Why study biogeochemistry(sciences?) at regional scales? Ken Davis Department of Meteorology The Pennsylvania State University.

Slides:



Advertisements
Similar presentations
An example of a large-scale interdisciplinary carbon problem Multidecadal climate variability Atmospheric evidence Ocean source? (upwelling, biological.
Advertisements

What can we learn about sink efficiencies from trends in CO 2 airborne fraction ? M. Gloor, J. Sarmiento, N. Gruber University of Leeds, Princeton University,
High resolution fossil\industrial CO 2 : Historical Context Kevin Gurney Purdue University Department of Earth and Atmospheric Science Purdue Climate Change.
Ocean Biogeochemistry (C, O 2, N, P) Achievements and challenges Nicolas Gruber Environmental Physics, ETH Zürich, Zurich, Switzerland. Using input from.
Summary discussion Top-down approach Consider Carbon Monitoring Systems, tailored to address stakeholder needs. CMS frameworks can be designed to provide.
National Assessment of Ecological C Sequestration and Greenhouse Gas Fluxes – the USGS LandCarbon Project Zhiliang Zhu, Project Chief, What.
Land-use effects on spatial and temporal patterns of carbon storage and flux in PNW forests David Wallin Department of Environmental Sciences Huxley College.
唐剑武 Recent advances in ecosystem nitrogen cycling: mechanism, measurement, and modeling of N 2 O emissions.
Impact of Changes in Atmospheric Composition on Land Carbon Storage: Processes, Metrics and Constraints Peter Cox (University of Exeter) Chris Huntingford,
Tropical vs. extratropical terrestrial CO 2 uptake and implications for carbon-climate feedbacks Outline: How we track the fate of anthropogenic CO 2 Historic.
Mathias Göckede College of Forestry Oregon State University The ORCA2 West Coast Project Synthesizing multiple approaches to constrain regional scale carbon.
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
Slides for IPCC. Inverse Modeling of CO 2 Air Parcel Sources Sinks wind Sample Changes in CO 2 in the air tell us about sources and sinks Atmospheric.
Spatial and Temporal Patterns of Carbon Storage and Flux in PNW Forests: David Wallin 1 Peter Homann 1 Mark Harmon 2 Warren Cohen 3 Robert Kennedy.
The North American Carbon Program: An Overview for AmeriFlux investigators Kenneth Davis The Pennsylvania State University Co-chair, NACP Science Steering.
Carbon Sequestration Akilah Martin Fall Outline Pre-Assessment  Student learning goals  Carbon Sequestration Background  Century Model Overview.
Uncertainty and Climate Change Dealing with uncertainty in climate change impacts Daniel J. Vimont Atmospheric and Oceanic Sciences Department Center for.
Carbon sequestration in China’s ecosystems, Jingyun Fang Department of Ecology Peking University Feb. 14, 2008.
The Global Carbon Cycle Humans Atmosphere /yr Ocean 38,000 Land 2000 ~90 ~120 7 GtC/yr ~90 About half the CO 2 released by humans is absorbed by.
Combination of mechanisms responsible for the missing carbon sink using bottom-up approach Haifeng Qian March 29, A Carbon Cycle and Climate Past,
NESTED GLOBAL INVERSION WITH A FOCUS ON NORTH AMERICA: COMPARISON WITH BOTTOM-UP RESULTS IN CANADA Jing M. Chen, University of Toronto Main Contributors:
QUESTIONS 1.How do elements in the lithosphere get transferred to the atmosphere? 2.Imagine an early Earth with a weak Sun and frozen ocean (“snowball.
The uptake, transport, and storage of anthropogenic CO 2 by the ocean Nicolas Gruber Department of Atmospheric and Oceanic Sciences & IGPP, UCLA.
Impacts of spatial and temporal correlations in regional atmospheric inverse estimates of greenhouse gas fluxes Timothy W. Hilton 1, Kenneth J. Davis 1,
Global Carbon Cycle Feedbacks: From pattern to process Dave Schimel NEON inc.
This work is supported by a National Science Foundation (NSF) collaboration between the Directorates for Education and Human Resources (EHR) and Geociences.
Interannual variability across sites: Bridging the gap between flux towers and flasks Goals Obtain a mechanistic understanding of tower-scale interannual.
Phenological responses of NEE in the subboreal Controls on IAV by autumn zero- crossing and soil thermal profile Dr. Desai.
Paul R. Moorcroft David Medvigy, Stephen Wofsy, J. William Munger, M. Dietze Harvard University Developing a predictive science of the biosphere.
Tuesday 11:00 – 1:50 Thursday 11:00 – 1:50 Instructor: Nancy Wheat Ecology Bio 47 Spring 2015.

