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Downslope Windstorms in Howe Sound: Two Case Studies Ruping Mo, Paul Joe National Lab for Coastal & Mountain Meteorology, Environment Canada Johnson Zhong,

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Presentation on theme: "Downslope Windstorms in Howe Sound: Two Case Studies Ruping Mo, Paul Joe National Lab for Coastal & Mountain Meteorology, Environment Canada Johnson Zhong,"— Presentation transcript:

1 Downslope Windstorms in Howe Sound: Two Case Studies Ruping Mo, Paul Joe National Lab for Coastal & Mountain Meteorology, Environment Canada Johnson Zhong, Cindy Yu, Ken Kwok, and Michel Gélinas Pacific Storm Prediction Centre, Environment Canada 15 th Conf. Mountain Meteorology 20–24 August 2012, Steamboat, CO, USA

2 Outline Geography and windstorm climatology Rules of thumb for the freak windstorms Case studies: 1.18 January 2010 – A major event 2.12 February 2010 – A minor event New heuristic rule Conclusions Test test test test

3 Page 3 – February 19, 2016 Howe Sound

4 Where is Howe Sound? Howe Sound Metro Vancouver Pam Rocks

5 Winds in Howe Sound – Climatology Data: Pam Rocks (WAS) – Jan to Mar, 1995 to 2012 (18 years)

6 Winds in Howe Sound – Climatology Sustained winds at Pam Rocks (WAS) Hourly, Jan – Mar, 1995 – 2012

7 Unusual/Freak Southeast Windstorms ???

8 Freak Southeast Windstorms 3014 Hourly, Jan–Mar, 1995–2012 (18 yrs)

9 Heuristic Rule /Rules of thumb Pre-frontal Strong Southeasterlies in the Strait of Georgia P YVR −P YQQ > 6.5 hPa Pressure Difference

10 Case 1: 18 Jan 2010 04:00 PST (12:00 UTC) P YVR −P YQQ > 6.5 hPa (MAX P dif = 11.9 hPa) SE wind warning issued at 20:00 PST 17 Jan

11 Case 1: 18 Jan 2010 Predicted by 1-km model (GEM-LAM-1km) WAS S2S Hwy

12 Page 12 – February 19, 2016

13 Case 1: 18 Jan 2010 Predicted by 1-km model (GEM-LAM-1km) Southwest wind aloft Possible critical layer for wave breaking Induced convective instability over water WAS Possible Critical Layer for SEly

14 Page 14 – February 19, 2016

15 Case 2: 12 Feb 2010 04:00 PST (12:00 UTC) P YVR −P YQQ > 6.5 hPa (MAX P dif = 8.1 hPa) SE wind storm was not predicted. Forecast amended after the fact. (1 st day of 2010 Olympics) Wind dir. unknown

16 Page 16 – February 19, 2016

17 Page 17 – February 19, 2016 First Day of Olympics PYVR−PYQQ > 6.5 hPa (MAX Pdif = 8.1 hPa) SE wind storm was not predicted. Forecast amended after the fact.

18 Case 3: 12 Jan 2010 Predicted by 1-km model (GEM-LAM-1km)

19 Page 19 – February 19, 2016

20 Page 20 – February 19, 2016

21 New rules of thumb Pre-frontal Strong Southeasterlies in the Strait of Georgia P YVR −P YQQ > 6.5 hPa Winds shift to southwest aloft! WSK Wind Profile

22 Page 22 – February 19, 2016

23 Potential hazard on Sea-to-Sky HWY

24 Conclusions Southeast windstorm in Howe Sound is a rare event It has quite an impact on mariners, but is difficult to predict It is likely related to a downslope windstorm due to orographic wave breaking Orographic effect leads to Wind shifting from SE to SW above mountain, which provide a possible critical layer aloft for orographic wave breaking Downslope windstorm could be a hazard on the Sea2Sky Hwy as well The development of LAM-1km model was accelerated for the Olympics and this is a serendipitous benefit of that

25 Thank You! Michael O’Toole’s “Storm Over Howe Sound”


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