global climate change coupled with an increasing world...
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Global climate change coupled with an increasing world population, provide a sufficient
rationale for the continued research of natural hazards. As the magnitude and frequency
of hazards increase, there are correspondingly more people placed in harms way. In
order to ensure adequate management practices, it is important to understand both the
physical and perceived risks that are associated with these hazards. I have conducted a
review of geomorphology literature to evaluate the role geomorphologists have in the
management of natural hazards. It is obvious that geomorphology contributes useful
research to the physical processes that cause natural hazards. Attributes such as
magnitude, frequency, and spatial scale of hazards are important elements in their
prediction. Some of the most useful geomorphologic contributions include a
multidisciplinary approach, the establishment of physical risk, prediction methods, and an
international area of focus on developing countries. Through such contributions, it is
hopeful that the urgency of research for both the physical and social aspects of natural
hazards will be fulfilled for the benefit of future management.
Introduction
In a valedictory address given in 1989, H.T. Verstappen stresses the importance
of focusing scientific efforts on global climate change and the study of natural hazards.
Dr. Verstappen is a geomorphologist at the Institute for Aerial Survey and Earth Sciences
in Enschede, Netherlands. He states, “large numbers of people in all parts of the world
are in imminent danger of falling victim to natural disaster, and the pace of global change
is such that we probably have only a few decades to respond adequately and to survive”
(Verstappen, 1989, p.162). Although this is an extreme statement, in 1989 his urgency
for new focus on this research is warranted (Verstappen, 1989).
The shifting global climate contributes to an increase in the magnitude and
frequency of natural hazards. In the same respect, the growing world population allows
for an increase of human lives and development to be placed in harms way. With this
increase comes greater devastation from such hazards as earthquakes, landslides, and
flooding. In order to diminish financial and human loss, it is important to understand
both the physical and perceived risks that are associated with natural hazards.
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I plan to conduct my thesis work on the risk perception of natural hazards in the
Bay Area of San Francisco. This study will be conducted by surveying homeowners in
the Bay Area on their awareness of hazard risks. It will include mapping the predicted
physical risk for the surveyed areas. By linking geomorphology to this study I hope to
gain a better understanding of how geomorphic research can contribute to the study of
natural hazards management.
Risk perception, or risk management, is a tool used to assess and mitigate all risk
presented by natural hazards. It involves a blend of policy-based and science-based
issues. The policy-based issues involve mitigation measures and management strategies
that deal with and help prevent the human and financial loss from hazards. The science-
based issues concern the physical processes of hazards and how they are predicted.
Specifically they include such items as prediction, spatial distribution, and magnitude and
frequency of hazards, all of which can be found within the field of geomorphology. I
chose to conduct a literature review on the role geomorphology plays in natural hazards
research to see where it can contribute to the science issues present in risk management.
The Role of Geomorphologists
“Between 1990 and 1999, 2808 disasters were recorded worldwide. Eighty-four
percent of them were related to geomorphology” (Alcántara-Ayala, 2002 p. 117). Figure
1 indicates that the large majority of hazards present today are geomorphologically
related. According to Alcántara-Ayala, geomorphological disasters include slides,
floods, earthquakes, volcanoes, windstorms, droughts, and wild fires (Alcántara-Ayala,
2002 p. 117). The science-based issues involved in risk analysis relate to such physical
processes. The remaining natural disasters mentioned include extreme temperatures and
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epidemics. This figure demonstrates the obvious role that geomorphologists play in
studying physical processes associated with natural hazards.
Figure 1. X-axis: year, Y-axis: number of occurrences. Alcántara-Ayala, 2002, p.116
Although studies of the physical system were incorporated into natural hazards
research during the fields’ inception, eventually the focus shifted to the social sciences.
Gares feels that at its current state, the field of natural hazards has a social science bias.
It is now the role of geomorphologists to provide in depth studies on the physical
processes of natural hazards, and incorporate them back into the natural hazards field
(Gares, 1994).
