African Easterly Waves Figure from Chris Landsea.

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Transcript of African Easterly Waves Figure from Chris Landsea.

Page 1: African Easterly Waves Figure from Chris Landsea.

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African Easterly Waves

Figure from Chris Landsea

Page 2: African Easterly Waves Figure from Chris Landsea.

A Hurricane Life

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Page 3: African Easterly Waves Figure from Chris Landsea.

Tropical Storm Genesis

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Page 4: African Easterly Waves Figure from Chris Landsea.

AEW early research

Dunn, G. E., 1940: ~ observed in Carribean westward traveling lower tropospheric “seeds” for tropical cyclones

Riehl, H., 1945: ~ origins of waves were over North Africa

Burpee, R. W., (1972): ~ origin in barotropic/baroclinic disturbances of African Easterly Jet

Burpee, R. W., (1974): ~ wavelength, period

Page 5: African Easterly Waves Figure from Chris Landsea.

Satellite Image

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Page 6: African Easterly Waves Figure from Chris Landsea.

10-15 N Pacific,June-Aug 1967

Page 7: African Easterly Waves Figure from Chris Landsea.

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AEW basic facts (1)

Statistics: Occur April/May through September/October ~ 60 per year in N. Atlantic 60% of tropical storms + Cat 1,2 hurricanes 85% of Cat 3,4, 5 hurricanes most East Pacific hurricanes traced back to AEW’s

wavelength 2000-2500 km (18o-23o lon) period 3-5 days

Origin: disturbance of African Easterly Jet

Page 8: African Easterly Waves Figure from Chris Landsea.

Riehl model

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Page 9: African Easterly Waves Figure from Chris Landsea.

AEW features noted early

“Inverted V” horizontal orientation

Page 10: African Easterly Waves Figure from Chris Landsea.

AEW features (cont)

Mesoscale feature of lower atmosphere (~ 0 - 5 km) Low level vorticity signal, decreasing with height Fair weather to west of trough; Upper level convergence, low level divergence Subsidence pattern

Active weather to east of trough Lower level convergence, upper level divergence Deep layer of moisture Convective precipitation

Intense waves can draw ITCZ north

Page 11: African Easterly Waves Figure from Chris Landsea.

Agee 1969 (Tropical Storm Anna)

Page 12: African Easterly Waves Figure from Chris Landsea.

Example

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Page 13: African Easterly Waves Figure from Chris Landsea.

African Easterly Jet

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Page 14: African Easterly Waves Figure from Chris Landsea.

Africa

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Page 15: African Easterly Waves Figure from Chris Landsea.

Skin Temperature

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Page 16: African Easterly Waves Figure from Chris Landsea.

850mb -700 mb Temperature

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JJALat vs Lon

Latitude vs Month Avg’d 0-10 E

June 1 Sept 1

Page 17: African Easterly Waves Figure from Chris Landsea.

Zonal wind

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JJA 600mb

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Winds averaged: 10 N - 20 N, 0 - 10 E

600

Height vs Time

SeptJune

Page 18: African Easterly Waves Figure from Chris Landsea.

Meridional (60 S - 60 N) Aug Temperature

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30 W

35 E

5 E

Note: low level T gradient ~ 15 N

Page 19: African Easterly Waves Figure from Chris Landsea.

Meridional (0-35 N) Aug T & U at 5 E

Zonal Wind

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Page 20: African Easterly Waves Figure from Chris Landsea.

Circulation Aug, 5 E

Zonal WindMerid’lWind

Omega

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Page 21: African Easterly Waves Figure from Chris Landsea.

Hurricane and Positive vorticity center tracks

(Thorncroft & Hodges 2001),J. Climate

20 years (1979-98) ECMWF reanalyses

Tracked systems with closed vorticity contours of at least + 5 x 10-6 s-1

Omitted systems that - lasted less than 2 days - traveled < 1000 km

Page 22: African Easterly Waves Figure from Chris Landsea.

Positive vorticity tracksMay-Oct 1995

600 mb

850 mb

(Thorncroft & Hodges 2001)

Page 23: African Easterly Waves Figure from Chris Landsea.

Positive vorticity tracksMay-Oct 1994

600 mb

850 mb

(Thorncroft & Hodges 2001)

Page 24: African Easterly Waves Figure from Chris Landsea.

Climatological 850mbTracks (1979-98)

Track density(shading > 6)

Genesis dens.(shading > 5)

(Thorncroft & Hodges 2001)

density = number/yr/(106 km2 )

“Growth rate”(Dark = growthLight = decay)

Page 25: African Easterly Waves Figure from Chris Landsea.

Climatological 850mbTracks (1979-98)

Track density(shading > 6)

Genesis dens.(shading > 5)

(Thorncroft & Hodges 2001)

density = number/yr/(106 km2 )

“Growth rate”(Dark = growthLight = decay)

Page 26: African Easterly Waves Figure from Chris Landsea.

Seasonal Cycle of Track Density (1979-98)

850 mb

600 mb

(Thorncroft & Hodges 2001)

May

Sept

June

Oct

May

Sept

Oct

June

Page 27: African Easterly Waves Figure from Chris Landsea.

Interannual VariabilityAEW activity (May-Oct)

(Thorncroft & Hodges 2001)

Number

Year

850 mb

600 mb

June

85 9080 9575

20

10

30

Page 28: African Easterly Waves Figure from Chris Landsea.

Interannual Variability AEW & Hurricane (May-Oct)

(Thorncroft & Hodges 2001)