|
Assimilation
of chlorophyll and nutrients into a 3-D marine carbon cycle model
(NASA-Carbon cycle)
Current
Work
Ecosystem
parameter optimization of a 3-D coupled physical and carbon cycle model
Abstract
An adjoint method
is applied to a three-dimensional global ocean biogeochemical model to
optimize the ecosystem parameters using SeaWiFS surface chlorophyll
observation. Identical twin experiments were conducted to test the
robustness of the optimization technique in recovering the generated
synthetic data, in which it was able to identify the most sensitive
parameters to be phytoplankton and zooplankton exudation, herbivore
egestion as fecal pellets, zooplankton grazing, and the assimilation
efficiency. The assimilation of SeaWiFS chlorophyll data yielded
significant reduction of the model-data misfit, especially in high
latitude regions. The regional experiments suggested that the
parameters in the high latitudes have higher seasonal variance than in
the lower latitudes. The optimized model run yields global net primary
production of 36 Pg C yr-1, which lies within the range suggested by
Antoine et al. [1996]. Additional constraints of nutrient data
from the World Ocean Atlas showed further reduction in the model-data
misfit and that assimilation with extensive data sets is necessary.
Schematic diagram of
the minimization
scheme
Observations
In this study,
the seasonal SeaWiFS
chlorophyll data is used. We averaged the monthly data from January
1997 to December 2003 into seasonal data sets. The data are
interpolated into the model grid for the assimilation purposes. Below
are the intrpolated seasonal chlorophyll data for boreal winter (a),
spring (b), summer (c), and fall (d).
 
(a)
(b)
 
(c)
(d)

Optimized model
chlorophyll
output
The
model-data misfit are reduced varying the
model control variable at three different region (north, tropic, and
south) and different seasons. Below are the optimized model chlorophyll
output (a posteriori) for winter (a), wpring (b), summer (c), and fall
(d).
 
(a)
(b)
 
(c)
(d)

References
Antoine, D., J-M. André,
and A. Morel (1996), Oceanic
primary production 2. Estimation at global scale from satellite
(coastal zone color scanner) chlorophyll, Global Biogeochem. Cycles,
10, 57-69.
|
|