Rosenfeld states that the global damage from natural disasters “has increased
three-fold from the 1960’s through the 1980’s, leaving more than three million dead and
causing the displacement of more than 800 million persons during that period”
(Rosenfeld, 1994, p. 27). Due to this recent increase in human and economic loss from
natural disasters, the international science community has taken action to predict and
mitigate future disasters. This effort includes incorporating sciences such as
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geomorphology into management and mitigation tasks. Geomorphologists are
researchers capable of understanding the extreme weather hazards that result from
continued global climate change. They are familiar with magnitude and frequency
concepts, which are critical when establishing a threshold of extreme events (Rosenfeld,
1994).
Disaster mitigation studies are inherently multidisciplinary, and geomorphologists
can contribute greatly to most areas of this research. Such studies include past changes of
landforms and processes, current geomorphic processes and their relationship to soils and
hydrology, anthropogenic changes made to the environment, and local land-use planning,
monitoring, and warning systems (Verstappen, 1989).
Although geomorphologists have done little work on risk studies thus far
(Slaymaker, 1996), they can contribute to the risk assessment process by “designing
hazard mitigation strategies in balance with the dynamics of processes within the region”
(Rosenfeld, 1994, p.35). They can also assess risk through their advanced knowledge of
geomorphology by developing prediction models, and through applied geomorphology
that helps manage for future events (Alcántara-Ayala, 2002).
Natural and Geomorphic Hazards
Defining Natural Hazards
Within geomorphology literature, natural hazards are defined in many ways. A
general definition given is that “the term natural hazard implies the occurrence of a
natural condition or phenomenon, which threatens or acts hazardously in a defined space
and time” (Alcántara-Ayala, 2002, p. 108). Such phenomena have been taking place
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since the earth was first formed. It was not until the presence of humans that such
occurrences transformed into natural “disasters” or “hazards”.
Humans play an important role in defining natural hazards. Alcántara-Ayala
defines natural hazards in relation to a state of disequilibrium. He considers this
occurrence to be a sudden disequilibrium between natural forces and the forces of the
social system. “The severity of such disequilibrium depends on the relation between the
magnitude of the natural event and the tolerance of human settlements to such an event
(Albala-Bertrand, 1993)” (Alcántara-Ayala, 2002, p.112). Clague chooses to neglect
hazards that are explicitly due to anthropogenic causes, such as forest fires. Instead he
defines natural hazards as being either geologically or geomorphologically controlled,
and threatening to communities, roads, and major developments (Clague, 1982).
Although he does not include human induced hazards, he does note the importance of
impacts to the human environment.
Distinguishing Natural Hazards From Geomorphic Hazards
Gares argues that unlike natural hazards, geomorphic hazards do not have a direct
affect on human life and usually occur over long temporal scales. Although most authors
do not make the distinction, Gares attempts to differentiate geomorphic hazards from
natural hazards. He defines geomorphic hazards as occurring due to the “instability of
the surface features of the earth” (Gares, 1994, p. 5). According to Gares, hazards do not
become geomorphic until they actually change the landscape (Gares, 1994).
Gares uses the example that earthquakes are a natural hazard and slope failure is a
geomorphic hazard, even if an earthquake causes it. Other specific examples of
geomorphic hazards include coastal erosion, soil erosion, mass movements, and fluvial
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erosion. When compared to natural hazards, Gares feels that geomorphic hazards tend to
have lower magnitude, higher frequency, slower onset rates, more widespread areal
extent, more diffuse spatial dispersion, more regular temporal spacing, and occur over a
longer temporal scale. This may provide difficulty in studies that incorporate both
natural hazards and geomorphic hazards (Gares, 1994).
