Current models predict that as
climate change intensifies, certain environmental gradients may experience the effects as changing rates of natural processes or impacts on distribution and characteristics of species within them. Given the interconnectedness of abiotic factors, long-term disturbances of one gradient have the possibility of affecting other gradients.
Soil characteristics Soil respiration, the process of soil naturally releasing carbon dioxide into the atmosphere, acts as an example of this. In areas where soil moisture is not limiting (with moisture being a key part of the respiration process), soil respiration increases with rising temperatures; thus, respiration patterns form the gradient, and higher emissions are observed in warmer ecosystems. Similarly, rate of precipitation has a positive correlation with respiration (as moisture no longer becomes a limiting factor). Thus, it not only is its own gradient (average precipitation across a range), but also connects with the respiration gradient and impacts it.
Altitude Altitude gradients are a key consideration in understanding migration patterns due to the effects of global warming. As temperatures increase, trees adapted to warmer climates will migrate uphill for access to sunlight, and thus populations of temperate or cold-adapted trees and the habitats suitable for them will shrink. == Environmental gradients in society ==