| one publication added to basket [283889] | The greenhouse effect, stratospheric ozone, marine productivity, and global hydrology: Feedbacks in the global climate system
Rampino, M.R.; Etkins, R. (1990). The greenhouse effect, stratospheric ozone, marine productivity, and global hydrology: Feedbacks in the global climate system, in: Paepe, R. et al. Greenhouse Effect, Sea Level and Drought. Proceedings of the NATO Advanced Research Workshop on Geohydrological Management of Sea Level and Mitigation of Drought, Fuerteventura, Canary Islands (Spain), March 1-7, 1989. NATO ASI Series C: Mathematical and Physical Sciences, 325: pp. 3-20. http://dx.doi.org/10.1007/978-94-009-0701-0_1 In: Paepe, R. et al. (Ed.) (1990). Greenhouse Effect, Sea Level and Drought. Proceedings of the NATO Advanced Research Workshop on Geohydrological Management of Sea Level and Mitigation of Drought, Fuerteventura, Canary Islands (Spain), March 1-7, 1989. Digitized reprint of the hardcover 1st edition 1990. NATO ASI Series C: Mathematical and Physical Sciences, 325. Kluwer Academic Publishers: Dordrecht. ISBN 978-94-009-0701-0. xix, 718 pp. http://dx.doi.org/10.1007/978-94-009-0701-0, more In: NATO ASI Series C: Mathematical and Physical Sciences. D. Reidel: Dordrecht; Boston; Lancaster. ISSN 0258-2023, more |
| Available in | Authors | | Document type: Conference paper
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| Abstract | The problems of greenhouse warming, ozone depletion and changes in global hydrology are inter-related through a number of feedback mechanisms. Recognized feedbacks act through two important loops involving changes in atmospheric chemistry, UV-B radiation at the earth’s surface, and marine productivity. Reliable predictions of future changes in global and regional climate require an understanding of the direction, magnitude and time constants of the various climatic and biochemical feedback processes. Changes in the amount and distribution of precipitation can also have important feedback effects on soil moisture, vegetation, cloudiness, ground and cloud albedo, ocean salinity (through changes in evaporation and runoff), bottom water formation and productivity. Model studies incorporating these and other feedbacks should be useful in determining the sensitivity of the climate system and anthropogenic changes. |
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