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Books on the topic 'Australian atmosphere'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

Lloyd, K. H. Upper atmosphere research. Canberra, ACT: AGPS Press, Australian Govt. Pub. Service, 1988.

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2

Force, Western Australian Greenhouse Task. Draft Western Australian greenhouse strategy. Perth, W.A: The Task Force, 2003.

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3

Australian and New Zealand Environment Council. Towards a national greenhouse strategy for Australia. Canberra: Australian Government Pub. Service, 1990.

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4

J, Blong R., ed. The greenhouse effect: Living in a warmer Australia. Kensington, N.S.W., Australia: New South Wales University Press, 1989.

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5

Moffatt, Ian. The greenhouse effect: Science and policy in the Northern Territory, Australia. Darwin, Australia: Australian National University, North Australia Research Unit, 1992.

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6

Whetton, Peter. Australian Region intercomparison of the results of some general circulation models used in enhanced greenhouse experiments. Australia: CSIRO, 1991.

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7

Garratt, J. R. Winds of change: Fifty years of achievements in the CSIRO Division of Atmospheric Research, 1946-1996. Collingwood, Australia: CSIRO Pub., 1998.

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8

Australian made: A multicultural reader. Sydney: Sydney University Press, 2010.

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9

Council, Australia Prime Minister's Science. Global climatic change: Issues for Australia. Canberra, A.C.T: AGPS Press, 1989.

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10

Evans, J. L. Envisaged impacts of enhanced greenhouse warming on tropical cyclones in the Australian region. Australia: CSIRO, 1990.

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11

TOGA Scientific Steering Group. Session. JSC/CCCO TOGA Scientific Steering Group: Report of the seventh session, Cairns, Queensland, Australia (11-15 July 1988). [Geneva?]: World Meteorological Organization, 1988.

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12

CAS/JSC Working Group on Numerical Experimentation. Session. Report of the sixth session of the CAS/JSC Working Group on Numerical Experimentation: Melbourne, Australia, 24-28 September 1990. [Geneva, Switzerland]: World Meteorological Organization, 1991.

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13

Syarif, La Ode Muhamad. The implementation of international responsibilities for atmospheric pollution: A comparison between Indonesia and Australia. Kebayoran Baru, Jakarta: Indonesian Center for Environmental Law, 2001.

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14

Coastal, Zone Management Workshop (1990 Perth Australia). Adaptive responses to climate change: Coastal zone management workshop : the proceedings, Perth, Australia, February 1990. Canberra: Australian Govt. Pub. Service, 1990.

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15

Rychtera, Miroslav. Atmospheric deterioration of technological materials: A technoclimatic atlas. Part B, Asia (excluding Soviet Asia), Australia and Oceania. Amsterdam: Elsevier, 1990.

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16

Crowley, Brian. Hotting up: How the greenhouse effect and ozone depletion will change Australia during the next 40 years. South Melbourne: Matchbooks, 1989.

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17

Australia. Bureau of Transport and Communications Economics. Transport and greenhouse: Costs and options for reducing emissions. Canberra: Australian Govt. Pub. Service, 1996.

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18

Walker, B. H. Effects of atmospheric and climate change on terrestrial ecosystems: Report of a workshop organized by the IGBP Coordinatin Panel on Effects of Climate Change on Terrestrial Ecosystems at CSIRO, Division of Wildlife and Ecology Canberra, Australia 29 February-2 March, 1988. Stockholm: IGBP, 1989.

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19

Australian upper atmospheric and space physics research in Antarctica, 1992. Kingston, Tas., Australia: Antarctic Division, Dept, of the Arts, Sport, the Environment and Territories, 1992.

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20

B, Burns G., Craven M, and Australian National Antarctic Research Expeditions., eds. Australian upper atmospheric and space physics research in Antarctica, 1987. Kingston, Tas., Australia: Antarctic Division, Dept. of Science, 1987.

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21

Rivett, Rohan. David Rivett. CSIRO Publishing, 2013. http://dx.doi.org/10.1071/9780643109964.

