On 12 August 2009, a series of satellite images revealed asymmetric shedding of atmospheric vortices in the lee of Mt. Snæfellsjökull, and their passage a distance of 120km across Faxaflói Bay and over the city of Reykjavík in West Iceland. After landfall, the vortices were detected by a network of surface weather stations. These observations are presented and with the aid of a numerical simulation, they are discussed in view of existing theories of orographic wakes and vortex shedding. In general, the flow is in line with existing knowledge, but there is a remarkable absence of vortices with anticyclonic rotation. Atmospheric conditions for vortices of this kind are most often favorable in late winter and spring and they are a forecasting challenge.
CITATION STYLE
Ágústsson, H., & Ólafsson, H. (2014). The advection of mesoscale atmospheric vortices over Reykjavík. Monthly Weather Review, 142(10), 3549–3559. https://doi.org/10.1175/MWR-D-13-00060.1
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