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72![Convective Boundary Layer
be spun up (i.e., its turbulence intensity must increase from near zero to the current ML value) as entrainment incorporates it into the ML. Over a land surface experiencing a strong diurnal c Convective Boundary Layer
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73![JOURN^L OF G•.OPH¾SIC^r•R•.SE^RCH VOt,UM•. 66, No. 1 J^NU^R¾ 1961 JOURN^L OF G•.OPH¾SIC^r•R•.SE^RCH VOt,UM•. 66, No. 1 J^NU^R¾ 1961](https://www.pdfsearch.io/img/ac2874421611811135bd2ed9e2987b3a.jpg) | Add to Reading ListSource URL: climate-dynamics.orgLanguage: English - Date: 2015-09-11 20:36:55
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75![1960ApJ442S
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77![Presentation of “Available Potential Energy and the Maintenance of the General Circulation” (E. LorenzBy Julian Westermeier Atmospheric General Circulation Dynamics – Tapio Schneider Presentation of “Available Potential Energy and the Maintenance of the General Circulation” (E. LorenzBy Julian Westermeier Atmospheric General Circulation Dynamics – Tapio Schneider](https://www.pdfsearch.io/img/408fc76b561988a488359572495d0f71.jpg) | Add to Reading ListSource URL: climate-dynamics.orgLanguage: English - Date: 2016-05-18 15:30:34
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78![](https://www.pdfsearch.io/img/b855678ed34aba0a300db9bb48d4285e.jpg) | Add to Reading ListSource URL: climate-dynamics.org- Date: 2015-09-11 20:37:00
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