## Abstract 1933 was warm, dry and sunny to an exceptional degree. Warmth was +2Β°F., rain 87 per cent, and sunshine 109 per cent for the 12βmonth period December to November. This was due chiefly to conditions in the summer, and therefore phenologically most effective, half year. Scotland, N. and E
Report on the phenological observations in the British Isles from December, 1931, to November, 1932. no. 42
β Scribed by J. Edmund Clark; Ivan D. Margary; C. J. P. Cave
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 205 KB
- Volume
- 60
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
The Report is again based on over 15,000 individual events, although Tables VII (Tree Records) and XIV (Hevingham Records) are wanting. But we have the cheering news that the latter, going back to 1736, will reappear with the records for 1932 and 1933, thanks to the Rev. A. F. Marsham, a son of Major H. L. Marsham.
Exceptional warmth again prevailed until February, which was also excessively dry. But the year was most notable for its wetness and dullness, above all, April, May and July. These gave half as much rain again as usual and only three quarters of the sunshine average. June and early autumn largely saved the situation for field and garden crops and gave a fine floral display from August on.
Table V shows lateness in plant events after April to early July, of ten days or more in England and Wales, but a bare week for the British Isles as a whole, since Scotland and Ireland fared much better. Worst were England SE, SW and Midlands. The Floral Isakairs (equal divergences from the average) show this well, with areas in the former over a fortnight late for all plants against ten days early in the latter.
Scarcity and lateness of the three butterflies in Tables IX and X were the response to the wet cold of late April and May. The same cause accounted for no bird in the main migrant table being early. Owing presumably to food shortage, the seven insectβfeeders up to May 9 averaged four days later than the other eight birds in the same period. The Spring migrant isophenes (equal appearance dates) lay much further south than usual, the reverse occurring in autumn, when the genial weather favoured lingering.
The additional notes received from many proved, as usual, of great value and form an important part of the letterpress. The names and stations of all our observers appear this year in Table II.
Tables III and V present the dates of the separate plants in each of the II Districts, with averages for England and Wales and for the British Isles, also corresponding averages for 35 years, which are confirmed after 40 pears. In an appendix are now tabulated the results decade by decade, with comparisons and ranges. Table A shows plant events by Districts, B and C by flowers, respectively, for England and Wales and for the British Isles. These tables summarise a presentation of our results from an aspect not previously attempted.
π SIMILAR VOLUMES
## Abstract 1931 was officially described as βwet and dull,β the emphasis is on the latter; yet it was the tenth successive year with excess of rain, the total being that of eleven average years. A new table gives for each of the thirteen districts the number of weeks showing βdecidedβ and βexcessi
## Abstract The year was remarkable for sunlessness generally, and also for wetness in England and Wales, b u t temperature after a cool winter remained close to normal. The result was a rather gloomy and inclement year due to lack of sunshine and excess of rain rather than to low temperature. Plan
## Abstract New organisation for phenologicalβecological research. Modifications in analysis and presentation of results; comparison of past and new methods; plants and insects. Explanatory: arrangement of tables, appendices and diagrams. New diagrams showing phenological events and meteorological
## Abstract Development of organisation. Meetings of the Main Conference and Executive Committee; steps taken. Presentation of records. The weather of 1938 and its effects. Explanation of diagrams. Conclusions; general principles. Evidence with reference to a dominant factor in relation to the resp