State of the Environment

2001

Atmosphere Theme Report

Australia State of the Environment Report 2001 (Theme Report)
Lead Author: Dr Peter Manins, Environmental Consulting and Research Unit, CSIRO Atmospheric Research, Authors
Published by CSIRO on behalf of the Department of the Environment and Heritage, 2001
ISBN 0 643 06746 9

Glossary

acid deposition
the deposition on the earth's surface, either in dry or wet form, of substances derived from natural and human-induced emissions of various compounds, especially those of sulfur and nitrogen which have been transformed by chemical processes in the atmosphere
acid rain
see acid deposition
aerosol
a suspension of particles, other than water or ice, in the atmosphere and ranging in size from approximately 5 nm to larger than 10 m in radius; may be either natural or caused by human activity and most of the latter are usually considered to be pollutants
air emissions inventory
a detailed listing of the amount of emissions to the atmosphere by type and source over time and space; used to establish emission standards
air NEPM
National Environment Protection Measure for Ambient Air Quality
air pollutant
any substance in air that could, in high enough concentrations, harm humans, animals, vegetation or material
air toxics
gaseous, aerosol or particulate pollutants (other than the six criteria pollutants (see criteria pollutants) which are present in the air in low concentrations with characteristics such as toxicity or persistence so as to be a hazard to human, plant or animal life
airshed
a body of air bounded by topography and meteorology in which a contaminant, once emitted, is contained for a reasonable period of time
albedo
reflectivity of the planet
ambient air
surrounding outdoor air
Antarctic Circumpolar Wave
alternating regions of relatively warm and cold water within the Southern Ocean that rotate around Antarctica
anthropogenic
of human origin or human induced
atmospheric inversion
a condition occurring when a cool layer of air gets trapped below a layer of warm air and is unable to rise. This 'ceiling' leads to a build up of polluted air close to the ground and prevents vertical mixing and dispersion of smoke and other air pollutants
background air quality
the naturally occurring mixture of air in the absence of events such as fires
benzene
a toxic chemical found in coal tar and cigarette smoke and used as an industrial solvent, as a petrol additive, and in some paints or varnishes; a known carcinogen
biogenic emissions
emissions from natural sources including vegetation, soils and the ocean
biomass burning
the combustion of organic waste matter, burning in slash-and-burn cultivation, fuel-wood use and land clearing through forest burning
biosphere
the collective name for living organisms on the planet
carbon accounting
issues associated with measuring, calculating and valuing the relative benefits of greenhouse gas mitigation measures
carbon dioxide equivalent
an atmospheric carbon dioxide concentration that would have the same radiative forcing effect as all of the human-produced greenhouse gases combined
carbon sequestration
the uptake and storage of carbon
carbon sink
a pool (reservoir) that absorbs or takes up released carbon from another part of the carbon cycle
carcinogen
a substance or activity that causes cancer
catalyst
a substance that changes the rate at which a chemical reaction takes place without taking part in the reaction itself
CFCs (chlorofluorocarbons)
synthetic products, which do not occur naturally and contain chlorine and fluorine; commonly used in various industrial processes and as refrigerants and, prior to 1990, as a propellant gas for sprays; deplete ozone in the stratosphere and are powerful greenhouse gases
climate
the average weather conditions of a place or region throughout the seasons
climate variability
the natural year-to-year and season-to-season variation of the climate system
criteria pollutants
air pollutants traditionally regarded as important in urban air - sulfur dioxide, carbon monoxide, nitrogen dioxide, ozone, particulate matter and lead (particulate and vapours)
El Nio
an extensive warming of the central and eastern Pacific that leads to a major shift in weather patterns across the Pacific. In Australia (particularly eastern Australia), El Nio events are associated with an increased probability of drier conditions
enhanced greenhouse effect
the addition to the natural greenhouse effect resulting from human activities such as the burning of fossil fuels and land clearing, which increase the atmospheric levels of greenhouse gases such as carbon dioxide, methane, nitrous oxide, ozone and CFCs; see greenhouse effect
ENSO (El Nio-Southern Oscillation)
a suite of events that occur at the time of an El Nio; at one extreme of the cycle, when the central Pacific Ocean is warm and the atmospheric pressure over Australia is relatively high, the ENSO causes drought conditions over eastern Australia; see El Nio ,
evapotranspiration
water withdrawn from soil by evaporation and/or plant transpiration
fossil fuel
