A composite analysis of satellite - based SST measurements reveals that in the tropical region the average strength of the storm - induced sea surface cooling can be explained by the superposition of an effect due to the storm intensity and an effect associated with the translation speed, and implies that the variability of
upper ocean stratification may not be an important factor in this region
Advancing the knowledge on the effects of sea ice deformations on
upper ocean stratification and ecosystem will have profound implications on our ability to forecast ongoing changes in Arctic Ocean.
Not exact matches
«With the hydrological cycle projected to change under global warming, impacting
upper -
ocean stratification and mixing, the results from this study have potentially important implications for understanding future tropical cyclone activity.»
•» According to Zhang (2007) thermal expansion in the lower latitude is unlikely because of the reduced salt rejection and
upper -
ocean density and the enhanced thermohaline
stratification tend to suppress convective overturning, leading to a decrease in the upward
ocean heat transport and the
ocean heat flux available to melt sea ice.
(2)
upper ocean physical responses, including
stratification and turbulent mixing that result in
One group of researchers favors «
stratification» as a cause — the tendency of climate warming of the
upper ocean to restrict seasonal overturning and reduce the supply of new atmospheric oxygen.
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)
Decreases in both upwelling and formation of deep water and increased
stratification of the
upper ocean will reduce the input of essential nutrients into the sunlit regions of
oceans and reduce productivity (Cox et al., 2000; Loukos et al., 2003; Lehodey et al., 2003; Sarmiento et al., 2004a).