Hazards 4- Future resilience and adaptation Flashcards
Key points about trends in geophysical hazards
-Hydro-meteorological hazards ( floods, storms, cyclones, droughts) have all become more common – possible link to climate change & deforestation.
-The frequency of tectonic hazards has remained static.
-Landslides have increased over time.
-The number of people affected by tectonic disasters has increased.
Trends in earthquakes (since 1980)
-No. of disasters has been 15-40 per year.
-Deaths have been variable, with some large events in some years.
-Mega disasters in 2004 ( Bande Aceh Tsunami) & 2010 ( Haiti earthquake) resulted in huge deaths – over 200,000 each.
-Economic losses have increased – more to lose as affluence increases.
Trends in volcanic eruptions (since 1980)
-The number of disasters is lower than earthquakes, and deaths are much lower.
-Only 7 eruptions have killed more than 100 people.
-Wider impacts can be great as large-scale evacuation is needed.
-If you look back in history it appears volcanoes & earthquakes are occurring more frequently, they aren’t. It is just they are now better monitored and recorded.
Reasons for the upwards trend in the number of disasters since 1960 (peak around 2000)
-Population increase- more people affected
-Urbanization rates high- more people in a small area
-Widespread poverty- people living in risky areas in insecure housing
-More expensive construction and belongings, increasing the cost of damage
-Inequality- increased risk for those lacking access to information and services
-Climate change- increasing the severity of climate, weather, river, and biological hazards
-Environmental degradation- reducing protection from natural systems
-More reporting- information through media
Graph showing disaster trends and influences on trends since 1960
Table showing the factors to consider when identifying and interpreting complex trends
More reasons for the varying impacts of disasters over time
-HICs have seen a decrease in the number of disaster-related deaths due to improved preparation & prediction. LICs have experienced little change, as lack the capital to make adjustments.
-Economic losses mainly in developed countries.
-It has been suggested that increased human activity has affected both the frequency & intensity of disasters e.g. Earthquakes can be triggered by human processes, such as mining & fracking e.g. UK.
-Earthquakes have caused an increasing number of deaths over time. This is largely due to the increasing number of people living in seismic areas which have increased 93% in 40yrs. Tsunamis affect large coastal areas in many regions.
-Predicted by 2050 – 3bn people will live in slums in dangerous locations.
Diagram showing the cycle of disaster and management strategies
Technology as a geophysical hazard adaptation
Examples: Smartphone apps related to advanced warning. Using GIS images to see creates maps to show where movement was greatest.
See examples in table below & in diagram on right.
Benefits: Warnings/evacuations can save lives.
Issues: Costly, mainly found in HICs/NEES. Possibility of cry wolf syndrome, property is still damaged.
Earthquakes- methods of predicting and forecasting
-Predicting the timing of earthquakes has so far proven impossible.
-There is some evidence that animals and birds sense danger before humans, but only just before the seismic waves reach a location.
-Modern seismic monitoring and communications allow for warnings to be given up to a minute before the shockwaves arrive (e.g. Japan).
-Foreshocks can be an indication of a larger event, but the pattern is not certain until afterward.
-The absence of earthquakes along a known fault is cause for concern as it shows that stress and strain are building up (e.g. San Andreas fault), instead of being released by smaller earthquakes.
-Earthquakes may travel along a fault line over time (e.g. Anatolian fault), so it is possible to say which part of the fault will move next (but not when).
-Some faults are unknown (e.g. Christchurch), and earthquakes are surprises.
Volcanoes- methods of predicting and forecasting
-Volcanoes have a fixed location, allowing constant monitoring. However, constant monitoring requires technology and is expensive, which is why so many volcanoes in developing countries are not monitored.
-Geological evidence of past eruptions provides clues about the type and extent of future eruptions.
-Measurements include gas emissions (e.g. SO2), harmonic tremors, building of the volcano flanks, and composition of magma. There are usually changes in these readings before an eruption, which allows relatively accurate predictions and warnings to be given, although the exact magnitude is more difficult to forecast.
Tsunamis- methods of predicting and forecasting
-Any sub-marine earthquake may create a tsunami, especially if it is of large magnitude on subduction zones with megathrusts.
-Warning systems exist in the Pacific and now also in the Indian Ocean (after 2004), based on seismograph readings locating epicenters and buoys monitoring the movement of the sea.
-Computer modeling (e.g. SIFT), has been used to predict arrival times and wave height, but it does not always accurately account for ocean depth or the shape of the seafloor.
Examples of land use zoning
-Prevention of building on low-lying coasts ( tsunamis).
-Avoid areas too close to volcanoes.
-Avoid areas where liquefaction is likely.
-Avoid the base of rock faces where debris & rocks might slide.
Benefits and issues of land use zoning
Benefits:
-Low cost
-Relocates people & infrastructure away from areas of high risk.
Issues:
-Prevents economic development in some coastal areas.
-Requires strict law enforcement.
Place examples of land use zoning
-Mt Etna, Italy – Hazard zones maps forecast biggest dangers. The greatest risk is above 1000m, on the flanks volcano, so no settlements are allowed in this area.
-Mocoa, Columbia – They have now carried out hazard mapping of landslide risk. The policy encourages relocation, but how do you relocate a population of 56,000 which is growing rapidly?
-Christchurch, NZ – In 1995 potential for liquefaction had been mapped. Had identified parts of the city built on silt, which had a high water table. Should have placed closer attention to this map when carrying out urban planning.
-Istanbul, Turkey – Hazard mapping can help authorities adapt. 30-70% chance of a mag 7 earthquake. Improved seismic design of airport and rail network in 2012. Buildings need to meet criteria or be demolished ( 6.5mn in the next 20 years). Progress slow.
Increasing preparedness: examples, benefits and issues, place examples
Examples:
-Earthquake kits ( essential household supplies – water, food, battery-powered radio, blankets) kept in a safe place at home.
-Preparation days
-Risk education
-Household adjustments – nail furniture, install ‘smart meters’ which cut off gas & prevent fires.
Benefits:
-Low cost – can be organized by NGOs.
-Can save lives at a local scale.
Issues:
-Property still damaged.
-Harder to implement in isolated rural areas.
Example:
-Great Californian Shake Out Campaign (Annually on 3rd Thursday in October) In 2019 – 6.5mn participants.
Insurance: benefits and issues, place examples
Benefits:
-Allows for economic recovery.
-Some companies require buildings to meet safety codes.
-May provide temporary accommodation after the event.
Issues:
-Does not save lives.
-Few people in developing countries can afford it.
-Insurance companies charge according to the degree of risk posed by a hazard and in areas of very high risk insurance may not be available.
-People might not perceive there to be a risk e.g. only 10% of Californians are insured, even though 10,000 earthquakes occur every year.
Examples of geophysical hazard adaptation
-Increased government planning (land-use zoning)
-Personal resilience (increased preparedness, use of insurance, adoption of new technology)