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Meteorology 415 Fall 2012

Meteorology 415 Fall 2012. Forecast Review Wednesday, November 1 4, 2012 Anchorage, AK (ANC). Anchorage, AK. Population (2010)[1] 291,826 (64th in U.S.) • Density 171.9/ sq mi (66.4/km2) • Urban 225,744 • Metro 380,821. Anchorage Observations.

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Meteorology 415 Fall 2012

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  1. Meteorology 415Fall 2012 Forecast Review Wednesday, November 14, 2012 Anchorage, AK (ANC)

  2. Anchorage, AK Population (2010)[1] 291,826 (64th in U.S.) • Density 171.9/sq mi (66.4/km2) • Urban 225,744 • Metro 380,821

  3. Anchorage Observations PANC 142353Z COR 01007KT 10SM -SN SCT007 SCT015 OVC070 M02/M04 A2931 RMK AO2 SLP927 P0000 60002 4/002 T10221044 11022 21033 56024= PANC 142353Z COR 01007KT 10SM -SN SCT007 SCT015 OVC070 M02/M04 A2931= PANC 142353Z 01007KT 10SM -SN SCT007 SCT015 OVC070 M02/M04 A2931= PANC 150017Z 01006KT 10SM SCT007 BKN015 OVC070 M02/M04 A2930 RMK AO2 SNE17 PRESENT WX VCSH ALQDS P0000= PANC 150017Z 01006KT 10SM SCT007 BKN015 OVC070 M02/M04 A2930= PANC 150037Z 36009KT 10SM FEW007 SCT015 OVC060 M02/M04 A2929 RMK AO2 SNE17 PRESENT WX VCSH ALQDS P0000= PANC 150037Z 36009KT 10SM FEW007 SCT015 OVC060 M02/M04 A2929= PANC 150053Z 36009KT 10SM FEW007 SCT015 OVC060 M02/M04 A2929 RMK AO2 SNE17 SLP923 PRESENT WX VCSH ALQDS CIG LWR NE-SE P0000 T10221044= PANC 150053Z 36009KT 10SM FEW007 SCT015 OVC060 M02/M04 A2929= PANC 150153Z 01010KT 10SM -SN FEW007 SCT015 OVC048 M02/M04 A2929 RMK AO2 SNB23 SLP922 CIG LWR NE-SE P0000 T10221044= PANC 150153Z 01010KT 10SM -SN FEW007 SCT015 OVC048 M02/M04 A2929= PANC 150245Z 01006KT 10SM BKN007 BKN015 OVC055 M02/M04 A2929 RMK AO2 SNE21 CIG HIR W-NW P0000= PANC 150245Z 01006KT 10SM BKN007 BKN015 OVC055 M02/M04 A2929= PANC 150253Z 01006KT 10SM BKN007 BKN015 OVC055 M02/M04 A2929 RMK AO2 SNE21 SLP923 CIG HIR W-NW P0000 60000 T10221044 55004= PANC 150253Z 01006KT 10SM BKN007 BKN015 OVC055 M02/M04 A2929= PANC 150315Z 01005KT 10SM -SN SCT007 BKN018 OVC055 M02/M04 A2929 RMK AO2 SNB15 CIG

  4. Anchorage Observations PANC 150329Z 01006KT 10SM -SN FEW007 SCT018 OVC060 M02/M04 A2929 RMK AO2 SNB15 CIG LWR NE-SE P0000= PANC 150329Z 01006KT 10SM -SN FEW007 SCT018 OVC060 M02/M04 A2929= PANC 150353Z 35007KT 10SM -SN FEW007 SCT018 OVC060 M02/M04 A2929 RMK AO2 SNB15 SLP923 CIG LWR E P0000 T10221044= PANC 150353Z 35007KT 10SM -SN FEW007 SCT018 OVC060 M02/M04 A2929= PANC 150453Z 35008KT 10SM FEW007 SCT018 OVC110 M02/M04 A2931 RMK AO2 SNE20 SLP927 LOW ST E P0000 T10221044= PANC 150453Z 35008KT 10SM FEW007 SCT018 OVC110 M02/M04 A2931= PANC 150553Z 35007KT 10SM FEW007 SCT018 BKN110 M03/M04 A2932 RMK AO2 SLP930 LOW ST NE-SE 4/002 60000 T10281044 11022 21028 53008= PANC 150553Z 35007KT 10SM FEW007 SCT018 BKN110 M03/M04 A2932= PANC 150653Z VRB05KT 10SM FEW007 SCT018 BKN130 M03/M05 A2932 RMK AO2 SLP932 LOW ST NE-SE T10281050= PANC 150653Z VRB05KT 10SM FEW007 SCT018 BKN130 M03/M05 A2932= PANC 150753Z 02003KT 10SM FEW007 SCT018 BKN130 M04/M06 A2933 RMK AO2 SLP936 LOW ST NE T10391056= PANC 150753Z 02003KT 10SM FEW007 SCT018 BKN130 M04/M06 A2933= PANC 150853Z 03005KT 10SM FEW005 BKN065 OVC130 M03/M05 A2935 RMK AO2 SLP941 LOW ST NE-E T10331050 410221044 53010= PANC 150853Z 03005KT 10SM FEW005 BKN065 OVC130 M03/M05 A2935= PANC 150953Z 02005KT 10SM FEW005 BKN070 M03/M04 A2935 RMK AO2 SLP943 LOW ST NE-E T10281044= PANC 150953Z 02005KT 10SM FEW005 BKN070 M03/M04 A2935= PANC 151053Z 08006KT 10SM FEW007 BKN070 M03/M06 A2936 RMK AO2 SLP944 T10331056= PANC 151053Z 08006KT 10SM FEW007 BKN070 M03/M06 A2936= PANC 151153Z 03005KT 10SM FEW007 BKN070 M03/M06 A2937 RMK AO2 SLP948 70004 T10331056 11028 21039 53007= PANC 151153Z 03005KT 10SM FEW007 BKN070 M03/M06 A2937= PANC 151153Z COR 03005KT 10SM FEW007 BKN070 M03/M06 A2937 RMK AO2 SLP948 70004 T10331056 11028 21039 53007 4/002=

  5. Anchorage Surface Map

  6. Anchorage Satellite Imagery

  7. Anchorage IR Imagery

  8. Anchorage Radar

  9. Anchorage Verifications

  10. Anchorage – Survey Scores

  11. Anchorage – Career Scores

  12. Up Close and Personal

  13. Anchorage Lessons Learned Elongated low pressure systems, that are not deepening, tend to produce only small amounts of precipitation away from the coast. The offshore component of the wind is crucial to precipitation type and amount in southern Alaska Despite a pronounced pressure gradient, it is also the change of the PGF with time that makes strong winds and also high gusts.

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