ABSTRACT

The land carbon cycle has been extensively studied yet its fundamental properties have not been fully understood. This chapter offers empirical evidence to demonstrate a general dynamic pattern that the land carbon cycle changes in a direction toward a moving attractor in response to global change. This general pattern is captured by a matrix equation. The relatively simple matrix equation can unify land carbon cycle models, accelerate computational efficiency for spin-up, diagnose model performance with new analytics, enable data assimilation with complex models to improve their predictive skills, and guide carbon cycle research with a new theoretical framework of dynamic disequilibrium.