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initial albedo– Earth’s planetary albedo– which will of course be modified as we change some of the feedback factors. The ice albedo feedback playing into the shortwave forcing. The cloud radiative feedback can influence both a combination of shortwave and long wave forcing. There’s the cloud albedo effect, which tends to be a negative feedback. But there’s also the greenhouse gas-like properties of clouds, the infrared absorbing properties of clouds which gives us a positive feedback. And as we vary this feedback factor, we can transition from where the negative cloud radiative feedbacks dominate to where the positive cloud feedback dominate. And these values are roughly equal to the best current estimates of what those feedback factors are. And so using those default settings gives us Amazing crappie fishing metal all over print stainless steel tumblersort of a mid-range climate sensitivity. And you’ll look at that in your problem set. The cloud feedback factor is set at a modestly negative value of minus 0.83. The water vapor feedback factor is 2. And the ice albedo feedback factor is 0.5. So these two, the water vapor feedback and the ice albedo feedback, are set at positive values. The cloud ready to feedback is set at a negative value. Assess the state of our current knowledge regarding the equilibrium climate sensitivity of Earth. This

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