A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
In Press
- Natural and anthropogenic climate change: Incorporating historical land cover change, vegetation dynamics and the global carbon cycle.
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- Modelling carbon cycle feedbacks during abrupt climate change
[A]
- Hard Choices: Climate Change in Canada. Wilfred Laurier Press
- Response to the comments by Peter Huybers.
- Sensitivity of the inorganic carbon cycle to future climate warming in the UVic coupled model.
[A]
- Variation of Labrador Sea water formation over the last glacial cycle in a climate
model of intermediate complexity
[A]
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A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
2004
- Tidally driven mixing in a numerical model of the ocean general circulation.
[A]
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A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
2003
- Meltwater pulse 1A from Antarctica as a trigger of the Bølling-Allerød warm interval.
[A]
[H]
[R]
- Detection of human influence on sea level pressure.
[R]
- Coupling of the hemispheres in observations and simulations of glacial climate change.
[A]
[R]
- Factors Contributing to Diurnal Temperature Range Trends in 20th and
21st Century Simulations of the CCCma Coupled Model.
[A]
[P]
[R]
- Evidence of change in the Sea of Okhotsk: Implications for the North Pacific.
[A]
[P]
[R]
- Radiative forcing of climate by historical land cover change.
[A]
[R]
- Southern Ocean upwelling and eddies: Sensitivity of the global overturning to the surface density range
[A]
[R]
- The ventilation of the North Atlantic Ocean during the Last
Glacial Maximum - A comparison between simulated and observed radiocarbon ages
[A]
[P]
[R]
- North Atlantic response to the above-normal export of sea-ice from the Arctic.
[A]
[R]
- A region of enhanced northward Antarctic Intermediate Water transport in a coupled climate model.
[A]
[R]
- Atlantic deep circulation controlled by freshening in the Southern Ocean.
[A]
[R]
- The science of climate change.
[P]
[R]
- On the link between the two modes of the ocean thermohaline circulation and
the formation of global-scale water masses.
[A]
[R]
- The impact of varying atmospheric forcing on the thickness of Arctic multi-year sea ice.
[A]
[R]
- The role of land-surface dynamics in glacial inception: A study with the UVic Earth System Model.
[A]
[R]
- The Neoproterozoic 'Snowball Earth': Dynamic ice over a quiescent ocean
[A]
[R]
- The role of the Atlantic freshwater balance in the hysteresis of the
meridional overturning circulation.
[A]
[R]
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A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
2002
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On the causes of glacial inception at 116 kaBP.
[A]
[R]
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Earth System Models of Intermediate Complexity: Closing the gap in the
spectrum of climate system models.
[A]
[H]
[R]
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Instability of glacial climate in a model of the
ocean-atmosphere-cryosphere system
[A]
[R]
- The role of the thermohaline circulation in abrupt climate change.
[A]
[R]
[H]
-
Improved representation of sea ice processes in climate models.
[A]
[R]
[P]
- Forcing of the deep circulation in simulations of the Last Glacial Maximum.
[A]
[R]
- Simulations of Heinrich Events in a coupled ocean-atmosphere-sea ice model.
[A]
[R]
-
Daily maximum and minimum temperature trends in a climate model.
[A]
[P]
[R]
- The Canada Basin 1989-1995: Upstream events and far-field effects of
the Barents Sea branch.
[A]
[R]
-
On the role of wind-driven sea ice motion on ocean ventilation.
[A]
[R]
- Distinguishing the influences of heat, freshwater and momentum fluxes on ocean circulation
and climate.
[A]
[R]
- Detecting anthropogenic influence with a multi model ensemble.
[A]
[R]
- The structure of the upper water column in the northwest North
Atlantic: modern vs. last Glacial maximum conditions.
[A]
[R]
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A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
2001
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Gender differences in introductory atmospheric and oceanic science
exams: Multiple choice versus constructed response questions.
[A]
[R]
-
Satellite altimetry observations of the Black Sea level
[R]
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Climate model simulations of effects of increased atmospheric CO2
and loss of sea ice on ocean salinity and tracer uptake.
[A]
[R]
-
The role of ice ocean interactions in the variability of
the North Atlantic thermohaline circulation.
[A]
[R]
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Simulating the ice-thickness distribution in a coupled climate model.
[A]
[R]
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Dependence of multiple climate states on ocean mixing parameters.
[A]
[R]
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Glacial Termination: Sensitivity to Orbital and CO2 Forcing in a
Coupled Climate System Model.
[A]
[R]
- Absence of deep-water formation in the Labrador Sea during the
last interglacial period
[A]
[R]
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Projection of climate change onto modes of atmospheric variability.
[A]
[R]
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The influence of sea ice physics on simulations of climate change.
[A]
[R]
- Importance of wind-driven sea ice motion for the formation of
Antarctic Intermediate Water in a global climate model
[A]
[R]
- The Science of Climate Change What do we know?
[A]
[R]
[H]
- The UVic Earth System Climate Model: Model description,
climatology and application to past, present and future climates
[A]
[P]
[R]
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A=Abstract,P=Paper (pdf or ps), H=HTML, R=Reference.
2000
-
The causes of 20th century warming. Science 290, 2081-2082.
[R]
-
Propagation characteristics of extratropical planetary waves observed
in the ATSR global sea surface temperature record
[R]
[P]
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Uncertainty in climate change. Nature,407, 571-572.
[R]
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Evaluation of ocean and climate models using present-day observations and forcing.
[A]
[P]
[R]
- Zwiers, F.W., and A. J. Weaver, 2000: The causes of 20th century warming. Science, 290, 2081-2082.
[R]
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The Canadian Centre for Climate Modeling and Analysis
global coupled model and its climate.
[A]
[P]
[R]
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Trends in Canadian precipitation intensity.
[A]
[P]
[R]
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The impact of rising atmospheric CO2 levels on low frequency North Atlantic climate variability.
[A]
[H]
[P]
[R]
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Data-model comparison of the Younger Dryas event.
[A]
[R]
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