1 / 6

(a)

(a). t 0 − 48 h. L. 1500 km. 1500 km. (b). t 0. L. AWB. 1500 km. 1500 km. Key. upper -tropospheric jet anticyclonic wave breaking PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind. precipitable water 500-hPa ascent. AWB. (a). t 0 − 96 h.

clovis
Download Presentation

(a)

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. (a) t0 − 48 h L 1500 km 1500 km (b) t0 L AWB 1500 km 1500 km Key upper-tropospheric jet anticyclonic wave breaking PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind precipitable water 500-hPa ascent AWB

  2. (a) t0 − 96 h L 1500 km 1500 km (b) t0 − 48 h L AWB 1500 km 1500 km (c) Key t0 upper-tropospheric jet anticyclonic wave breaking PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind precipitable water 500-hPa ascent AWB AWB 1500 km 1500 km

  3. (a) t0 − 96 h L AWB 1500 km 1500 km (b) t0 − 48 h L AWB L 1500 km 1500 km (c) Key t0 upper-tropospheric jet anticyclonic wave breaking PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind precipitable water 500-hPa ascent L AWB 1500 km 1500 km

  4. (a) t0 − 96 h H 1500 km 1500 km (b) t0 − 48 h H 1500 km 1500 km (c) Key t0 upper-tropospheric jet PV filament PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind upper-tropospheric subtropical anticyclone precipitable water 500-hPa ascent H 1500 km 1500 km H

  5. (a) t0 − 96 h H 1500 km 1500 km (b) t0 − 48 h H 1500 km 1500 km (c) Key t0 upper-tropospheric jet PV debris PV contour on the 350 K isentropic surface 300–200-hPa layer-averaged irrotational wind upper-tropospheric subtropical anticyclone precipitable water 500-hPa ascent H 1500 km 1500 km H

  6. (a) Strong TTN = 34 14.71% 2.94% 20.59% (5) (1) (7) 5.88% (2) 17.65% (6) 38.24% (13) 1.79% (1) (b) Weak TTN = 56 10.71% 16.07% (6) (9) 7.14% (4) 33.93% (19) 30.36% (17) 6.67% (1) (c) Trough induced N = 15 20.00% (3) 73.33% (11) Midlatitude Trough Cutoff PV Streamer Subtropical Disturbance PV Debris Unclassifiable

More Related