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Atmospheric temperature changes by volcanic eruptions: GPS radio occultation observations in the 2010 Icelandic and 2011 Chilean cases

机译:火山喷发引起的大气温度变化:2010年冰岛和2011年智利案例中的GPS无线电掩星观测

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摘要

Volcanic plumes modify atmospheric temperatures. Wang et al. (2009) reported localized temperature changes associated with the Mt Chaiten eruption in May 2008 using the deviation of GPS radio occultation temperature data from the NCEP global forecast system model. On 14 April 2010, a large scale eruption started under the glacier Eyjafjallajökull in Southern Iceland, and Puyehue-Cordón Caulle (Puyehue), in Chile, started eruption on 4 June, 2011. Here we study instantaneous and localized temperature changes with these two eruptions following the method of Wang et al. (2009). Post-eruption negative temperature anomalies at the 250 hPa plane were clearly observed in the Eyjafjallajökull eruption. In the Puyehue eruption, however, such anomalies were not so clear due possibly to insufficient accuracy of the forecast model. By comparing the temperature profiles in the downwind areas of the two eruptions, we found that significant temperature decreases occurred at ~ 10.5 and ~ 11.5 km altitude in the Eyjafjallajökull and the Puyehue cases, respectively. These results generally agree with Wang et al. (2009), but post-eruption temperature changes seem to be influenced by additional factors, e.g. volcanic explosivity and local climatology.
机译:火山羽改变大气温度。 Wang等。 (2009年)报道了使用GPS无线电掩星温度数据与NCEP全球预报系统模型的偏差,于2008年5月与柴滕山喷发相关的局部温度变化。 2010年4月14日,冰岛南部的Eyjafjallajökull冰川下开始大规模喷发,而智利的Puyehue-CordónCaulle(Puyehue)于2011年6月4日开始喷发。在这里,我们研究了这两次喷发的瞬时和局部温度变化。按照王等人的方法。 (2009)。 Eyjafjallajökull火山喷发清楚地观察到了喷发后250 hPa平面的负温度异常。但是,在Puyehue喷发中,由于预报模型的准确性不足,因此此类异常不太明显。通过比较两次喷发顺风区域的温度分布,我们发现在Eyjafjallajökull和Puyehue案例中,分别在〜10.5和〜11.5 km高度处出现了明显的温度下降。这些结果大体上与Wang等人一致。 (2009年),但喷发后的温度变化似乎受到其他因素的影响,例如火山爆发性和当地气候。

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