Patterns in environmental quality and sustainability Flashcards
definition of global warming and climate change
the observed century-scale rise in the average temperature of the Earth’s climate system and its related effects, which has been noticed since the 1980s
(rainfall, temperature, sea level, habitats, drought, floods and storms)
WHILE IT IS IMPORTANT TO NOTE THE GENERAL RISE OF TEMPERATURE, IT IS EVEN MORE IMPORTANT TO BE CONGNISANT OF THE EXTREMES!!
definition of the greenhouse effect
The process by which certain gases (water vapour, carbon dioxide, methane and chlorofluorocarbons) allow short-wave radiation from the sun to pass through the atmosphere and heat up the earth, but trap an increasing proportion of long-wave radiation from the earth. This radiation leads to a warming of the atmosphere.
the enhanced greenhouse effect
the increasing amount of greenhouse gases in the atmosphere as a result of human activities, and their impact on atmospheric systems, including global warming
insolation and its effects on weather systems (+ redistribution of energy)
incoming solar radiation
Solar energy drives all weather systems and climates (wind energy is second order solar energy). The earth absorbs most of this energy in tropical areas, whereas there is a loss of engird from more polar areas. To compensate for this there is a redistribution of energy to higher latitudes from lower latitudes, caused by wind- and ocean circulation.
radiation
convection
conduction
radiation — the emission of electromagnetic waves such as X-ray, short wave and long wave; as the sun is a very hot body, radiating at a temperature of about 5,700°C, most of its radiation is in the form of very short wavelengths such as ultraviolet and visible light
convection — the transfer of heat by the movement of a gas or liquid
conduction — the transfer of heat by contact
insolation and the atmosphere
Only 50% of the insolation at the top of the atmosphere actually gets through the earth’s surface. 30% is reflected, 20% absorbed by atmospheric gases (especially oxygen and ozone at high altitudes, and CO2 and water vapour are low altitudes), scattering accounts for 6% lost insolation, (cumulus/thick) clouds reflect 23%, earth reflects 7% of insolation (planetary albedo).
long-term and short-term variations of climate change
In long timescales, the earth’s temperature changes whenever the input of solar energy changes:
- earth’s orbit changes slightly, creating ice ages and seasons
- sunspots and solar eclipses also reduce solar energy temporarily and alter wind patterns.
On a shorter timescale, changes in the atmospheric composition can change global temperature dramatically.
factors that effect earth’s albedo
melting ice sheets (positive feedback)
hence, indirectly greenhouse gases
irrigation (darker soil in deserts)
overexploation of lakes and rivers; decreasing water surface
factors effecting climate change
- As ice melts, albedo/reflectivity reduces and insolation absorbed increases and temp. rises.
- Increased burning of fossil fuels (coal, natural gas, oil) makes the atmosphere absorb and reradiate more heat, increasing global temperature.
- Burning of rainforest releases CO2 — leaves fewer trees to absorb CO2. The atmospheric concentration, ppm, increases exponentially (double whammer).
- Methane produced by domestic animals and landfills: cattle convert up to 10% of their food into methane. As global warming increases, bogs (marsh) trapped in permafrost will melt and release vast quantities of methane. Methane increases at a rate of 1% per annum.
- Chlorofluorocarbons (CFCs; aerosols) are synthetic chemicals that destroy ozone, as well as absorbing long-wave radiation. CFCs increase at a rate of 1% per annum and are up to 100 000 times more efficient at trapping heat than CO2. They also create holes in the ozone layer.
- Transport pollution contribute to greenhouse gases
all disturbed the natural balance:
CO2 from humans, animals = CO2 taken by trees
O2 given out by trees = O2 used by humans and animals
implications of climate change
- Sea levels will rise (thermal expansion & ice melt), causing flooding, displacing hundreds of millions of people.
- Storm severity and frequency will increase (owing to more atmospheric energy)
- Agricultural patterns will change (leaving less time for farmers to grow)
- Droughts, fire, erosion, landslides, sedimentation, avalanches, pests and diseases intensity and frequency increases
- Up to 40% of species of wildlife will become extinct
However, this is just a fragment of what will expect us, and with a big uncertainty no knows exactly what will await us, except that everything will become more extreme. For instance, some suggest that certain areas might get colder, such as northwest Europe if the Gulf stream shuts down.
soil degradation
the decline in quantity and quality of soil. It includes:
- erosion by wind (28%) and water (56%)
- biological degradation (the loss of humans and plant/animals life)
- physical degradation (loss of structure, changes in permeability) (4%)
- chemical degradation (acidification, declining fertility, changes in pH, salinisation, chemical toxicity) (12%)
All this will increase with climate change.
predicting soil erosions
calculated by the universal soil loss equation A = RKLSCP, with factors that increase susceptibility to erosion
Ecological Conditions:
- Erosivity of soil R
- Erodibility K
- Length-slope factor LS
- Land-use type
- Crop management C
- Soil conservation P
Causes of soil and land degradation include:
- the reduction of the natural vegetive cover which renders the topsoil more susceptible to erosion, as when huge areas of forest are cleared for logging, fuelwood, farming or other human uses (although some areas are becoming greener, such as Europe’s forest cover)
- unsustainable land-use practices such as excessive irrigation, inappropriate use of fertilisers and pesticides, and overgrazing by livestock
- groundwater over-abstraction, leading to dry soils, leading to physical degradation
- atmospheric deposition of heavy metals and persistent organic pollutants, making soils less able to sustain the original land cover and land use
Again climate change will intensify this problem. // Nature takes 500 years to replace 25mm of topsoil lost to erosion.
