Guy Schurgers
Biographic Data
| ID | 6016875 |
|---|---|
| NAME | Guy Schurgers |
| GIVEN NAMES | Guy |
| FAMILY NAME | Schurgers |
| SIGNATURE | SCHURGERS G |
| AFFILIATIONS | University of Copenhagen |
| ORCID | 0000-0002-2189-1995 |
| VERIFIED | Yes |
| TOTAL WORKS | 10 |
| TOTAL CITATIONS | 16 |
| AUTHOR COUNT | 10 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 2 |
Warming of northern peatlands increases the global temperature overshoot challenge
A strong mitigation scenario maintains climate neutrality of northern peatlands
Increased vegetation growth and carbon stock in China karst via ecological engineering
The large influence of climate model bias on terrestrial carbon cycle simulations
Global vegetation models and terrestrial carbon cycle models are widely used for projecting the carbon balance of terrestrial ecosystems. Ensembles of such models show a large spread in carbon balance predictions, ranging from a large uptake to a release of carbon by the terrestrial biosphere, constituting a large uncertainty in the associated feedback to atmospheric CO 2 concentrations under global climate change. Errors and biases that may cont…
Impacts of land use on climate and ecosystem productivity over the Amazon and the South American continent
The Amazon basin is characterized by a strong interplay between the atmosphere and vegetation. Anthropogenic land use and land cover change (LULCC) affects vegetation and the exchange of energy and water with the atmosphere. Here we have assessed potential LULCC impacts on climate and natural vegetation dynamics over South America with a regional Earth system model that also accounts for vegetation dynamics. The biophysical and biogeochemical imp…
The dominant role of semi-arid ecosystems in the trend and variability of the land CO 2 sink
The difference is found at the margins The terrestrial biosphere absorbs about a quarter of all anthropogenic carbon dioxide emissions, but the amount that they take up varies from year to year. Why? Combining models and observations, Ahlström et al. found that marginal ecosystems—semiarid savannas and low-latitude shrublands—are responsible for most of the variability. Biological productivity in these semiarid regions is water-limited and strong…
Simulated carbon emissions from land-use change are substantially enhanced by accounting for agricultural management
It is over three decades since a large terrestrial carbon sink (S T ) was first reported. The magnitude of the net sink is now relatively well known, and its importance for dampening atmospheric CO 2 accumulation, and hence climate change, widely recognised. But the contributions of underlying processes are not well defined, particularly the role of emissions from land-use change (E LUC ) versus the biospheric carbon uptake (S L ; S T =S L -E LUC…
Enhanced science–stakeholder communication to improve ecosystem model performances for climate change impact assessments
In recent years, climate impact assessments of relevance to the agricultural and forestry sectors have received considerable attention. Current ecosystem models commonly capture the effect of a warmer climate on biomass production, but they rarely sufficiently capture potential losses caused by pests, pathogens and extreme weather events. In addition, alternative management regimes may not be integrated in the models. A way to improve the quality…
Trees tracking a warmer climate: The Holocene range shift of hazel ( Corylus avellana ) in northern Europe
Palaeoecological records provide a rich source of information to explore how plant distribution ranges respond to climate changes, but their use is complicated by the fact that, especially when based on pollen data, they are often spatially too inaccurate to reliably determine past range limits. To solve this problem, we focus on hazel ( Corylus avellana), a tree species with large and heavy fruits (nuts), which provide firm evidence of the local…
Robustness and uncertainty in terrestrial ecosystem carbon response to CMIP5 climate change projections
We have investigated the spatio-temporal carbon balance patterns resulting from forcing a dynamic global vegetation model with output from 18 climate models of the CMIP5 (Coupled Model Intercomparison Project Phase 5) ensemble. We found robust patterns in terms of an extra-tropical loss of carbon, except for a temperature induced shift in phenology, leading to an increased spring uptake of carbon. There are less robust patterns in the tropics, a …
Increased vegetation growth and carbon stock in China karst via ecological engineering
Trees tracking a warmer climate: The Holocene range shift of hazel ( Corylus avellana ) in northern Europe
Palaeoecological records provide a rich source of information to explore how plant distribution ranges respond to climate changes, but their use is complicated by the fact that, especially when based on pollen data, they are often spatially too inaccurate to reliably determine past range limits. To solve this problem, we focus on hazel ( Corylus avellana), a tree species with large and heavy fruits (nuts), which provide firm evidence of the local…
