Rhinelander, wi Meteorology 415 – Fall 2012 Ninth Forecast Review.

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Presentation transcript:

Rhinelander, wi Meteorology 415 – Fall 2012 Ninth Forecast Review

Rhinelander, wi Population (2000) Total8,135 Density 1,002.5/sq mi (387.1/km 2 )

Rhinelander obs KANJ Z AUTO 12009KT 10SM FEW080 OVC100 10/05 A2983 RMK AO2 SLP T = KANJ Z AUTO 12009KT 10SM FEW080 OVC100 10/05 A2983 RMK AO2 SLP T = KANJ Z AUTO 11004KT 10SM OVC060 10/07 A2983 RMK AO2 RAB2359E42 SLP102 P0001 T = KANJ Z AUTO 11004KT 10SM OVC060 10/07 A2983 RMK AO2 RAB2359E42 SLP102 P0001 T = KANJ Z AUTO 12009KT 10SM -RA OVC065 12/06 A2979 RMK AO2 RAB02E11B34 SLP089 P0000 T = KANJ Z AUTO 12009KT 10SM -RA OVC065 12/06 A2979 RMK AO2 RAB02E11B34 SLP089 P0000 T = KANJ Z AUTO 13011G19KT 10SM -RA OVC070 12/06 A2976 RMK AO2 SLP077 P T = KANJ Z AUTO 13011G19KT 10SM -RA OVC070 12/06 A2976 RMK AO2 SLP077 P T = KANJ Z AUTO 10004KT 5SM RA OVC055 11/08 A2974 RMK AO2 SLP073 P0007 T = KANJ Z AUTO 10004KT 5SM RA OVC055 11/08 A2974 RMK AO2 SLP073 P0007 T = KANJ Z AUTO 15009KT 9SM -RA BKN030 OVC037 11/08 A2970 RMK AO2 SLP058 P0006 T = KANJ Z AUTO 15009KT 9SM -RA BKN030 OVC037 11/08 A2970 RMK AO2 SLP058 P0006 T = KANJ Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08 A2968 RMK AO2 P0005 T = KANJ Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08 A2968 RMK AO2 P0005 T = KANJ Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08A2968= KANJ Z AUTO 15010G21KT 7SM -RA BKN026 BKN055 OVC085 11/08A2968= KANJ Z AUTO 16010G16KT 10SM SCT024 BKN030 OVC055 11/08 A2967 RMK AO2 RAE24 P0005 T = KANJ Z AUTO 16010G16KT 10SM SCT024 BKN030 OVC055 11/08 A2967 RMK AO2 RAE24 P0005 T = KANJ Z AUTO 14013G19KT 10SM SCT018 BKN027 OVC085 11/08 A2964 RMK AO2 RAE24 PRESFR P0005 T = KANJ Z AUTO 16008G17KT 10SM BKN016 BKN025 OVC110 11/09 A2963 RMK AO2 RAE24 SLP034 P T KANJ Z AUTO 14013G19KT 10SM SCT018 BKN027 OVC085 11/08 A2964 RMK AO2 RAE24 PRESFR P0005 T = KANJ Z AUTO 16008G17KT 10SM BKN016 BKN025 OVC110 11/09 A2963 RMK AO2 RAE24 SLP034 P T

Rhinelander - OBS KANJ Z AUTO 18010G18KT 10SM BKN012 OVC100 11/09 A2964 RMK AO2 T = KANJ Z AUTO 18010G18KT 10SM BKN012 OVC100 11/09 A2964 RMK AO2 T = KANJ Z AUTO 18009KT 10SM OVC013 11/09 A2965 RMK AO2 SLP041 T = KANJ Z AUTO 18009KT 10SM OVC013 11/09 A2965 RMK AO2 SLP041 T = KANJ Z AUTO 19009KT 10SM OVC012 11/09 A2966 RMK AO2 SLP043 T = KANJ Z AUTO 19009KT 10SM OVC012 11/09 A2966 RMK AO2 SLP043 T = KANJ Z AUTO 19008KT 10SM FEW012 BKN021 OVC035 12/09 A2966 RMK AO2 T = KANJ Z AUTO 19008KT 10SM FEW012 BKN021 OVC035 12/09 A2966 RMK AO2 T = KANJ Z AUTO 20006KT 10SM FEW013 SCT031 BKN047 11/09 A2966 RMK AO2 T = KANJ Z AUTO 20006KT 10SM FEW013 SCT031 BKN047 11/09 A2966 RMK AO2 T = KANJ Z AUTO 19007KT 10SM FEW028 BKN050 11/09 A2966 RMK AO2 SLP043 T = KANJ Z AUTO 19007KT 10SM FEW028 BKN050 11/09 A2966 RMK AO2 SLP043 T =

Rhinelander – surface map

rhinelander – upper air

rhinelander satellite

Rhinelander -radar

Rhinelander verifications

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