Science themes: 1.Improved understanding of the carbon cycle. 2.Constraints and feedbacks imposed by water. 3.Nutrient cycling and coupling with carbon.
The role of the Chequamegon Ecosystem-Atmosphere Study in the U.S. Carbon Cycle Science Plan Ken Davis The Pennsylvania State University The 13 th ChEAS.
Climate Change and Ecosystems IV Presidential Meeting CGDD & IFHC Sao Paulo, Brazil March 7, 2009 Thomas E. Lovejoy Biodiversity Chair, The Heinz Center.
CarboEurope, IMECC and GHG- Europe Mike Jones School of Natural Sciences Trinity College Dublin.
Why Establish an Ecosystem-Atmosphere Flux Measurement Network in India? Dennis Baldocchi ESPM/Ecosystem Science Div. University of California, Berkeley.
The Merton Report an AIMES/IGBP-ESA partnership As Earth System science advances and matures, it must be supported by robust and integrated observation.
Land-Atmosphere Interaction : Vegetation Feedback P. Friedlingstein Stephen Guendert Arts & Sciences Climatic Studies 4/1/15.
Identifying Grand Challenges in Climate Change Research: Guiding DOE’s Strategic Planning: Report on the DOE/BERAC workshop March Crystal City For.
CarboEurope: Future - Annette Freibauer MPI for Biogeochemistry, Jena.
The impacts of land mosaics and human activity on ecosystem productivity Jeanette Eckert.
MJ Apps, Canadian Forest Service Nov 2004 Why regional carbon budgets? Scientific and Policy Background Scientific and policy requirements for comprehensive.
Translation to the New TCO Panel Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University.
Three-dimensional flows and NEE: Results from the Chequamegon Ecosystem-Atmosphere Study (ChEAS) Ken Davis, Weiguo Wang, Chuixiang Yi and others, The Pennsylvania.
Earth System Feedbacks: Vulnerability of the Carbon Cycle to Drought and Fire Canberra, Australia 5-8 June 2006 – Part I 8-9 June 2006 – Part II (Australia.
Earth System Model. Beyond the boundary A mathematical representation of the many processes that make up our climate. Requires: –Knowledge of the physical.
Joint Canada-Mexico-USA (North American*) Carbon Program Planning Meeting January 25–26, 2007 *By North America we mean the North American land, adjacent.
The Role of Virtual Tall Towers in the Carbon Dioxide Observation Network Martha Butler The Pennsylvania State University ChEAS Meeting June 5-6, 2006.
Investigating the Carbon Cycle in Terrestrial Ecosystems (ICCTE) Scott Ollinger * -PI, Jana Albrecktova †, Bobby Braswell *, Rita Freuder *, Mary Martin.
Global Terrestrial Observing System linking the world’s terrestrial monitoring systems to provide a global vision of the Earth we share.
Upscaling and Uncertainty Analysis of Greenhouse Gas Emission Inventories Linda Nol Analysis for the Dutch fen meadow landscapes.
WP11 highlights: introduction and overview EU FP6 Integrated Project CARBOOCEAN ”Marine carbon sources and sinks assessment” 5 th Annual & Final Meeting.
CONSTRUCTING REGIONAL CO 2 FLUXES USING FLUX-TOWER UPSCALING AND ATMOSPHERIC BUDGETS Results from the Chequamegon Ecosystem- Atmosphere Study (ChEAS) and.
CarboEurope: The Big Research Lines Annette Freibauer Ivan Janssens.
Designing Systems to Address Outstanding Issues in Climate Change Betsy Weatherhead.
A challenge to the flux-tower upscaling hypothesis? A multi-tower comparison from the Chequamegon Ecosystem-Atmosphere Study K.J. Davis 1, D.R. Ricciuto.
PBL FTS Institute Retreat June 16-19, 2008 – Chorus ATM-Group Simultaneous use of greenhouse gas concentration measurements and meteorological measurements.
The GLOBE-Carbon Cycle project joins NASA carbon cycle science with the International GLOBE Education program to bring the most cutting edge research and.
Influence of Land Cover Heterogeneity, Land-Use Change and Management on the Regional Carbon Cycle in the Upper Midwest USA Ankur R Desai, Kenneth J Davis:
This work is supported by a National Science Foundation (NSF) collaboration between the Directorates for Education and Human Resources (EHR) and Geociences.
What research results are policy relevant? Annette Freibauer.
Surprises in the anthropogenic carbon budget Why OCB is so important! Jorge Sarmiento Princeton University Co-lead author of the US Carbon Cycle Science.
ESF workshop on methane, April 10-12, years of methane : from global to regional P. Bousquet, S. Kirschke, M. Saunois, P. Ciais, P. Peylin, R.
| Paul Lucas 1 Future energy system challenges for Africa: Insights from Integrated Assessment Models 1 st Africa Sustainable Development Forum.
Carbon Sequestration Akilah Martin Fall 2005.
North American Carbon Program
Old and Not-So-Old Research Progress/Plans for Ankur Desai Penn State University, Department of Meteorology Cheas 2003 Meeting, Woodruff, WI, 29 June –
CARBON, WATER, LAND USE & CLIMATE
Science-Policy Interface
Regional Carbon Fluxes in WI:
Presentation transcript:

Why study biogeochemistry(sciences?) at regional scales? Ken Davis Department of Meteorology The Pennsylvania State University

Hypotheses Most students of environmental sciences are in the field (primarily? secondarily?) because they are interested in helping society to protect/manage/improve the environment of the earth. Graduate programs that educate students about the societal application of their research and involve them in these applications will provide the best educational experiences for those students.

Pasteur’s quadrant Scientific merit low high Societal value / broader impacts low high don’t go here pure curiosity- driven science pure applied research Pasteur’s quadrant (Stokes, 1997)

Hypotheses Investigating the societal applications of one’s research causes one to pose new and different scientific questions. These scientific questions are often both good basic research and of high societal value. Regional biogeosciences research often falls within Pasteur’s quadrant.

Why are we focusing on regional scales? There is a methodological challenge

Example: Carbon cycle science We know the global budget very well from atmospheric measurements, but we don’t know the processes responsible. Flux towers - we have a decent chance of understanding the processes the yield observed fluxes, but it is very hard to extrapolate these to explain the global budget of atmospheric CO 2

Inherent spatial and temporal scales of methods of studying the (carbon) cycle

1 ppm yr -1 ~ 2 PgC yr -1. Fossil fuel emissions are ~ 6 PgC yr -1. Sink is implied! Interannual variability!

