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Zoology and wildlife conservation

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Abstracts » Zoology and wildlife conservation

Cycling around the South pole

Article Abstract:

Interannual variations in the Antarctic region influence the global temperature by changing temperature gradients between the Equator and the poles. These temperature gradients are responsible for the dynamics of oceans and the atmosphere. The influence of variability in the Antarctic on the formation rates of deep and bottom waters will affect global temperatures on longer timescales. The interannual variations appear to be due to the El Nino/Southern Oscillation signals that predominate interannual climate alteration in high latitudes.

Author: Cane, Mark A., Yuan, Xiaojun, Martinson, Douglas G.
Publisher: Macmillan Publishing Ltd.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 1996
Analysis, Environmental aspects, Global temperature changes, Antarctic regions, Ocean currents

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Closing of the Indonesian seaway as a precursor to east African aridification around 3-4 million years ago

Article Abstract:

Research proposing an alternative explanation of the aridification of Africa occurred approximately three to four million years ago is presented. It is suggested that the closure of the Indonesian seaway could have caused the aridification process.

Author: Cane, Mark A., Molnar, Peter
Publisher: Macmillan Publishing Ltd.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 2001
History, Climatology, Arid regions climate

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Nature, nurture and landscape

Article Abstract:

A physically based theory is needed to study the erosion in mountain regions. Thermochronometric methods to rock now exposed at the surface are applied to quantify erosion rates.

Author: Molnar, Peter
Publisher: Macmillan Publishing Ltd.
Publication Name: Nature
Subject: Zoology and wildlife conservation
ISSN: 0028-0836
Year: 2003
Science & research, Natural resources, Mountains, Natural resources industry software

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Subjects list: Research
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