High Impact Weather Events in the Transition Seasons: Linked to Global Change? Jonathan E. Martin...

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High Impact Weather Events in the Transition Seasons:

Linked to Global Change?

Jonathan E. MartinUniversity of Wisconsin-Madison

2132 UTC 26 October 2010

Supertyphoon Megi – 17 October 2010

00 UTC 20 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 21 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 22 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 23 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 24 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 25 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

00 UTC 16 October 2010

00 UTC 22 October 2010

00 UTC 22 October 2010and PV

00 UTC 22 October 2010and PV

Defant and Taba 1957

Tropopause Pressure (mb) 1 January 1956

Defant and Taba 1957Defant and Taba 1957

Likely that jet superpositions underlie some fraction of extreme weather events

Can jet superpositions be objectively identified?

Likely that jet superpositions underlie some fraction of extreme weather events

300 hPa Wind Speed0000 UTC 27 April 2010

Can jet superpositions be objectively identified?

Likely that jet superpositions underlie some fraction of extreme weather events

A A`

A A`

A A`

A A`

0000 UTC 24 October 2010B B`

0000 UTC 24 October 2010B B`

0000 UTC 24 October 2010B B`

0000 UTC 24 October 2010B B`

00 UTC 24 October 20100.5 PVU isertel, Δp` (shaded), Wind speed at 348K

Subtropical/Polar jet Superpositions

Subtropical Jet tied to the Hadley Circulation

Subtropical Jet tied to the Hadley Circulation

Polar Jet tied to mid-latitudebaroclinicity

Subtropical Jet tied to the Hadley Circulation

Polar Jet tied to mid-latitudebaroclinicity

Warmer planet encourages a quicker northward return of the ITCZ

Warmer planet encourages a quicker northward return of the ITCZ

Extends the period of possible jet superpositions

Warmer planet encourages a quicker northward return of the ITCZ

Extends the period of possible jet superpositions

More frequent, extreme weather in mid-latitudes??

Warmer planet encourages longer TC season in West Pacific

Warmer planet encourages longer TC season in West Pacific

Extends the period of possible jet superpositions

Warmer planet encourages longer TC season in West Pacific

Extends the period of possible jet superpositions

More frequent, extreme weather in mid-latitudes??

Next Steps

Next Steps

Construct 50 year climatology of jet superpositions

Next Steps

Construct 50 year climatology of jet superpositions

Consider relationships between jet superpositions and various categories of high impact weather

Next Steps

Construct 50 year climatology of jet superpositions

Consider relationships between jet superpositions and various categories of high impact weather

Provide a synoptic-dynamic context for predictions of increased frequency of extreme weather in a warmer climate

Next Steps

Construct 50 year climatology of jet superpositions

Consider relationships between jet superpositions and various categories of high impact weather

Provide a synoptic-dynamic context for predictions of increased frequency of extreme weather in a warmer climate

Provide more tenable physical linkages between traditional climate science and traditional weather systems science

1800 UTC 1 May 2010

1800 UTC 1 May 2010

1800 UTC 1 May 2010

1800 UTC 1 May 2010

1800 UTC 1 May 2010