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Featured researches published by G. Stinson.


Nature | 2008

Mountain pine beetle and forest carbon feedback to climate change

Werner A. Kurz; Caren C. Dymond; G. Stinson; Gregory J. Rampley; Eric T. Neilson; Allan L. Carroll; T. Ebata; L. Safranyik

The mountain pine beetle (Dendroctonus ponderosae Hopkins, Coleoptera: Curculionidae, Scolytinae) is a native insect of the pine forests of western North America, and its populations periodically erupt into large-scale outbreaks. During outbreaks, the resulting widespread tree mortality reduces forest carbon uptake and increases future emissions from the decay of killed trees. The impacts of insects on forest carbon dynamics, however, are generally ignored in large-scale modelling analyses. The current outbreak in British Columbia, Canada, is an order of magnitude larger in area and severity than all previous recorded outbreaks. Here we estimate that the cumulative impact of the beetle outbreak in the affected region during 2000–2020 will be 270 megatonnes (Mt) carbon (or 36 g carbon m-2 yr-1 on average over 374,000 km2 of forest). This impact converted the forest from a small net carbon sink to a large net carbon source both during and immediately after the outbreak. In the worst year, the impacts resulting from the beetle outbreak in British Columbia were equivalent to ∼75% of the average annual direct forest fire emissions from all of Canada during 1959–1999. The resulting reduction in net primary production was of similar magnitude to increases observed during the 1980s and 1990s as a result of global change. Climate change has contributed to the unprecedented extent and severity of this outbreak. Insect outbreaks such as this represent an important mechanism by which climate change may undermine the ability of northern forests to take up and store atmospheric carbon, and such impacts should be accounted for in large-scale modelling analyses.


Proceedings of the National Academy of Sciences of the United States of America | 2008

Risk of natural disturbances makes future contribution of Canada's forests to the global carbon cycle highly uncertain

Werner A. Kurz; G. Stinson; Gregory J. Rampley; Caren C. Dymond; Eric T. Neilson

A large carbon sink in northern land surfaces inferred from global carbon cycle inversion models led to concerns during Kyoto Protocol negotiations that countries might be able to avoid efforts to reduce fossil fuel emissions by claiming large sinks in their managed forests. The greenhouse gas balance of Canadas managed forest is strongly affected by naturally occurring fire with high interannual variability in the area burned and by cyclical insect outbreaks. Taking these stochastic future disturbances into account, we used the Carbon Budget Model of the Canadian Forest Sector (CBM-CFS3) to project that the managed forests of Canada could be a source of between 30 and 245 Mt CO2e yr−1 during the first Kyoto Protocol commitment period (2008–2012). The recent transition from sink to source is the result of large insect outbreaks. The wide range in the predicted greenhouse gas balance (215 Mt CO2e yr−1) is equivalent to nearly 30% of Canadas emissions in 2005. The increasing impact of natural disturbances, the two major insect outbreaks, and the Kyoto Protocol accounting rules all contributed to Canadas decision not to elect forest management. In Canada, future efforts to influence the carbon balance through forest management could be overwhelmed by natural disturbances. Similar circumstances may arise elsewhere if global change increases natural disturbance rates. Future climate mitigation agreements that do not account for and protect against the impacts of natural disturbances, for example, by accounting for forest management benefits relative to baselines, will fail to encourage changes in forest management aimed at mitigating climate change.


Global Change Biology | 2011

An inventory-based analysis of Canada's managed forest carbon dynamics, 1990 to 2008.

