Improving Marine Ecosystem Models Use of Data Assimilation

  • Slides: 19
Download presentation
Improving Marine Ecosystem Models: Use of Data Assimilation and Mesocosm Experiments Joseph Vallino ASLO

Improving Marine Ecosystem Models: Use of Data Assimilation and Mesocosm Experiments Joseph Vallino ASLO Meeting Santa Fe NM, Feb. 1999 Ecosystems Center Marine Biological Laboratory, Woods Hole MA

Mesocosm Experiment · Additions: – NO 3 (5 m. M), PO 4 (0. 5

Mesocosm Experiment · Additions: – NO 3 (5 m. M), PO 4 (0. 5 m. M), Si (7 m. M) – Leaf litter leachate (300 m. M DOC) · Treatments: – Control: – Organic Matter: Bag B – Daily Nutrients: Bag C – DOM + Nutrients: · Samples Taken: – NO 3, NH 4, PO 4, Si, O 2 DIC – PAR – POC, PON, DOC, DON – Chl a – PP (14 C and O 2 incubations) – Bacterial No. and productivity – Phyto- and zooplankton counts – DI 13 C, DO 15 N – Size fractionated d 13 C and d 15 N D C B A Bag D

Mesocosm Food Web Model · Aggregated, coupled C and N model · Emphasis on

Mesocosm Food Web Model · Aggregated, coupled C and N model · Emphasis on OM processing · Holling type II and III growth kinetics · State Eqns: 10 – Auto. – Osomo. – Hetero. – Detritus – DIN – DOM-L – DOM-R C, N C N C N · Parameters – 29 Kinetic – 10 Initial cond.

Data Assimilation Problem · State Model: · Mapping to Observations: e. g. , POC(t)

Data Assimilation Problem · State Model: · Mapping to Observations: e. g. , POC(t) = A(t) + H(t) + B(t) + DC (t) · Objective Function: Measurement error

Optimization Routines Tested

Optimization Routines Tested

Optimization Results

Optimization Results

Local and Global Optima Raw Data Model y(x) L L a x Local Optima

Local and Global Optima Raw Data Model y(x) L L a x Local Optima Solution y(x) G b Global Optima Solution y(x) x x

Model Errors · Aggregation Error Concentration True Model P 1 P 2 True parameter

Model Errors · Aggregation Error Concentration True Model P 1 P 2 True parameter values Z Time P 1+2 = P 1 + P 2 · Process Errors Concentration Approx. Model P 1+2 Z Estimated aggregated parameter values N Time – Organic matter production and consumption. – Constant parameter values, such as C: N ratio of phytoplankton. – Mortality closure scheme. – Etc.

Conclusions · Mesocosms useful for process based modeling – However, should separately model bag

Conclusions · Mesocosms useful for process based modeling – However, should separately model bag walls, etc. · Optimization Routines – Simulated annealing, if computation limits permits – PRAXIS (no Grad. ) or Levenberg-Marquardt (w/ Grad. ) routines – Adjoint useful for computationally intense problems · Integrate model development with experimental observations · Improve model robustness based on aggregation techniques – Holistic versus reductionist approach · Establish modeling benchmarks

Acknowledgements Chuck Hopkinson Hap Garritt Linda Deegan Ishi Buffam Anne Giblin Michele Bahr John

Acknowledgements Chuck Hopkinson Hap Garritt Linda Deegan Ishi Buffam Anne Giblin Michele Bahr John Hobbie Jane Tucker · Funding: - National Science Foundation, LMER and LTER programs - Lakian Foundation · Manuscript submitted: JMR – Available at: http: //eco 25. mbl. edu/