March 26th, 2018

Buoy 46006 located 650NM west of Eureka, CA and 1,234 miles S/SE of buoy 46001 in the Gulf of Alaska was analyzed for a rise in sea surface water temperature.  Both buoy's are located in depths over 4km deep and monitor sea surface temperature 1m beneath the surface.  The difference in the hour readings in the following graph is that 46006 reports in every 10 minutes, and 46001 reports in once an hour.  We can see a rise in sea surface temperatures at buoy 46006 just after a week of the initial surge recorded on 46001.  The second spike in the upper graph is the 7.9 earthquake, and I spiked the lower graph for visual perspective of time.  This is evidence of geothermal heat being a major contributor to our oceans.  This increased heat increases water vapor that accumulates into clouds and rain cooling the surface inland.  This also demonstrates, through mass dissipation, that our oceans are natural chilling towers for a huge nuclear reactor that we call the "Core."  This in turn becomes the major driving mechanism for cloud cover and precipitation that drives our climates.