Meso-α: Easterly wave critical layer Isolated recirculation regions Inertia gravity waves

10
Meso-α: Easterly wave critical layer Isolated recirculation regions Inertia gravity waves 200 – 2,000 km 1 Consideration of horizontal scales exposes the challenging nature of the problem Meso-γ: VHTs, Congestus, Precip. Driven downdrafts, Gust fronts 2 – 20 km Synoptic Easterly Waves Hydro instability of ITCZ Subtropical intrusions 2,000 – 8,000 km Meso-β: TC, MCS, gravity waves 20 – 200 km ln E ln k Downscal e Enstroph y Cascade Upscale Energy Cascade

description

Consideration of horizontal scales exposes the challenging nature of the problem. ln E. Downscale Enstrophy Cascade. Meso-β: TC, MCS, gravity waves 20 – 200 km. Upscale Energy Cascade. ln k. Synoptic Easterly Waves Hydro instability of ITCZ Subtropical intrusions 2,000 – 8,000 km. - PowerPoint PPT Presentation

Transcript of Meso-α: Easterly wave critical layer Isolated recirculation regions Inertia gravity waves

Page 1: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Meso-α:Easterly wave critical layer Isolated recirculation regionsInertia gravity waves 200 – 2,000 km

1

Consideration of horizontal scales exposes thechallenging nature of the problem

Meso-γ:VHTs, Congestus, Precip. Driven downdrafts, Gust fronts2 – 20 km

SynopticEasterly WavesHydro instability of ITCZSubtropical intrusions2,000 – 8,000 km

Meso-β:TC, MCS, gravity waves 20 – 200 km

ln E

ln k

Downscale Enstrophy Cascade

Upscale Energy Cascade

Page 2: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Wave-Pouch Tracking Methodology

• Front page imagery– Methodology for determining initial position

• Phase speed determination– Zonal method (RH & v)– Oblique method

• Track creation– Methodology for determining level

• Meso- diagnostics– Zeta, OW, RH, Vertical Shear

• Satellite/analysis (over to LeeJoice)

Page 3: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves
Page 4: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves
Page 5: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Nondevelopers Developers

Wave-ITCZ Interaction

Diabatically

activated?

SAL / mid-level dry air:

Killed or Survived?

No pouch

Shallow pouch above PBL

Shallow pouch within PBL

Deep pouch

Shallow pouch

Deep pouch

Intensified on ITCZ

Excited new

waves

97L

PG01L X No No No NA

PG02L NoMaybe. SAL

to east

PG03L XMaybe.

In SAL

PG04L XMaybe.

In SAL

PG05L X

PG06L XMaybe.

In SAL

2009 GRIP / PREDICT Dry Run Summary

Page 6: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Nondevelopers Developers

Wave-ITCZ Interaction

Diabatically

activated?

SAL / mid-level dry air:

Killed or Survived?

No pouch

Shallow pouch above PBL

Shallow pouch within PBL

Deep pouch

Shallow pouch

Deep pouch

Intensified on ITCZ

Excited new

waves

PG07L

PG08L X

PG09L

PG10LClaudette

PG11L

Ana

PG12L

BillX X

PG13L

2009 GRIP / PREDICT Dry Run Summary

Page 7: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Nondevelopers Developers

Wave-ITCZ Interaction

Diabatically

activated?

SAL / mid-level dry air:

Killed or Survived?

No pouch

Shallow pouch above PBL

Shallow pouch within PBL

Deep pouch

Shallow pouch

Deep pouch

Intensified on ITCZ

Excited new

waves

PG14L

PG15L X

PG16L

PG17L

Danny

PG18L

PG19L

PG20L

ErikaX

2009 GRIP / PREDICT Dry Run Summary

Page 8: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Nondevelopers Developers

Wave-ITCZ Interaction

Diabatically

activated?

SAL / mid-level dry air:

Killed or Survived?

No pouch

Shallow pouch above PBL

Shallow pouch within PBL

Deep pouch

Shallow pouch

Deep pouch

Intensified on ITCZ

Excited new

waves

PG21L

PG22L

PG23L

PG24LX

Shear

PG25L

FredX

PG26L X Killed

PG27L

2009 GRIP / PREDICT Dry Run Summary

Page 9: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

Nondevelopers Developers

Wave-ITCZ Interaction

Diabatically

activated?

SAL / mid-level dry air:

Killed or Survived?

No pouch

Shallow pouch above PBL

Shallow pouch within PBL

Deep pouch

Shallow pouch

Deep pouch

Intensified on ITCZ

Excited new

waves

PG28L

PG29L

TD08L

PG30L

PG31L

PG32L

Henri

PG33L

2009 GRIP / PREDICT Dry Run Summary

Page 10: Meso-α: Easterly wave critical layer  Isolated recirculation regions Inertia gravity waves

New Diagnostics Wish List

• ‘Diabatic Activation’ (i.e., persistent convective activity). Use visible/infrared/microwave satellite imagery

• Warm & dry air from middle level tropical atmosphere or African continent (SAL products, real time ? …)

• Trade wind inversion (real time)• CAPE (real time)• CIN (real time)