The nucleation of the uncontaminated atmosphere . of discrepancies the nucleationappears to show the effect of conflicting causes. On November 29,with no sun, the nucleation persists from the fairly high reading ofthe day before, although the other curves drop. Warm rain andfurther increase of vapor pressure on the 30th cut it down, and itascends very slowly during the cloudy days following. A decreaseaccompanies the rise in temperature and vapor pressure of December5, which is quickly reversed by the sunshine and northwest wind ofthe 6th. The nucleation curve remains nearly level, as does tha
The nucleation of the uncontaminated atmosphere . of discrepancies the nucleationappears to show the effect of conflicting causes. On November 29,with no sun, the nucleation persists from the fairly high reading ofthe day before, although the other curves drop. Warm rain andfurther increase of vapor pressure on the 30th cut it down, and itascends very slowly during the cloudy days following. A decreaseaccompanies the rise in temperature and vapor pressure of December5, which is quickly reversed by the sunshine and northwest wind ofthe 6th. The nucleation curve remains nearly level, as does that ofthe water vapor, during the two cloudy days succeeding. The sun- 104 NUCLEATION OF THE UNCONTAMINATED ATMOSPHERE. shine of the 9th and nth gives maxima which themselves rise withthe moisture and temperature curves, while all drop on the 12th. Therise on December 13 seems to accompany the sudden fall in tempera- W| 1 1 1 1 1 1 1 1 1 1 r- 20- ti 0 ti .0 $0 «. ^ jt % k x>, 0 0 xx, p xx ?*- i 5- J»,5„«i, !i-l4\ Upr^M \A [_VO I >—.
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Keywords: ., bookcentury1900, bookdecade1900, bookpublisherwashi, bookyear1906
