Thousands of years ago the circulation of the North Pacific
ocean changed substantially, releasing large quantities of carbon dioxide to the atmosphere, scientists in Scotland have found.
Not exact matches
«Our work pinpoints the time when the
ocean began accumulating oxygen at levels that would
substantially change the
ocean's chemistry and it's about 250 million years earlier than what we knew for the atmosphere.
The researchers also found that some
oceans are more sensitive to
changes in temperature and will have
substantially larger gains from achieving the Paris Agreement.
In Balmaseda et al. paper, they show very nicely the
changes in the
ocean heat content (OHC) since the late 1950s and how during the last decade the OHC has
substantially increased in the deep
ocean while in the first 300 and 700 meters it has stalled.
The GRACE observations over Antarctica suggest a near - zero
change due to combined ice and solid earth mass redistribution; the magnitude of our GIA correction is
substantially smaller than previous models have suggested and hence we produce a systematically lower estimate of ice mass
change from GRACE data: we estimate that Antarctica has lost 69 ± 18 Gigatonnes per year (Gt / yr) into the
oceans over 2002 - 2010 — equivalent to +0.19 mm / yr globally - averaged sea level
change, or about 6 % of the sea - level
change during that period.
But a new study published in the journal Science Advances has concluded that another impact of global climate
change might help coral reefs survive increasing sea temperatures: «even a modest sea level rise can
substantially reduce temperature extremes within tide - dominated reefs, thereby partially offsetting the local effects of future
ocean warming,» the authors of the study write.
A
change in
ocean heat content can also alter patterns of
ocean circulation, which can have far - reaching effects on global climate conditions, including
changes to the outcome and pattern of meteorological events such as tropical storms, and also temperatures in the northern Atlantic region, which are strongly influenced by currents that may be
substantially reduced with CO2 increase in the atmosphere.
[A] nthropogenic climate
change is expected to lead to a greater incidence of high - intensity hurricanes, which together with rising sea level, will produce increased risk of storm surge flooding, while hurricanes are projected to produce
substantially more precipitation as the atmosphere and
oceans warm.