| Peter Huybers cv |
Department of Earth and Planetary Sciences |
Harvard University |
20 Oxford St., Cambridge, MA 02138 USA
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phuybers@fas.harvard.edu, (617)495-8391
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Publications
- Huybers and Tziperman, Integrated summer insolation
forcing and 40,000 year glacial cycles: the perspective from an
icesheet/energy-balance model, Paleoceanography, 2008.
pdf and
code
- Huybers and Molnar, Tropical cooling and the onset of
North American glaciation, Climate of the Past, 2007.
pdf
- Huybers, Gebbie, and Marchal, Can paleoceanographic
tracers constrain meridional circulation rates?, Journal of Physical Oceanography, 2007.
pdf
- Huybers, Glacial variability over the last 2Ma: an
extended depth-derived agemodel, continuous obliquity pacing, and
the Pleistocene progression, Quaternary Science Reviews, 2007.
pdf and supplemental material
(also posted at NCDC)
- Gebbie and Huybers, Meridional circulation
during the Last Glacial Maximum explored through a combination of
South Atlantic d18O observations and a geostrophic inverse model,
G-cubed, 2006.
pdf
- Tziperman, Raymo, Huybers, and Wunsch, Consequences of
pacing the Pleistocene 100 kyr ice ages by nonlinear phase locking to
Milankovitch forcing, Paleoceanography, 2006. pdf
- Huybers and Curry, Links between annual,
Milankovitch, and continuum temperature variability, Nature,
2006. pdf and supplemental material
- Huybers, comment on ``Hockey sticks, principal
components, and spurious significance'' by McIntyre and McKitrick
[2005], Geophysical Research Letters, 2005. pdf and supplemental material (An edited version of
this paper was published by AGU. Copyright 2005 American Geophysical
Union.)
- Huybers and Wunsch, Obliquity pacing of the late Pleistocene
glacial terminations, Nature,
2005. pdf
- Huybers and Wunsch, A depth-derived Pleistocene
age-model: uncertainty estimates, sedimentation variability, and
nonlinear climate change, Paleoceanography, 2004. pdf
- Huybers, Comments on: 'Coupling of the hemispheres in
observations and simulations of glacial climate change': by
A. Schmittner, O.A. Saenko, and A.J. Weaver [Quaternary Science
Reviews 22 (2003) 659-671], Quaternary Science Reviews,
2004. pdf
- Huybers and Wunsch, Rectification and precession-period
signals in the climate system, Geophysical Research Letters, 2003. pdf
Manuscripts
- Huybers and Denton, Interpolar climate symmetry at
orbital time scales and the duration of Southern Hemisphere
summer, submitted.
pdf
- Stine, Huybers, and Fung, Changes in the phase of the annual cycle of surface temperature , submitted.
pdf
- Huybers and Langmuir, Feedback between deglaciation
and volcanic emissions of CO2 , submitted.
pdf
- Perron and Huybers, Is there an orbital signal in the polar layered
deposits on Mars? , submitted.
pdf
- Tingley and Huybers, The spatial mean and dispersion of surface temperatures
over the last 1200 years: warm intervals are also variable
intervals , submitted.
pdf
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Research
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Glacial cycles. Over the last three million years the amount
of ice on the Earth has alternately waxed so as to cover much of the
high-latitude continents and waned to the relatively ice-free
conditions in the North which we have today. The cause of these
massive shifts in climate remains unclear, not for lack of
hypotheses, of which there are many, but instead for lack of any
single compelling theory. Thus one aim is to distinguish between
the competing hypotheses (e.g. Huybers
and Wunsch, 2005; Huybers,
2007). Another is to explore the causes of glaciation during
the Plieocene and early Pleistocene, associated with seemingly more
regular 40,000 year variations in ice-volume (Huybers,
2006;
Huybers and Tziperman, 2008). Glacial cycles are unlikely to be
understood in isolation, and I've also found it useful to explore
their relationship with changes in tropical Pacific sea surface
temperatures (Huybers
and Molnar, 2007), as well as with changes in Antarctic
temperature (Huybers
and Denton, submitted). Most recently Taylor Perron and I have
looked at whether orbital variation control the layered deposits on
the North Polar Cap of Mars (submitted).
Much more remains to be done.
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Past atmospheric conditions. How do recent surface air
temperature variations compare to past variations? Instrumental
records of temperature are sparse before 1850 and wholly absent before
1600, so that tracing out the history of past temperature variability
requires the use proxies for temperature. Proxies include tree rings,
ice-cores, corals, and lake and marine sediments. How best to
determine temperatures from these proxies has been the subject of some
research and much debate (e.g. Huybers,
2005). Martin Tingley and I are working on a Bayesian
Hierarchical model to estimate spatial average temperature from noisy
proxies of local temperature variability. Konrad Hughen
and I are exploring Arctic surface temperatures and modes of
atmospheric circulation over the last four centuries. |
Past ocean circulation. Reconstruction of past ocean
circulation provides allows us to gauge the natural range and modes of
ocean circulation, permits testing of our models over a wider range of
conditions, helps place modern changes in context, and (to me) is of
inherent interest. That said, reliably deducing ocean circulation
from paleoceanographic data is challenging (see e.g.
Huybers et al., 2006), but if you ask the right questions and make
some suitable assumptions, progress is always possible (e.g. Gebbie
and Huybers, 2007). Along with Carl Wunsch, Jake Gebbie, and
Eli Tziperman,
we are continuing to study the past ocean circulation using a
combination of modeling and data analysis. |
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Climate change across space and time scales. Many fascinating
phenomena straddle modern and paleo-climate time-scales. Indeed,
climate variability is intimately linked across an enormous range of
time-scales (e.g. Huybers
and Curry, 2006). Determination of the spatial and temporal
scaling associated with climate variability seems fundamental to
understanding the relevant physics. I'm now attempting to assess how
the spectrum of climate variability changes with the background
climate state. I'm also trying to better assess the spatial extent
associated with the Younger-Dryas event. |
People
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Graduate Students: Martin Tingley and Eddie Haam. |
Research Staff: Geoffrey (Jake) Gebbie. |
Opportunities
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Feel free to contact me if you are interested in conducting
either graduate or postdoctoral work with me. |
Last updated in August, 2007. visitors:
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