Doktorarbeit / Dissertation, 2010
107 Seiten, Note: Sehr Gut
Geowissenschaften / Geographie - Meteorologie, Aeronomie, Klimatologie
This dissertation investigates the impact of Saharan dust on the North Atlantic Ocean, focusing on its effects on the local sea surface temperature and the larger scale circulation. The primary aim is to understand how dust-induced changes in the ocean interact with other existing dynamical features, and to determine the magnitude and extent of these impacts.
The primary keywords and focus topics of this dissertation include Saharan dust, sea surface temperature (SST), sea surface height (SSH), aerosol radiative forcing, North Atlantic circulation, Rossby waves, AMOC, meridional heat transport, and ocean modeling.
Saharan dust alters atmospheric opacity, which changes radiative forcing at the ocean surface. This affects the heat budget of the mixed layer, leading to changes in sea surface temperature (SST) and ocean circulation.
Satellite data and models show that strong dust outbreaks can lead to a decrease in SST of approximately 0.2°C to 0.5°C on sub-seasonal to interannual time-scales.
Yes, 3D simulations indicate that dust-induced buoyancy anomalies can increase or decrease meridional transport at specific latitudes, impacting the overall AMOC.
Dust-induced signals advected towards the African coast trigger westward propagating Rossby waves, which are part of the ocean's dynamical adjustment to the buoyancy source.
Including dust is crucial for accurate climate change studies, as changing dust loads in response to a changing climate can significantly influence ocean heat transport and circulation.
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