Title: U.S. ECoS U.S. Eastern Continental Shelf Carbon Budget: Modeling, Data Assimilation, and Analysis
1U.S. ECoSU.S. Eastern Continental Shelf Carbon
BudgetModeling, Data Assimilation, and Analysis
- A project of the NASA Earth System Enterprise
- Interdisciplinary Science Program
- Ocean Carbon Biogeochemistry Workshop
- Woods Hole, MA, July 2006
2U.S. ECoSScience Team
- Eileen Hofmann (ODU) project oversight, 1D
modeling - Marjorie Friedrichs (ODU) 1D modeling and data
assimilation - Chuck McClain (GSFC) project oversight,
remote sensing data - Sergio Signorini (GSFC) satellite data
analysis - Antonio Mannino (GSFC) carbon cycling
- Cindy Lee (SUNY-SB) carbon cycling
- Jay OReilly (NOAA) satellite data
analysis - Dale Haidvogel (RU) circulation
modeling - John Wilkin (RU) circulation
modeling - Katja Fennel (RU) biogeochemical
modeling - Sybil Seitzinger (RU) food web and
nutrient dynamics - Jim Yoder (URI) food web and
nutrient dynamics - Ray Najjar (PSU) oxygen data,
climate modeling - David Pollard (PSU) climate modeling
3U.S. ECoS
Goal To develop carbon budgets for the U.S. east
coast continental shelf (Mid-Atlantic Bight
and South Atlantic Bight)
Research Questions
- 1. What are the relative carbon inputs to the MAB
and SAB from - terrestrial run-off and in situ biological
processes? - 2. What is the fate of DOC input to the
continental shelf from - estuarine and riverine systems?
- 3. What are the dominant food web pathways that
control carbon - cycling and flux in this region?
- 4. Are there fundamental differences in the
manner in which carbon - is cycled on the continental shelves of the
MAB and SAB? - 5. Is the carbon cycle of the MAB and SAB
sensitive to - climate change?
4Outline of Presentation
- Theme 1 Development and implementation of
circulation, biogeochemistry, and carbon cycling
models for the east coast of the U.S. - Theme 2 Data analysis effort includes
historical in situ measurements and
satellite-derived data - Theme 3 Limited field measurement effort
- Theme 4 Implementation of data assimilative
models - Theme 5 Interfacing circulation and
biogeochemical models with climate models
5Theme 1 Circulation and biogeochemical modeling
Northeast North American shelf model (NENA)
6Theme 1 Circulation and biogeochemical modeling
Simulated Salinity
WOA98 Salinity 10m August
4m August 2002
North-south gradients agree, simulations produce
mesoscale variability
Wilkin, Haidvogel
7Theme 1 Circulation and biogeochemical modeling
Hindcasts 2002 onward Boundary forcing
cold bias in HyCOM solutions Tides make a
difference Georges Bank, reduced gradients
Wilkin, Haidvogel
8Theme 1 Circulation and biogeochemical modeling
Nitrification
Water column
Mineralization
NH4
NO3
Uptake
Phytoplankton
Grazing
Chlorophyll
Zooplankton
Mortality
Large detritus
Small detritus
Fennel et al., in press, GBC
Nitrification
N2
NH4
NO3
No DOM yet
Denitrification
Aerobic mineralization
Organic matter
Sediment
9Theme 1 Circulation and biogeochemical modeling
Sources and sinks of nitrogen Role of
shelf denitrification
Fennel et al., in press, GBC
10Theme 1 Circulation and biogeochemical modeling
Simulated annual air-sea flux of CO2 Explicit
inorganic carbon cycling Positive values
indicate uptake by ocean Outer Mid-Atlantic
Bight continental shelf is a sink for atmospheric
CO2 No net uptake off NJ due to outgassing
during summer from upwelling
Fennel
11MAB atmospheric CO2 uptake estimates
12Theme 2 Satellite and in situ data analyses
Intercomparison of Chlorophyll-a Algorithms May
14, 2000
OC4v4
Clark
First coastal intercom-parison Inner shelf
differences
Carder
GSM01
OReilly, Signorini, McClain
13Theme 2 Satellite and in situ data analyses
In situ productivity measurements
Phase good, models differ, models too high. SAB
tough due to intrusions.
Satellite productivity measurements
OReilly
14Annual PP, mean and ratio to mean
OReilly
15Maxmin annual PP(1998-2005)
OReilly
16Theme 2 Satellite and in situ data analyses
SAB variability Analyses of forcing functions
and chlorophyll (response), 1998-2005 Top- size
of North Atlantic Subtropical gyre
(chl-based) Middle- Cape Fear River
discharge Bottom- Chlorophyll
Signorini, McClain
17Theme 2 Satellite and in situ data analyses
Analyses of forcing functions and response at 3
sites Sea surface height anomaly (green) and
NASG size (blue) May reflect seasonal migration
of Gulf Stream frontoffshore in spring, onshore
in fall
Signorini, McClain
18 SST trend Chl trend
OReilly
19Theme 2 Satellite and in situ data analyses
Analyses of World Ocean Database for study
region focus on MLD and dissolved O2.
