Theoretical investigations on potential impacts of high-latitude volcanic emissions of heat, aerosols and water vapor and their interactions with clouds and precipitation.

M. B. Yarker, D. Paimazumder, C. Cahill, Jonathan Dehn, A. Prakash, N. Mölders
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引用次数: 12

Abstract

Augustine Volcano (located in the Cook Inlet of South Central Alaska at 59.4 o N and 153.4 o W) erupted in January 2006 and released, among other things, water vapor, radiation heat, and aerosols into the atmosphere. To determine the potential impact of volcanic emissions and ashfall on local weather, 16 simulations assuming artificial emission and ashfall scenarios were performed with the Weather Research and Forecasting model for 24 consecutive days starting the day before the first eruption. These simulations include (1) the control simulation without consideration of any volcanic perturbation, (2) four simulations with simplified scenarios for each individual volcanic factor (radiative heat from the caldera, water vapor, cloud condensation nuclei (CCN) and/or ice nuclei (IN) aerosols, and albedo change due to ashfall), and (3) 11 simulations containing all possible combinations of these factors. These 11 simulations serve to examine interactions among impacts of the different perturbations under the assumed scenarios. The impact of volcanic factors on local weather depends on the synoptic situation, emission strength, (combination of) volcanic factors, and interaction among impacts of factors if they occur concurrently. ANalysis Of VAriance shows that the greatest (statistically significant at the 95% or higher confidence level) volcanic impact occurs on relatively humid days and immediately downwind of the volcano (<50 km). Depending on relative humidity and temperature conditions, volcanic heat release can increase condensation and/or cloud top levels or reduce cloudiness. Due to non-linear cloud microphysical processes, meteorological responses to volcanic factors can diminish or enhance the impacts of the individual factors when factors occur concurrently. As an example, depending on the ambient conditions, concurrently occurring volcanic factors can lead to a decrease in precipitation at one time and an increase at another time. These findings indicate that in the immediate vicinity of erupting volcanoes, predicted cloud conditions and precipitation may be inaccurate due to the unknown volcanic forcing.
高纬度火山释放热量、气溶胶和水蒸气的潜在影响及其与云和降水的相互作用的理论研究。
奥古斯丁火山(位于阿拉斯加中南部的库克湾,北纬59.4度,西经153.4度)于2006年1月喷发,释放出水蒸气、辐射热和气溶胶等物质。为了确定火山排放和火山灰对当地天气的潜在影响,从第一次喷发前一天开始,使用天气研究与预报模型连续24天进行了16次人工排放和火山灰情景模拟。这些模拟包括(1)不考虑任何火山扰动的控制模拟,(2)对每个单独的火山因子(来自火山口的辐射热、水蒸气、云凝结核(CCN)和/或冰核(IN)气溶胶以及由火山灰引起的反照率变化)简化情景的4个模拟,以及(3)包含这些因子所有可能组合的11个模拟。这11个模拟用于检验在假设情景下不同扰动影响之间的相互作用。火山因子对当地天气的影响取决于天气情况、喷发强度、火山因子(组合)以及同时发生时各因子影响之间的相互作用。方差分析表明,火山影响最大(95%或更高置信水平的统计显著性)发生在相对潮湿的日子和火山的直接下风(<50公里)。根据相对湿度和温度条件,火山释放的热量可以增加凝结和/或云顶水平或减少云量。由于云微物理过程的非线性,当各因素同时发生时,对火山因素的气象响应可以减弱或增强个别因素的影响。例如,根据环境条件的不同,同时发生的火山因素可能导致降水在一个时间减少,在另一个时间增加。这些发现表明,在火山喷发附近,由于未知的火山强迫,预测的云条件和降水可能不准确。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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