G. Stinson; Werner A. Kurz; Carolyn Smyth; Eric T. Neilson; Caren C. Dymond; Juha M. Metsaranta; Céline Boisvenue; Gregory J. Rampley; Q. Li; Thomas White; D. Blain

Canadas forests play an important role in the global carbon (C) cycle because of their large and dynamic C stocks. Detailed monitoring of C exchange between forests and the atmosphere and improved understanding of the processes that affect the net ecosystem exchange of C are needed to improve our understanding of the terrestrial C budget. We estimated the C budget of Canadas 2.3 × 106 km2 managed forests from 1990 to 2008 using an empirical modelling approach driven by detailed forestry datasets. We estimated that average net primary production (NPP) during this period was 809 ± 5 Tg C yr−1 (352 g C m−2 yr−1) and net ecosystem production (NEP) was 71 ± 9 Tg C yr−1 (31 g C m−2 yr−1). Harvesting transferred 45 ± 4 Tg C yr−1 out of the ecosystem and 45 ± 4 Tg C yr−1 within the ecosystem (from living biomass to dead organic matter pools). Fires released 23 ± 16 Tg C yr−1 directly to the atmosphere, and fires, insects and other natural disturbances transferred 52 ± 41 Tg C yr−1 from biomass to dead organic matter pools, from where C will gradually be released through decomposition. Net biome production (NBP) was only 2 ± 20 Tg C yr−1 (1 g C m−2 yr−1); the low C sequestration ratio (NBP/NPP=0.3%) is attributed to the high average age of Canadas managed forests and the impact of natural disturbances. Although net losses of ecosystem C occurred during several years due to large fires and widespread bark beetle outbreak, Canadas managed forests were a sink for atmospheric CO2 in all years, with an uptake of 50 ± 18 Tg C yr−1 [net ecosystem exchange (NEE) of CO2=−22 g C m−2 yr−1].


Philosophical Transactions of the Royal Society B | 2008

Could increased boreal forest ecosystem productivity offset carbon losses from increased disturbances

Werner A. Kurz; G. Stinson; Greg Rampley

To understand how boreal forest carbon (C) dynamics might respond to anticipated climatic changes, we must consider two important processes. First, projected climatic changes are expected to increase the frequency of fire and other natural disturbances that would change the forest age-class structure and reduce forest C stocks at the landscape level. Second, global change may result in increased net primary production (NPP). Could higher NPP offset anticipated C losses resulting from increased disturbances? We used the Carbon Budget Model of the Canadian Forest Sector to simulate rate changes in disturbance, growth and decomposition on a hypothetical boreal forest landscape and to explore the impacts of these changes on landscape-level forest C budgets. We found that significant increases in net ecosystem production (NEP) would be required to balance C losses from increased natural disturbance rates. Moreover, increases in NEP would have to be sustained over several decades and be widespread across the landscape. Increased NEP can only be realized when NPP is enhanced relative to heterotrophic respiration. This study indicates that boreal forest C stocks may decline as a result of climate change because it would be difficult for enhanced growth to offset C losses resulting from anticipated increases in disturbances.


Tellus B | 2010

Implications of future disturbance regimes on the carbon balance of Canada's managed forest (2010-2100).

Juha M. Metsaranta; Werner A. Kurz; Eric T. Neilson; G. Stinson

Recent increases in fire and insect disturbances have contributed to a transition of Canada’s managed forest carbon balance from sink to source. Further increases in area burned could contribute positive feedback to climate change. We made probabilistic forecasts of the recovery of C sinks in Canada’s managed forest between 2010 and 2100 under two assumptions about future area burned by wildfire: (1) no increase relative to levels observed in the last half of the 20th century and (2) linear increases by a factor of two or four (depending on region) from 2010 to 2100. Recovery of strong C sinks in Canada’s managed forest will be delayed until at least the 2030s because of insect outbreaks, even if predicted increases in area annually burned do not occur. After 2050, our simulations project an annual probability of a sink near 70% with no increase in area burned and 35% with increasing area burned. All simulations project a cumulative C source from 2010–2100, even if annual area burned does not increase. If the sink strength of terrestrial ecosystems is reduced because of increasing natural disturbances, then it will become more difficult to achieve global atmospheric CO2 stabilization targets.


