21 October Start/Stop Times

 

Flight 1

 

Start                Stop                Maneuver

16:19:48         16:24:43         Towards A’; Descent 12K’ to 5K’

16:24:43         16:27:19         Near A; Descent 5K’ to 3.5K’ (End of 1st file)

16:38:14         16:47:34         Near A towards B’; 500’ (2nd file)

16:47:34         17:05:59         B’ to C; 500’

17:06:31         17:27:17         C to E; 500’

17:28:33         17:49:35         E to C; 1.5K’

17:50:41         18:15:38         C to E; 1K’

18:16:42         18:42:33         E to C; Porpoise 300’ to 2K’

18:42:33         18:46:10         C; Ascent to 7K’

18:46:10         18:54:28         C; Descent to 1.5K’

18:54:28         19:03:59         C towards G; Porpoise 300’ to 2K’

19:05:18         19:14:32         G’ to C; 500’

19:15:00         19:38:44         C to D’; 500’

 

Flight 2

 

Start                Stop                Maneuver

22:15:45         22:35:33         D’ to C; Porpoise 300’ to 2K’

22:36:23         22:58:36         C to E’; 500’

23:00:09         23:23:39         E’ to C; 1.5K’

23:24:34         23:49:27         C to E’, 1K’

23:50:44         00:14:47         E’ to C, Porpoise 300’ to 2K’

00:14:47         00:19:05         C; Ascent to 7K’

00:19:05         00:24:34         C; Descent 7K’ to 3K’

00:24:34         00:33:37         C towards G; Porpoise 300’ to 3K’

00:34:51         00:39:56         G’ to C; 500’

00:40:41         01:11:21         C to B’; Porpoise 300’ to 2K’

01:11:21         01:15:35         B’ to A, Ascent

 

Initial Impressions: This pair of flights sampled the terrain effects off Cape Fairweather as an elongated trough associated with a landfalling low approached the northeastern GOA.  It bears some resemblance to the case of 12 October in that it appears that the aircraft observations were collected in the vicinity of a hybrid-type barrier jet.  In general, the low-level winds were from the east at about 15 knots near C, from the ESE at 25-35 knots farther offshore, and then were less from the east and weaker near E.  The windshift near the southwestern end of the C-E flight stack was on the order of 30-50 degrees and 15 knots on the first flight, and about 50 degrees and 20 knots on the second flight.  These transitions tended to be very abrupt, especially during the second flight.  At first glance, it does not appear that the abruptness of this windshift is associated with a landfalling front per se, but rather the interaction of the synoptic system with the terrain-induced perturbation near the coast.  As in other cases of this ilk, relatively cold and dry air was emanating out of Cross Sound and swept up into the enhanced flow just offshore of the Fairweathers.