Science. 1982 May 7;216(4546):628-30. doi: 10.1126/science.216.4546.628.
The surface temperature effects of the 18 May 1980 eruption of Mount St. Helens Volcano were examinedfor 1 day immediately after the eruption; 24-hour temperature differences and Model Output Statistics errors as well as the detailed temporal evolution of surface temperature at selected stations were used. During the daytime hours immediately after the eruption, the temperature was suppressed by the volcanic plume by as much as 8 degrees C. That night, low-level volcanic dust produced temperature enhancements of up to 8 degrees C. These effects quickly diminished the next day as the volcanic dust cloud dissipated and moved toward the east. The net local effect of the eruption appears to be warming, in contrast to cooling which might be expected over climatic time scales.
研究了 1980 年 5 月 18 日圣海伦斯火山喷发后 1 天内的表面温度效应;使用了喷发后 24 小时的温度差异和模型输出统计误差以及选定站点的表面温度详细时间演变。在喷发后立即的白天时段,温度被火山羽流抑制了多达 8 摄氏度。那天晚上,低层火山尘埃产生了高达 8 摄氏度的温度升高。随着火山尘云消散并向东移动,这些影响在第二天迅速消失。与气候时间尺度上可能出现的降温相比,这次喷发的净本地效应似乎是升温。