are level, easy to build on, and they have very fertile soils. Coastal areas, in addition, offer access to, and sometimes a much desired view of, the ocean. In the United States, the federal government is most concerned with flooding in what is called the 100-year floodplain. The 100-year flood recurrence interval refers to a probability of at least 1% that an area will be flooded in any given year. This corresponds to the flood levels expected on the long-term average of once every one hundred years, hence the often misinterpreted term "100-year flood" (USGS 1995). It is important to note that only the outermost edges of the 100-year floodplain have a risk as low as 1% per year (Platt 1996). As one moves closer to the stream channel or tide line, the risk increases progressively. This kind of recurrence terminology, unfortunately, has the effect of making the flood hazard sound remote and not worthy of attention by those at risk. People think that they will be gone or not using the area anymore by the time the next flood event is expected to occur. This misunderstanding is cause for great concern. To the engineers and hydrologists who delineate the 100-year floodplain, flooding events are random, meaning that the probability of their recurrence is the same each year (1 in 100 or 1%). For those at risk, however, there has been a demonstrated tendency to assume that a severe hazard occurrence such as a 100-year flood is followed by a period of lessened hazard activity (Burton, Kates, and White 1993). This partly explains why activity in and occupance of hazardous areas increases. Experience with the flood hazard is frequency-dependent and as such, new arrivals to the hazardous area may be less accurate in their judgement of the flooding risk. This is especially important with respect to the prospects of global change; flood frequencies and magnitudes might increase both because of changes in climate and rising sea levels and because of increasing numbers of people moving into flood-prone areas, rapid urbanization, and poverty. The threat to life and property associated with flooding is expected to increase without intervention -- that is, even if climate will not change in the future. Appropriate intervention aimed at reducing disaster proneness must address population increases in the hazardous floodplain directly as well as upstream watershed management (e.g., farm management techniques to reduce filling up of stream channels with sediment) and the over-reliance on technology, structural protection measures, and insurance, all of which foster a false sense of safety behind levees and insurance policies. Living with nature, rather than over-engineering and conquering it, clearly calls for a new approach to floodplain management. |
| Focus Issue 1 -- Part 2: Six Feet of Water Over
the Desert Floor: South Africa
In 1981, the small town of Laingsburg in the Small Karoo in South Africa (an inland semi-desert area) experienced one of the worst floods in the history of the country. Along with a mortality level unprecedented in South Africa for flood events, the flood changed the natural and urban landscape of the affected area beyond imagination. Like that of many towns in the Karoo, the pre-flood urban landscape of Laingsburg was characterized by older houses and municipal buildings with charming styles of architecture dating back to earlier times. Most of these were destroyed in the disastrous flood, fundamentally altering the character of the town. Moreover, the flood significantly changed the natural course of the Buffels River causing changes in town lay-out and zoning in its wake. The flood was an extraordinary event in many respects. First, the weather patterns at the time were highly unusual. In the winter, the southern part of the country is commonly affected by low pressure systems that move from the south-west and bring cold fronts. Usually the fronts don't have much effect on the Small Karoo in terms of significant rainfall (it is, after all a semi-arid area), or the effects are very short-lived as the fronts pass over swiftly. On this occasion, however, the atmospheric circulation over the subcontinent gave rise to a condition known as a "cut-off low" or a low pressure system that is effectively "anchored" in place by the way neighboring pressure systems are positioned over one area. This almost stationary low gave rise to very high volumes of rainfall over a larger area including Laingsburg -- rainfall that also persisted for an unusual amount of time. Second, and unsurprisingly, people did not expect and were unprepared for the suddenness and volume of the flood. Given the low expectancy of floods in the semi-arid area, many houses, shops, and even a senior citizens’ home had been built along the banks of the river. During the event, as the flood waters began to rise, curious passers-by came down to the banks to watch the exciting event. Cars traveling on the nearby main highway that connects Johannesburg and Cape Town (the N1) slowed or stopped to see the rushing waters. According to eyewitnesses, several vehicles had pulled over on the bridge crossing the Buffels River itself to watch in fascination. As the first torrent of water roared down the river bed, part of the bridge and the occupants of the vehicles on it were swept away. There were other tragedies and instances of heroism; as the water rose, residents of the old age home who were able climbed onto the roof of their building but were unable to escape. A married couple was swept downstream as they attempted to save other victims, but both were strong enough swimmers to be able to swim ashore and escape dangerous debris. A third aspect makes this flood unusual: the patterns of destruction affected not the poorest people of town (as is often the case given typical socioeconomics of floodplain occupation), but the better-off. Buildings near the river were largely owned and occupied by higher-income, white people in a town that at the time was still segregated by apartheid. Ironically, the flood devastated these areas and left the poorer townships on the hillside and on higher ground mostly untouched. Today, the town has been rebuilt although without its former charm. Travelers on the N1, some of whom knew the town before the flood, drive through the center of the small town to find a sign in the middle of the main street that indicates the flood level. It stands at well over 6 feet tall in the desert landscape. QUESTIONS: · Why are flood losses (lives and property) increasing and what can be done to stop this trend? |
| The Role of Geography in Hazard and Global Change Research |
These developments in the hazards field have been influenced by and have helped to shape the global environmental change research agenda. For example, research has focused on the difficulty of discerning natural versus human shares in causing global changes, the heavily politicized and ethically loaded debate over how to mitigate the impacts of global change, the role of technology in causing and responding to global change, and the economic challenges and social choices we face in responding to global changes. The hazard research agenda has been extended to include large-scale, regional-to-global, slow-onset, and cumulative hazards in response to the needs of the global change research community (Burton, Kates and White 1993; Mitchell 1989). Likewise, the global change community has borrowed impact assessment methodologies, notions of risk and uncertainty, and other concepts and approaches from hazards research to address global problems.
In addressing these complex questions, geography can play a pivotal role. Both the hazards and global change fields have traditionally been interdisciplinary and in the last few years, geographers have become increasingly involved. Geographic scale is crucial to understanding hazards distribution, impact, and reduction (Cutter 1994). The discovery of new hazards and the rediscovery of older ones with more dispersed and cumulative impacts necessitate the globalization of risk and hazard management systems. Unfortunately, because of the enormous difficulties of conducting truly global studies, much hazard research continues to be in the form of local or regional case studies. The articulation between local and global processes will continue to challenge geographers and other researchers.
Geographers also contribute their expertise on the linkages among physical processes and human contexts. This helps us to understand better the causal mechanisms that bring about hazards and disasters, and is of great importance to hazard management. This expertise also helps define the areal extent of the hazard, one of the important characteristics of hazards.
In summary, many linkages exist between hazards and global environmental change research, and geographers have much to contribute. In fact, geographers with expertise in environment-society interactions at different scales, an interest in historical and future trends, and a keen awareness of the ways in which different societies perceive these relations are situated at the intersection of hazards and global change research.