2017
DOI: 10.5194/acp-2017-17
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Quantifying the global atmospheric power budget

Abstract: The power of atmospheric circulation is a key measure of the Earth's climate system. The mismatch between predictions and observations under a warming climate calls for a reassessment of how atmospheric power $W$ is defined, estimated and constrained. Here we review published formulations for $W$ and show how they differ when applied to a moist atmosphere. Three factors, a non-zero source/sink in the continuity equation, the difference between velocities of gaseous air and condensate, and interaction between t… Show more

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Cited by 2 publications
(2 citation statements)
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References 65 publications
(197 reference statements)
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“…Furthermore, the global integral of Eq. (8) produces an estimate of condensation-driven global circulation that likewise is in a satisfactory agreement with observations (Makarieva et al, 2013c(Makarieva et al, , b, 2017c. Since…”
Section: Ciad and Potential Energysupporting
confidence: 78%
“…Furthermore, the global integral of Eq. (8) produces an estimate of condensation-driven global circulation that likewise is in a satisfactory agreement with observations (Makarieva et al, 2013c(Makarieva et al, , b, 2017c. Since…”
Section: Ciad and Potential Energysupporting
confidence: 78%
“…• VMPI The maximum potential intensity (MPI) is positively correlated with the intensity variation, and the larger the value the greater the intensity variation. There is a correlation between MPI and TC intensity [20,33]. The MPI of a TC is determined by the storm radius at which environmental parameters such as sea-level pressure, SST, and relative humidity are present [20].…”
Section: Explainable Analysismentioning
confidence: 99%