Removal of vegetation and topsoil frequently results in
- increased surface runoff and stream discharge
- reduction of water infiltration (chemical contamination) and groundwater recharge (falling levels)
- development of erosional gullies and sand dunes
- change in the surface microclimate that enhances aridity
- drying up of wells and springs
- reduction of seed germination of native plants (invasion of alien plants)
Socio-economic impacts include a lack of farm productivity, rural unemployment, migration, silting of dams and reservoirs, hunger and malnutrition. This is no a poor-nations-problem.
the current state of soil degradation
In 1990, over 30% of soils were considerable to moderately or severely damaged. The main points:
- Soil is one of the world’s most important resource
- Soil is a non-renewable resource that is easily destroyed
- Farms must use methods to preserve soil quality (protection against erosion and pollution - organic farming, afforestation, pasture extension, benign crop production)
- Urban development causes great damage to soil
- Soil must be managed in a sustainable way
Tackling soil degradation and contaminated soil
Tackling soil degradation:
- physical barriers: embankments and windbreaks, vegetation cover and soil husbandry
- mechanical: bunding, terracing (which additionally also increases cultivated area), contour ploughing, shelter belts such as tress or hedges (to key is to prevent or slow the movement of rainwater downslope and wind).
- the crop should be in the soil for as long as possible due to the strengthening roots, which is the reason why farms often leave the root structures in the field. Also, increased organic material allows the soil to hold more water, thus preventing aerial erosion and stabilising the soil structure.
Tackling contaminated soils:
- flossing the soil and leaching the soil away
- applying chemicals such as gypsum to replace sodium ions on the clay and colloids with calcium
- reducing evaporation losses to lessen the upward movement of water in the soil
more causes (socio-economic) of soil degradation
Natural disaster
Degradation due to biogeographical causes
Population change
Degradation occurs when population growth exceeds environmental thresholds (neo-Malthusian), or when decline causes collapse of adequate management
Underdevelopment
Resources exploited to benefit world economy or developed countries, leaving little profit to manage or restore degraded environments
Internationalism
Taxation and other forces interferer with the market, triggering overexploitation, commercialisation
Colonial legacies
Trade links, communications, rural-urban linkages, cash crops and other “hangovers” from the past promote poor management of resources exploitation.
Inappropriate technology and advice
Promotion of wrong strategies and techniques that result in land degradation
Ignorance & Attitude
Linked to inappropriate technology & advice: a lack of knowledge of what leads to degradation, plus blaming attitudes of institutions and people, lack of awareness
War and civil unrest
Overuse of resources in national emergencies and concentrations of refugees, leading to high population pressures in safe locations.
Water usage increases with population growth, resulting in:
- overexploitation of rivers
- half of the wetlands disappeared
- 20% of freshwater species are endangered or extinct
- many important aquifers are being depleted
- water tables are dropping alarmingly
water stress
when per capita water supply is less than 1,700 cubic metres per year
This will be a severe problem in many regions like Africa, Middle East and south Asia, which may lead to conflicts. Currently, 2.3 billion live under water stress, 3.5 billion (48% of the world projected population) in 2025.
water scarcity
depends on precipitation and water availability, population growth, demand for water, affordability of supplies and infrastructure.
- physical water scarcity: water consumption exceeds 60% (unsustainable) of the useable supply. Then countries depend on imports and desalination plants (e.g. Saudi Arabia and Kuwait).
- economic water scarcity: physically sufficient water but additional storage and transport facilities are needed, required expensive water-development projects (e.g sub-saharan). Due to inefficient technology in LEDCs farmers use twice as much water as in MEDCs yet yields are three times lower.
how many people die from poor water quality
how many lack access to safe water, adequate sanitation, and wastewater treatment
because of overpopulation in urban areas, ineffecient aid flows (curruption) and numerous other factors:
Inadequate water quality causes 4 million deaths annually from water-related diseases, particularly cholera, hepatitis and malaria (parasitic diseases). Water quality is affected by sewage, fertilisers, pesticides, heavy metals and acids from industry and transport.
1.1 billion lack access to safe water, 2.6 billion are without adequate sanitation, 4 billion do not have their wastewater treated to any degree.
climate change and the hydrogical cycle
While the world as a whole will get wetter as warming speeds up the hydrological cycle, increased evaporation will make drought conditions more prevalent. Most places will experience more unpredictable, intense and variable precipitation, with longer dry periods between them, so that traditional agricultural and water management practices are no longer useful.
- To manage water well, it is crucial to know how much water is available in any basin and what it is used for.
policies tackling climate change
carbon dioxide tax
water policies to allocate water efficiently and limit consumption to safe levels. Tradable water rights could improve water management in the long term but are not realistic short-term options in most developing countries.
Climate change will require investing in new technologies and improving the application of existing technologies. Water supplies can be enhanced by desalinating seawater or brackish water and reusing treated wastewater - RECYCLING.
agriculture and climate change
Climate change will depress agricultural yields, and so we will need to increase productivity while protecting the environment. Efforts to mitigate climate change will put more pressure on land, and with growing populations, more carnivores tastes and increased demand for dairy products, the world will require highly productive and diverse agricultural landscapes.