What secret knowledge. 0.8C is SFA in geological terms over the Holocene Optimum.
Are you aware of the geophysical phenomenon happening in perfect timing with "climate change"?
I've been bring it up for years but did you listen, did you try to deviate from the CO2 to accept the geological aspect which has repeated over and over again in just the past few million years alone?
You were razzing Beaver about grade 9 physics which is odd for other reasons all on it's own but long before high school or even grade school you learned some fascinating physics about magnetism but are today ignoring it.
I'm going to go over this one more time. It explains the end of the Wisconsonian Glaciation and todays "climate change" and it's all based on Physics. The names I listed above would have given you a clue but again you flipped it off so I'm going to tell you what these Mofos discovered. Beaver is going to love this BTW.
Ocean currents and jetstreams create their own magnetic fields that interact with the planets magnetosphere. From 1974 to present the magnetic north pole (which sat in James Bay during the last ice age before moving and trigging the Holocene Optimum) has be taking a rapid journey northward and dragging and taking these ocean currents and jetstreams along for the ride.
Start here:
https://www.google.ca/#q=geomagnetism+and+ocean+currents It explains what those fellows back in the 40's were on to and why climate is changing as the pole moves.
This one is a good read:
DigiTool - Results - Full
Electromagnetic fields generated by ocean currents and the potential for using geomagnetic data in ocean and climate studiesCreator
Tyler, Robert H.ContributorMysak, Lawrence (advisor)Date1995AbstractThe ocean currents flowing through the earth's main magnetic field are known to induce secondary magnetic fields. Hence, variations in the ocean circulation induce variations in the net magnetic field. This research is aimed at exploring the potential for using geomagnetic data to study variability in ocean circulation and climate. First, general relativity theory is used to formally establish the proper set of electromagnetic equations to be used for observers in a rotating (accelerating) frame of reference observing a medium (the ocean, in this case) with relative velocity. Extra terms due to rotation are derived and described and a generalized Schiff's charge density is shown to be potentially significant for the application to ocean circulation. We extend the theory of electromagnetic fields generated by ocean currents. Many analytical solutions are found for idealized ocean features including sheared flow, jets, and a Stommel gyre. Results indicate that the ocean-induced magnetic fields will typically have magnitudes of 10's-100's of nT within the ocean. Outside of the ocean, the magnitudes are smaller (typically 1-10 nT) but decay on scales set by the horizontal scale of the ocean feature. We investigate the time-scales associated with the adjustment of electromagnetic fields generated by low-frequency ocean currents. We find that the time scales can be quite long, prohibiting a quasistatic assumption in the treatment of the electromagnetic fields generated by the important tidal, inertial, and diurnal-frequency ocean currents. Three-dimensional explicit time-dependent and steady-state finite-difference numerical models are constructed to study the electromagnetic fields generated by more realistic ocean current and conductivity features. The ocean currents generate electromagnetic forces on the fluid at the surface of the earth's core. If these forces lead to significant core motion, the effect of the oceans on the generation and variability of the earth's magnetic field may be nontrivial. We estimate the form and magnitude of these forces and make comparisons with observations. Despite many uncertainties, we find evidence to suggest the ocean forcing mechanism may be significant and conclude that this process should be further investigated in the context of a larger study. This work indicates that it is likely that the geomagnetic record has captured oceanic signals. From a preliminary data analyses we find that aside from the oceanic tidal signals, the magnetic record shows other signals of possible oceanic origin including an apparent correlation between magnetic records from the equatorial Pacific and the Southern Oscillation Index. We discuss the prerequisites that are necessary to extract information about ocean circulation variability from the geomagnetic record.SubjectGeophysics.Physical Oceanography.Physics, Electricity and Magnetism.DegreeDoctor of PhilosophyDepartmentDepartment of Atmospheric and Oceanic Sciences.RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.URL of this record
http://digitool.Library.McGill.CA:80/R/-?func=dbin-jump-full&object_id=39884&silo_library=GEN01
When the wrong people get funded you get wrong outcomes. Stuff your CO2 where the sun don't shine.
urpose - SourceWatch
