Unit 1:  What Are Environmental Hazards? 
             Background Information
 
 
 
Introduction to Environmental Hazards and this Module 
 
    The first half of the 1990's was riddled with unprecedented disasters -- earthquakes in Northridge, California (1994), and Kobe, Japan (1995); tropical cyclones and flooding in Bangladesh (1991); volcanic eruptions (Mt. Pinatubo in the Philippines in 1991); flooding during 1993 in the Northwest US and along the Mississippi River; and the most costly disaster to date in the US, Hurricane Andrew (1992), to name just a few of the most notable ones. Will climate change and other global environmental changes mean that we will see even more disasters in the future? Or are disasters like those mentioned above already evidence of the worsening interaction of hazards and global environmental changes?

    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):

  1. Are societies becoming more vulnerable to environmental hazards and disasters? If so, which hazards may intensify in the future as a consequence of global environmental changes?
  2. What social/physical factors influence changes in human occupance of hazard zones?
  3. How do people respond to environmental hazards and what accounts for differential adjustments (in the short term) and adaptation (in the longer term)?
  4. How do societies mitigate the risk of environmental hazards and prepare for future disasters?
  5. How do local risks and hazards become the driving forces behind global environmental changes?
    These questions not only guide Units 2 and 3 and the accompanying activities, they also mark the frontier of contemporary hazards research.

    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? 
 
    Before we look at specific hazards, hazard characteristics, and trends in hazard occurrences, let’s begin with a simple yet profound question -- When is something a hazard? You may think it’s a silly question. Floods, earthquakes, severe thunderstorms, pesticides, and toxic or oil spills immediately come to mind, somehow implying that all these things are inherently hazardous. At least two arguments challenge the notion that things are inherently hazardous, however. The first is that if no people (or things that people value, such as their homes and belongings, a beautiful landscape, or a clean beach) are harmed, then a phenomenon isn’t hazardous; the event would simply happen without anyone or anything being affected negatively. "Well," you might say, "but what about animals or ecosystems?" That question simply proves the point; it indicates that you value animals or ecosystems as important, precious, or beautiful and that you feel something could harm them. From this perspective, a severe windstorm that topples trees, uproots vegetation, and injures creatures on the ground would be a hazard to animals and ecosystems.

    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.
 

  1. But, after all, there is at least one or two things about that weather (or, if you please, effects produced by it) which we residents would not like to part with. If we hadn’t our bewitching autumn foliage, we should still have to credit the weather with one feature which compensates for all its bullying vagaries -- the ice-storm: when a leafless tree is clothed with ice from the bottom to the top -- ice that is as bright and clear as crystal; when every bough and twig is strung with ice-beads, frozen dewdrops, and the whole tree sparkles cold and white, like the Shah of Persia’s diamond plume. Then the wind waves the branches and the sun comes out and turns all those myriads of beads and drops to prisms that glow and burn and flash with all manner of colored fires, which change and change again with inconceivable rapidity from blue to red, from red to green, and green to gold -- the tree becomes a spraying fountain, a very explosion of dazzling jewels; and it stands there the acme, the climax, the supremest possibility in art or nature, of bewildering, intoxicating, intolerable magnificence. One cannot make the words too strong.
    1. -- Mark Twain. 1876. The Weather -- Address at the New England’s Society’s 71st Annual Dinner, New York City, December 22, 1876. (Cited from New England’s disastrous weather, p.226.)
       
  2. They like to tell the one about the farmer selling apples under a big sign that reads ‘Apples from Chernobyl.’ ‘You must be mad,’ a passerby said. ‘No one wants to buy apples from Chernobyl.’ ‘Sure they do,’ the farmer said. ‘Some buy them for their mothers-in-law, some people buy them for their wives.’ Others downplay the risk. ‘All I know is that we’ve been eating the food around here for almost 10 years, and we feel fine,’ said Olina Nikolayeva, 65, one of several hundred people who have moved back into the Ukrainian village of Opachichi, 15 miles from the reactor. ‘You can eat the apples, but you have to bury the seeds deep in the ground,’ Nikolayeva said. ‘You can eat mushrooms, but only up to 10 kilograms. And if you feel too much radiation, you have to drink some vodka.’
    1. -- Excerpt from Filipov, David. 1996. In Chernobyl soil, fatalism thrives. The Boston Sunday Globe, April 21: 17. © Reprinted courtesy of David Filipov. The Boston Globe 1996.
     
