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EAPS Graduate Program
EAPS Graduate Degree Programs
Program in Atmospheres, Oceans, and Climate (PAOC)
Prof. R. Alan Plumb, Director
Degrees Offered: S.M., Sc.D., Ph.D.
Atmospheric and oceanic sciences and the study of climate are founded
on the basic principles of physics, mathematics, and chemistry, with
particular emphasis on the fundamentals of fluid mechanics. The Program
in Atmospheres, Oceans, and Climate (PAOC) involves many scientific
disciplines, including dynamical and chemical oceanography, atmospheric
dynamics and chemistry, and geochemistry. In all areas, PAOC emphasizes
the synthesis of theoretical, observational, and modeling approaches.
Graduate admissions
information.
PAOC offers students ample opportunity for complex, interdisciplinary
work. For this reason, our programs are flexible and serve primarily
to guide students through an organized body of study and research.
In fact, our four educational programs overlap considerably. Students
select one of these programs but may switch to another as their research
interests develop.
- Atmospheric Science – In the atmospheric
science program, emphasis is placed on an integrated approach involving
theory, modeling, experiments, and data analysis. Study areas include
atmospheric dynamics, synoptic meteorology, atmospheric convection,
dynamics of the middle atmosphere, tropical meteorology, atmospheric
chemistry, and atmospheric radiation. Because of its cross-disciplinary
nature, the program often includes study in mathematics and/or chemistry.
Recent areas of research have included the ozone hole, the dynamics
of hurricanes, adaptive sampling, and air-sea interaction.
- Climate Physics and Chemistry - The newest of
the PAOC degree programs, the climate physics and chemistry program
was created to capitalize on the overlapping nature of the atmospheric,
oceanic, and geological sciences as they relate to climate and climate
change. Students have access to unique expertise in all aspects
of climate including paleoclimatology and the geological record,
all of atmospheric and oceanic physics and chemistry, fluid dynamical
modeling of the climate system, hydrology, and geophysics. Ongoing
research activities include the study of high latitude North Atlantic
deep-sea cores as records of the climate of the past 200,000 years;
coupled models of air-sea interaction developed in MIT’s Climate
Modeling Initiative; studies of possible mechanisms of the Permo-Triassic
Mass extinction; Atlantic Climate Variability; and global biogeochemical
cycles.
- Physical Oceanography - The program covers a
wide range of physical oceanography research and includes modeling,
theory, observations of the ocean at sea and from space, and laboratory
models. Students explore the ocean’s general circulation,
mixing processes, and coastal and upper ocean processes. Recent
PAOC research in this field includes: the construction of the first
three-dimensional time-evolving estimates of the oceanic general
circulation, employing both a new numerical model and global observations;
the role of mesoscale eddies in the ocean circulation and their
interactions with biological fields; deep convection and thermohaline
circulation; and the study of the interactions of the tropical oceans
with mid-latitudes.
- Chemical Oceanography - Inorganic, organic,
radioactive, and stable isotopic geochemistries are used as tools
to understand: the ocean, its sediments, and the seafloor crust
as a biogeochemical system; the role of this system in regulating
climate change; and its impact on the geological evolution of the
Earth. Elemental chemical variability and speciation are used to
establish anthropogenic impact on ocean chemistry and the role of
trace metals in the nutrition of marine organisms. Beginning with
weathering, global biochemical cycles are followed from rain, rivers,
and groundwaters into the ocean, and their subsequent fate in sediments
and seafloor hydrothermal systems is studied. Biomarker molecules
are used to trace the early history of the Earth, ice age climate
history, and the fate of biogenic compounds as they are transformed
by microbes in the ocean and sediments. Radioactive isotopes are
used to quantify rates of processes in the marine system and establish
reliable geochronologies of sedimentary and other climate archives.
Stable isotope ratios of elements ranging from hydrogen, helium
and other noble gases, carbon, nitrogen, and trace metals such as
iron, zinc, and molybdenum are all under active investigation. Field
work takes place on continents, coastal vessels, and open-ocean
research vessels; computer modeling and interpretation of this data
is integral to this effort.
The PAOC graduate programs in oceanography are joint doctoral programs
within the MIT/Woods Hole Oceanographic Institution (WHOI) Joint Program.
WHOI, located about 70 miles south of Boston, is one of the world’s
leading oceanographic research centers, with extensive laboratory
facilities and an impressive fleet of research ships and submersibles
operating around the world. PAOC students may reside and conduct research
at either MIT or WHOI, and much effort has been made to render communication
and travel between the institutions as easy as possible. All students
are jointly supervised by MIT faculty and WHOI staff and have access
to all of the capabilities and expertise of both institutions.
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