emerging modules for the asm: biogeochemistry
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Emerging modules for the ASM: Biogeochemistry. By Clara Deal with contributions from Scott Elliott. Introduction - Critical issues Complex interconnectivity Sparse observations Emerging modules? Example of overall system Existing ecosystem models Biogeochemical component models - PowerPoint PPT PresentationTRANSCRIPT
Emerging modules for the ASM: Biogeochemistry
By Clara Deal with contributions from Scott Elliott
Outline
Introduction - Critical issues
Complex interconnectivity
Sparse observations
Emerging modules?
Example of overall system
Existing ecosystem models
Biogeochemical component models
Important features to resolve
Pan-Arctic approach
Complex interconnectivity demands consideration of an ecology of advection.
• different shelf characteristics – freshwater input
• stratification
• currents
Figure (and slide title) modified from Carmack et al. 2006
Marine biogeochemistry in the Arctic remains seriously under sampled.
A first time series for Franklin Bayhttp://www.cases.quebec-ocean.ulaval.ca/
CABANERA
There is a critical need for gridded nutrient data beyond WOA.
One Growing Family Tree: U.S. CCSM and abrupt change
Land model is NSF/DOE CLM with coupled C/N and global dynamic veg
Emerging: Boreal albedo/veg connections (DOE Impacts)Emerging: Methane from permafrost (DOE Impacts)
Ocean model is NSF/DOE POP with global eco and C/N /P/Fe/Si
Emerging: Ice algae and DMS (DOE Epscor in CICE)Emerging: High latitude specialists (DOE Epscor in CICE)Emerging: Marine clathrate CH4 release (DOE Impacts)
Regional evolution of CCSM biogeochemistry:
RACM incorporating Walsh ecodynamics in seaNo terrestrial Arctic grid in this family as yet
(slide from Scott Elliott)
A couple emerging biogeochemistry modules were mentioned yesterday during session 2. Current state of Regional Arctic Models.
• RCAO – Döscher/Jones
RCO Model – SCOBI bio-chemistry (Baltic Sea)
• ECCO2 – Heimback/Menemenlis
Lifetime, transport and fate of riverine DOC in the Arctic Ocean (Manizza et al. in press)
A few coupled physical-biological models have been applied to Arctic waters.
References Model and submodels
Dim.
Ice ecosystem
High-latitude waters
Coupled sea ice model
Shuert and Walsh 1993; Walsh et al. 1994 & 2004
ecosystem, carbonate system
3-D none Bering and Chukchi Sea
none
Wassman and Slagstad 1993; Slagstad et al. 1999
ecosystem, carbonate system
3-D, 1-D
none Greenland and Barents Sea
none
Lavoie et al. 2005 & 2009
ecosystem 1-D yes Mackenzie Shelf in the Beaufort Sea
dynamic
Jin et al. 2006, 2007 & 2009; Deal et al. 2000
ecosystem, DMS submodel
1-D yes SE Bering Sea, Chukchi Sea shelf; Gulf of AK
non-dynamic
Nishi and Tabeta 2005
ecosystem 1-D yes Lake Saroma non-dynamic
Important features to resolve:
• Horizontal transport – nutrients, biomass
• Ocean stratification
• Timing of ice retreat and algal release
• Mixing zone and euphotic layer depths
Timing of ice retreat impacts phytoplankton bloom timing and shapes the structure and function of food web.
Extreme seasonality in ice cover results in highly variable mixing zones and euphotic layer depths – in space and time.
Pan-Arctic approach
• contiguous domains
• controls – e.g. nutrients and light
• “ecology of advection”
“Food webs and physical-biological
Coupling on pan-Arctic shelves: Unifying concepts and
comprehensive perspectives”
Eddy Carmack, Paul Wassman