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      Seasonal and interannual variation in evapotranspiration, energy balance and surface conductance in a northern temperate grassland

      , ,
      Agricultural and Forest Meteorology
      Elsevier BV

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          A biochemical model of photosynthetic CO2 assimilation in leaves of C 3 species.

          Various aspects of the biochemistry of photosynthetic carbon assimilation in C3 plants are integrated into a form compatible with studies of gas exchange in leaves. These aspects include the kinetic properties of ribulose bisphosphate carboxylase-oxygenase; the requirements of the photosynthetic carbon reduction and photorespiratory carbon oxidation cycles for reduced pyridine nucleotides; the dependence of electron transport on photon flux and the presence of a temperature dependent upper limit to electron transport. The measurements of gas exchange with which the model outputs may be compared include those of the temperature and partial pressure of CO2(p(CO2)) dependencies of quantum yield, the variation of compensation point with temperature and partial pressure of O2(p(O2)), the dependence of net CO2 assimilation rate on p(CO2) and irradiance, and the influence of p(CO2) and irradiance on the temperature dependence of assimilation rate.
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            The Interpretation of the Variations in Leaf Water Potential and Stomatal Conductance Found in Canopies in the Field

            P. Jarvis (1976)
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              Variation among biomes in temporal dynamics of aboveground primary production.

              Interannual variability in aboveground net primary production (ANPP) was assessed with long-term (mean = 12 years) data from 11 Long Term Ecological Research sites across North America. The greatest interannual variability in ANPP occurred in grasslands and old fields, with forests the least variable. At a continental scale, ANPP was strongly correlated with annual precipitation. However, interannual variability in ANPP was not related to variability in precipitation. Instead, maximum variability in ANPP occurred in biomes where high potential growth rates of herbaceous vegetation were combined with moderate variability in precipitation. In the most dynamic biomes, ANPP responded more strongly to wet than to dry years. Recognition of the fourfold range in ANPP dynamics across biomes and of the factors that constrain this variability is critical for detecting the biotic impacts of global change phenomena.
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                Author and article information

                Journal
                Agricultural and Forest Meteorology
                Agricultural and Forest Meteorology
                Elsevier BV
                01681923
                July 2002
                July 2002
                : 112
                : 1
                : 31-49
                Article
                10.1016/S0168-1923(02)00041-2
                d3358bf6-d69b-488c-8e85-58297a5fe623
                © 2002

                http://www.elsevier.com/tdm/userlicense/1.0/

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