3.1 - Immutability of Hazards
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Understanding the Speed of Onset
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Today, we're discussing how the speed of onset can vary among different hazards. For example, flash floods occur very quickly, leaving little to no warning. Can anyone think of other disasters with similar characteristics?
Earthquakes! Those happen suddenly too.
Exactly! Earthquakes occur without warning. Now, can someone provide an example of a disaster that allows for preparation time?
Cyclones, because we can predict when they're coming.
Right! Cyclones offer more time for warning and preparation. Remember, we can summarize this with the acronym S.O.S. - Speed of Onset Semantics.
How does this relate to disaster management?
Great question! Understanding speed helps us allocate resources and plan effectively. Let's move on to spatial dispersion.
Hazards and Tectonic Plates
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To understand earthquakes, we need to look at tectonic plates. Who can tell me what happens at plate boundaries?
They can collide, slide, or move apart?
Correct! These movements can trigger earthquakes. Can you describe one type of plate boundary?
Convergent boundaries, where plates collide?
Yes! Convergent boundaries can cause significant pressures that lead to earthquakes. Remember the mnemonic 'C-S-D': Collide, Subduct, Diverge for plate interactions.
What about divergent boundaries?
Great point! Divergent boundaries involve plates moving apart. Each type can influence different earthquake characteristics.
The Immutability of Hazards
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Now, can we avoid hazards? Think carefully and give me your thoughts.
No, I remember you said they have always existed.
Exactly! Hazards have been present throughout history and will continue to be. This immutability is crucial in our disaster management strategies.
Why is it important to understand this?
Understanding their immutability helps prioritize preparedness and mitigation efforts. Remember, 'Plan, Prepare, Protect'—three Ps of disaster readiness.
So, even if we can't stop them, we can prepare for them?
Absolutely! That's the essence of effective disaster risk management.
Introduction & Overview
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Quick Overview
Standard
The section emphasizes that hazards are immutable and cannot be avoided. It covers the different speeds at which various hazards occur, the impact of tectonic plate movements on earthquakes, and the predominance of hydro-meteorological disasters, particularly floods and droughts, in global disaster data from 1980 to 2005.
Detailed
Immutability of Hazards
This section explores the nature of hazards within the context of disaster risk management. Key aspects include the speed of onset, spatial dispersion, and temporal spacing of hazards. Hazards like earthquakes and flash floods occur suddenly, leaving little time for a response, while cyclones allow for better preparation due to longer warning times.
Hazards are classified based on their physical processes, as seen with earthquakes occurring along tectonic plate boundaries through convergent, divergent, and subduction processes. The discussion highlights that despite advancements in forecasting, hazards themselves cannot be avoided; historical data from 1980 to 2005 reveals that a significant percentage of disasters are hydro-meteorological, with floods accounting for 35% of reported events and causing over 70% of human casualties. This emphasizes the necessity for improving disaster preparedness and the importance of understanding hazards’ immutable nature.
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Speed of Onset of Hazards
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Chapter Content
Now, coming another important feature is the speed of onset like, if we consider a flood, it is a flash flood, it is very sudden without warning, very quick or is it a kind of slow process like in case of cyclone, we have much time to predict so, we have; we can prepare our self, we have better early warning system and we can take time but in case of earthquake, we do not have any time, it is very sudden or in case of flash flood, we have less time also consider to other kind of a flood.
Detailed Explanation
The speed of onset of a disaster is crucial for disaster risk management. Some disasters occur suddenly, like flash floods or earthquakes, where there’s little to no time for preparation. Others, such as cyclones, develop slowly, offering more time for warning and preparation. Understanding this speed allows for better risk management and response strategies.
Examples & Analogies
Think of it like preparing for a race. If you know the race is going to start in a few minutes (like a flash flood), you have very little time to get ready. However, if you know the race is scheduled for next week (like a cyclone), you can train and prepare extensively.
Spatial and Temporal Dispersion of Hazards
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Or so, speed of onset is very important and when you are considering the hazards in disaster risk management and the spatial dispersion; area likely to be affected by particular event. And temporal spacing also very important; what time, when and it is happening, are they random, are they occurring in a cyclic process in a recurring process or they are one-time events, so these are important features when we are dealing with hazards.
Detailed Explanation
Spatial dispersion refers to the areas likely to be affected by specific hazards, while temporal dispersion deals with the timing of these events. Understanding where and when hazards are likely to occur can help in planning and preparing for future events, whether they are one-time occurrences or part of a recurring pattern.
Examples & Analogies
Consider planning a picnic. If you know it often rains in your area during certain months, you would likely avoid planning your picnic at that time. Similarly, knowing the areas prone to specific hazards helps in planning safety measures.
Earthquake Hazard Processes
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In case of just for an example, maybe we can see that in case of earthquake; earthquake occurs along the boundaries of the tectonic plates of the earth crust. this is one hazard and when this is the source of the hazards and when this happen and this happens, we can see that these plates come in contact with each other and the pressure builds up an earthquake occurs.
Detailed Explanation
Earthquakes happen when tectonic plates in the Earth’s crust interact. These plates may collide (convergent boundaries), one may slide beneath another (subduction), or they may move apart (divergent boundaries). When the pressure built up from these movements is released, it causes an earthquake.
Examples & Analogies
Imagine a crowded elevator where everyone is pushing against the walls. Eventually, when the pressure is too much and someone yields, it can lead to a sudden jolt or movement similar to how an earthquake occurs when built-up pressure between tectonic plates is released.
