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So coaches don't do anything in these simulations.
In these simulations, an entity's next move is almost entirely independent of all its previous moves.
In these simulations, meltwater inputs from retreating Northern Hemispheric ice-sheets were not taken into account.
In these simulations all boundary conditions are fixed at values for 83 kyr ago.
The semimajor axis of the planet in these simulations was set to be 1.165 and 1.195 a.u.
In these simulations, the additional buffering capacity associated with the presynaptic pipette solution (OGB-6F) were taken into account.
In these simulations we treat the switching (p), PCD (c), and structure (r) parameters as probabilities (still holding r fixed).
The semimajor axis of the planet in these simulations was set to be 0.975, 1.000, 1.025 and 1.050 a.u.
The polarity of the nucleated vortex in these simulations did not change sign when the external field was reversed.
Confidence, too: People who take charge in these simulations tend to be decisive, making calls from the gut, and quickly.
An IGRF geomagnetic field is used in these simulations.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com