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convection and circulation to the hydrologic cycle and Arctic river runoff, to sea-ice formation and freshwater transport, and to the thermohaline circulation. Such relationships need to be more thoroughly investigated. The NAO and PNA circulation features, which occur predominantly over the ocean basins, are connected with distinct changes in ocean temperature and circulation. They may indicate the existence of a coupled interaction between thAmazing dragon purple all over print stainless steel tumblere atmosphere and ocean that is crucial to understanding and predicting dec-cen variability. frequency variability, which has been emphasized through annual averaging and time filtering. The cause of these low-frequency fluctuations is still debatable. Of course, higher-frequency fluctuations exist as well. These fluctuations are due to the internal variability of the climate system, and are governed by, among other things, the atmospheric circulation’s response to forcing and to changing boundary conditions. derive from numerical models. Without better observations and improved model representations, we cannot properly evaluate how the ocean’ s storage capacities, uptake rates, and uptake efficiencies will change as climate changes. The sun’s radiation, volcanic

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