Sting jet
A sting jet is a meteorological phenomenon which has been postulated to cause some of the most damaging winds in extratropical cyclones, developing according to the Shapiro-Keyser model of oceanic cyclones.
Contents
Concept
![](/w/images/thumb/0/03/European_Windstorm_Conceptual_Model.jpg/300px-European_Windstorm_Conceptual_Model.jpg)
Following reanalysis of the Great Storm of 1987, led by Professor Keith Browning at the University of Reading, researchers identified a mesoscale flow where the most damaging winds were shown to be emanating from the evaporating tip of the hooked cloud head on the southern flank of the cyclone. This cloud, hooked like a scorpion's tail, gives the wind region its name the "sting jet".[2]
It is thought that a zone of strong winds, originating from within the mid-tropospheric cloud head of an explosively deepening depression, are enhanced further as the "jet" descends, drying out and evaporating a clear path through snow and ice particles. The evaporative cooling leading to the air within the jet becoming denser, leading to an acceleration of the downward flow towards the tip of the cloud head when it begins to hook around the cyclone centre. Windspeeds in excess of 80 kn (150 km/h) can be associated with the sting jet.[3]
It has since been reproduced in high-resolution runs with the mesoscale version of the Unified Model. The sting jet is distinct from the usual strong-wind region associated with the warm conveyor belt and main cold front. There are indications that conditional symmetric instability also plays a role in its formation but the importance of these processes remains to be quantified.[4][5]
One North Atlantic storm, Cyclone Tilo (November 6–11, 2007) has also been analysed and found not to display a sting jet, despite displaying strong surface winds and a fractured cold front.[5]
Globally
The sting jet mechanism has been considered less significant in Pacific Northwest windstorms which occur over the Pacific Ocean (which impact the Northwestern United States and British Columbia).[6] Evidence of mesoscale high wind areas has not been noted in most large windstorms occurring there, along with cloud geometry associated with the phenomena being absent in satellite imagery of major Pacific Northwest storms.[6] High resolution computer models of the phenomena have also shown realistically strong winds without the need for sting jet dynamics.[6]
List of sting jet cyclones
Cyclone | Type | Date | Reference | Location |
---|---|---|---|---|
Great Storm of 1987 | European windstorm | October 15-17, 1987 | [7][8][9] | Southern England |
Oratia | European windstorm | October 30, 2000 | [9][10] | North Sea (Lincolnshire to Norway) |
Anna | European windstorm | February 26, 2002 | [11] | Central Pennines, England |
Jeanette | European windstorm | October 27, 2002 | [12][13] | Wales and the English Midlands |
Erwin | European windstorm | January 2005 | [13][14][15][16] | Northern England |
Friedhelm | European windstorm | December 8, 2011 | [17][18][19] | Central Belt Scotland |
Ulli | European windstorm | January 3–4, 2012 | [20][21][22][23][24][25] | Central Belt Scotland |
List of proposed sting jets
Cyclone | Type | Date | Reference | Location |
---|---|---|---|---|
New Year's Day Storm | European Windstorm | January 1, 1992 | [26][27] | Norway |
Renate | European windstorm | October 3, 2006 | [27] | Bay of Biscay and Aquitaine, France |
"Oeste storm" | European windstorm | December 23, 2009 | [28] | Portugal |
October 2010 North American storm complex | Great Lakes cyclone | October 26–27, 2010 | [20] | Midwest USA |
2011 Halloween nor'easter | Nor'easter | October 30–31, 2011 | [20][29] | Northeastern USA |
Unnamed | Extratropical cyclone | March 12, 2012 | [30] | Upper Midwest USA |
Gong | European windstorm | January 19, 2013 | [28] | Portugal |
St Jude storm (Christian) | European windstorm | October 28, 2013 | [31][32] | Possibly developing over East Anglia then over the North Sea, skirting the Netherlands coast to Germany/Denmark. |
Cyclone Tini/storm Darwin | European windstorm | February 12, 2014 | [33] | Southern Ireland, Irish Sea, Wales. |
Arthur | Extratropical cyclone ex–Hurricane | July 5, 2014 | [34][35] | Canadian Maritimes |
Elon (Nathan) | European windstorm | January 9, 2015 | [36][37][38] | Scotland |
External links
- The Sting Jet: Forecasting the damaging winds in European Cyclones, UK Met Office
- The 1987 Great Storm - What is a Sting Jet?, UK Met Office
- EUMeTrain webcast, "Sting Jets" Prof. Geraint Vaughan, School of Earth, Atmospheric and Environmental Sciences, The University of Manchester
Further reading
- Quarterly Journal of the Royal Meteorological Society 140: 96 – 110, January 2014 Idealised simulations of sting-jet cyclones
- Do North Pacific sting jet cyclones exist?
- NOAA Conditional Symmetric Iinstability (CSI) homepage
References
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- ↑ Meteorological glossary Booty.org, retrieved 2007-17-10
- ↑ Cyclonic storms UWERN newsletter, retrieved 2007-17-10
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