Abstract
The cloud-base diameters of 40 cumulus clouds traversed by aircraft on 14 days of the Cooperative Convective Precipitation Experiment (CCOPE) are shown to increase with the vertical shear of the horizontal wind through cloud base. The relationshiup is stronger when only the largest clouds sampled in each of the 16 populations are considered. The relationship is strongest when the cloud diameter is normalized by the maximum achievable cloud height, as estimated by the parcel equilibrium height. Assuming a cloud diameter - height ratio of around 1, this implies that larger shear enables clouds to reach a larger fraction of their maximum possible size given the thermodynamic conditions. Alternatively, larger shear may lead to clouds with larger diameter-height ratios. The correct interpretation is probably a combination of the two. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 1480-1491 |
| Number of pages | 12 |
| Journal | Monthly Weather Review |
| Volume | 117 |
| Issue number | 7 |
| DOIs | |
| State | Published - 1989 |
| Externally published | Yes |
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