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environment and sea ice. Recent modelling studies have highlighted the key position that dynamical upling to an ocean mannequin plays in shaping the climatic response to seaice loss. In response to imposed Arctic ice loss, ocean dynamical upling amplifies warming of the Arctic troposphere, drives patterned warming of the mid latitude and tropical oceans, and promotes increased planetarywave amplitudes. What these results imply for stormtrack responses Is sophisticated due to mpetition between lower and upper tropospheric modifications and the interplay between storm tracks and stationary waves. A new strategy of sample scaling that mbines data from greenhousewarming simulations and targeted seaice loss simulations permit us to separate the Arctic and tropical drivers of the upled response to ice loss. This separation reveals how storm tracks over the Pacific and Atlantic basins shift equatorward and customarily weaken in response to ice loss, with a level of mpetitors from tropical driving. The impact of midlatitude ocean warming in response to ice loss can be isolated. This is acmplished by extracting the midlatitude seasurface temperature response to seaice loss from atmosphereocean GCM simulations and

[Hot mariashirts] Pitbull dog summer paradise dog lover hawaiian shirt
Pitbull dog summer paradise dog lover hawaiian shirt

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