Although this is an interesting perspective, Gares is the only author to make such
a distinction. Alcántara-Ayala does not distinguish differences between natural hazards
and geomorphic hazards. Instead he terms such events as earthquakes, landslides,
volcanic activity, and flooding as both natural hazards and geophysical events. The true
distinction between the two comes from the presence of vulnerability. Natural disasters
will occur only when both natural vulnerability and human vulnerability are present in
the same space and time. If human vulnerability is not present then the process is simply
a geophysical event (Alcántara-Ayala, 2002). So although he does not choose to make a
definitive distinction between the two, he does define natural hazards as processes having
direct impacts on humans.
In 1996, Slaymaker was the first to classify geomorphic hazards into the three
sub-groups: endogenous (processes that occur “within” the Earth), exogenous (occurring
“outside” of the Earth), and those induced by climate and land-use change (Slaymaker,
1996). Eight years later, Alcántara-Ayala uses this same classification for geomorphic
hazards. He states that volcanism and neotechtonics are examples of endogenous
geomorphic hazards, while floods, karst collapse, snow avalanche, channel erosion,
sedimentation, mass movement, tsunamis, and coastal erosion are given as examples of
exogenous geomorphic hazards. Desertification, permafrost, degradation, soil erosion,
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salinization, and floods are given as examples of geomorphic hazards induced by climate
and land-use change (Alcántara-Ayala, 2002).
Other authors choose to ignore the human element and define geomorphic hazards
strictly in relation to prediction and probability. Panizza defines a geomorphological
hazard as “the probability that a certain phenomenon reflecting geomorphological
instability will occur in a certain territory in a given period of time” (Panizza, 1987, p.
225). An instable landform will occur through disequilibrium with the natural
environment, and only through a shift or change can this landform move toward an
equilibrium state (Panizza, 1987). According to Slaymaker, geomorphologists tend to
define a geomorphic hazard as “the probability of a change of a given magnitude
occurring within a specified time period in a given area” (Slaymaker, 1996, p.1).
Magnitude & Frequency of Geomorphic Hazards
Even though numerous definitions for what constitutes a “geomorphic hazard”
can be found, all authors seem to agree that the magnitude and frequency of the hazard is
an important distinction. Gares, Slaymaker, and Alcántara-Ayala feel that magnitude,
frequency, temporal scale, and spatial scale are all key geomorphic concepts correlated to
natural hazards (Gares, 1994; Slaymaker, 1996; Alcántara-Ayala, 2002). Magnitude
covers the characteristics of the hazard and frequency describes how often the event is
likely to occur (Alcántara-Ayala, 2002).
Table 1 is very useful in showing the impact of frequency and magnitude, and
how different geomorphological hazards are broken down. It shows the 3 classes of
geomorphic hazards mentioned earlier: exogenous, endogenous, and climate or land-use
induced, in relation to magnitude and frequency. A downfall of this table is that it does
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not show a distinction between site, local, regional, and national hazards. However, it
does show that there can be an important distinction made between high magnitude and
low magnitude hazards (Slaymaker, 1996). It is also interesting to note that many
hazards can be found in both categories.
Table 1. Categories of geomorphic hazards. Slaymaker, 1996, p.2
Specific physical attributes of hazards can prove useful in future management
practices. The magnitude and frequency of past geomorphic hazards can indicate trends
in geomorphological instability, and potentially help predict when and where hazards will
occur in the future (Panizza, 1987). Traditionally, geomorphologists have concentrated
their efforts on large (regional) scales. However, for proper implementation of mitigation
and risk management, a smaller (local) scale must be examined (Rosenfeld, 1994).
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Specific Contributions
The previous literature has established that geomorphology can indeed benefit the
field of natural hazards. Now it is important to focus on the specific contributions
geomorphology can make to natural hazards management including a multidisciplinary
approach, the establishment of geomorphological risk, prediction methods, and an
international area of focus.
