Ml. Clapp et al., INFRARED-SPECTROSCOPY OF SULFURIC-ACID WATER AEROSOLS - FREEZING CHARACTERISTICS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D7), 1997, pp. 8899-8907
A low-temperature flow cell has been used in conjunction with a Fourie
r transform infrared (FT-IR) spectrometer to study sulfuric acid/water
aerosols. The aerosols were generated with a wide range of compositio
n (28 to 85 wt %), including those characteristic of stratospheric sul
fate aerosols, and studied over the temperature range from 240 K to 16
0 K. The particles exhibited deep supercooling, by as much as 100 K be
low the freezing point in some cases. Freezing of water ice was observ
ed in the more dilute (<40 wt % sulfuric acid) particles, in agreement
with the predictions of Jensen et al. and recent observations by Bert
ram et al. In contrast with theoretical predictions, however, the enti
re particle often does not immediately freeze, at least on the timesca
le of the present experiments (seconds to minutes). Freezing of the en
tire particle is observed at lower temperatures, well below that chara
cteristic of the polar stratosphere.