The upper ocean phytoplankton blooms are impacted by the rain and impact the thermal structure.
Not exact matches
«These conditions will cause changes in
phytoplankton growth and
ocean circulation around Antarctica, with the net effect of transferring nutrients from the
upper ocean to the deep
ocean,» said lead author J. Keith Moore, UCI professor of Earth system science.
In colder
oceans, the separating layer (thermocline) does not form, or only for parts of the year, so
phytoplankton at the top receives nutrients from the deeper sea and provides oxygen for the the
upper and deeper layers (as well as nutrients, when
phytoplankton decomposes).
(5) modulation of the
upper ocean heating via
phytoplankton and their associated optical properties.
Once the CO2 concentration of the
upper ocean is depleted by growth and sinking of
phytoplankton, the timescale for gas exchange with the atmosphere is about a year for a one - hundred meter
ocean mixed layer, typical of the tropics.
Sea butterflies are most abundant in the
upper 50 meters of the
ocean, grazing on abundant
phytoplankton.
Oxygen enters the
ocean through two ways: interactions between its surface and the atmosphere, and as a photosynthesis byproduct from
phytoplankton in
upper layers of the
ocean, much in the same way plants on land produce oxygen.
The Ekman upwelling from the wind stress curl associated with these structures plays an important role in
ocean circulation theory, as well as in
ocean biology from upwelling of nutrients from the deep water into the
upper ocean where they can be utilized by
phytoplankton.
Phytoplankton in the
ocean's
upper layer (that is, the populations observed from space) rely on vertical nutrient transport to sustain productivity, so intensified stratification during a rising MEI period (Fig. 2b) is accompanied closely by decreasing NPP (Fig. 2b)(r2 5 0.73, P, 0.005)