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![Page 1: Synoptic composites of the ET lifecycle of North Atlantic TCs: Factors determining post-transition evolution Contributions from: Clark Evans Jenni Evans.](https://reader035.fdocuments.in/reader035/viewer/2022070404/56649f335503460f94c5018d/html5/thumbnails/1.jpg)
Synoptic composites of the ET lifecycle of North Atlantic TCs:
Factors determining post-transition evolution
Contributions from:
Clark Evans
Jenni Evans
![Page 2: Synoptic composites of the ET lifecycle of North Atlantic TCs: Factors determining post-transition evolution Contributions from: Clark Evans Jenni Evans.](https://reader035.fdocuments.in/reader035/viewer/2022070404/56649f335503460f94c5018d/html5/thumbnails/2.jpg)
Motivation: TCs never lose their diapers…
TCs that intensify after extratropical transition
TCs that weaken after extratropical transition
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Motivation: Hurricanes cannot be considered passive in midlatitude flow
Ivan (2004)
Karl (2004)
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Motivation: The Impact of Hurricane Karl on 72hr Ensemble Forecasts
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Cyclone Predictability is a function of its structure
• Predictability is a function of cyclone structure
• Model interpretation/trust is a function of structure
• MPI is a function of cyclone structure
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The role of the downstream and upstream long-wave patternhas been shown to play a critical role in determining TC evolution after ET (McTaggart-Cowan et al. 2003)
Tropical cyclones aren’t passive features upon entering the midlatitude flow
The details of tropical development and extratropical transition can dramatically influence the hemispheric long wave pattern
NWP models often obtain their worst forecast skill when a hurricane is about to enter the midlatitude flow (Harr and Jones 2003).
Understanding the reasoning behind these requires improved understanding of extratropical transition.
Motivation: Previous Research
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Some questions raised:
• What are the structural aspects of tropical cyclones that favor constructive interaction What are the structural aspects of tropical cyclones that favor constructive interaction with a midlatitude trough?with a midlatitude trough?
• What are the structural aspects of the midlatitude trough that favor constructive What are the structural aspects of the midlatitude trough that favor constructive interaction with a TC?interaction with a TC?
• What factors determine the rapid or slow transition of a TC?What factors determine the rapid or slow transition of a TC?
• What factors determine intensification or decay after extratropical transition of the What factors determine intensification or decay after extratropical transition of the cyclone?cyclone?
• What are the determining factors for post-ET structure of the cyclone: cold core vs. What are the determining factors for post-ET structure of the cyclone: cold core vs. warm-seclusion? warm-seclusion?
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34 North Atlantic Transitioning Cyclones Examined
Bonnie (1998) Gordon (2000)
Danielle (1998) Isaac (2000)
Earl (1998) Michael (2000)
Ivan (1998) Nadine (2000)
Jeanne (1998) Allison (2001)
Karl (1998) Erin (2001)
Mitch (1998) Gabrielle (2001)
Nicole (1998) Humberto (2001)
Cindy (1999) Karen (2001)
Dennis (1999) Michelle (2001)
Floyd (1999) Cristobal (2002)
Gert (1999) Gustav (2002)
Harvey (1999) Isidore (2002)
Irene (1999) Josephine (2002)
Jose (1999) Fabian (2003)
Alberto (2000) Isabel (2003)
Florence (2000) Kate (2003)
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Cyclone Phase Space• Unifies the fundamental structural description of Unifies the fundamental structural description of
cyclones into a multi-dimensional continuum cyclones into a multi-dimensional continuum ((MWR 2003a,bMWR 2003a,b) : ) :
B: B: 900-600hPa: Storm-relative thermal asymmetry900-600hPa: Storm-relative thermal asymmetry
-V-VTTLL:: 900-600hPa: Thermal wind (cold vs. warm core)900-600hPa: Thermal wind (cold vs. warm core)
-V-VTTUU:: 600-300hPa: Thermal wind (cold vs. warm core)600-300hPa: Thermal wind (cold vs. warm core)
• Will be focusing on a cross section of B vs –VWill be focusing on a cross section of B vs –VTTLL here. here.
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Cyclone Phase Space
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Cyclone Phase Space: ET Example [Floyd]
Transition begins (time=TB) when B > 10m => significant thermal gradient.
Transition ends (time=TE) when cyclone is cold-core
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TE
TE+24h
TE+48h
TB
TMID
TB-24h
TB-48h
34-Cyclone Composite Mean Phase NOGAPS-analysis based Trajectory with key milestones labeled
Composite Mean ET Structural Evolution Summary
TB-72h
TE+72h
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Compositing Method• NOGAPS 1°x1° operational analyses from 34 storms
1998-2003
• Storm-center-relative composites. No coordinate rotation for storm motion.
