作者: Haroon S. Kheshgi , Benjamin S. White
DOI: 10.3402/TELLUSB.V48I1.15660
关键词:
摘要: A nonlinear convolution integral is developed to model the response of ocean carbon sink changes in atmospheric concentration CO 2 . This can accurately represent complex cycle models which behavior stems from dependence solubility seawater on partial pressure, often represented by buffer factor. The kernel be constructed a such an arbitrary change emissions, along with functional Once has been constructed, either analytically or experiment, representation used estimate responses other Thus method used, e.g., explore alternative emissions scenarios for assessments climate change. derivation given, and reproduce two models: one-dimensional diffusive model, three-dimensional ocean-general-circulation tracer model. DOI: 10.1034/j.1600-0889.1996.00002.x