When and where do Radiative–Convective and Radiative–Advective Equilibrium regimes occur on modern Earth?
Energy balance and lapse rate regimes qualitatively characterize the low, mid, and high latitudes of Earth’s modern climate. Currently we do not have a complete quantitative understanding of the spatio-temporal structure of energy balance regimes (e.g., Radiative Convective Equilibrium or RCE, and R...
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| Format: | Text |
| Language: | English |
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Unknown
2021
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| Online Access: | https://dx.doi.org/10.6082/uchicago.2925 https://knowledge.uchicago.edu/record/2925 |