The atmosphere plays a vital role in maintaining the heat balance on the earth by absorbing the IR radiation received from the sun and re-emitted by the earth
Greenhouse effect
Phenomenon that keeps the earth warm enough to sustain life
The air is a combination of gaseous elements that have a remarkable uniformity in terms of their contribution to the totality of life
Oxygen (O2) supports life on earth, nitrogen (N2) is an essential macro-nutrient for plants, and carbon (IV) oxide (CO2) is essential for photosynthetic activity of plants
The atmosphere is a carrier of water from the ocean to land, which is vital for the hydrological cycle
Any major disturbance in the composition of the atmosphere resulting from anthropogenic activities may lead to disastrous consequences or may even endanger the survival of life on earth
The three main gaseous elements in the atmosphere below 100 km
Nitrogen (N2) - 78.09%
Oxygen (O2) - 20.95%
Argon (Ar) - 0.93%
Trace gases
Gases that exist in small quantities, measured in parts per million by volume (ppmv), parts per billion by volume (ppbv) or microgram per cubic meter (μgm-3)
If the concentrations of trace compounds or other pollutants are increased due to human activities and bioaccumulate over time, it becomes hazardous to life
Layers of the atmosphere
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Troposphere
Contains 75% of the atmosphere's mass, temperature and pressure drops with increasing altitude
Stratosphere
Lies directly above the troposphere, extends from about 15 km above the earth's surface
Mesosphere
Directly above the stratosphere, extending from 50 to 80 km above the Earth's surface, very rarefied atmosphere
Thermosphere
Extends from 80 km above the Earth's surface to outer space, temperature is hot and may be as high as thousands of degrees
Exosphere
The final layer, gradually gets thinner as it reaches into the vacuum of space at around 700 km above the earth's surface
When analysing markets, a range of assumptions are made about the rationality of economic agents involved in the transactions
The Wealth of Nations was written
1776
Rational
(in classical economic theory) economic agents are able to consider the outcome of their choices and recognise the net benefits of each one
Rational agents will select the choice which presents the highest benefits
Consumers act rationally by
Maximising their utility
Producers act rationally by
Selling goods/services in a way that maximises their profits
Workers act rationally by
Balancing welfare at work with consideration of both pay and benefits
Governments act rationally by
Placing the interests of the people they serve first in order to maximise their welfare
Rationality in classical economic theory is a flawed assumption as people usually don't act rationally
Marginal utility
The additional utility (satisfaction) gained from the consumption of an additional product
If you add up marginal utility for each unit you get total utility
Burning can equally be viewed as emission of combustion products that includes greenhouse gases into the atmosphere and the loss of biomass useful as valuable material resource
The extent of biomass burning generally in Africa and particularly in Nigeria coupled with the complexity of the reactions involved; alongside its health implications constitute an important motivation to view it as a global problem deserving priority attention and careful multisided investigation because air has no boundary i.e. it is transboundary
Burning vegetation releases large amounts of particulates (solid carbon combustion particles) and gases, including greenhouse gases that helps warm the Earth
Greenhouse gases may lead to an increased warming of the Earth or human-initiated global climate change
Studies suggest that biomass burning has increased on a global scale over the last 100 years, and computer calculations indicate that a hotter Earth resulting from global warming will lead to more frequent and larger fires
Biomass burning particulates impact climate and can also affect human health when they are inhaled, causing respiratory problems
Biomass burning, once believed to be a tropical phenomenon, has been demonstrated by satellite imagery to also be a regular feature of the world's boreal forests
Recent estimates indicate that almost all biomass burning is human-initiated and that it is increasing with time
With the formation of greenhouse and chemically active gases as direct combustion products and a longer-term enhancement of biogenic emissions of gases, biomass burning may be a significant driver for global change
The historic data indicate that biomass burning has increased with time and that the production of greenhouse gases from biomass burning has increased with time
The bulk of biomass burning worldwide may be significantly reduced
Policy options for mitigating biomass burning
Marketing of timber as a resource
Improved productivity of existing agricultural lands to reduce the need for conversions of forests to agricultural lands
Animal grazing could be replaced by stall feeding in tropical savannas grasslands
Incorporate crop wastes into the soil, instead of burning, as is the present practice throughout the world
Use crop wastes as fuel for household heating and cooking rather than cutting down and destroying forests for fuel as is presently done
Cooking and heating with solid fuels such as cow dung, wood agricultural residuals, coal is about the largest source of indoor air pollution globally
When used in cooking stoves, these fuels emit substantial amounts of pollutants including respirable particles, carbon-monoxide, nitrogen, sulphur oxides and benzene