  3. I grew up in the 1970s in Taipei. Every summer of my childhood it was unbearably hot and humid, and quite often a typhoon attacked Taiwan. Even though this was twenty years ago, I can vividly recall what happened to our home and neighborhood year after year until the government constructed underground waterworks. It happened almost every June. The rain brought by the typhoon flooded the school up to its second floor. All the houses in our compound were covered with water on the first floor. As soon as we were warned to expect a downpour, we started to clear the gutter around the house and tried to place our furniture on higher ground. All we could do was to grab our valuables; refrigerators, beds, and the piano all got soaked in the water. We had to spend the nights at our neighbors’ home on the third floor. We counted the hours in the dark in fear and simply could do nothing else because of the black out and the suspension of the water supply. Some neighbors were more happy-go-lucky than we were and went as far as to sit around a table playing Majong by candlelight to kill time. The ruined furniture, electric appliances, and mud from the hillside formed a heap on the street. The talk of the day centered on how much each family had lost and whose car had been soaked with mud and water. The neighborhood stores got a lot of business since everyone rushed to buy and hoard food. The neighbors got acquainted with each other after going through the same experiences. After a while, everything went back to normal. Flooding was an event to go through each summer. It would be a surprise if there was no devastating typhoon in June. The government was never blamed, but instead when residents received food sent by the agencies, they expressed gratitude toward the government. The children were happy not to have to go to school. It was an opportunity for them to go rafting on the flooded streets. Seldom would neighbors speak of moving away because they could not afford to buy an apartment elsewhere. The nightmares of typhoons finally stopped haunting us in 1986 when the government finished the underground water works.
    1. -- A graduate student at Taiwan National University. 1996. Personal account of typhoon and flood memories. Provided by Nora Chiang, Taiwan National University.
       
  4. I think the economic logic behind dumping a load of toxic waste in the lowest wage country is impeccable and we should face up to the fact that ... underpopulated countries such as Africa are vastly underpolluted.
    1. -- Lawrence Summers (Former Chief Economist of the World Bank) December 1991; cited in Puckett, Jim. 1994. Disposing of the waste trade: Closing the recycling loophole. The Ecologist 24, 2: 53-58 (quote from p.53).
  1. Floods in Bulozi (Western Zambia)
  2. 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 ...
               -- Excerpt from a poem translated from Sibetta, O.K. 1983. Fa Manunga Wa Lyambai, Lusaka, Neczam. Source: Namafe, Charles and Frances Slater. 1995. Floods: Friends or enemies? Geographical Education 8, 3: 57-62 (complete poem on p.57) 
     
    All of these excerpts demonstrate that a "hazard" isn’t always a hazard and is definitely not always perceived as one. A hazard to some is to others a business opportunity, a spiritual moment, a joyful experience, a culturally significant if not defining moment, a down-played or even denied reality, "no big deal" at all, or just a common everyday kind of event. On the other hand, what is "normal" or even necessary to some is loaded with the most dreadful fears for another. Wildfires are a case in point; while certain tree species need fires for their seeds to be liberated from protective cones to insure the species’ reproduction and survival, the owner of a multi-million dollar home destroyed by the same fire is likely to have a very different perspective.

    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
 
    The terms risk, hazard, and disaster are often used interchangeably although each has a precise and distinct meaning. Hazard is the broadest term and reflects a potential threat to humans as well as the impact of an event on society and the environment. Risk refers to the likelihood or probability of occurrence of an event. Hazards include risk (i.e., a probability), impact (or magnitude), and contextual (sociopolitical) elements. Quite simply, hazards are threats to people and the things they value (Cutter 1993). They are in part socially constructed by people’s perceptions and their experiences. Moreover, people contribute to, exacerbate, and modify hazards. Thus, hazards can vary by culture, gender, race, socioeconomic status, and political structure as well. Disasters, in contrast to risks and hazards, are singular or interactive hazard events (like those mentioned in the first section) that have a profound impact on local people or places either in terms of injuries, property damages, loss of life, or environmental impacts. Finally, vulnerability is the potential for loss or the capacity to suffer harm from a hazard. The term, used in various ways by researchers, can generally be applied to individuals, society, or the environment.
 