Multidisciplinary Approach
The field of natural hazards “involves conflicts between physical and human
systems” and is an obvious subject of study for geographers (Gares, 1994, p. 1). It is
only through a multidisciplinary approach that hazards research can manage for the
future. “Amongst geoscientists, geomorphologists with a geography background might
be best equipped to undertake research related to the prevention of natural disasters given
the understanding not only of the natural processes, but also of their interactions with the
human system” (Alcántara-Ayala, 2002, p.108). D. Alexander, M. Panizza, and H.T.
Verstappen are all geomorphologists who incorporate their advanced understanding of
geomorphological processes with social issues for a more thorough understanding of
natural hazards (Alcántara-Ayala, 2002).
Prior to 1960, natural hazards were approached from an almost strictly physical
perspective. It was not until the 1960s and 1970s that social and economic characteristics
were implemented. Many of the geomorphology articles mentioned in this review
promote the inclusion of more social, political, and economic characteristics into
geomorphology research. This will allow for an easier collaboration with other fields of
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study. It will also cause management and the general public to show more interest in
geomorphic hazards (Gares, 1994).
Establishing Geomorphological Risk
By including both social and physical elements in hazards research,
geomorphological risk can be established. The field of geomorphology plays an
important role in establishing this risk. “The risk approach to geomorphic hazards
enables a fuller incorporation of both expert analysis and societal synthesis in the solution
of the natural hazards problem” (Slaymaker, 1996, p.6). The risk approach mentioned
here transcends past the simplicity of previous geomorphic hazard studies that mostly
focus on physical processes.
Throughout the 1990s, the studies have extended even further to include
perceptions of hazards, which is an important factor in developing risk management
approaches. Alcántara-Ayala stresses the importance for researchers to involve
themselves not only in the science of natural hazards, but also in the risk assessment and
management programs (Alcántara-Ayala, 2002). Those dealing with geomorphological
risk and especially those trying to mitigate this risk must also deal with the organizational
problems of a social, economic, and political nature, that contribute to this risk (Panizza,
1987).
A geomorphic hazard multiplied by the social and economic vulnerability of a
region produces the geomorphological risk present there (Panizza, 1987). It is the
probability that the social and economic structures of an area can withstand the
geomorphological instabilities present. It is important to note that geomorphological risk
is impossible to predict without knowing the social and economic make-up of a particular
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location. A fantastic example of this is that “erosion is a hazard that may not involve any
risk in a desert area, whereas in a densely populated or highly industrialized area, it could
represent a high risk” (Alcántara-Ayala, 2002, p.228).
It is important in hazards management to weigh options and focus research based
on the severity of risk. Slaymaker specifically defines how geomorphologists can
establish this risk. He mentions three main steps geomorphologists can take when
determining geomorphological risk. The first is the mapping of geomorphic hazard
domains, which can also be ranked according to degree of instability. The second step is
to assess the vulnerability present. This is where human and economic loss is evaluated.
The final step is to prioritize georesources, which would place the highest priority on
urban land since this is where human life is most consolidated (Slaymaker, 1996).
Methods for Prediction
Methods for predicting hazards are probably where geomorphologists can
contribute the greatest to management efforts. Although these methods are not
guaranteed to predict the next big disaster, they can help with making emergency
decisions, aide in mitigation measures, and reduce future risk in an area. Some basic
methods used to predict hazards include geographic information systems (GIS), remote
sensing, modeling, and statistical techniques.
The mapping of landforms coupled with land-use and infrastructure, emergency
services, risk management, public awareness, training, regulation, and social insurance is
now possible due to the advent of GIS. It allows for the mapping, modeling, and
decision-making tools to handle all of these elements. When this technology is paired
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with the Global Positioning System (GPS) and satellite remote sensing, geographic data
collection is greatly improved (Rosenfeld, 1994).
Geomorphological hazards prediction also benefits from the technology of remote
sensing. Such techniques can “delineate geomorphic zones with distinctive origins,
surficial materials, and erosional sensitivities” (Rosenfeld, 1994, p.33). Remote sensing
has a great influence upon monitoring events and therefore has increased in the frequency
of its use. Remote sensing techniques are most useful with large-scale hazards and can
provide useful hazard zoning maps and assist in structural mitigation (Rosenfeld, 1994).