Enhanced science–stakeholder communication to improve ecosystem model performances for climate change impact assessments
In recent years, climate impact assessments of relevance to the agricultural and forestry sectors have received considerable attention. Current ecosystem models commonly capture the effect of a warmer climate on biomass production, but they rarely sufficiently capture potential losses caused by pests, pathogens and extreme weather events. In addition, alternative management regimes may not be integrated in the models. A way to improve the quality…
Robustness and uncertainty in terrestrial ecosystem carbon response to CMIP5 climate change projections
We have investigated the spatio-temporal carbon balance patterns resulting from forcing a dynamic global vegetation model with output from 18 climate models of the CMIP5 (Coupled Model Intercomparison Project Phase 5) ensemble. We found robust patterns in terms of an extra-tropical loss of carbon, except for a temperature induced shift in phenology, leading to an increased spring uptake of carbon. There are less robust patterns in the tropics, a …
Trees tracking a warmer climate: The Holocene range shift of hazel ( Corylus avellana ) in northern Europe
Palaeoecological records provide a rich source of information to explore how plant distribution ranges respond to climate changes, but their use is complicated by the fact that, especially when based on pollen data, they are often spatially too inaccurate to reliably determine past range limits. To solve this problem, we focus on hazel ( Corylus avellana), a tree species with large and heavy fruits (nuts), which provide firm evidence of the local…
The dominant role of semi-arid ecosystems in the trend and variability of the land CO 2 sink
The difference is found at the margins The terrestrial biosphere absorbs about a quarter of all anthropogenic carbon dioxide emissions, but the amount that they take up varies from year to year. Why? Combining models and observations, Ahlström et al. found that marginal ecosystems—semiarid savannas and low-latitude shrublands—are responsible for most of the variability. Biological productivity in these semiarid regions is water-limited and strong…
Simulated carbon emissions from land-use change are substantially enhanced by accounting for agricultural management
It is over three decades since a large terrestrial carbon sink (S T ) was first reported. The magnitude of the net sink is now relatively well known, and its importance for dampening atmospheric CO 2 accumulation, and hence climate change, widely recognised. But the contributions of underlying processes are not well defined, particularly the role of emissions from land-use change (E LUC ) versus the biospheric carbon uptake (S L ; S T =S L -E LUC…
Enhanced science–stakeholder communication to improve ecosystem model performances for climate change impact assessments
In recent years, climate impact assessments of relevance to the agricultural and forestry sectors have received considerable attention. Current ecosystem models commonly capture the effect of a warmer climate on biomass production, but they rarely sufficiently capture potential losses caused by pests, pathogens and extreme weather events. In addition, alternative management regimes may not be integrated in the models. A way to improve the quality…
The large influence of climate model bias on terrestrial carbon cycle simulations
Global vegetation models and terrestrial carbon cycle models are widely used for projecting the carbon balance of terrestrial ecosystems. Ensembles of such models show a large spread in carbon balance predictions, ranging from a large uptake to a release of carbon by the terrestrial biosphere, constituting a large uncertainty in the associated feedback to atmospheric CO 2 concentrations under global climate change. Errors and biases that may cont…
Impacts of land use on climate and ecosystem productivity over the Amazon and the South American continent
The Amazon basin is characterized by a strong interplay between the atmosphere and vegetation. Anthropogenic land use and land cover change (LULCC) affects vegetation and the exchange of energy and water with the atmosphere. Here we have assessed potential LULCC impacts on climate and natural vegetation dynamics over South America with a regional Earth system model that also accounts for vegetation dynamics. The biophysical and biogeochemical imp…
Increased vegetation growth and carbon stock in China karst via ecological engineering
A strong mitigation scenario maintains climate neutrality of northern peatlands
Warming of northern peatlands increases the global temperature overshoot challenge
Environmental Science (10 works) · Climate change (9 works) · Geography (9 works) · Ecology (8 works) · Atmospheric sciences (6 works) · Geology (6 works) · Biology (5 works) · Carbon sink (5 works) · Climate variability and models (5 works) · Climatology (5 works)