On the electricity of rain and snow
In connection with a theory of the electricity of thunderstorms published in the ‘Philosophical Transactions,’ measurements of the charges of rain were made in 1908, and it appeared advisable that these should be continued for a second year. 1. The removal of the Simla Meteorological Office near the end of 1908 offered a suitable site, and the hut containing the apparatus was accordingly dismantled and set up afresh in the grounds of the new building. In all essentials the arrangement of the instruments remained as described in the previous paper, but it was found after the removal and readjustment of the instruments that the electrical capacity of the rain receiver had changed from 141 cm. to 150 cm. The rain gauge was also readjusted so that each tip of the bucket now corresponded to 0·11 mm. of rain instead of 0·14, as before the alteration. The apparatus for recording the potential gradient was modified so that it could be used during fine weather for registering the normal potential gradient. This was effected by fixing a more powerful radium collector to the insulated rod passing out into the open. The new site was found to be much less frequented by spiders than the old, so that practically no difficulty was experienced from discharging of the apparatus by their webs. All the instruments worked satisfactorily throughout the rainy season and only a very few periods of rain were not successfully investigated.