Observations and Coupled Terrestrial-Coastal Ocean Modeling of Carbon-Cycle Exchange in the...
description
Transcript of Observations and Coupled Terrestrial-Coastal Ocean Modeling of Carbon-Cycle Exchange in the...
Observations and Coupled Terrestrial-Coastal Ocean Modeling of Carbon-Cycle Exchange in the Mississippi-Atchafalaya
Basin and Northern Gulf of MexicoSteven Lohrenz (U. Mass Dartmouth)
Wei-Jun Cai (U. Georgia)Hanqin Tian (Auburn)
Ruoying He (N. Carolina State U.)Zuo Xue (N. Carolina State U.)
Katja Fennel (Dalhousie)Charles Hopkinson (U. Georgia)
Stephan Howden (U. Southern Miss.)
Acknowledgements• Project is funded through the NASA
Interdisciplinary Research in Earth Sciences and the NASA Carbon Monitoring System programs
• Additional funding, data and cruise support provided by NSF, NOAA, EPA, and USGS
Overview• Introduction
– Coupled models for the study of carbon dynamics in complex systems– Uncertainties in coastal carbon budgets– Current projects:
• NASA IDS: Coupled Terrestrial-Ocean Models - A Case Study in the Gulf of Mexico• Carbon Monitoring System Projects: Phase 1 and Phase 2
• Approach– Descriptions of the models
• Dynamic Land Ecosystem Model• Coastal Ocean Biogeochemical Model
– Model integration• Results to Date
– Data development – Model refinement and validation– Integration of terrestrial and ocean models
• Next Steps
Introduction: Coupled modeling approaches to examine carbon dynamics in complex systems
• Current research in carbon cycle science often focuses on specific subsystems (e.g., ocean, forest, tundra, urban, etc.)
• However, interactions among subsystems can lead to nonlinear relationships in their response to changes in external forcing
• Such interactions complicate efforts to predict how systems will behave and may produce unintended consequences for carbon management efforts
Introduction: Uncertainties in Coastal Carbon Budgets
• Carbon fluxes in the coastal margins remain poorly constrained in global carbon budgets
• Large uncertainties remain particularly in the temporal and spatial patterns of variability
• Reductions in uncertainties as well as ability to project changes in carbon fluxes in response to climate- and human-related activities will benefit carbon management efforts
P. Coble
Najjar presentation and numerous posters by Cai, Herrmann, Friedrichs, Alin, Signorini, Wang, Vlahos, and others
NASA IDS Project - Coupled Terrestrial-Ocean Models: A Case Study in the Gulf of Mexico
• Changing climate and land use practices can dramatically alter hydrologic and biogeochemical processes in terrestrial environments
• Such changes influence the delivery of water, carbon and nutrients into rivers, estuaries, and coastal ocean waters
• Here, we use the Mississippi River watershed and northern Gulf of Mexico as a case study to illustrate linkages between terrestrial and ocean ecosystems
NASA Carbon Monitoring System Projects
• Phase 1: Estimation of land ocean atmosphere carbon fluxes ‐ ‐and exchanges in the Mississippi River– Land-ocean C and nutrient fluxes– Coastal margin air-sea C exchange– Coastal to open ocean C exchange
• Phase 2: Development of observational tools and coupled models of land-ocean-atmospheric fluxes and exchanges in the Mississippi River watershed and Gulf of Mexico in support of carbon monitoring– Advances the Phase 1 effort by using coupled terrestrial and ocean
models– Develop geo-referenced products– Estimate uncertainties
Approach: Coupled Terrestrial-Ocean Models
Dynamic Land Ecosystem Model used to estimate spatial and temporal patterns of delivery of water, carbon, and nitrogen and compared to data-based observations
DLEM terrestrial outputs linked to a physical-biogeochemical model to characterize coastal carbon fluxes and ecosystem dynamics
Modeling efforts will be supported by field survey-based and satellite-based observations of carbon fluxes and other biogeochemical processes
Tian et al., 2010a,b; Tian et al.,2011, Tian et al.,2012
Hoffman et al., Ann. Rev., 2011;Fennel et al., 2011 and in prep.
Hyun and He (2010); Xue et al. in prep
Approach
Approach: Dynamic Land Ecosystem Model
Tian et al., 2010a,b; Tian et al.,2011, Tian et al.,2012, Tao et al. 2013Dynamic Land-Ecosystem Model (DLEM2.0) See Tian et al., poster 241, Tuesday
Conceptual Model of DLEM
Coupling of biogeochemical and hydrological cycles (C,N,P,H2O) in DLEM
See Tian et al., poster 241, Tuesday
NASA IDS Terrestrial Domain: Mississippi-Atchafalaya Basin
• The drainage basin for the Mississippi-Atchafalaya river system covers 41% of the conterminous U.S.
• Among the ten largest rivers in the world with respect to water and sediment discharge and the largest in the North American continent
Temperate or sub-polar needleleaf forest
Tropical or sub-tropical broadleaf evergreen
Temperate or sub-polar broadleaf deciduous
Mixed Forest
Temperate or sub-polar shrubland
Temperate or sub-polar grassland
Sub-polar or polar grassland-lichen-moss
Wetland
Cropland
Barren Lands
Urban and Built-up
Water
Tian et al.
