1. Impacts of Climate and basin- scale variability on the seeding and production of Calanus finmarchicus in the Gulf of Maine and Georges Bank Avijit Gangopadhyay With Bisagni, Gifford and Batcheldar GLOBEC meeting, WHOI 23 April 2007

2. List of Investigators Avijit Gangopadhyay (PI – Basin-scale physical modeling) Jim Bisagni (UMass Dartmouth) – Satellite SST field, Hydrographic analysis Dian Gifford (URI) – Zooplankton data analysis Hal Batchelder (OSU) – IBM modeling

3. Goals and Objectives to probe the connections between Calanus finmarchicus distributions and the physical oceanographic properties, climate variability, and basin-scale circulation changes that are likely to affect the copepod’s transport onto Georges Bank. We will do this using a combination of numerical model simulations and observational data.

4. Bio-physical Hypotheses Hypothesis: The occurrence of large populations of Calanus finmarchicus in the coupled GB/GoM system REQUIRES (1) high seed stocks (supply) of diapausing C.finmarchicus in the deeper ocean regions nearby (GOM basins and the Slope Sea), (2) that the deep C. finmarchicus stocks terminate diapause at the appropriate time to be synchronous with continental shelf spring blooms, and (3) a nutrient enriched, highly productive ecosystem in the GB/GoM to sustain high growth and survival rates of Calanus that will provide seed for the subsequent year. Prediction A: Overwintering Calanus finmarchicus seed stocks are LOW and GB/GoM productivity is HIGH when the water masses of the Slope Sea have little influence (input) from Labrador-Irminger Gyre (Labrador Slope Water) water masses (due to the relatively nutrient replete bottom waters and low Calanus supply in Warm Slope Waters), but C. finmarchicus recruitment is good because of a near-perfect match between the time of diapause awakening and the time of the spring bloom, the latter of which is large because of the higher concentration of nutrients in deep warm slope waters. Prediction B: Overwintering C. finmarchicus seed stocks are HIGH and GB/GoM productivity is LOW when the water masses of the Slope Sea have a large proportion of Labrador Sea water (due to the relatively nutrient-depleted bottom waters and high C. finmarchicus supply in cold Labrador Slope Water), but recruitment and productivity are poor because of the generally low springtime productivity (low nutrients) and a timing mismatch between diapause awakening, ascent and reproduction and the NW Atlantic spring bloom.

5. Methodology Set up and run an individual based model (IBM) for the Northwest Atlantic, using the high-NAO (1980-1993) and low-NAO (1962- 1971) forced physical fields from an ongoing eddy-resolving North Atlantic simulation. Perform a set of eddy-resolving basin-scale model simulations during 1988-1999 starting from already existing high-NAO simulations (from the ongoing NASA project) and run the IBM to study the interannual variability of C. finmarchicus seeding and production in this region. Analyze long-term in-situ physical and biological datasets and satellite-derived sea surface temperature (SST) along with in-situ physical, biological, and chemical data collected during the GLOBEC core-measurement period (1995-1999), and validate the basin-scale physical and biological fields to develop a broader understanding of C. finmarchicus seeding and production. Generate four-dimensional high-resolution (5-km) physical fields using basin-scale fields and available data during 1993-1999, and run a series of IBM simulations at higher resolution in order to address questions relating ecosystem variability on the Scotian Shelf, on Slope Sea and within the Gulf of Maine and on Georges Bank to the large-scale fluctuations of the NAO.

6. Ongoing NASA project Basin scale modeling for North Atlantic High and Low NAO simulations Focus on Gulf Stream and Labrador Sea Nutrient Dynamics – Depletion vs. Dilution Physics and nutrient flux experiments

7. ROMS North Atlantic Model Low NAO simulation loses excess heat as compared to High NAO simulation Is the NCEP climatology overestimating the heat loss in the system ? High NAO Model Simulation using SOC Climatology (1980-1993), January 6 Low NAO Model Simulation using NCEP Climatology (1963-1971), January 6 North Atlantic Model Simulation January 6. by McGillicuddy et. al Source: www.whoi.edu

8. North Atlantic Heat Flux Comparison of Monthly Mean Climatology of SOC and NCEP during 1980-1993 for January shows differences on the order of 100 W/m 2 JAN NCEP JAN SOC JAN SOC- NCEP

