TABLE XII.--_Diurnal Variation of Thunderstorms._

+--------------------+-----+-----+-----+-----+-----+------+------+------+------+------+------+-------+

| Hour. | 0-2.| 2-4.| 4-6.| 6-8.|8-10.|10-12.|0'-2'.|2'-4'.|4'-6'.|6'-8'.|8'-10'|10'-12'|

+--------------------+-----+-----+-----+-----+-----+------+------+------+------+------+------+-------+

| Finland (76) | 2.3 | 2.0 | 2.2 | 3.0 | 4.6 | 12.1 | 18.9 | 19.2 | 16.1 | 10.1 | 6.1 | 3.4 |

| Edinburgh (64) | 1.7 | 2.0 | 1.4 | 1.7 | 4.7 | 14.2 | 22.4 | 23.7 | 11.9 | 9.2 | 5.1 | 2.0 |

| Belgium (77) | 3.0 | 2.9 | 1.7 | 1.8 | 2.0 | 6.4 | 12.9 | 21.6 | 19.4 | 15.8 | 8.4 | 4.1 |

| Brocken (78) | 1.6 | 2.5 | 1.3 | 1.3 | 4.2 | 3.1 | 12.1 | 28.6 | 22.4 | 10.1 | 7.2 | 5.6 |

| Switzerland (72) | 3.1 | 2.3 | 2.1 | 1.6 | 2.0 | 7.3 | 13.8 | 20.9 | 20.8 | 14.6 | 8.0 | 3.5 |

| Italy (77) | 1.3 | 1.6 | 1.4 | 2.0 | 3.0 | 8.5 | 19.5 | 26.5 | 16.6 | 9.8 | 8.3 | 1.5 |

| Hungary (i.) (67) | 2.1 | 1.9 | 1.9 | 2.1 | 2.9 | 11.5 | 18.1 | 22.0 | 17.9 | 10.7 | 6.2 | 2.8 |

| " (ii.) (67) | 6.9 | 4.2 | 2.3 | 2.0 | 2.0 | 5.0 | 9.9 | 16.9 | 18.2 | 10.7 | 11.7 | 10.0 |

| " (iii.) (75)| 2.3 | 1.9 | 2.0 | 2.4 | 2.7 | 7.9 | 16.1 | 22.1 | 19.1 | 12.7 | 7.6 | 3.2 |

| " (iv.) (75) | 2.6 | 2.2 | 1.9 | 1.9 | 3.6 | 13.3 | 19.9 | 20.7 | 15.2 | 9.2 | 6.2 | 3.3 |

| Trevandrum (74) | 5.6 | 4.9 | 4.3 | 1.3 | 1.4 | 2.0 | 13.3 | 24.5 | 15.9 | 13.3 | 7.6 | 5.9 |

| Agustia (74) | 2.9 | 2.9 | 0.3 | 0.0 | 1.7 | 2.9 | 15.1 | 36.1 | 22.2 | 9.3 | 4.6 | 2.0 |

+--------------------+-----+-----+-----+-----+-----+------+------+------+------+------+------+-------+

32. _Daily Variation._--The figures in Table XII. are again

percentages. They are mostly based on data as to the hour of

commencement of thunderstorms. Data as to the hour when storms are

most severe would throw the maximum later in the day. This is

illustrated by the first two sets of figures for Hungary (67). The

first set relate as usual to the hour of commencement, the second to

the hours of occurrence of lightning causing fires. Of the two other

sets of figures for Hungary (75), (iii.) relates to the central plain,

(iv.) to the mountainous regions to north and south of this. The hour

of maximum is earlier for the mountains, thunder being more frequent

there than in the plains between 8 A.M. and 4 P.M., but less frequent

between 2 and 10 P.M. Trevandrum (8 deg. 31' N., 76 deg. 59' E., 195

ft. above sea-level) and Agustia (8 deg. 37' N., 77 deg. 20' E., 6200

ft. above sea-level) afford a contrast between low ground and high

ground in India. In this instance there seems little difference in the

hour of maximum, the distinguishing feature being the great

concentration of thunderstorm occurrence at Agustia between noon and 6

P.M.

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