any hydrocarbon deposit that can be burned for heat or power, such as coal, oil and natural gas; produces carbon dioxide when burnt
fugitive emissions
these are greenhouse gases emitted in an uncontrolled manner
greenhouse effect
a term used to describe the role of atmospheric trace gases - water vapour, carbon dioxide, methane, nitrous oxide, ozone, in keeping the earth's surface warmer than it would be otherwise; see enhanced greenhouse effect
greenhouse gases
those gases that, by affecting the radiation transfer through the atmosphere, contribute to the greenhouse effect
halons
halons include bromofluorocarbons and bromochlorofluorocarbons, which are very stable chemicals that are involved in ozone depletion in a similar manner to CFCs
haze
the presence of very small airborne particles in concentrations large enough to impede vision
HCFCs (hydrochlorofluorocarbons)
chemicals used as interim replacements for CFCs, largely as refrigerants
hydrocarbon
an organic molecule containing hydrogen and carbon; the major components of petroleum
Indian Ocean Dipole
a warm water region in the area around Indonesia and New Guinea, and a relatively colder region in the central Indian Ocean west of Australia; gives rise to rain-producing systems that extend across Australia from north-west to south-east
indoor air quality
the totality of attributes of indoor air that affect a person's health and wellbeing
infrared radiation
radiation invisible to the human eye, which has less energy and longer wavelengths than visible light
katabatic winds
downhill flows of cool air
La Nia
warming of the western equatorial Pacific warm pool, north of New Guinea, accompanied by cooling in the equatorial eastern Pacific Ocean. La Nia is often associated with above average rainfall in eastern Australia; see El Nio
monsoon
seasonal pattern of wind and rainfall
morbidity
the proportion of sickness in a locality
mortality
relative frequency of death, or death rate
ozone depletion
the process whereby the natural equilibrium between chemical reactions forming and destroying stratospheric ozone is disturbed by the release of manufactured chemicals
ozone layer
a region in the stratosphere where there is a small, but significant, amount of ozone
particles
microscopic or submicroscopic solid or liquid matter, such as soot, dust or smoke
person-year
a unit of measurement, based on the amount of work done by one person in a year consisting of a standard number of person-days
photochemical smog
air pollution caused by chemical reactions among various substances and pollutants in the atmosphere in the presence of sunlight; ozone is a major constituent
photolysis
a process whereby sunlight causes the chemical bonds in a molecule to break
recirculation
recycling of pollutants over an area or within an airshed in response to reversal in winds
sinks
processes or places that remove or store gases, solutes or solids in accumulating parts of the environment
smog
see photochemical smog
SOI (Southern Oscillation Index)
an indicator based on the pressure gradient between the quasi-stationary low pressure region over Indonesia and the centre of the subtropical high pressure cell over the eastern Pacific Ocean; traditionally, Darwin and Tahiti are used as the sites for determining the magnitude of the Southern Oscillation; a negative SOI is associated with higher than normal pressures over Darwin and drought conditions over much of eastern Australia; see Southern Oscillation
Southern Oscillation
a fluctuation in the atmospheric circulation, in particular over the tropical areas of the Pacific and Indian Oceans; in general, when atmospheric pressures are high over the eastern Pacific Ocean they tend to be low in the eastern Indian Ocean and vice versa; the fluctuation between the two produces a marked variation in parameters such as the sea-surface temperature and rainfall over a wide area of the Pacific and has a cycle of two to seven years; the phenomenon is strongly linked to the El Nio; see SOI
standard temperature and pressure
refers to 0C and 1 atmosphere (101.325 kPa)
stratosphere
region of the atmosphere about 15 to 50 km above the earth's surface where typically the temperature changes little or increases with height; the ozone layer occurs in the stratosphere
troposphere
the lower layer of the atmosphere extending to about 15 km above the earth's surface where typically the temperature decreases with height; nearly all clouds form and weather processes are found in this region
ultraviolet (UV) radiation
electromagnetic radiation of higher frequencies and shorter wavelengths than visible light; UV radiation is divided into three ranges: UV-A (320-400 nm), UV-B (280-320 nm) and UV-C (40-290 nm)
volatile organic compound (VOC)
carbon containing compounds occurring in ambient air as gases or vapour with boiling points between 50C and 260C. The VOCs that participate in smog formation reactions are called reactive organic compounds (ROCs). Examples of VOCs include benzene, xylene and toluene
Walker Circulation
an east-west air circulation confined to equatorial regions of the Pacific Ocean and driven principally by the oceanic temperature gradient