 
Types of Hazards
 
    It is the interaction among nature, society, and technology that produces hazards, risks, and disasters, many of which may be amplified by global environmental changes currently underway. Hazards arise from many different sources (summarized in Table 1 below), and considerable research effort has focused on developing typologies of hazards to establish some order in an ever-increasing list of hazards (e.g., Hohenemser, Kates, Slovic 1985; Cutter 1993). Many of the typologies use the causes or origins of hazard events as the classifying principle. In most cases, however, hazards are multi-causal so that most researchers now refrain from proposing single cause-based typologies of hazards. Yet it is possible to classify hazards according to the area in which they mainly originate. Those originating from natural processes are referred to as natural hazards. Examples include earthquakes, volcanic eruptions, floods, hurricanes, blizzards, and tornadoes. These phenomena vary regionally and seasonally and may trigger secondary hazards. For example, landslides and tsunamis can follow earthquakes. Thunderstorms may be accompanied by heavy rains that can cause mudflows, flash floods, and conventional flooding. Hazards also arise from rather common natural events such as hail, coastal erosion, heat waves, and droughts, all of which can cause considerable damage to the natural environment and society.

    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.
 

Table 1: Origins of Environmental Hazards
 
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
Source:  Compiled by authors.
 
 
 
Hazard Characteristics
 
    The characteristics of hazards that enable us to compare hazards over time and space include magnitude, intensity, frequency, and duration. After all, we are not just interested in the type and occurrence of hazardous events; we also want to know whether there are any systematic changes in their severity.

    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).

 
Table 2: Richter Scale
 
Richter Number*
Energy Release (in ergs)
In Multiples of Base**
Mercalli Number
1-2
4.47 x 1012
1-31.6
I
3
7.94 x 1014
1,000
II-III
4
2.51 x 1016
31,600
IV-V
5
7.94 x 1017
1,000,000
VI-VII
6
2.51 x 1019
      31,600,000
VIII
7
7.94 x 1020
  1,000,000,000
IX-X
2.51 x 1022
31,600,000,000
XI-XIII
*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. 
Source:  Adapted from Burton, Kates, and White. 1993. Environment as hazard, 2nd edition.  Guilford Press, p. 37. 
© 1993 Guildord Press.  Reprinted with the permission of Guilford Press. I. Burton, R. Kates, and G. White. 
 
 
Table 3: Modified Mercalli Scale
 
Class
Intensity value and description
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.
Source:  Zirbes, Madeleine. October 14, 1997.  Modified Mercalli Intensity Scale.  United States Geological Survey, National Earthquake Information Center.  http://wwwneic.cr.usgs.gov/neis/general/handouts/mercalli.html  (June 21, 1998).
 
 
 
Table 4: Saffir-Simpson Hurricane Scale*
 
Category           
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. 
Source:  Maher, Brian and Jack Beven. March 31, 1998.  The Saffir-Simpson Hurrican Scale. The National Hurricane Center.  http://www.nhc.noaa.gov/aboutsshs.html (June 17, 1998).
 
 
    Frequency describes how often an event of a given magnitude or intensity occurs. This can be given in qualitative terms such as "frequent" or "rare," or in more quantitative estimates such as recurrence intervals. For floods, a recurrence interval of 10 years suggests that in any year, a flood of that magnitude has a 1 in 10 (10%) chance of occurring. Duration is another temporal dimension that describes how long an event persists. This can range from periods as short as several minutes to periods as long as decades or more.

  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: 

· If you knew someone who was about to move into an area delineated as a floodplain, what would you say to this person? 
· 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 
 
    At the beginning of this unit, we posed five questions that we will address in this module:

  1. Are societies becoming more vulnerable to environmental hazards and disasters? If so, which hazards may intensify in the future as a consequence of global environmental changes?
  2. What social/physical factors influence changes in human occupance of hazard zones?
  3. How do people respond to environmental hazards and what accounts for differential adjustments (in the short term) and adaptation (in the longer term)?
  4. How do societies mitigate the risk of environmental hazards and prepare for future disasters?
  5. How do local risks and hazards become the driving forces behind global environmental changes?
    A number of factors prohibit simple answers to these questions. First, as we demonstrated above our perceptions and conceptualizations of hazards have changed over time. We no longer think of hazards as singular, purely natural events (as in "acts of God") or as purely technical disasters (brought about by "human fault or failure") but rather as more complex phenomena involving the interaction of natural, social, and technological systems. Thus, hazard typologies based only on the origin of events in the geophysical or the technological realms are no longer tenable; neither is the resulting distinction between purely natural and purely technological hazards. Second, we now think of impacts of, and responses to, hazards as embedded in our social and environmental systems. It is increasingly difficult, if not impossible, to separate the impacts of specific disasters or hazards from broader social and environmental issues. As a consequence, hazard management systems have become more complex and politicized as the range of management alternatives has expanded to include not only geotechnically expedient "solutions" but also options that require decisions made on the basis of social choices (Mitchell 1990; Kates 1985).

    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.