相关实验视频
Updated: Jun 22, 2026

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Flow Cytometric Analysis of Particle-bound Bet v 1 Allergen in PM10
Published on: November 19, 2016
概括
一层平流层的尘埃和气溶层,可能来自危地马拉火山喷发,在1974年11月在美国西南部造成了不寻常的天空颜色. 这种现象是通过白天的天空和黄昏的光观察到的.
科学领域:
- 大气科学 大气科学
- 火山学 火山学是一门学科.
- 遥感 遥感 遥感 遥感
背景情况:
- 1974年11月中旬,在巴哈加利福尼亚州和亚利桑那州南部观测到不寻常的大气光学现象,包括蓝色的白天天空和彩色的黄昏光,在巴哈加利福尼亚州和亚利桑那州南部观测到.
- 这些视觉线索通常与重大火山爆发有关,这些火山喷发将物质注入平流层.
研究的目的:
- 研究1974年11月在美国西南部观测到的尘埃和气溶层的起源和性质.
- 为了确定导致观察到的光学现象的大气颗粒物的来源.
主要方法:
- 对白天天空和黄昏光的视觉观测进行分析.
- 利用红外卫星观测来追踪大气现象.
- 与其他观察报告进行交叉引用以排除潜在来源.
主要成果:
- 在海拔20公里处发现了一层明显的尘埃和气溶.
- 通过卫星和其他数据,被排除了颗粒物的海洋起源.
- 观察到的现象与火山喷发的时间和地点有很强的相关性.
结论:
- 1974年11月在巴哈加利福尼亚州和亚利桑那州南部的尘埃和气溶层可能是1974年10月危地马拉火山喷发的结果.
- 火山气溶可以在很大的地理区域显著影响大气光学.
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