Eventually, a high -
pressure ridge moved from the North Atlantic into the United States, shutting down rainfall and setting the stage for a heat wave to emerge.
Not exact matches
Tradewind flow over the basin remains lighter than normal as low
pressure systems
moving eastward from the United States cause the
ridge to the north to weaken.
«Normal» low
pressure systems meeting a high
pressure ridge simply stall out and remain in that area either until they dissipate or the high
pressures moves!!!! What a hoot!