Fate of emitted CO 2 ~45% of fossil fuel emissions absorbed by something in the earth system Large interannual variability in sink strength Governed by climate variability (e.g. ENSO)? Anthropogenic land-use emissions ~ 2 GtC yr -1  implies even larger sink Source: Sarmiento and Gruber, Physics Today, 2003

Chequamegon Ecosystem- Atmosphere Study (ChEAS) region

Photo credit: UND Citation crew, COBRA WLEF tall tower (447m) CO 2 flux measurements at: 30, 122 and 396 m CO 2 mixing ratio measurements at: 11, 30, 76, 122, 244 and 396 m WLEF CO 2 flux and mixing ratio observatory

WLEF Lost Creek Willow Creek Sylvania

Example of the research direction hypothesis A motivation to manage the earth’s climate may alter our research direction. Example: If forest area is increasing (potential cause of the terrestrial sink of carbon), how will this alter the earth’s albedo, thus feed back to climate? (new Pasteur’s quadrant question emerges)

Potential (personal) motivations for pursuing regional biogeochemistry Methodological challenge. You’re curious. Accounting – reporting. Someone (government?) wants to know the numbers. See Kyoto protocol, etc. Personal pragmatism – you can do it, it advances your career. You want to be famous. You want to be rich. You want to help manage the future climate and ecological health of the planet. We need to develop the ability to predict the future. See SOCCR, IPCC.

My Motivation Maintain the environmental integrity of the earth, while protecting human quality of life. Requires that we develop the capacity to predict the future climate - immense scientific challenge. Underlying value – we believe it is valuable to maintain the earth as a good place for life. Advice: Examine your motivations and values. Guide your work appropriately.

We need to be able to validate our predictive models with observations and experiments. See the IPCC for a good example.

Science plan Via observations and experiments, gain a predictive understanding of the earth’s (carbon) cycle. Local-scale observations and experiments are best for developing process understanding required for predictive models (e.g. soil flux measurements, biomass inventories). Global-scale measurements make sure we get to the correct end-result when we up-scale. Regional methods are a key step in evaluating our ability to upscale our local process understanding to the globe. Method-hopping - see M. Goulden’s talk.

State of carbon cycle prediction Terrestrial system is very relevant - human management is changing atmospheric CO 2 rapidly at a time scale (~100 years) where terrestrial ecosystems will respond in a very dynamic (and unpredictable) fashion. Friedlingstein et al. (2006)

Wish: Detect climate-driven trends in local observations, hindcast these trends with process-models, match to experimental results, improve predictability. Long-term data that represents specific processes is most easily obtained at a local scale. Regional-scale methods are needed to evaluate our ability to upscale the local understanding. flux time N years of observations required(?) Flux tower time series Multi-decade terrestrial carbon cycle model prediction and uncertainty Manipulative experiment

Example of one potential long-term observation that we can use to develop process models - flux towers.

Flux tower time series - can we predict them? Do they represent regional processes? Gap-filled fluxes from the 5 sites used in TRIFFID analysis Harvard and Howland: Coherent between 1996 and 2000, then breaks down. UMBS and Morgan Monroe: coherent (similar PFT, climate) WLEF: 2002 missing, coherent with UMBS and Morgan Monroe

Model performance: Interannual variability Ricciuto, Penn State Ph.D. - paper in preparation.

Observed interannual variability: Only local processes? Probably not. Gap-filled fluxes from the 6 midwestern flux tower sites. Interannual variability of similar plant functional types appears to be coherent. Similar processes, linked to climate, influencing sites as far as several hundred kilometers apart in a similar way? Work in preparation. LC = wetland; WC, MMSF, UMBS = mature hardwood; Syl = mixed old growth; WLEF = mixed

Why (eco?)regions? Ecoregions have similar ecological processes, human management and climate, and often correspond to governmental boundaries (reporting). Regions are big enough to test process understanding over large scales, but not so large as to easily get the right answer (agreement between “top-down” and “bottom- up” methods) for the wrong reason (aggregated errors and the errors cancel) (?)

What is the value to society of improving carbon cycle/climate prediction? If we endeavor to manage the climate of the planet, uncertainty leads us to either: 1) not do a good enough job and suffer the consequences of environmental harm, or 2) devote too many resources to management, resulting in unnecessary damage to the quality of human life. Thus developing predictive skill for the earth’s climate has very practical and significant benefits to society, while also addressing a very challenging scientific question. Pasteur’s quadrant. Motivation for regional biogeosciences.