The associated plots compare raw temperature changes in the
atmosphere to the atmosphere’s natural variability. Variability is measured by
the standard deviations of each time series of temperature data from around the
world. The world map in the upper left shows six outlined regions whose
temperature time series are displayed in temperature-versus-time plots below.
In that upper left map plot of raw temperature anomalies, and in the six time
series below, obvious raw increases in temperature are obvious.
What is less obvious is the natural variability in the
various parts of the world. The upper right plot shows the over-land region of
the Arctic to have the highest. (If you recall the discussion on the polar
vortex, where north-to-south snakelike swings in the jet stream, known as
Rossby waves, have major effects on air temperatures, this huge variation in
that part of the world makes sense.) By contrast the tropics are extremely
consistent in their temperatures.
So warming over the poles is to a large extent masked by the
huge swings in atmospheric temperature there, while smaller increases in the
tropics, which have less impact on the ecosystems there, are not so easily
noticed. But dividing the temperature anomalies by their standard deviations
produces a measure of how extreme the temperature increase is. The middle right
map, “Global Warming Level of Emergence” closely resembles the map of standard
deviations around the world, showing when an air temperature anomaly would
become statistically significant.
Tomorrow: system response times to change.
Be brave, and be well.
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