Along with the methods mentioned above, there are an abundance of methods for
predicting individual hazards such as flooding and landslides. Flood prediction can be
accomplished by using measured properties from past small floods to predict future large
floods. Theoretical models based on assumed principles of flooding can be created.
Assumptions about the sediments, landforms, and erosional scars of past floods to predict
future occurrences can also be accomplished for flood prediction (Baker, 1994).
Landslide prediction can occur through evaluating spatial patterns of environmental
factors such as rainfall intensity (Zhou, 2002). Soil wetness modeling and topographic
attributes can also be used when predicting landslides (Gritzner, 2001).
International Area of Focus
Finally, geomorphology can contribute to the management efforts in developing
countries. This is a topic found throughout geomorphic hazards literature. Many reasons
are provided for this international focus on developing countries. First of all, developing
countries are generally located within close proximity to geomorphological hazard zones
such as severe flooding, or seismic and volcanic activity. Secondly, developing countries
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are usually in a state of poor economic, social, and political conditions, which provide
greater susceptibility to human and financial loss from hazards (Alcántara-Ayala, 2002).
Finally, much of the destruction from natural hazards comes from lack of mitigation in
hazard prone areas. In developing countries, it is usually not the lack of education or
knowledge of the hazard that prevents mitigation, but the “lack of resources or
unwillingness to divert limited national wealth to such causes” (Rosenfeld, 1994, p.27).
Panizza feels that vulnerability to hazards will be high in areas of low social organization,
with a lack of prediction and monitoring techniques, and an inefficient intervening
governing body (Panizza, 1987).
“As the severity of disasters increase, there is an exponential rise in the number of
casualties among the poorer nations” (Rosenfeld, 1994, p.31). Table 2 shows that the
global death toll from natural hazards is highest in developing countries (Alcántara-
Ayala, 2002). The table does show significant impacts from hazards in countries such as
Japan, USA, France, and Switzerland, but it is obvious that the impacts are much greater
in countries such as Bangladesh, India, China, Guatemala, Colombia, and Mexico
(Alcántara-Ayala, 2002).
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Table 2. Some of the major geomorphology related natural disasters of the world form
1990 to 1999. (Data source: EM-DAT and the *Office of US Foreign Disaster
Assistance). Alcántara-Ayala, 2002, p. 111.
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Conclusion
“It is clear that the conceptualization (of natural hazards) has changed from a
perspective of a merely physical or natural event, towards the integration of the human
system” (Alcántara-Ayala, 2002, p.118). I feel that geomorphological hazard research
should also follow in this trend. More recently, geomorphology literature is breaking into
“Applied Geomorphology” which transcends past the physical studies to include human
impacts, mitigation measures, and management implications.
By incorporating geomorphology into my own studies of risk perception I will
greatly enhance the science-based issues involved and have a better understanding of the
methods for predicting hazards. My assessment of the vulnerability present from both
physical and perceived risk will also be improved. Providing more appropriate scientific
methods for prediction and implementing international training programs for increased
education will reduce vulnerability to natural hazards in the future (Alcántara-Ayala,
2002).
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References
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of natural disasters in developing countries. Geomorphology 47(2): 107-124.
Baker, V. 1994. Geomorphological understanding of floods. Geomorphology 10(1): 139-
156.
Clague, J.J. 1982. The role of geomorphology in the identification and evaluation of
natural hazards. pp. 17-43 in R.G. Craig and J.L. Craft (eds), Applied Geomorphology.
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Gares, P.A, D.J. Sherman, and K.F. Nordstrom. 1994. Geomorphology and natural
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Gritzner, M., W.A. Marcus, R. Aspinall, and S.G. Custer. 2001. Geomorphology 37(1):
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Panizza, M. 1987. Geomorphological hazard assessment and the analysis of
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