罗马尼亚北部泥炭沼泽记录的1500年风成史:与西欧比较的粉尘通量和沉积控制

GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series Pub Date : 2016-01-01 DOI:10.4316/GEOREVIEW.2016.0.0.343

Andrei-Marian Panait

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引用次数: 0

摘要

尘埃是由从不同来源(干旱或半干旱地区)通过风成过程到达大气的小颗粒组成的。尘埃在气候系统中起着重要作用，因为它可以引起大气辐射特性的变化;反射或吸收太阳辐射，或间接地影响云的形成和降水模式。沙尘的输送和沉积随时间和空间的变化而变化，主要受气候特征(如降水、风速、气团运动)的控制。

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A 1500 year aeolian history as recorded in a peat bog from northern Romania: dust fluxes and deposition control in comparison with Western Europe

Dust consists of small particles that reached the atmosphere from various sources (arid or semi-arid regions) via aeolian processes. Dust plays an important role in climate systems due to the changes it can induce in the radiative properties of the atmosphere; reflecting or absorbing solar radiation, or, indirectly, by affecting cloud formation and precipitation patterns. Dust transport and deposition can vary over time and space, and it is controlled mainly by climatic characteristics (e.g., precipitation, wind speed, the movement of air masses)

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GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series

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审稿时长

6 weeks