Not exact matches
Over the course of coming decades, though, trade wind speed is expected to decrease from
global warming, Thunell says, and the result will be less phytoplankton production at the surface and less oxygen utilization at
depth, causing a concomitant increase in the
ocean's oxygen content.
The estimated increase of observed
global ocean heat content (
over the
depth range from 0 to 3000 meters) between the 1950s and 1990s is at least one order of magnitude larger than the increase in heat content of any other component.
OHC may be one of the best measures of the top of atmosphere imbalance available - averaged
over long time periods,
global, representing (for the full
depth of the
oceans) ~ 93 % of the energy changes.
Monitoring the
ocean to its full
depth with consistently calibrated instrumentation all
over the globe — and doing so for decades at a time — is critical to track how
global warming impacts the
oceans» ecosystems and biogeochemical processes.
The IPCC tells us that
Over the period 1961 to 2003,
global ocean temperature has risen by 0.1 °C from the surface to a
depth of 700 m.
The ARGO network has remedied the inadequacy of the
ocean measurements to some extent, but they still only measure down to 2000 metres - whereas the the
global oceans are
over twice that
depth on average.