The seasonal climate may relate to changes
in the ocean circulation pattern prior to 4.6 Ma that resulted in an increased temperature and atmospheric pressure gradient between the east coast of North America and the Atlantic Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier conditions.
One of the most significant potential mechanisms is a
shift in an ocean circulation pattern known as thermohaline circulation, which would have widespread consequences for Europe and the U.S. East Coast.
Ongoing
changes in ocean circulation patterns, which are helping to drive warm water from other parts of the sea closer to the Antarctic continent, are also believed to be a major factor.
They showed that temperatures warmed in both the North Pacific and Greenland, likely due to changes
in ocean circulation patterns.
For instance, the Medieval Climatic Anomaly was characterised by relatively high solar activity, low volcanic activity and possible changes
in ocean circulation patterns.
In its discussion of specific examples, such as a catastrophic change
in ocean circulation patterns, the report emphasizes predicted risks that the FAR concluded were minimal through the rest of the century.
In this case, it is possible that the instability is
in the ocean circulation patterns — and that the mass balances potentially caused by angular momentum shifts lead the propagation of the resultant temperature shifts.
Ongoing changes
in ocean circulation patterns, which are helping to drive warm water from other parts of the sea closer to the Antarctic continent, are also believed to be a major factor.
This can lead to major climatic changes such as a change in rainfall patterns, changes
in ocean circulation patterns, warming in some areas, dramatic cooling in others, rising sea levels and coastal flooding, due to melting ice sheets and thermal expansion of seawater.