cheezyWXguy wrote:Ntxw wrote:One good lesson learned this early season is that hot SSTs do not necessarily translate to big activity. This is actively being shown in the Atlantic and EPAC of reverse effect. EPAC is generating ACE with normal to below normal SSTA (Dora) while Atlantic is dealing with dry air and unfavorable winds, regardless of SST. It's the atmosphere that really is the determining player.
Suspect activity may pick up in the Atlantic once the hemispheric pattern cools and breaks down the stagnant trough-ridge pattern in the mid latitudes.
Isn’t the premise behind an active season despite an El Niño that warmer than normal ssts would lead to more rising air to counter the suppression caused by El Niño?
That can be a premise, and likely has played a role in muting some of the atmospheric response of ENSO CPAC not coupling, but one question is, much of the oceans is also experiencing this rise in heat, not just the Atlantic, so can one weigh more than the other? To what effect? I don't think we really understand it yet. I think in an island, the tipping balance might occur, but what happens when the weights are on all sides?
The real global budget lies in equatorial Africa to Indian Ocean and western Pacific and it hasn't pulled the forcing back to the MC, rather gradually moving east out into the Pacific.