Approach: SABGOM
Hoffman et al., Ann. Rev., 2011;Fennel et al., 2011 and in prep.See He et al., poster 242, Tuesday
Spatial and temporal patterns of cropland in the Mississippi-Atchafalaya River Basin during 1901-2008 (Tian et al.)
Results to Date
800
850
900
950
1000
1050
1100
1150
1200
1250
1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001
Crop
are
a (1
000
km2 )
Crop_area
75% 0
75% 0
75% 0
1900 1950
2005
• Assemble terrestrial data sets for model input
– Land cover– Historical and
projected climate– Land use– Disturbance and
regrowth– Manure/fertilizer– Population data
Results to Date• Model refinement and validation
Comparison of simulated (blue line) and observed (red dots) total inorganic carbon in the vicinity of the Mississippi River outflow region Xue et al. in prep
0
200
400
600
800
1000
1200
1400
1965 1970 1975 1980 1985 1990 1995 2000 2005 2010
Rive
r disc
harg
e (k
m3 /
year
)
River Discharge
DLEM-estimatedUSGS Observation
2
7
12
17
22
27
32
1954 1959 1964 1969 1974 1979 1984 1989 1994 1999 2004 2009
DIC
expo
rt (T
g C/
yr)
DIC DLEM-simulated (MARB)
Raymon and Cole,2003 (MRB)
See Tian et al., poster 241, Tuesday
DLEM-simulated total N export (DIN+DON+PON) driven by land use/cover change (LUCC, including land management), climate change and all the environmental changes
Relative contributions from LUCC and climate
Tian et al.
Results to Date
DLEM simulated (a) Dissolved Inorganic Nitrogen (DIN, NO3+NH4) and (b) Dissolved Inorganic Carbon (DIC) input from the Mississippi-Atchafalaya River Basin system in the first decade of the 20th and 21st centuries
See He et al., poster 242, Tuesday
Higher DIN in recent decade due to population growth and land use practices
Results to Date• Data set development: extensive ship-based observations in the
northern Gulf of Mexico region from 2003 - 2012Jun 24-31 2003 R/V Pelican
Aug 1-8 2004 R/V Pelican
Oct 3-7 2005 R/V Pelican
Apr 27 - May 1 2006 R/V Pelican
Jun 6-11 2006 OSV Bold (EPA)
Sep 6-11 2006 OSV Bold (EPA)
Jul 10 - Aug 4 2007 R/V Brown (NOAA)
May 1-8 2008 R/V Pelican
31 Oct-7 Nov 2008 R/V Pelican
Jan 8-20 2009 R/V Cape Hatteras
Apr 19 - May 1 2009 R/V Cape Hatteras
July 18 - 30 2009 R/V Cape Hatteras
Oct 28 - Nov 9 2009 R/V Sharp
Mar 11-21 2010 R/V Cape Hatteras
Jul 21 – Aug 13 2012 R/V Ronald H. Brown www.gulfcarbon.org
• Huang et al., 2012, Biogeosci. and in review• Guo et al., 2012, Limnol. Oceanogr.• Cai et al., 2011, Nature Geosci.• Cai et al., 2011, Ann. Rev. Mar. Sci.• Two Ph.D. dissertations, other papers in prep.
Results to Date
Model refinement and validation
Positions (red dots) of in situ observations and three sub-regions (near field, intermediate, and far field) where area-mean time series comparisons were made. Also shown is 50 m isobath
See He et al., poster 242, Tuesday
Model refinement and validation
Time series comparisons between observed (red) and simulated (blue) NO3 and chlorophyll in three sub-regions of the northern Gulf
See He et al., poster 242, Tuesday
Model refinement and validation
Comparison between simulated (left) and observed (right) seasonal mean surface Chl-a concentration
See He et al., poster 242, Tuesday
See He et al., poster 242, Tuesday
Next Steps
• Temperature and precipitation under high (A2) and low (B1) emissions scenarios
• These data will provide inputs to the land ecosystem model
• Outputs include freshwater discharge and export of carbon and nitrogen, which feed into coastal model
450
650
850
1050
1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Prec
ipita
tion
(mm
/yr)
A2_precipitation
B1_precipitation
Historical _preciptation
8
10
12
14
16
18
1900 1920 1940 1960 1980 2000 2020 2040 2060 2080 2100
Tem
pera
ture
(o C/y
r)
A2_temperature
B1_temperature
Historical_temperature
Next Steps
• Develop both hindcasts (1900-1910, 2000-2010) and forecasts (2090-2100)
• Examine sensitivity to different drivers:– Climate (temperature, precipitation, solar radiation, relative humidity)– Land cover change– Land management including nitrogen fertilizer use, irrigation– Atmospheric CO2 concentration– Atmospheric nitrogen deposition– Tropospheric ozone pollution
• For forecasts, use two IPCC climate scenarios (A2, B1) including different land use scenarios, freshwater, and nutrient loading climate projections
Future Applications
LandCarbon Management
Land Use PracticesWater and Forest Management
Agriculture, FertilizerGHGs
Energy and BiofuelsDevelopment
Ocean Carbon ReservoirLong term Sequestration
of Carbon?
Coastal MarginAir-sea flux of CO2
Nutrients and HypoxiaOcean Acidification
Wetlands LossCoastal Restoration
Water QualityFisheries Habitat
Sea Level RiseRiver Export
Export
• Model development will provide decision support for issues related to carbon management, water quality, and ecosystem sustainability
Thank you!
www.gulfcarbon.org