Figure 5 - uploaded by Andrés Antico
Content may be subject to copyright.
Example of the behavior of the box model for the carbon cycle formulated by Sarmiento and Toggweiler (1984) (see text for more details). Redrawn from Watson and Orr (2003).
Source publication
Contexts in source publication
Context 1
... example of the behavior of the model formulated by Sarmiento and Toggweiler (1984) is given by Watson and Orr (2003). This is done by disturbing the model with an exponentially increasing release of CO 2 into the atmosphere (see figure 5, top panel). The model is started at an equilibrium state and the atmospheric CO 2 perturbation increases 1% per year for 150 years, and then there is no input. ...
Context 2
... model is started at an equilibrium state and the atmospheric CO 2 perturbation increases 1% per year for 150 years, and then there is no input. The atmospheric CO 2 concentration follows this forcing and begins to decrease by ocean uptake when the the atmospheric CO 2 perturbation ceases (see figure 5, middle panel). The deep ocean is the sink for the atmospheric CO 2 excess. ...
Similar publications
We analyze global and regional changes in CO2 fluxes using
two simple models, an airborne fraction of anthropogenic emissions
and a linear relationship with CO2 concentrations. We show
that both models are able to fit the nonanthropogenic (hereafter
natural) flux over the length of the atmospheric concentration
record and that departures in the air...
Climate change involves a direct response of the climate system to forcing which is amplified or damped by feedbacks operating in the climate system. Carbon-cycle feedbacks alter the land and ocean carbon inventories and so act to reduce or enhance the increase in atmospheric CO2 from carbon emissions. The prevailing framework for carbon-cycle feed...
Soil organic carbon (SOC) dynamics are vital in the context of climate change and sustainable soil management. The ẟ13C signatures of SOC are powerful indicators and tracers of C fluxes through soils and of transformation processes within soils. Depth gradients of ẟ13C can be considered as their archive. However, many different drivers and processe...