Latest discussion from PREDICT http://catalog.eol.ucar.edu/cgi-bin/predict/htmlwrap?file_url=/predict/report/weather/20100901/report.weather.201009011400.discussion.html Earl and Fiona remain embedded in regions of high precipitable water (PW) and appear to be partially interacting as the distance between them decreases (image 2). A PW loop for the last 36 h (not shown) reveals that an area of high PW values (>55 mm) was stripped away from Fiona and pulled to the northwest where it appears it could be ingested into the eastern side of the Earl circulation and possibly "turbo-charging" Earl (an "earl-y" bird special at the Café Vapor Maximus?). Our interpretation of prior GFS runs that quickly pulled Fiona north-northwestward, weakened it, and ingested it into the outer circulation of Earl is that the model mistook the convection associated with this northwestward moisture surge as a weakening and dissipating Fiona whereas in reality Fiona slowed, moved more westward, and retained its TC status. An infrared image for 1200 UTC 1 Sep shows convection around Earl and Fiona and the convection to the northwest of Fiona that was previously stripped away from Fiona (image 3). Objective satellite techniques (ADT, AMSU) estimate that the maximum surface winds in Fiona this morning to be approximately 50 kts. The broad circulation of high PW has been slightly siphoned off by Earl and the moisture and convection is being drawn into Earl may be the signature responsible for the GFS capture of Fiona as noted above. Early morning convection has subsided and cloud tops are gradually warming, with little new convection and the vorticity and divergence aloft are diagonally stacked with the strong upper level northeasterlies (image 4). Although it appeared for a while that Fiona possessed a partial eye signature in the Martinique radar, the eye appeared to open up, and was likely only a rain structure that imitated an eye (not shown) after satellite investigation. ![]() ![]() ![]() |