Science | 2009

Wood Energy: Protect Local Ecosystems

Brian D. Titus; Douglas G. Maynard; Caren C. Dymond; G. Stinson; Werner A. Kurz

In their Policy Forum paper “Wood energy in America” (13 March, p. [1432][1]), D. deB. Richter Jr. et al. argue cogently for deployment of advanced wood combustion (AWC) systems to meet a range of objectives, and they demonstrate the potential economic and energy values of community-based AWC in


Ecological Applications | 2017

Moving beyond the concept of “primary forest” as a metric of forest environment quality

Pierre Y. Bernier; David Paré; G. Stinson; S. R. J. Bridge; B. Kishchuk; T. C. Lemprière; Evelyne Thiffault; Brian D. Titus; W. Vasbinder

The United Nations Food and Agriculture Organization (FAO) has been reporting country-level area in primary forests in its Global Forest Resource Assessment since 2005. The FAO definition of a primary forest (naturally regenerated forest of native species where there are no clearly visible indications of human activities and the ecological processes are not significantly disturbed) is generally accepted as authoritative and is being used in policy making. However, problems with this definition undermine our capacity to obtain globally coherent estimates. In addition, the current reporting on primary forests fails to consider the complementarily of non-primary forests toward the maintenance of ecosystem services. These issues undermine the appropriate tracking of changes in primary and non-primary forests, and the assessment of impacts of such changes on ecosystem services. We present the case for an operational reconsideration of the primary forest concept and discuss how alternatives or supplements might be developed.


Environmental Monitoring and Assessment | 2018

The North American Forest Database: going beyond national-level forest resource assessment statistics

W. Brad Smith; Rubí Angélica Cuenca Lara; Carina Edith Delgado Caballero; Carlos Isaías Godínez Valdivia; Joseph S. Kapron; Juan Carlos Leyva Reyes; Carmen Lourdes Meneses Tovar; Patrick D. Miles; Sonja N. Oswalt; Mayra Ramírez Salgado; Xilong Alex Song; G. Stinson; Sergio Armando Villela Gaytán

Forests cannot be managed sustainably without reliable data to inform decisions. National Forest Inventories (NFI) tend to report national statistics, with sub-national stratification based on domestic ecological classification systems. It is becoming increasingly important to be able to report statistics on ecosystems that span international borders, as global change and globalization expand stakeholders’ spheres of concern. The state of a transnational ecosystem can only be properly assessed by examining the entire ecosystem. In global forest resource assessments, it may be useful to break national statistics down by ecosystem, especially for large countries. The Inventory and Monitoring Working Group (IMWG) of the North American Forest Commission (NAFC) has begun developing a harmonized North American Forest Database (NAFD) for managing forest inventory data, enabling consistent, continental-scale forest assessment supporting ecosystem-level reporting and relational queries. The first iteration of the database contains data describing 1.9 billion ha, including 677.5 million ha of forest. Data harmonization is made challenging by the existence of definitions and methodologies tailored to suit national circumstances, emerging from each country’s professional forestry development. This paper reports the methods used to synchronize three national forest inventories, starting with a small suite of variables and attributes.


Ecological Modelling | 2009

CBM-CFS3 : A model of carbon-dynamics in forestry and land-use change implementing IPCC standards

Werner A. Kurz; Caren C. Dymond; Thomas White; G. Stinson; C.H. Shaw; Gregory J. Rampley; Carolyn Smyth; B.N. Simpson; Eric T. Neilson; J.A. Trofymow; Juha M. Metsaranta; Mike Apps


Global Change Biology | 2012

Reconciling estimates of the contemporary North American carbon balance among terrestrial biosphere models, atmospheric inversions, and a new approach for estimating net ecosystem exchange from inventory-based data

Daniel J. Hayes; David P. Turner; G. Stinson; A. David McGuire; Yaxing Wei; Tristram O. West; Linda S. Heath; Bernardus de Jong; B. G. McConkey; Richard A. Birdsey; Werner A. Kurz; A. R. Jacobson; Deborah N. Huntzinger; Yude Pan; W. Mac Post; R. B. Cook

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Werner A. Kurz

Natural Resources Canada

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Carolyn Smyth

Natural Resources Canada

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J.A. Trofymow

Natural Resources Canada

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Brian D. Titus

Natural Resources Canada

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