Sentences with phrase «different ocean physics»

And each of these regimes leads to very different ocean (and ice) flux as a result of very different ocean physics.

Not exact matches

It may sound a bit nitpicking, but water sloshing in a bathtub is a gravity wave, water height in the ocean varying on decadal or longer scales must be totally different physics.
Setting aside the effects of the deep ocean, etc, — ie just using a single unified reservoir's heat capacity — and using only fast feedbacks (I didn't introduce any slow feedbacks anywhere in this particular series of comments), the expectation based on physics is that each delayed response T curve (each of which must correspond to a different value of heat capacity, for the same ECS) must have a maximum or minimum when it intersects the instantaneous response curve (my Teq value)-- maximum if it was below Teq before, minimum if it was above — because it is always going toward Teq.
The weakening of the Walker circulation arises in these models from processes that are fundamentally different from those of El Nià ± o — and is present in both mixed - layer and full - ocean coupled models, so is not dependent on the models» ability to represent Kelvin waves (by the way, most of the IPCC - AR4 models have sufficient oceanic resolution to represent Kelvin waves and the physics behind them is quite simple — so of all the model deficiencies to focus on this one seems a little odd).
The physics of warming water already in the oceas, land ice melt, and transfers between ocean and land will play different roles - they are not expected to contribute in the same proportions as the planet warms.
My post on the cool - skin layer of the ocean hyper - links to 3 different papers on the topic, and those three papers cites numerous others in support of the physics, math, and observations involved.
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