9. North Atlantic Heat Flux Comparison of Annual Mean Climatology of SOC and NCEP during 1980-1993 show similar differences as January on the order of 100 W/m 2 ANNUAL NCEP ANNUAL SOC ANNUAL SOC- NCEP

10. North Atlantic Heat Flux Net Heat Flux is given as Q net = Q H +Q E +Q LW +Q SW where, Q H = Sensible Heat Loss Q E = Latent Heat Loss Q LW = Longwave Loss Q SW = Shortwave Heat Gain Is the NCEP climatology underestimating/overestimating any of these components?

11. North Atlantic Heat Flux The NCEP Climatology overestimates the Net Heat Loss for the North Atlantic Region due to overestimation of Latent and Sensible Heat Loss terms and underestimation of Shortwave Gain term. This overestimation is leading to spurious results in the Low NAO Model simulation. Functional regression is used resolve the overestimation in NCEP Climatology as follows: Slope (m) and Intercept (y) are determined for each month using the SOC and NCEP climatologies for 1980-1993 (High NAO) SOC(high NAO) = m*NCEP(high NAO) + y m and y are used to adjust the NCEP Climatology for 1958- 1971 (Low NAO) Predicted NCEP (low NAO) = m*NCEP(low NAO) y, also Predicted NCEP (high NAO) = [SOC(high NAO)-y] / m

12. North Atlantic Heat Flux SOC(high NAO) = 0.9139 * NCEP(high NAO) + 26.19 Predicted(low NAO) = 0.9139 * NCEP(low NAO) + 26.19 January Example

13. North Atlantic Heat Flux ANNUAL NCEPANNUAL SOCANNUAL SOC-NCEP ANNUAL ADJUSTED NCEPANNUAL SOCANNUAL SOC- ADJUSTED NCEP High NAO 1980-1993 Results

14. Model Results

15. Hypothesis The Gulf Stream position is northward (southward) during High (Low) NAO years. The model is spun-up using Levitus climatology for the North Atlantic Basin and subsequently forced with adjusted NCEP High and Low NAO fields. GS mean positions are computed at different depths for both High and Low NAO simulations for comparison

16. Gulf Stream path analysis  Isotherms typical of Gulf Stream signature at different depths are used to obtain frontal location.  Nearest neighbor connected component theory is used to ascertain to continuity of the front  Frontal location derived from every 3 day model output are averaged to obtain mean frontal position DepthIsotherm 5m18 o C 50m17 o C 100m16 o C 200m15 o C 400m12 o C

17. Gulf Stream Mean Positions for High and Low NAO Climatology simulations at 5m, 50m, 100m, 200m and 400m 5m 100m 400m 50m 200m

18. Upper Layer Integrated Path  Model simulation validates our hypothesis that GS is northward (southward) during High (Low) NAO years

19. Current/Future Work The High NAO simulation will be used as initial condition to run the ROMS model for GLOBEC years (1995-1999) SOC forcing available from 1980-1999 will be used to force the model instead of the NCEP climatology Model output will be used to track the 1998 event of southwestward inflow of Labrador Current Melding of ROMS with FORMS for 1995-1999 using 5- day SST fields

20. Proposed Biological simulations Individual-based models (HPB) Lagrangian pathways Zooplankton data as initial and validation fields (DG) Seeding vs. production hypothesis testing Impact of Labrador water inflow on Slope sea and GOMGB regions

21. Creating high resolution fields Use Feature oriented regional modeling system (FORMS) for GOMGB (Gangopadhyay et al., 2003; Brown et al. 2007a-b) 270 non-dimensional structure functions for temperature and salinity along and across seven features in the Gulf/Bank Calibrate with SST 5-day composite (Bisagni’s lab) Use basin-scale simulations as background Multiscale Objective analysis will meld basin-to- regional scale fields Use these high-resolution fields for biological simulations

22. Summary NASA-funded Basin-scale simulation is complete Wind forcing fields during 1980-1999 are ready and are being used to force the model for different simulations Will use this set-up to start GLOBEC period simulations and nowcasting Biological IBM towards understanding impact of climate and BSV on calfin seeding and production