Rhinelander, wiMeteorology 415 – Fall 2012

Ninth Forecast Review

Rhinelander, wiPopulation (2000)

 • Total 8,135

 • Density 1,002.5/sq mi (387.1/km2)

Rhinelander obs• KANJ 192355Z AUTO 12009KT 10SM FEW080 OVC100 10/05 A2983 RMK AO2 SLP102

60004 T01000050 10111 20089 56016=

• KANJ 200055Z AUTO 11004KT 10SM OVC060 10/07 A2983 RMK AO2 RAB2359E42 SLP102 P0001 T01000067=

• KANJ 200155Z AUTO 12009KT 10SM -RA OVC065 12/06 A2979 RMK AO2 RAB02E11B34 SLP089 P0000 T01170061=

• KANJ 200255Z AUTO 13011G19KT 10SM -RA OVC070 12/06 A2976 RMK AO2 SLP077 P0000 60001 T01220061 58023=

• KANJ 200355Z AUTO 10004KT 5SM RA OVC055 11/08 A2974 RMK AO2 SLP073 P0007 T01110083=

• KANJ 200455Z AUTO 15009KT 9SM -RA BKN030 OVC037 11/08 A2970 RMK AO2 SLP058 P0006 T01060083 401220022=

• KANJ 200518Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08 A2968 RMK AO2 P0005 T01060083=

• KANJ 200518Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08A2968=

• KANJ 200527Z AUTO 16010G16KT 10SM SCT024 BKN030 OVC055 11/08 A2967 RMK AO2 RAE24 P0005 T01060083=

• KANJ 200539Z AUTO 14013G19KT 10SM SCT018 BKN027 OVC085 11/08 A2964 RMK AO2 RAE24 PRESFR P0005 T01060083= KANJ 200555Z AUTO 16008G17KT 10SM BKN016 BKN025 OVC110 11/09 A2963 RMK AO2 RAE24 SLP034 P0005 60019 T01060089 10122 20094

Rhinelander - OBS• KANJ 200609Z AUTO 18010G18KT 10SM BKN012 OVC100 11/09 A2964 RMK AO2

T01110089=

• KANJ 200655Z AUTO 18009KT 10SM OVC013 11/09 A2965 RMK AO2 SLP041 T01110089=

• KANJ 200755Z AUTO 19009KT 10SM OVC012 11/09 A2966 RMK AO2 SLP043 T01110089=

• KANJ 200822Z AUTO 19008KT 10SM FEW012 BKN021 OVC035 12/09 A2966 RMK AO2 T01170094=

• KANJ 200836Z AUTO 20006KT 10SM FEW013 SCT031 BKN047 11/09 A2966 RMK AO2 T01110094=

• KANJ 200855Z AUTO 19007KT 10SM FEW028 BKN050 11/09 A2966 RMK AO2 SLP043 T01110094 51008=

Rhinelander – surface map

rhinelander– upper air

rhinelandersatellite

Rhinelander-radar

Rhinelanderverifications

Class Consensus

Class Consensus

Class Consensus

Rhinelander-scores

rhinelander– up close and personal

rhinelander – lessons learned

• 3 hour POP’s are challenging and should be given lower probabilities even in short range predictions.

• A well developed vort-max and its surface circulation will usually spawn one wave of organized showers to the south of the circulation center. Precip amounts are typically a quarter of an inch or less (unless there are convective elements)

• Clouds and showers at night will keep temperatures in a narrow range, especially in a site surrounded by water.