You are not currently logged in.
Access JSTOR through your library or other institution:
The Role of Climate in the Distribution of Vegetation
John R. Mather and Gary A. Yoshioka
Annals of the Association of American Geographers
Vol. 58, No. 1 (Mar., 1968), pp. 29-41
Stable URL: http://www.jstor.org/stable/2561817
Page Count: 13
You can always find the topics here!Topics: Vegetation, Climate models, Grasses, Climatic zones, Climatology, Evapotranspiration, Coniferous forests, Climatic factors, Savannas, Precipitation
Were these topics helpful?See somethings inaccurate? Let us know!
Select the topics that are inaccurate.
Preview not available
Vegetation develops in response to many different stimuli including climatic, edaphic, and cultural conditions. The degree to which the distribution of vegetation can be explained on the basis of climatic conditions depends in part on the proper selection of active climatic factors. Temperature and precipitation by themselves are poor descriptors of climate. Potential evapotranspiration, water surplus, and water deficit (combined in a moisture index) are found to be more useful. An analysis of the vegetation distribution in conterminous United States shows that the Thornthwaite moisture index and annual potential evapotranspiration are not only able to differentiate among the mid-latitude grassland, forest, and desert biochores but also to provide climatic limits for formation classes within each of the biochores. For example, it is possible to identify on the basis of numerical data an oak-hickory climate as distinct from the birch-maple, and a bunch grass climate distinct from the sagebrush. The problem of non-climatically controlled vegetation associations such as the low latitude pines and savanna are also discussed.
Annals of the Association of American Geographers © 1968 Association of American Geographers