Stephanie Evers

Dr. Stephanie Evers


Research Focus & Metrics

Academic Career Length

9Years (2018-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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21 January 2020 in Nature Communications
Verified
Journal Article
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HCHannah V. Cooper
Hannah V. Cooper
SEStephanie Evers
Stephanie Evers
Paul AplinPaul Aplin
Paul Aplin
NCNeil Crout
Neil Crout
MDMohd Puat Bin Dahalan
Mohd Puat Bin Dahalan
SSSofie Sjogersten
Sofie Sjogersten
Conversion of tropical peat swamp forest to drainage-based agriculture alters greenhouse gas (GHG) production, but the magnitude of these changes remains highly uncertain. Current emissions factors for oil palm grown on drained peat do not account for temporal variation over the plantation cycle and only consider CO2 emissions. Here, we present direct measurements of GHGs emitted during the conversion from peat swamp forest to oil palm plantation, accounting for CH4 and N2O as well as CO2. Our results demonstrate that emissions factors for converted peat swamp forest is in the range 70–117 t CO2 eq ha−1 yr−1 (95% confidence interval, CI), with CO2 and N2O responsible for ca. 60 and ca. 40% of this value, respectively. These GHG emissions suggest that conversion of Southeast Asian peat swamp forest is contributing between 16.6 and 27.9% (95% CI) of combined total national GHG emissions from Malaysia and Indonesia or 0.44 and 0.74% (95% CI) of annual global emissions.

1 October 2018 in Engineering Geology
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Journal Article
Closed access
CMChris Marshall
Chris Marshall
DLDavid J. Large
David J. Large
AAAhmed Athab
Ahmed Athab
SEStephanie Evers
Stephanie Evers
ASAndrew Sowter
Andrew Sowter
SSSofie Sjögersten
Sofie Sjögersten

9 January 2018 in Global Biogeochemical Cycles
Verified
Journal Article
Closed access
PDF file
TSThomas Smith
Thomas Smith
SEStephanie Evers
Stephanie Evers
CYCatherine Yule
Catherine Yule
JGJ. Y. Gan
J. Y. Gan

16 May 2018 in Journal of Geophysical Research: Atmospheres
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Journal Article
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CRChristopher Thomas Roulston
Christopher Thomas Roulston
Clare Paton-Walsh (Murphy)Clare Paton-Walsh (Murphy)
Clare Paton-Walsh (Murphy)
TSThomas Smith
Thomas Smith
EGElise-Andrée Guérette
Elise-Andrée Guérette
SEStephanie Evers
Stephanie Evers
GWG. R. Van der Werf
G. R. Van der Werf
Southeast Asia experiences frequent fires in fuel‐rich tropical peatlands, leading to extreme episodes of regional haze with high concentrations of fine particulate matter (PM2.5) impacting human health. In a study published recently, the first field measurements of PM2.5 emission factors for tropical peat fires showed larger emissions than from other fuel types. Here we report even higher PM2.5 emission factors, measured at newly ignited peat fires in Malaysia, suggesting that current estimates of fine particulate emissions from peat fires may be underestimated by a factor of 3 or more. In addition, we use both field and laboratory measurements of burning peat to provide the first mechanistic explanation for the high variability in PM2.5 emission factors, demonstrating that buildup of a surface ash layer causes the emissions of PM2.5 to decrease as the peat fire progresses. This finding implies that peat fires are more hazardous (in terms of aerosol emissions) when first ignited than when still burning many days later. Varying emission factors for PM2.5 also have implications for our ability to correctly model the climate and air quality impacts downwind of the peat fires. For modelers able to implement a time‐varying emission factor, we recommend an emission factor for PM2.5 from newly ignited tropical peat fires of 58 g of PM2.5 per kilogram of dry fuel consumed (g/kg), reducing exponentially at a rate of 9%/day. If the age of the fire is unknown or only a single value may be used, we recommend an average value of 24 g/kg.

7 August 2019 in Scientific Reports
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Journal Article
Open access
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SWSusan Waldron
Susan Waldron
LVLeena Vihermaa
Leena Vihermaa
SEStephanie Evers
Stephanie Evers
MGMark H. Garnett
Mark H. Garnett
JNJason Newton
Jason Newton
AHAndrew C. G. Henderson
Andrew C. G. Henderson
Southeast-Asian peat swamp forests have been significantly logged and converted to plantation. Recently, to mitigate land degradation and C losses, some areas have been left to regenerate. Understanding how such complex land use change affects greenhouse gas emissions is essential for modelling climate feedbacks and supporting land management decisions. We carried out field research in a Malaysian swamp forest and an oil palm plantation to understand how clear-felling, drainage, and illegal and authorized conversion to oil palm impacted the C cycle, and how the C cycle may change if such logging and conversion stopped. We found that both the swamp forest and the plantation emit centuries-old CO2 from their drainage systems in the managed areas, releasing sequestered C to the atmosphere. Oil palm plantations are an iconic symbol of tropical peatland degradation, but CO2 efflux from the recently-burnt, cleared swamp forest was as old as from the oil palm plantation. However, in the swamp forest site, where logging had ceased approximately 30 years ago, the age of the CO2 efflux was modern, indicating recovery of the system can occur. 14C dating of the C pool acted as a tracer of recovery as well as degradation and offers a new tool to assess efficacy of restoration management. Methane was present in many sites, and in higher concentrations in slow-flowing anoxic systems as degassing mechanisms are not strong. Methane loading in freshwaters is rarely considered, but this may be an important C pool in restored drainage channels and should be considered in C budgets and losses.

31 May 2023 in CATENA
Verified
Journal Article
Open access
SDSelva Dhandapani
Selva Dhandapani
SEStephanie Evers
Stephanie Evers
Doreen BoydDoreen Boyd
Doreen Boyd
CEChris D Evans
Chris D Evans
SPSusan Page
Susan Page
SSSofie Sjogersten
Sofie Sjogersten