Historical Perspective of Hazards
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Now when we are talking about hazards, can we avoid hazard? No, historically hazards were there, it is there and it will remain. So, we cannot avoid hazard basically.
Detailed Explanation
Hazards are a natural part of our environment and have always existed; they will continue to occur. While we can’t avoid hazards entirely, we can learn to manage, prepare for, and respond to them effectively. Understanding their inevitability is key to strengthening disaster risk management strategies.
Examples & Analogies
It's like the changing seasons; we know winter will come every year. Instead of trying to avoid it, we prepare with warm clothes and heating systems to make the season more manageable.
Statistics on Disasters
Chapter 5 of 8
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Now, looking into the disaster; number of disasters from 1980’s to 2005, you can look as I told also before, it is the flood that is the most reported disastrous event. 35% of the all disasters are from 1980 to 2005 are flood disasters. Another one is also big share is the wind storm, earthquake is only 11%, an extreme temperature is 11%, so overall 90% of disasters are related to hydro-meteorological disasters, that is very important finding.
Detailed Explanation
From the statistics gathered between 1980 and 2005, floods were the most common disasters, accounting for 35% of all reported incidents. Other events, such as wind storms and earthquakes, made up a smaller percentage. This demonstrates that the majority of disaster risks are related to water and weather phenomena, which is crucial for prioritizing disaster risk management efforts.
Examples & Analogies
Think of these statistics as a pie chart, where the largest slice represents floods. If you know floods contribute the most to disaster risks, you're more likely to focus on flood prevention measures, similar to how a student might spend more time studying the most difficult subjects for exams.
Loss of Human Life Due to Disasters
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Also, when we are looking into the loss of human life from 1980 to 2005, we can see that nearly 70% of loss of life are related to hydro-meteorological factors. So, hydro-meteorological disasters are very critical, particularly when we are looking into developing countries or underdeveloped countries.
Detailed Explanation
The data shows that approximately 70% of deaths due to disasters from 1980 to 2005 were connected to hydro-meteorological factors like floods and droughts. This highlights the critical importance of addressing these types of disasters, especially in developing countries where resources and infrastructure to manage such risks may be limited.
Examples & Analogies
Imagine a community that is largely dependent on agriculture. If floods or droughts strike, they may not only face loss of life but also economic devastation, similar to how a business struggling with economic downturn might be forced to shut down.
Regional Distribution of Disasters
Chapter 7 of 8
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Similarly, flood 9%, earthquake is only 14%, here is the regional distribution of natural disasters from 1980 to 2005. You can see that Asia is one of the biggest source of disaster, it is one of the hotspot compared to any other region, when we are talking about disasters. And it is the hydro-meteorological particularly, the flood and drought which play a big share of the all disasters and disaster impacts.
Detailed Explanation
Asia has been identified as a significant hotspot for disasters. The majority of disasters are related to hydro-meteorological events like floods and droughts. Understanding the regional distribution is essential for directing resources and planning interventions in the most affected areas.
Examples & Analogies
Think of targeted charity work; if a charity knows that a particular region suffers from frequent floods, they’re more likely to send resources and aid to that area rather than somewhere that doesn’t experience as many disasters.
Trends in Disaster Incidence
Chapter 8 of 8
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Here is also you can see from 1991 to 2002, the growth of disasters. So, actually it is increasing in all continents particularly in Asia, so in 1990’s and 2002, you can see in Asia’s, these disasters are actually more and more reported and more and more human losses and property damage are reported.
Detailed Explanation
Over the years from 1991 to 2002, there was an observable increase in the number of reported disasters worldwide, especially in Asia. This trend indicates that disaster incidents are becoming more frequent and highlights the importance of developing effective responses and risk reduction strategies.
Examples & Analogies
Consider how increased smartphone usage has transformed how we communicate. Just as we adapt to more frequent use of technology, communities must adapt to the increasing frequency of disasters by improving their readiness and response strategies.
Key Concepts
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Hazard Speed: Understanding how quickly different hazards occur impacts management strategies.
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Immutability of Hazards: Hazards cannot be avoided despite advances in disaster preparedness.
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Hydro-Meteorological Dominance: The majority of disasters from 1980 to 2005 were hydro-meteorological.
Examples & Applications
Flash floods occur suddenly, often with little to no warning, making them challenging to manage effectively.
Earthquakes are primarily associated with the movement of tectonic plates, which release energy suddenly.
Memory Aids
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Rhymes
Flash floods so fast, earthquakes hit too, prepare for hazards, that's what we must do!
Stories
Imagine a village threatened by floods and earthquakes. The villagers learned to prepare, understanding that these hazards would always be nearby, teaching them to respect natural forces.
Memory Tools
P.P.P. - Plan, Prepare, Protect for hazards you'll never neglect.
Acronyms
S.O.S. for Speed of Onset Semantics—that helps manage risks better.
Flash Cards
Glossary
- Speed of Onset
The rate at which a hazard event occurs, affecting the time available for warning and response.
- Spatial Dispersion
The geographical distribution of a hazard and the area that may be affected.
- Temporal Spacing
The frequency and timing of hazard events, which can be random or cyclic.
- Tectonic Plates
Massive segments of Earth's lithosphere that move and interact at their boundaries, leading to geological events such as earthquakes.
- Convergent Boundaries
Areas where two tectonic plates collide, often causing earthquakes and mountain formation.
- Divergent Boundaries
Regions where tectonic plates are moving apart, which can create new crust and lead to geological activity.
- Subduction Zone
A region where an oceanic plate is pushed beneath a continental plate, potentially causing earthquakes.
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