By R. Fantechi, N.S. Margaris
Complaints of the knowledge Symposium within the EEC Programme in Climatology held in Mytilene, Greece, April 15-18, 1984
Read Online or Download Desertification in Europe: Proceedings of the Information Symposium in the EEC Programme on Climatology, held in Mytilene, Greece, 15–18 April 1984 PDF
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Extra resources for Desertification in Europe: Proceedings of the Information Symposium in the EEC Programme on Climatology, held in Mytilene, Greece, 15–18 April 1984
2 a-c. The annual mean temper ature change Values above 4 K are found over North Africa . In winter there is 4 to 5 K. is a zonal distrib ution with values exceed ing 4 K in the northe rn part of the study area. The distrib ution in summer shows a temper ature increa se of 2 - 3 K in centra l and eastern Europe and one exceed ing 4 K over the southe rn Medite rranean and wester n parts of North Africa . Statis tical tests were only perform ed for the season s showing signifi cant change s at the 5% level everyw here except for a small area coverin g Greece and Bulgar ia in summer.
The effect of soil moisture on circulation and rainfall in a tropical model. Quaterly Journal of the Royal Meteorological Society 103(435), pp. 29-46. 49. J. , 1975. The effects of changing the solar constant on the climate of a General Circulation Model. J. Atmos. Sci. 32, pp. 2044-2059. ~ 33 ~ ~. 51. 52. 53. 54. , 1977. Geographical Patterns of Climatic Change 1000 BC - 1700 AD. NOAA Report 7-35207. , 1980. Scenario for a warm high co 2 world. Nature 283, pp. 17-21. , 1981. Detecting C0 2-induced climatic change.
Winter temperature variability increases in Spain and southern France but decreases over the whole rest of the Mediterranean Basin. 5°C. These patterns are in fact related to higher mean sea level pressures in a warm world for most of Europe, except for the Mediterranean basin. The effects of precipitation changes may be even more important for land ressources. In general, the warm period shows lower annual rainfall over most of Europe with a maximum decline in northern Italy and South central France where an increase in variability is also observed.