Human impact on our environment
has created a variety of societal problems that need solutions based
on thorough scientific understanding of our natural systems.
I have focused on studies
of water movement in natural systems (mainly oceans and groundwater),
using natural and anthropogenic trace substances such as radiocarbon,
oxygen-18, radioactive hydrogen and its decay product helium-3. We also
use measurements of noble gases in groundwater to reconstruct continental
paleotemperature records.
In the ocean, we use these
substances either as regional or global "dyes" to investigate
the movement of water from the ocean surface into the deep basins and
to study circulation patterns in the deep ocean. We also apply radioactive
isotopes to determine the age of specific water masses. Our studies
add to basic understanding of ocean circulation and further our knowledge
of the oceans role in climate variability. Our field work is currently
concentrated in polar oceans.
The same principles are
used to investigate groundwater flow in shallow and deep aquifers, providing
results that are relevant for environmental risk and impact studies.
Groundwater ages also provide a chronology for paleoclimate records
reconstructed from groundwater flow systems. A new line of research
is the release of SF6 and 3He into rivers and
estuaries to study mixing and gas exchange.
Schlosser, P., G. Boenisch,
M. Rhein and R. Bayer. Reduction of deepwater formation in the Greenland
Sea during the 1980s: evidence from tracer data, Science, 251,
1054-1056, 1991.
Stute, M., P. Schlosser,
J. Clark and W.S. Broecker. Paleotemperatures in the southwestern United
States derived from noble gases in ground water, Science, 256,
1000-1003, 1992.
Clark, J. F., P. Schlosser,
M. Stute, and H. J. Simpson, SF6-3He tracer release
experiment: a new method of determining longitudinal dispersion coefficients
in large rivers, Environment Science and Technology, 30, 1527-1532,
1996.