Climate change and its impacts.

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THE SUBJECT OF THIS PROJECT

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CLIMATE CHANGE AND ITS IMPACTS

In the past 10 years a great deal of scientific evidence that earth is undergoing significant climate change due to what has been called “global warming”. The climate weather change is expected to result in primary environmental impacts such as changing weather patterns (increased rainfall, storms, draughts) as well as a rise in sea levels due to melting of the polar icecap. The secondary impacts will be felt by people living in the affected regions – land use patterns will change and people will have to adjust to new environmental conditions. Some regions, of course, will benefit and some will be adversely affected. The state will have to be able to analyze the situation, plan for a new future, and mobilize resources.

For this project assess some of the likely impacts on Brunei Darussalam – especially the possibility of a 0.5 to 1.0 meter rise in sea levels. What can be done in Brunei Darussalam to plan for and alleviate any negative impacts?

International efforts have been underway (international meetings and agreements) to try to reverse the global warming trend by reducing the amount of greenhouse gases emitted into the atmosphere. What has been the Brunei Darussalam government’s policy in this regard? Examine their involvement in the international negotiations.

INTRODUCTION

WHAT IS “GLOBAL WARMING”?

Global warming, as defined in the Oxford dictionary is the increase in temperature of the earth’s atmosphere, caused when certain gases, especially carbon dioxide, trap the sun’s heat. These gases are called the ‘Greenhouse Gases’, namely (the major contributors) carbon dioxide, CFCs1, methane and nitrous oxide. The natural2 greenhouse gases are CO23, CH44, O35, halocarbons and nitrous oxide. Though, these gases are also contributed by human activities. Combustion of fossil fuels increases the concentration of these natural greenhouse gases in the atmosphere. These gases let in sunlight but tend to insulate the planet against the loss of heat. Thus, a higher concentration means a warmer climate.

  • Carbon Dioxide – Of all the ‘anthropogenic’6 greenhouse gases, carbon dioxide has by far the greatest impact on the global heat budget (heat budget = amount of heat absorbed – the amount radiated back into space). Contributing to carbon dioxide’s greenhouse potency is its persistence: as much as 40 percent of it tends to remain in the atmosphere for centuries. The accumulation of atmospheric carbon dioxide is promoted not only by combustion but also by tropical deforestation.

  • Aerosols – They are not categorized as gases, but they are minute solid particles, sometimes covered by a liquid film, finely dispersed in the atmosphere. They too, are produced by combustion, but they also come from natural sources, primarily volcanoes. Aerosols tend to ease global warming on regional and global scales by blocking or reflecting light (sun’s rays). Unlike carbon dioxide, aerosols are not as dangerous because they have short atmospheric residence times (less than a week) and consequently are concentrated near their sources.

  • Methane – It is the greenhouse gas in importance to CO2 in radiative forcing and its concentration has increased. Sources of methane are both industrial and biogenic7. Industrial sources include leakage from natural gas transmission and distribution systems and escape from coalmines and oil and natural gas wells. Biogenic emissions are the result of anaerobic decomposition of organic matter in natural wetlands, rice paddies and landfills. Methane is also produced as a by-product of animal digestion, particularly in ruminants8 and by termites and other insects.  

  • Nitrous Oxide – It has also increased and even though it is accumulating more slowly than CO2 or CH4, its effective warming potential per unit mass emitted today will, after 20 years, be about 270 times greater than that of carbon dioxide. It now appears that nitrous oxide emissions are primarily biogenic in origin; previous estimates of large industrial sources have been due to measurement error. The biogenic emissions stem from biomass9 burning, natural, disturbed and cultivated soils and, possibly, from nitrogen-containing groundwater and the oceans.

  • CFCs – CFCs, HFCs10 and HCFCs11 are considered the greatest villain and they are totally man-made. They are the synthetic gases produced only in chemical factories. CFCs, HFCs and HCFCs are chemically very stable – at least until they get to the upper levels of the atmosphere. CFC gases have been added to the atmosphere since 1930, when they were first commercially produced for refrigerators. Since then they have also been used for air conditioning, fire extinguishers, aerosols, cleaning solvents (especially in the electronics industry), and food containers. While these gases have been around for only about 70 years, they have been added to the atmosphere at such rapid rates that they have become very important greenhouse gases. In the past few decades, their use has grown rapidly, with measured increase rates in the atmosphere of as high as 12 percent per year. One report has stated that CFC gases already account for 25 percent of the greenhouse effect.  

  • Ozone – It is an allotrope12 of oxygen which contains three atoms in each molecule instead of two as in normal atmospheric oxygen. Ozone is not that ‘fresh’ smell you get at the seaside! It is, however, that nasty smell you get when your photocopier or other electrical device starts ‘arcing’, or making electrical sparks. Ozone is another by-product of fossil fuel combustion but is produced through a set of complex photochemical reactions rather than being produced directly. Because nitrogen oxides are so important for its formation, the largest quantities of ozone are produced where traffic pollution is at its worst. Because this low level, or tropospheric13, ozone is a strong absorber of infrared radiation.
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By looking at these statistics, we know which of the greenhouse gases is the most hazardous. As stated in the last page, carbon dioxide is considered to be the most effective heat absorber because most of it lingers in the atmosphere for a longer period of time than the other greenhouse gases. But the table above shows the effectiveness of the gases when they are present in the same length of time.

Studying the Greenhouse Effect.

Researchers use high-speed computers to study how carbon dioxide concentration may affect surface temperature.  The computers manipulate mathematical models, sets ...

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