• ±40° longitude
• -20° to +30° latitude (never extending outside 0°-90°N)
• Raw field and anomaly from NCAR/NCEP Reanalysis2 30-year monthly-mean are both composited.
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34-Cyclone Composite Mean Evolution 320K Potential Vorticity
TB-24h TB
TE TE+24h
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34-Cyclone Composite Mean Evolution:320K PV Cross Sections
TB-24h TB
TETE+24h
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Boxes represent the calculated one standard deviation spread about the 34-cyclone consensus mean trajectory for each time
Variability About the Composite Mean
Considerable variability about mean once transition completed=> posttropical phase can take many forms….
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Floyd (1999): Non-intensifying cold-core development
Hugo (1989): Explosive cold-core development
Charley (1986): Schizophrenia
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Dennis (1999): “ET-Interruptus”.Cindy (1999): Absorption.
Keith (1988): Explosive warm-seclusion development
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Three key subcomposites
• Fast [<=12hr] vs. Slow [>=48hr] Transitioning
• Post-ET Intensification (N=6) vs. Weakening (N=11)
• Post-ET Cold-Core (N=15) vs. Warm-Seclusion (N=6)
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TB: Fast (left) vs. Slow (right) Transitioning
Strengthen (N=6)
500mb Height
& Anom.
SST & Anom.
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Strengthen (N=6)
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TB: Post-ET Weakening (left) vs. Intensification (right)
Strengthen (N=6)
500mb Height
& Anom.
SST & Anom.
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Strengthen (N=6)
Post-ET Weakeners (Solid) vs. Intensifiers (Dotted): T-Test: 75%, 90%, 95%, 99%
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Two post-ET intensifiers:What determines whether the storm re-acquires warm-core structure?
Gustav (2002) Irene (1999)
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TE: Post-ET Cold-core (left) vs. warm-seclusion (right)
Strengthen (N=6)
320K PV
320K PV
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Post-ET Cold-core (Solid) vs. Warm-seclusion (Dotted): T-Test: 75%, 90%, 95%, 99%
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Strengthen (N=6)
Post-ET Cold-core vs. Warm-Seclusion: Statistics
# Cases Latitude
at TB
Longitude at TB
Best-Track Intensity at
TB (hPa)
Mean radius of gale force winds at TB(km)
Post-ET Warm-
seclusion
6 32.5 -72.7 982.0 259.8
Post-ET Cold-core
15 36.2 -57.9 986.5 171.1
T-test: 90% T-test: 95%
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Eliassen-Palm (EP) Flux and its Divergence
Outward eddy momen-tum flux
Outward eddy heat flux
Analyses performed by Clark Evans
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EP- Flux
All Strengthening Weakening Cold-Core Warm-Seclusion
Outward eddy momen-tum flux
Outward eddy heat flux
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Summary• A well-defined 34-member ensemble mean trajectory through
cyclone phase space is calculated for ET in the North Atlantic.
• TC diabatic PV destruction aloft leads to a lifting of the mid-latitude tropopause, erosion and narrowing of the approaching trough
• TC advects an environment into the trough that has static stability 10-20% lower than prior to TC arrival, enhancing Eady growth rate.
• Variability from this mean trajectory is small in the tropical phase, and then increases dramatically once extratropical transition has completed:– cold-core intensifying/decay, warm-seclusion, merger, tropical.
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Summary• Post-ET Weakening:
– Positively tilted UL trough, SSTs near normal and below 26.5C on average
• Post-ET Strengthening:– Negatively tilted UL trough, SSTs above normal and above 26.5C on average
• Post-ET Cold-core evolution:– Broad UL trough, considerably smaller than average TC size
• Post-ET Warm-seclusion evolution:– Narrowing UL trough, considerably larger than average TC size, scale
matching (Molinari et al. 1995; Hanley et al. 2001).
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Summary• Introduction of trough into TC leads to eddy PV forcing. The adiabatic
secondary circulation that results (Molinari et al. 1995) attempts to restore thermal wind balance.
• The momentum component of the EP forcing far precedes the thermal flux component.
• Thus, it appears that the development of frontal structure (increase in ‘B’) within the TC during ET may be initially a consequence of the TC’s adiabatic response to the eddy momentum forcing
• This eddy forcing is over a deeper layer and at lower isentropic level than with Elena-type rapid intensification.
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Summary• Post-ET intensifiers have a marked increase in the magnitude of eddy PV flux
compared to weakeners
• Post-ET warm seclusion is associated with a narrower depth of cyclonic eddy PV flux at a level comparable to Molinari et al. (1995)
• Speculation: Whether a trough interaction with a TC leads to RI or ET and warm-seclusion is a matter of timing of the interaction during the cyc. phase trajectory
• With an average track error of 300-500km at 3-5 days, and the subtle sensitivities just shown, it is evident why the long-wave pattern decreases markedly during ET