the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evidence of tropospheric uplift into the stratosphere via the tropical western Pacific cold trap
Xiaoyu Sun
Katrin Müller
Mathias Palm
Christoph Ritter
Denghui Ji
Tim Balthasar Röpke
Justus Notholt
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Saharan dust can reach the high Arctic within only a few days, but it was unclear whether such rapid transport occurs regularly. Using atmospheric models, satellite observations, and 21 years of air-mass trajectories, we identify a recurrent pathway across the North Atlantic. This pathway becomes increasingly important at higher Arctic latitudes and efficiently carries large dust particles northward, with potential consequences for Arctic clouds and climate.
Saharan dust can reach the high Arctic within only a few days, but it was unclear whether such rapid transport occurs regularly. Using atmospheric models, satellite observations, and 21 years of air-mass trajectories, we identify a recurrent pathway across the North Atlantic. This pathway becomes increasingly important at higher Arctic latitudes and efficiently carries large dust particles northward, with potential consequences for Arctic clouds and climate.