Jökull

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Jökull - 01.01.2001, Qupperneq 73

Jökull - 01.01.2001, Qupperneq 73
Observations on the cloud (dry fog) which appeared in June 1783 S. P. van Swinden Professor of Physics in the University of Franeker Originally published in Latin under the title; Observationes nebulam, quae mense Junio 1783 Apparuit, spectantes in Ephemerides Societatis Meteorologicae Palatinae, Observationes Anni 1783, Mannheim, Germany 1785 translated to English by Dr. Susan Lintleman. Nothing memorable occurred in June until the 19  day when the haze, about which we are now con- cerned, began to appear here in Franeker. This haze lasted steadily from the recorded day of the 19  un- til the 30  . It was distinguished from usual clouds by its constancy, density, and especially by very great dryness. From the 23  day, on which the haze was the strongest, onwards the hygrometer showed a very great dryness. This was the driest time of the whole month. Days 19, 20, and 21, were a little damp with sun. Neither a lightning storm on the evening of the 20  , nor a stronger wind on the 21  , dispersed the haze. From the 18  –21  the atmosphere was thor- oughly covered by haze; from 22–25 June it was half– clear, clear, or mixed with little clouds. Across the haze, the sun was perceived deep red, with brilliance at the edge; even at midday, we were able to gaze at the sun with our naked eyes without injury.1 Objects scattered further were scarcely and only unintelligi- bly perceived. These were the usual effects of this haze, but on the 24  day it brought with it as a com- panion a sulfurous odor2 very readily perceived by the senses, crawling through everything, even closed houses. Men with delicate lungs experienced that same sensation, as if they were turned towards a place in the neighborhood of burning sulfur. They were un- able to contain a cough, as soon as they were exposed to air. I myself experienced this, and many others, first in the city, then in the country. The heat was great enough. The sulfurous haze of this day brought very great loss to the vegetable realm, which I shall speak of soon more fully. And so in June we had 11 days, not only continuous, but notable for the presence of the haze. Before this year, I had never seen it for more than 3 days in this month, often none at all, and at the lowest point sometimes not at all for subsequent years, as from 1774-1783, years in which no haze appeared in June. On 3 and 9 July the genuine haze again appeared. On other days the air was foggy, or vaporous in the morning and the evening, as often happens when the days are warm. In truth I hesitate to refer this type of haze as the genuine haze, which appeared in June; but on the 12  to 20  the genuine haze, similar to that in June, was present, then in truth disappeared.3 People could gaze at the sun at midday, implying that the haze had optical depth in excess of 1.0 (e.g. Stothers, 1984). Here van Swinden must be referring to the smell of sulfuric acid, a conclusion that is supported by his own description of what effect the haze had on people (see below). In Franeker the intensity of Laki haze diminished considerably around 20 July, but as will be apparent later this is not the last date of its appearance. JÖKULL No. 50 73
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