Energy, water, and species richness. | |||
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(a) | Species richness of North American trees increases most predictably with actual evapotranspiration, which is determined by the amount of solar radiation, temperature, and water availability. | (b) | Vertebrate species richness in North America increases most predictably with potential evapotranspiration, a measure of energy availability but not water availability, and is highest in regions of high solar radiation and temperature. |