Bill, I'd guess that it's a combination of the first major warm-core subsidence high of the spring still cut off from GoM moisture and near-surface evapo-transpiration with increased insolation. Later on, the vegetation leafs out and all the northern lakes open up. At least that's what I remember from my years growing up in New England. Similar "indian summer" setups get moisture from warm ground and vegetation, and the "January thaw" setup usually sucks up quite a bit of frozen stuff and gets less insolation.