By Leo J. Fritschen (auth.), B. A. Hutchison, B. B. Hicks (eds.)
The results of meteorological phenomena upon wooded area produc tivity and forestry operations were of shock for a few years. With the evolution of system-level reviews of wooded area eco procedure constitution and serve as within the overseas organic software and in other places, extra primary interactions among woodland ecosystems and the ambience got clinical atten tion however the emphasis on meteorological and climatological results on wooded area procedures remained. extra lately, as recogni tion has built of power and genuine difficulties linked to the atmospheric shipping, dispersion, and deposition of airborne toxins, the results of wooded area canopies upon boundary-layer meteorological phenomena has come less than clinical scrutiny. seeking to the long run, with emerging atmospheric con centrations of C02 and lengthening festival for the finite fresh-water assets of the earth, curiosity within the position of forests in worldwide C02 and water balances can be anticipated to accentuate. therefore, the character of woodland canopy-atmosphere interac tions, that's to assert, the meteorological phenomena taking place in and above woodland canopies, are of significance to a large choice of clinical and social-issues. calls for for woodland meteorological info presently exceed degrees of information and given the commercial constraints of technological know-how in most cases and environmental sciences particularly, possibilities for significant advancements in scien tific help within the close to destiny are slender. regrettably, experiences of environmental phenomena in and above forests are high priced and logistically tough. timber, the ecological dominants of wooded area ecosystems, are the most important of all terrestrial organisms.
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Additional resources for The Forest-Atmosphere Interaction: Proceedings of the Forest Environmental Measurements Conference held at Oak Ridge, Tennessee, October 23–28, 1983
Example text
1966. Micrometeorological determination of water loss from various surfaces. In: Atmospheric and SoilPlant-Water Relationships. Technical Report ECON 2-66P-A. U. S. Army Electronic Command, Ft. Huachuca, Az. Fritschen, L. , C. H. Driver, C. Avery, J. Buffo, R. Edmonds, R. Kinerson, and P. Schiess: 1969. Dispersion of air tracers into and within a forested area. S. Army Electronic Command, Atmospheric Sciences Laboratory, Ft. Huachuca, AZ. Fritschen, L. , L. Cox and R. Kinerson: 1973. A 28-meter Douglas-fir in a weighing lysimeter.
In: Extended Abstracts of the 16th conference on Agriculture and Forest Meteorology. Am. Meteorol. Soc. Boston, Mass. 245 pp. : 1976. Crown structure and distribution of biomass in a lodgepole pine stand. USDA Forest Service Res. Paper RM-165. Fort Collins, Co. Gay, L. , K. R. Knoerr and M. O. Braaten: 1971. Solar radiation variability on the floor of a pine plantation. Agr. Meteorol. 8:39-50. : 1966. The Climate Near the Ground. Harvard University Press. Cambridge, Mass. 611 pp. Gisborne, H. : 1941.
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