It is proposed that certain characteristic stratifications accompany cumulus and cumulonimbus, and on the basis of a thermal theory characteristic magnitudes are estimated for the properties of their updraughts, and the size which must be attained by cumulus before showers form and their transformation into cumulonimbus occurs.

Ludlam, F.H. (0AD) ‘Cumulus and cumulonimbus convection’, Tellus A: Dynamic Meteorology and Oceanography, {volume}({issue}), p. {page}. Available at: https://doi.org/10.3402/tellusa.v18i4.9689.

Ludlam, F H. “Cumulus and cumulonimbus convection”. Tellus A: Dynamic Meteorology and Oceanography, vol. {volume}, no. {issue}, 0AD, p. {page}, doi:10.3402/tellusa.v18i4.9689.

Ludlam, F. H. (0AD). Cumulus and cumulonimbus convection. Tellus A: Dynamic Meteorology and Oceanography, {volume}({issue}), {page}. https://doi.org/10.3402/tellusa.v18i4.9689

Ludlam, F. H.. 0AD. “Cumulus and Cumulonimbus Convection”. Tellus A: Dynamic Meteorology and Oceanography {volume} ({issue}): {page}. https://doi.org/10.3402/tellusa.v18i4.9689.

1. Ludlam FH. Cumulus and cumulonimbus convection. Tellus A: Dynamic Meteorology and Oceanography. 0AD;{volume}({issue}):{page}. DOI: https://doi.org/10.3402/tellusa.v18i4.9689

1. Ludlam FH. Cumulus and cumulonimbus convection. Tellus A: Dynamic Meteorology and Oceanography. 0AD;{volume}({issue}):{page}. doi:10.3402/tellusa.v18i4.9689

Ludlam FH, ‘Cumulus and Cumulonimbus Convection’ (0AD) {volume} Tellus A: Dynamic Meteorology and Oceanography {page} DOI: https://doi.org/10.3402/tellusa.v18i4.9689

[1]F. H. Ludlam, “Cumulus and cumulonimbus convection”, Tellus A: Dynamic Meteorology and Oceanography, vol. {volume}, no. {issue}, p. {page}, 0AD, doi: 10.3402/tellusa.v18i4.9689.

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Original Research Papers

Cumulus and cumulonimbus convection

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