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Titlebook: Global Change and Terrestrial Ecosystems in Monsoon Asia; T. Hirose,B. H. Walker Book 19961st edition Kluwer Academic Publishers 1996 bios

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Environmental regulation of surface conductance for evaporation from vegetation,on as leaf area index diminishes. The model is also successfully tested by comparison with canopy conductances of emergent trees measured in the .forest. The constraint of vegetation surface conductance and evaporation via environmental regulation by irradiance, air saturation deficit and root zone water supply are discussed.
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The basis for variation in leaf longevity of plants,ell as experimental results on various plant species. The theory, which is extended to seasonal environments, is general and applicable to seasonal as well as aseasonal environments. The theory simulated the bimodal geographic distribution of evergreenness.
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Factors determining distributions of tree species and plant functional types,ion types was produced and used to estimate the minimal number of vegetation types needed. The resulting set of 40 potential dominant vegetation types may serve as an initial basis for a structural-functionally based set of world plant functional types.
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The boreal forests of north-eastern Eurasia,namics in the oceanic part of the region. It is suggested that as a result of global warming one may expect a strong alteration in vegetation pattern, especially in the northern and mountain areas..Nomenclature: Mainly Vorobiev (1968), Wild trees and scrubs of the (Russian) Far East, Nauka, Leningra
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Composition, dynamics and disturbance regime of temperate deciduous forests in Monsoon Asia, important in the other two forest types. Fire seems to be important in the warm temperate deciduous forest, and both fire and large scale blowdowm seems important in the cool temperate mixed broadleaf/conifer forest. These differences in forest composition and disturbance regimes associated with cl
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Tropical seasonal forests in monsoon Asia: With emphasis on continental southeast Asia,n hectares of forest mainly tropical moist forests are being lost each year. There is a widespread recognition that agriculture and the burning of tropical moist forests contribute to global warming but to a much lesser extent than the combustion of fossil fuels and industrial activities in the deve
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Terrestrial transects for global change research,-term changes in biome boundaries and vegetation distribution. The proposed initial set of IGBP terrestrial transects are located in four key regions: (.) humid tropical forests undergoing land use change, (.) high latitudes including the transition from boreal forest to tundra, (.) semi-arid tropic
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