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Inadvertent climate modification due to anthropogenic lead

机译:人为铅导致的无意气候变化

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Aerosol particles can interact with water vapour in the atmosphere, facilitating the condensation of water and the formation of clouds. At temperatures below 273 K, a fraction of atmospheric particles act as sites for ice-crystal formation. Atmospheric ice crystals-which are incorporated into clouds that cover more than a third of the globe(1)-are thought to initiate most of the terrestrial precipitation(2). Before the switch to unleaded fuel last century, the atmosphere contained substantial quantities of particulate lead; whether this influenced ice-crystal formation is not clear. Here, we combine field observations of ice-crystal residues with laboratory measurements of artificial clouds, to show that anthropogenic lead-containing particles are among the most efficient ice-forming substances commonly found in the atmosphere(3). Using a global climate model, we estimate that up to 0.8 Wm(-2) more long-wave radiation is emitted when 100% of ice-forming particles contain lead, compared with when no particles contain lead. We suggest that post-industrial emissions of particulate lead may have offset a proportion of the warming attributed to greenhouse gases.
机译:气溶胶颗粒可以与大气中的水蒸气相互作用,从而促进水的冷凝和云的形成。在低于273 K的温度下,一小部分大气颗粒充当冰晶形成的场所。大气冰晶(被并入覆盖全球三分之一以上的云中(1))被认为是引发大部分陆地降水的原因(2)。在上世纪改用无铅燃料之前,大气中含有大量的微粒铅。是否影响冰晶形成尚不清楚。在这里,我们将对冰晶残留物的现场观察与对人造云的实验室测量相结合,以表明人为的含铅颗粒是大气中常见的最有效的制冰物质之一(3)。使用全球气候模型,我们估计,当100%的冰形成颗粒中含有铅时,与之相比,无颗粒中含有铅时,多发射的长波辐射最多可达0.8 Wm(-2)。我们建议工业化后排放的铅颗粒可能抵消了部分因温室气体引起的变暖。

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