Siewert, Najjar
20Theme 2 Satellite and in situ data analyses
MLD based on ?T 0.2C
Siewert, Najjar
21Theme 2 Satellite and in situ data analyses
MAB outer shelf annual cycles of the oxygen
anomaly
0-30 m
30-60 m
60-100 m
Siewert, Najjar
22Theme 2 Satellite and in situ data analyses
MAB Sea-to-air oxygen flux
Outer Shelf
Slope
Mid-Shelf
Inner Shelf
Siewert, Najjar
23Themes 1 and 2 Modeling and satellite analyses
Fennel, Wilkin, OReilly, Signorini, McClain
24Themes 1 and 2 Modeling and satellite analyses
Model-data comparisons
? Model crashes in summer (no tides)
Fennel, Wilkin, OReilly
25Themes 1 and 2 Modeling and satellite analyses
Fennel, Wilkin, OReilly
26Themes 1 and 2 Modeling and satellite analyses
Satellite-derived primary production (PP) using
VGPM2
VGPM2 applied to NENA-simulated fields
Modeled PP using NENA
Fennel, Wilkin, OReilly
27Themes 1 and 2 Modeling and satellite analyses
Model-data comparison
Wilkin, OReilly
28Theme 3 Field measurements
Chesapeake Bay and adjacent coastal waters ODU
monthly cruises and NASA NIP (Mannino)
- ODU cruises - one day, 8 hour cruise, 4 stations
- NIP grid of stations, 3-4 day cruises
Carbon, nutrients, chl a, pigments, absorb.,
Estimate fluxes - model Algorithm
development ARCHIVED SAMPLES 2002 to present
29Theme 3 Field measurements
From cruises in Southern MAB, including lower
Chesapeake Bay. 30 Mar 1 Apr cruise
? Spring conditions well mixed except where
influenced by rivers.
Mannino
30Theme 3 DOC CDOM field measurements
From cruises in Southern MAB, including lower
Chesapeake Bay. Seasonal algorithms needed.
Offset due to net community production of DOC and
bleaching from spring to summer.
Mannino
31Themes 2 3 Satellite and field measurements
Aqua-MODIS-based CDOM
Mannino
Based on in situ aCDOM and in situ reflectance
ratios
32Themes 2 3 Satellite and field measurements
Aqua-MODIS-based DOC (mM)
Mannino
33Theme 4 Biogeochemical data assimilation
Developed a 1-D data assimilative Modeling
Testbed This framework includes mixing,
advection, diffusion, attenuation, sinking
subroutines This framework requires forcing
fields T, MLD, PAR, w, Kv boundary and initial
conditions ecosystem model subroutine adjoint
of ecosystem model subroutine biogeochemical
data for evaluation/assimilation This
framework will be used to Perform parameter
sensitivity/optimization analyses Test new
parameterizations and formulations Compare
multiple models at a single site Compare model
performance at various sites
34Theme 4 Biogeochemical data assimilation
Comparison of simulated nitrate from 1D and 3D
models at a site on MAB continental shelf
5 m
3D
55 m
115 m
1D
Friedrichs
35Theme 4 Biogeochemical data assimilation
Identical Twin Numerical Experiments - Use
SeaWiFS and in situ data
Chl2C_m PhyIS PhyMR Vp0 ZooGR CoagR Sremin
7 (of 18) parameters can be independently
estimated
Friedrichs
36DOM modeling
Jean-Noel Druon
371-D MAB results
38Theme 5 Climate Modeling
How will coastal regions respond to climate
change, and what are the feedbacks on the carbon
cycle? Force the circulation/biogeochemical
model with climate change scenarios Present day
scenario 1980-2000 100 years later scenario
2080-2100 Using RegCM3
39Theme 5 Climate Modeling
Winter Summer
Simulated precipitation
Observed precipitation
Pollard, Najjar
40Theme 5 Climate Modeling
Six-hourly precipitation fields from a
10-year simulation using present conditions
Pollard, Najjar
41Summary
U.S. ECoS Goal To develop carbon budgets for the
U.S. east coast continental shelf waters
- Circulation model shows observed features for
SSS, SST. More evaluation (e.g., MLD) needed.
Tides, BCs make a difference. - Biogeochemical model captures chl variability.
Chl too low in gyre. More tracer evaluation
needed (e.g., oxygen) - Denitrification significantly influences air-sea
carbon flux in model. MAB air-sea flux agrees
with observations. - Satellite productivity algorithms give MAB
results close to observed. Issues in SAB. - Interannual variability and long-term trends in
chl, PP, SST.
42Summary
U.S. ECoS Goal To develop carbon budgets for the
U.S. east coast continental shelf waters
- Riverine gyre influences on chl seen in SAB.
- Field data have allowed development of CDOM and
DOC products for MAB - Model and satellite productivity issues need
resolution. - 1D models and data allow parameters for 3D models
to be constrained. - DOM poised to be included in 3D model.
- Regional climate model set up and ready for
climate change runs
43Summary
U.S. ECoS Goal To develop carbon budgets for the
U.S. east coast continental shelf waters
- No component can do this by itselfsynthesis
approach - Requires modeling effort coupled with satellite
and in situ data analysis - Ongoing effortobservationalists and modelers
working together