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Sir David Rivett was an Australian chemist and Chief Executive Officer of CSIR between 1927 and 1945. He became Chairman from 1945 to 1949, retiring when CSIR was reorganised and became CSIRO. Because of Sir David's unique contributions to many fields of science and his efforts directed towards CSIR's early development, CSIR became Australia's major research agency. In April 1961 the Prime Minister of Australia, Sir Robert Menzies, commenting on the death of Rivett, said: 'David Rivett was one of the greatest Australians of our time. He combined an absolute first class mind and great scientific attainments with a generous outlook and a quiet, but pervading, enthusiasm. Scientific research in Australia owes a great deal to him'. The international scientific journal Nature in its issue of June 10, 1961, said that Rivett was 'a man who had contributed perhaps more than any other to the present healthy state of Australian science. ... Rivett and his colleagues contrived, in a country woefully weak in research, to create an atmosphere in which it could flourish... Once one had gained his confidence he was a magnificent friend and backer; he believed in delegating responsibility and with it any credit that accrued, but in times of adversity he it was who wished to shoulder the blame'. This is an eBook version of the hardback originally published in 1972.

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22

Cameron, Alexia. Affected Labour in a Café Culture: The Atmospheres and Economics of 'Hip' Melbourne. Taylor & Francis Group, 2018.

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23

Affected Labour in a Café Culture: The Atmospheres and Economics of 'Hip' Melbourne. Routledge, 2018.

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24

Cameron, Alexia. Affected Labour in a Café Culture: The Atmospheres and Economics of 'Hip' Melbourne. Taylor & Francis Group, 2018.

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25

Hameed, Saji N. The Indian Ocean Dipole. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.619.

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Discovered at the very end of the 20th century, the Indian Ocean Dipole (IOD) is a mode of natural climate variability that arises out of coupled ocean–atmosphere interaction in the Indian Ocean. It is associated with some of the largest changes of ocean–atmosphere state over the equatorial Indian Ocean on interannual time scales. IOD variability is prominent during the boreal summer and fall seasons, with its maximum intensity developing at the end of the boreal-fall season. Between the peaks of its negative and positive phases, IOD manifests a markedly zonal see-saw in anomalous sea surface temperature (SST) and rainfall—leading, in its positive phase, to a pronounced cooling of the eastern equatorial Indian Ocean, and a moderate warming of the western and central equatorial Indian Ocean; this is accompanied by deficit rainfall over the eastern Indian Ocean and surplus rainfall over the western Indian Ocean. Changes in midtropospheric heating accompanying the rainfall anomalies drive wind anomalies that anomalously lift the thermocline in the equatorial eastern Indian Ocean and anomalously deepen them in the central Indian Ocean. The thermocline anomalies further modulate coastal and open-ocean upwelling, thereby influencing biological productivity and fish catches across the Indian Ocean. The hydrometeorological anomalies that accompany IOD exacerbate forest fires in Indonesia and Australia and bring floods and infectious diseases to equatorial East Africa. The coupled ocean–atmosphere instability that is responsible for generating and sustaining IOD develops on a mean state that is strongly modulated by the seasonal cycle of the Austral-Asian monsoon; this setting gives the IOD its unique character and dynamics, including a strong phase-lock to the seasonal cycle. While IOD operates independently of the El Niño and Southern Oscillation (ENSO), the proximity between the Indian and Pacific Oceans, and the existence of oceanic and atmospheric pathways, facilitate mutual interactions between these tropical climate modes.

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26

Baseline 97-98 (Baseline Atmospheric Program Australia 1997-1998). Bureau of Meteorology and CSIRO, 2001.

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27

Greenhouse Coordination Council (Western Australia), ed. A revised greenhouse strategy for Western Australia, 1994. [Western Australia]: The Council, 1995.

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28

Living in the Hothouse: How Global Warming Affects Australia. Scribe Publications Pty Ltd., 2005.

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29

Behera, Swadhin, and Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

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The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespread fish mortality during the event. Quite opposite of this characteristic change in the ocean condition, cold SST anomalies prevail in the eastern equatorial Pacific during the El Niño Modoki events, but with the warm anomalies intensified in the central Pacific. The boreal winter condition of 2004 is a typical example of such an event, when a tripole pattern is noticed in the SST anomalies; warm central Pacific flanked by cold eastern and western regions. The SST anomalies are coupled to a double cell in anomalous Walker circulation with rising motion in the central parts and sinking motion on both sides of the basin. This is again a different feature compared to the well-known single-cell anomalous Walker circulation during El Niños. La Niña Modoki is the opposite phase of the El Niño Modoki, when a cold central Pacific is flanked by warm anomalies on both sides.The Modoki events are seen to peak in both boreal summer and winter and hence are not seasonally phase-locked to a single seasonal cycle like El Niño/La Niña events. Because of this distinction in the seasonality, the teleconnection arising from these events will vary between the seasons as teleconnection path will vary depending on the prevailing seasonal mean conditions in the atmosphere. Moreover, the Modoki El Niño/La Niña impacts over regions such as the western coast of the United States, the Far East including Japan, Australia, and southern Africa, etc., are opposite to those of the canonical El Niño/La Niña. For example, the western coasts of the United States suffer from severe droughts during El Niño Modoki, whereas those regions are quite wet during El Niño. The influences of Modoki events are also seen in tropical cyclogenesis, stratosphere warming of the Southern Hemisphere, ocean primary productivity, river discharges, sea level variations, etc. A remarkable feature associated with Modoki events is the decadal flattening of the equatorial thermocline and weakening of zonal thermal gradient. The associated ocean-atmosphere conditions have caused frequent and persistent developments of Modoki events in recent decades.

