Convection over the Arctic polynya
by Mikhail Varentsov, Lomonosov Moscow State University, Moscow, Russia
Aerial photo of the polynya in the White sea of the Arctic ocean, formed due tidal currents, which remains unfreezing even in the strongest frosts. In a such frosty weather the beautiful convective boundary layer is developed over the warm water.
Taken on 3
Submitted on 15 February 2018
Credit: Mikhail Varentsov (distributed via imaggeo.egu.eu)
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