It is gravitationally compressed which is suffocating as opposed to
coolING in feedback loops.
Not exact matches
It's also likely, Russell and his colleagues say, that the drying
in Indonesia created a
feedback loop that amplified ice age
cooling.
The margin of error
in various «forcings» and
feedback loop strengths is so big that there is a reasonable probability that global climate will
cool in the next decade.
The study, which has not yet been peer reviewed, brings new importance to a
feedback loop in the ocean near Antarctica that results
in cooler freshwater from melting glaciers forcing warmer, saltier water underneath the ice sheets, speeding up the melting rate.
In fact, it was one of my criticisms earlier that AGW theory seems overly intent on finding positive feedback loops, while not considering negative feedbacks seriously enough — one such potential negative feedback is that on a warmer Earth, more water is evaporated into clouds, in turn cooling things back of
In fact, it was one of my criticisms earlier that AGW theory seems overly intent on finding positive
feedback loops, while not considering negative
feedbacks seriously enough — one such potential negative
feedback is that on a warmer Earth, more water is evaporated into clouds,
in turn cooling things back of
in turn
cooling things back off.
The new study, published
in Nature Geoscience, identified a negative
feedback loop in which higher temperatures lead to an increase
in concentrations of natural aerosols that have a
cooling [continue reading...]
The same
feedback loop was working to fund «Global
Cooling»
in the 1970s.
It's even possible that that the Triple R played a role
in sustaining itself by reducing North Pacific storm activity and preventing vertical mixing of
cooler sub-surface ocean water, culminating
in a self - reinforcing
feedback loop by which atmospheric ridging led to warm SSTs, which
in turn led to more ridging, and so on.
What happened
in the Arctic, was a slow, very slow and gradual decrease
in cooling, caused by progressively longer warmer seasons, with a
feedback loop of warm air reducing albedo, with reduced albedo increasing warm air.
The new study, published
in Nature Geoscience, identified a negative
feedback loop in which higher temperatures lead to an increase
in concentrations of natural aerosols that have a
cooling effect on the atmosphere.