Greenhouse effect climate change and

Bolin, B. (1986). How much CO2 will remain in the atmosphere In "The Greenhouse Effect, Climate Change, and Ecosystems," SCOPE Report 29 (B. Bolin, B. R. D66s, J. Jager, and R. A. Warrick, eds). Wiley, Chichester. 

Bolin B., Doos B. R., lager 1., and Warrick R. A. (1986) The Greenhouse Effect, Climatic Change, and Ecosystems. Wiley, New York. 

Bohn, B. et al. (1986) The Greenhouse Effect, Climate Change and Ecosystems (SCOPE29), John Wiley Sons, Chichester, UK. 

DOOs BR, Jager J, Wanick RA, editors. The greenhouse effect, climatic change and ecosystems. Scope 29. New York John Wiley Publishers, 1986 393-473... 

Derwent, R.G., Collins, W.J., Johnson, C.E., Stevenson, D.S. 2001. Transient behavior of tropospheric ozone precursors in a global 3-D CTM and their indirect greenhouse effects. Climatic Change 49 463 87. 

Lai, Rattan (2001b). Potential of Desertification Control to Sequester Soil Carbon and Mitigate the Greenhouse Effect. Climate Change 15 35-72. 

As a source of clean energy, hydrogen is also going to be the permanent answer to another global problem caused by utilization of fossil fuels, such as the greenhouse effect, climate change, acid rains, ozone layer depletion, pollution and oil spills. 

Penner, J. E Cloud Albedo, Greenhouse Effects, Atmospheric Chemistry, and Climate Change, J. Air Waste Manage. Assoc., 40, 456-461 (1990). 

Hydrates have also been the source of speculation of long-range climate change and safety in the greenhouse effect (Leggett, 1990). Hydrates in climate change are discussed in Section 7.8. 

Effect on Human Health. Direct effects on human health of the emitted greenhouse gases are believed to be small. Other links between climate change and human health have not been well established, although modest effects could result. For example, temperature increases could stress human health such as heat stress, but in cold areas they could reduce stress. Some diseases... 

Climate Change and the Greenhouse Effect. A Briefing from the Hadley Centre, Hadley Centre for Climate Prediction and Research, UK Meteorological Office, Exeter, December 2005 (see also New Scientist, 12 February 2005, 41). 

The possible effects of a decrease in stratospheric ozone concentrations include (1) an increase in skin cancers, (2) an increase in damage to crops and trees, (3) stratospheric cooling leading to large-scale climate changes, and (4) additional production of tropospheric ozone as more and more uv radiation is able to penetrate into the atmosphere closer to Earth. In addition, CFCs themselves, like carbon dioxide and other compounds mentioned in Chapter 11, are greenhouse gases. 

---