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  • Language: en
  • Pages: 12

"Problems of Environmental Management," by Gordon J. MacDonald

  • Type: Book
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  • Published: 1971
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  • Publisher: Unknown

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Too Late for Gordon and Khartoum
  • Language: en
  • Pages: 402

Too Late for Gordon and Khartoum

  • Type: Book
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  • Published: 1887
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  • Publisher: Unknown

None

Gordon G. MacDonald
  • Language: en
  • Pages: 9

Gordon G. MacDonald

  • Type: Book
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  • Published: 1924
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  • Publisher: Unknown

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Gordon G. MacDonald
  • Language: en
  • Pages: 2

Gordon G. MacDonald

  • Type: Book
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  • Published: 1923
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  • Publisher: Unknown

None

Ice Ages and Astronomical Causes
  • Language: en
  • Pages: 338

Ice Ages and Astronomical Causes

It is not possible to understand the present or future climate unless scientists can account for the enormous and rapid cycles of glaciation that have taken place over the last million years, and which are expected to continue into the future. A great deal has happened in the theory of the ice ages over the last decade, and it is now widley accepted that ice ages are driven by changes in the Earth's orbit. The study of ice ages is very inter-disciplinary, covering geology, physics, glaciology, oceanography, atmospheric science, planetary orbit calculations astrophysics and statistics.

Down to the Sea
  • Language: en
  • Pages: 81

Down to the Sea

  • Type: Book
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  • Published: 1978
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  • Publisher: Unknown

None

Global Climate and Ecosystem Change
  • Language: en
  • Pages: 258

Global Climate and Ecosystem Change

Humankind's ever-expanding activities have caused environmental changes that reach beyond localities and regions to become global in scope. Disturbances to the atmosphere, oceans, and land produce changes in the living parts of the planet, while, at the same time, alterations in the biosphere modify the atmosphere, oceans, and land. Understanding this complex web of interactions poses unprecedented intellectual challenges. The atmospheric concentrations of natural trace gases-carbon dioxide (C0 ), methane (CH. ), nitrous oxide (N0), and lower-atmosphere ozone 2 2 (Os)-have increased since the beginning of the industrial revolution. Industrial gases such as the chlorofluorocarbons (CFCs), whi...