the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Tropospheric low ozone and its diurnal cycle over the Western Pacific warm pool from solar absorption FTIR observations
Xiaoyu Sun
Mathias Palm
Katrin Müller
Denghui Ji
Sharon Patris
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.