| Date Time MST |
Temp °F |
RH % |
DewPt °F |
Wind mph |
Dir ° |
Gust mph |
Dir ° |
Press in Hg |
Solar W/m^2 |
Prec in |
|---|---|---|---|---|---|---|---|---|---|---|
| 2019-08-19 01:25 | 55.5 | 59.9 | 41.8 | 8.9 | 342 | 10.8 | 342 | 24.877 | 0.0 | 0.00 |
| 2019-08-19 01:20 | 56.8 | 67.8 | 46.3 | 8.6 | 348 | 9.5 | 350 | 24.877 | 0.0 | 0.00 |
| 2019-08-19 01:15 | 58.2 | 67.0 | 47.3 | 6.8 | 348 | 8.8 | 349 | 24.875 | 0.0 | 0.00 |
| 2019-08-19 01:10 | 57.5 | 68.2 | 47.1 | 5.3 | 334 | 5.7 | 325 | 24.873 | 0.0 | 0.00 |
| 2019-08-19 01:05 | 58.0 | 67.6 | 47.4 | 5.1 | 329 | 5.8 | 325 | 24.871 | 0.0 | 0.00 |
| 2019-08-19 01:00 | 58.5 | 67.3 | 47.8 | 4.4 | 301 | 5.6 | 314 | 24.871 | 0.0 | 0.00 |
| 2019-08-19 00:55 | 57.7 | 66.8 | 46.8 | 5.8 | 320 | 6.6 | 341 | 24.870 | 0.0 | 0.00 |
| 2019-08-19 00:50 | 55.8 | 72.6 | 47.1 | 5.4 | 340 | 6.6 | 338 | 24.871 | 0.0 | 0.00 |
| 2019-08-19 00:45 | 56.2 | 79.1 | 49.8 | 3.5 | 327 | 4.8 | 331 | 24.873 | 0.0 | 0.00 |
| 2019-08-19 00:40 | 58.1 | 72.3 | 49.2 | 3.0 | 340 | 3.7 | 331 | 24.873 | 0.1 | 0.00 |
| 2019-08-19 00:35 | 59.2 | 70.7 | 49.7 | 2.8 | 351 | 3.6 | 324 | 24.873 | 0.0 | 0.00 |
| 2019-08-19 00:30 | 59.7 | 68.4 | 49.3 | 3.4 | 324 | 4.1 | 311 | 24.872 | 0.1 | 0.00 |
| 2019-08-19 00:25 | 58.9 | 70.2 | 49.2 | 4.0 | 305 | 4.7 | 304 | 24.872 | 0.1 | 0.00 |
| 2019-08-19 00:20 | 57.7 | 71.7 | 48.6 | 4.1 | 322 | 5.1 | 329 | 24.872 | 0.1 | 0.00 |
| 2019-08-19 00:15 | 57.2 | 74.2 | 49.1 | 2.6 | 316 | 3.8 | 328 | 24.872 | 0.1 | 0.00 |
| 2019-08-19 00:10 | 57.3 | 75.5 | 49.7 | 2.6 | 322 | 3.7 | 285 | 24.872 | 0.2 | 0.00 |
| 2019-08-19 00:05 | 58.4 | 74.3 | 50.2 | 3.8 | 292 | 4.4 | 291 | 24.872 | 0.0 | 0.00 |
| 2019-08-19 00:00 | 60.3 | 67.8 | 49.6 | 3.8 | 327 | 4.8 | 342 | 24.872 | 0.0 | 0.00 |
| 2019-08-18 23:55 | 60.6 | 67.8 | 49.9 | 3.4 | 342 | 4.3 | 346 | 24.870 | 0.1 | 0.00 |
| 2019-08-18 23:50 | 59.1 | 71.6 | 50.0 | 2.8 | 357 | 4.0 | 21 | 24.870 | 0.0 | 0.00 |
| 2019-08-18 23:45 | 59.1 | 75.5 | 51.3 | 3.6 | 21 | 4.2 | 21 | 24.870 | 0.0 | 0.00 |
| 2019-08-18 23:40 | 59.6 | 77.7 | 52.6 | 4.3 | 14 | 5.1 | 16 | 24.872 | 0.0 | 0.00 |
| 2019-08-18 23:35 | 61.4 | 75.7 | 53.7 | 1.9 | 28 | 4.6 | 28 | 24.872 | 0.0 | 0.00 |
| 2019-08-18 23:30 | 60.4 | 78.8 | 53.8 | 0.7 | 275 | 1.7 | 275 | 24.872 | 0.1 | 0.00 |
| 2019-08-18 23:25 | 61.0 | 73.9 | 52.6 | 1.6 | 287 | 2.0 | 293 | 24.872 | 0.1 | 0.00 |
| 2019-08-18 23:20 | 61.2 | 74.3 | 52.9 | 1.8 | 293 | 2.1 | 315 | 24.873 | 0.1 | 0.00 |
| 2019-08-18 23:15 | 60.5 | 79.3 | 54.1 | 0.8 | 308 | 1.8 | 308 | 24.876 | 0.1 | 0.00 |
| 2019-08-18 23:10 | 61.0 | 78.9 | 54.4 | 0.9 | 328 | 1.7 | 343 | 24.875 | 0.1 | 0.00 |
| 2019-08-18 23:05 | 61.2 | 79.1 | 54.6 | 0.1 | 325 | 0.6 | 320 | 24.875 | 0.2 | 0.00 |
| 2019-08-18 23:00 | 61.2 | 79.3 | 54.8 | 0.2 | 320 | 1.1 | 340 | 24.876 | 0.1 | 0.00 |
Forecasting the timing and magnitude of tropical cyclone rapid intensification (RI) remains an ongoing forecasting problem. Although the ability of deterministic tropical cyclone intensity models to forecast such events has improved, their skill remains inadequate. Thus, forecasters have relied on other tools such as the SHIPS suite of probabilistic statistical rapid intensity models to aid… Read more »
Forecasting the timing and magnitude of tropical cyclone rapid intensification (RI) remains an ongoing forecasting problem. Although the ability of deterministic tropical cyclone intensity models to forecast such events has improved, their skill remains inadequate. Thus, forecasters have relied on other tools such as the SHIPS suite of probabilistic statistical rapid intensity models to aid… Read more »
The Joint Typhoon Warning Center (JTWC) was established in 1959. The mission of JTWC is to provide analysis, forecast and decision support to enable DoD and other decision makers to plan, prepare, and protect against the threat of tropical cyclones, tsunamis and other weather impacts. This presentation will provide a brief history and overview of… Read more »
Leads are quasi-linear openings within the interior of the polar ice pack, where the ocean is exposed directly to the atmosphere. Due to the extreme air-water temperature contrast (20 to 40 K), turbulent and radiative heat fluxes over leads can be two orders of magnitude larger than those over the ice surface in winter and… Read more »
Discussion will begin at 11:15 a.m. Refreshments will be served at 10:45 a.m. in the weather lab Convective transport from the marine boundary layer (MBL) to the upper troposphere (UT) is investigated using airborne in situ measurements of chemical species over the tropical western Pacific (TWP). Using 42 trace gas species with photochemical… Read more »