The broad surface low centered in the Eastern Gulf (which may never become tropical) has really been pumping out the moisture/convection in the direction of the northern extension of the tropical wave along 95W in the Bay of Campeche (f/k/a 92L). The barely detectable cyclonic feature once associated with 92L appears to be currently centered near 94W, 24N. As best I have been able to observe, the center of that feature slowed and curved a little more northward over the past day or two, since it left the Yucatan, and did not cross into Northern Mexico. In other words . . . I think there is still something there. So my question is: Could some of the moisture in the Gulf coming from the North and East wrap into former 92L and regenerate it?