Movement of the Gulf Stream’s Destabilization Point
The Gulf Stream is the western boundary of the North Atlantic sub-tropical gyre that transports heat and salt from the Gulf of Mexico to the deep Atlantic. This mighty ocean current follows the coast of Florida up to Cape Hatteras in North Carolina after which it starts to meander like a winding river. This point is called its ‘destabilization point’ and it has been moving westward in the last 2 decades at the rate of 25 kilometers per year.
The Gulf Stream meanders have the potential to create underwater cyclones and troughs that stir the nearby currents. The recent migration of the destabilization point has enhanced the frequency of deep ocean stirring of the nearby Deep Western Boundary Current and these events have become more common since 2008.
The westward movement of the destabilization point is hypothesized to be related to the warming of shallow water along the continental shelf in the coastal region from Massachusetts to North Carolina (the ‘Mid-Atlantic Bight’). The interactions between the Gulf Stream and the Deep Western Boundary Current when they cross below each other at Cape Hatteras could be the reason for this new warming trend observed.
- Nate
Image Credits: NASA http://bit.ly/2m2md3U
Source: http://bit.ly/2lgzjcl http://bit.ly/2m6llrQ