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Comment on Week in review – science edition by Jim D

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What does it amplify? It amplifies the response. Also known as a positive feedback.


Comment on Week in review – science edition by Robert I. Ellison

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n this cartoon universe we have a forcing of 3.7 W/m2 and feedbacks of – 3.7 W/m2 at a specific temperature.

ECS = ERF/total feedbacks

So yes – net feedbacls are negative. Always – except perhaps in glacial/interglacial transitions.

Comment on Week in review – science edition by Jim D

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Compete circle. It is loose language that confuses you. You have one word for feedback and response and therefore can’t distinguish them. The size of the response depends on the net feedback.

Comment on Week in review – science edition by Jim D

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Yes, because you don’t understand the conventional circuit definition where there can be a net positive feedback (see feedback loop).

Comment on Week in review – science edition by Robert I. Ellison

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It amplifies radiant imbalances at TOA that are the origin of warming or cooling. But net feedbacks necessarily reduce radiant imbalances to zero at energy equilibrium.

Comment on Week in review – science edition by Robert I. Ellison

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Forcing causes changes in the system that feedback into energy imbalances at toa. That’s the ‘conventional’ understanding.

Comment on Week in review – science edition by Robert I. Ellison

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No it is not ‘loose language – it is how feedbacks to forcing work. ECS is the temperature at which 3.7 W/m2 is negated.

ECS = ERF/total feedbacks – at an energy equilibrium at TOA.

This is beyond a joke even for me.

Comment on Week in review – science edition by Jim D

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It’s the response that reduces the imbalance when you think about it. You don’t need a feedback, just the Planck Response. Confused yet?


Comment on Week in review – science edition by Jim D

Comment on Week in review – science edition by Jim D

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You have one word for two completely different things. You can have a response without a feedback and that reduces the imbalance too.

Comment on Week in review – science edition by Robert I. Ellison

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Not even close – you can’t have a forcing without it causing a temperature change – and multiple feedbacks from the response cancels out the forcing at a specific temperature..

Comment on Week in review – science edition by Jim D

Comment on Politics of climate expertise by Jim Rose

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Reblogged this on <a href="http://utopiayouarestandinginit.com/2018/12/28/politics-of-climate-expertise/" rel="nofollow">Utopia - you are standing in it!</a>.

Comment on Week in review – science edition by Robert I. Ellison

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The Planck response is the temperature increase considering only the temperature (Plank) feedback. In reality of course all feedbacks happen concurrently.

ECS(Planck response) = ERF/Planck feedback = 3.7 Wm^-2 / 3.2 W m^-2 k^-1 = 1.2 K

Consistent with the IPCC, Isaac Held, the University of Albany post graduate climate modelling course notes and the Judith Curry blog post. You are the odd one out #jiminy and it is all because the temperature (Planck) feedback doesn’t seem to be real for you. A very odd oversight that you cling to with aberrant tenacity.

Do you have a different mathematical model? Any other standard means of calculating the Planck response for the forcing and the Planck feedback?

Comment on Week in review – science edition by Robert I. Ellison

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Does a warmer planet emit exponentially more IR or not?


Comment on Week in review – science edition by Jim D

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You know what the Planck Response is (dF/λo), and maybe you know what the actual response is (dF/λ), where F is the forcing, and maybe you even understand that when the actual response is larger than the Planck Response, there has been a positive feedback (λ < λo), and when it is less there is a negative feedback, and when it is the same, there has been no feedback (λ=λo). This is not a difficult thing to understand. Which part do you have trouble with?

Comment on Week in review – science edition by Geoff Sherrington

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JimD,
You find that out when you read it. There is new info there. Geoff

Comment on Week in review – science edition by Jim D

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Yes, the IR emission responds to warming but the proportionality (λ) depends on feedbacks. Without feedbacks, it is λo.

Comment on Week in review – science edition by Jim D

Comment on Week in review – science edition by Robert I. Ellison

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λo is the temperature (Planck) feedback: -3.2 W^-2 K^-1

λ=λ0+λ1+λ2+… < 0 in current day conditions. Not difficult to verify. Just add up the estimates in any of the sources given.

http://www.atmos.albany.edu/facstaff/brose/classes/ATM623_Spring2015/Notes/Lectures/Lecture03%20–%20Climate%20sensitivity%20and%20feedback.html#Decomposing-the-feedback-into-additive-components

"QUESTION: what is the sign of λ?

Could there be energy balance for a planet with a positive λ? Think about your experiences timestepping the energy budget equation."

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