An isotope of helium that is useful in ocean tracer studies.
There are two sources for Helium-3 in the ocean: volcanic
sources at mid-ocean ridge crests and the decay of man-made
tritium. The former source makes helium-3 a unique tracer
due to its being injected into the middle of the water column.
This leads, for example, to a stark contrast in helium-3 content
between incoming and outgoing deep waters in the Pacific.
It also provides a dramatic picture of the relative movement
of helium poor NADW and helium rich
(due to sources in the Pacific) ACC
water. The helium-3 tritium decay (sometimes
called trituigenic) source is much larger than the deep sea
sources, with the global average of the latter being
about 4 at/cm2/s as opposed to a northern hemisphere average
of about 32 at/cm2/s for the former.
Helium-3 is used in combination with tritium to date water
on timescales of 0-10 years with a resolution of around 0.1 years
(in North Atlantic surface waters).
It is better to treat them as separate but related
tracers on longer timescales or in the presence of extensive
mixing. Their relationship is a diagnostic of vertical versus
horizontal mixing, and has been used to assess an upper limit
to vertical mixing that is consistent with physical estimates.
This has also been used to show that horizontal mixing is the
dominant mechanism of thermocline ventilation in subtropical
gyres.
See Sarmiento (1988) and
Broecker and Peng (1982).