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30

Global change: A research strategy for Australia, 1992-1996. Canberra: Australian Academy of Science, 1992.

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31

Climate change in Australia: Environmental, socioeconomic, and political considerations. Canberra: Centre for Resource and Environmental Studies, Australian National University, 1990.

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32

Godfrey, Lowe, and Western Australia. State Greenhouse Effect Committee., eds. Greenhouse 88: Planning for climatic change : Western Australian conference proceedings : a conference held in Perth, November 3-5, 1988 and convened by the State Greenhouse Effect Committee, the Western Australian Water Resources Council, the Environmental Protection Authority, and the Commission for the Future. Perth: Western Australian Water Resources Council & Environmental Protection Authority, 1989.

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33

The Garnaut Review 2011 Australia In The Global Response To Climate Change. Cambridge University Press, 2011.

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34

Submission on the Future directions for Australia's national greenhouse strategy discussion paper. Perth, Australia: The Centre, 1997.

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35

Scott, Andrew C. Burning Planet. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198734840.001.0001.

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Raging wildfires have devastated vast areas of California and Australia in recent years, and predictions are that we will see more of the same in coming years as a result of climate change. But this is nothing new. Since the dawn of life on land, large-scale fires have played their part in shaping life on Earth. Andrew C. Scott tells the whole story of fire's impact on our planet's atmosphere, climate, vegetation, ecology, and the evolution of plant and animal life. It has caused mass extinctions, and it has propelled the spread of flowering plants. The exciting evidence we can now draw on has been preserved in fossilized charcoal, found in rocks hundreds of millions of years old, from all over the world. These reveal incredibly fine details of prehistoric plants, and tell us about climates from deep in earth's history. They also give us insight into how early hominids and humans tamed fire and used it. Looking at the impact of wildfires in our own time, Scott also looks forward to how we might better manage them in future, as climate change has an increasing effect on our world.

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36

Milner, Andrew, and J. R. Burgmann. Science Fiction and Climate Change. Liverpool University Press, 2020. http://dx.doi.org/10.3828/liverpool/9781789621723.001.0001.

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Despite the occasional upsurge of climate change scepticism among Anglophone conservative politicians and journalists, there is still a near consensus among climate scientists that current levels of atmospheric greenhouse gas are sufficient to alter global weather patterns to disastrous effect. The resultant climate crisis is simultaneously both a natural and a socio-cultural phenomenon and in this book Milner and Burgmann argue that science fiction occupies a critical location within this nature/culture nexus. Science Fiction and Climate Change takes as its subject matter what Daniel Bloom famously dubbed ‘cli-fi’. It does not, however, attempt to impose a prescriptively environmentalist aesthetic on this sub-genre. Rather, it seeks to explain how a genre defined in relation to science finds itself obliged to produce fictional responses to the problems actually thrown up by contemporary scientific research. Milner and Burgmann adopt a historically and geographically comparatist framework, analysing print and audio-visual texts drawn from a number of different contexts, especially Australia, Britain, Canada, China, Finland, France, Germany, Japan and the United States. Inspired by Raymond Williams’s cultural materialism, Pierre Bourdieu’s sociology of culture and Franco Moretti’s version of world systems theory, the book builds on Milner’s own Locating Science Fiction to produce a powerfully persuasive study in the sociology of literature.

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37

Exposure standards for atmospheric contaminants in the workplace in Western Australia: This document incorporates Regulation 322 of the Occupational Health, Safety and Welfare Regulations 1988, and, Adopted National Exposure Standards for Atmospheric Contaminants in the Occupational Environment [NOHSC: 1003(1991)] declared by the National Occupational Health and Safety Commission. [Western Australia]: The Commission, 1991.

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