Convective-scale diagnostics Rob Rogers NOAA/AOML Hurricane Research Division.
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Transcript of Convective-scale diagnostics Rob Rogers NOAA/AOML Hurricane Research Division.
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Convective-scale diagnostics
Rob RogersNOAA/AOML Hurricane Research Division
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• Advances in forecasts of tropical cyclone (TC) intensity, and rapid intensity change (RI) in particular, lag advances in TC track forecasts
• Multiscale nature of these processes major reason for this• environmental - O(1000 km) - troughs, shear• vortex - O(1-100 km) - symmetric/asymmetric dynamics, VRWs• convective – O(1 km) – convective bursts, vortical hot towers• turbulent – O(1-100 m) - surface fluxes, entrainment/detrainment• microscale – O(1mm) -- hydrometeor production, latent heat release
• Large-scale fields generally explain about 35% of skill in RI forecasts (e.g., RI index). How much can smaller-scale processes explain?
• Numerical model forecasts of rapid intensity change (RI) should improve as resolution increases
• For some cases it does, in others it does not – why?
• Robust diagnostic techniques for isolating impacts of physical processes of various scales on RI important for improved physical understanding, model evaluation and improvement
Motivation
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Kaplan et al. 2009
35% of skill explained by Rapid Intensification
Index (RII)
Motivation
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Summary of diagnostics
Vortex-scale diagnostics• test of initial vortex structure, environment-vortex-convective interactions, resolution• symmetric structure of tangential, radial, vertical wind
• radial distribution• vertical structure• time evolution
Convective-scale diagnostics• test of physical parameterizations (microphysical, convective), resolution • statistics of vertical motion, mass flux
• time-height vertical profiles• vertical structure of distributions• time evolution of distributions
• masking with 0.1 g/kg hydrometeor concentration used to approximate Doppler sensitivity and facilitate comparison with observations
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40
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2005
-08-
27_0
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:00
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-08-
27_0
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-08-
27_1
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:00
2005
-08-
27_1
8:00
:00
2005
-08-
28_0
0:00
:00
2005
-08-
28_0
6:00
:00
2005
-08-
28_1
2:00
:00
2005
-08-
28_1
8:00
:00
2005
-08-
29_0
0:00
:00
2005
-08-
29_0
6:00
:00
2005
-08-
29_1
2:00
:00
Peak
win
d (k
t)
27-9 km
9-3 km
BT
40
60
80
100
120
140
160
RI BTRI 9:3 km RI 27:9 km
• Hurricane Katrina (2005) • Underwent RI from Cat 3 to Cat 5 as it traversed Gulf of Mexico• Both resolutions produced RI, but both delayed• Good observational coverage (multiple P-3 flights with Doppler)
Example
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00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
50 100 150 200
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
50 100 150 20000Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
50 100 150 200
0
5
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0
5
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0
5
10
15
20
25
30
35
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50
55
radius (km)
radius (km) radius (km)
RI
RI
RI
Time-radius Hovmoller of axisymmetric 10-m wind from H*Wind and HWRF-x
Vortex-scale diagnostics: Wind field size & structure
H*Wind
HWRF-x 27:9 km HWRF-x 9:3 km
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IKE
0
20
40
60
80
100
120
140
8/27
00Z
8/27
03Z
8/27
06Z
8/27
09Z
8/27
12Z
8/27
15Z
8/27
18Z
8/27
21Z
8/28
00Z
8/28
03Z
8/28
06Z
8/28
09Z
8/28
12Z
8/28
15Z
8/28
18Z
8/28
21Z
8/29
00Z
8/29
03Z
8/29
06Z
8/29
09Z
8/29
12Z
IKE
(TJ)
IKE_H values for Hurricane Katrina
IKE_H 9:3km
IKE_H 27:9km
IKE_H H*Wind
0
50
100
150
200
250
8/27
00Z
8/27
03Z
8/27
06Z
8/27
09Z
8/27
12Z
8/27
15Z
8/27
18Z
8/27
21Z
8/28
00Z
8/28
03Z
8/28
06Z
8/28
09Z
8/28
12Z
8/28
15Z
8/28
18Z
8/28
21Z
8/29
00Z
8/29
03Z
8/29
06Z
8/29
09Z
8/29
12Z
IKE
(TJ)
IKE_TS values for Hurricane Katrina
IKE_TS 9:3km
IKE_TS 27:9km
IKE_TS H*Wind
0
50
100
150
200
250
0
20
40
60
80
100
120
140
obs 9:3 km obs 9:3 km27:9 km 27:9 km
Time series of integrated kinetic energy (IKE) for 10-m winds thresholded by tropical storm and hurricane force winds from H*Wind and HWRF-x
Vortex-scale diagnostics: Wind field size & structure
IKE thresholded by tropical storm-force winds IKE thresholded by hurricane-force winds
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25 50 75 100
2
4
6
8
10
12
14
16
hei
gh
t (k
m)
2
4
6
8
10
12
14
16
2
4
6
8
10
12
14
16
25 50 75 100 25 50 75 100
25 50 75
2
4
6
8
10
12
14
16
hei
gh
t (k
m)
2
4
6
8
10
12
14
16
2
4
6
8
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12
14
16
25 50 75 100 25 50 75 100100
radius (km)
radius (km)
radius (km)
radius (km)
radius (km)
radius (km)
Axisymmetric tangential (shaded, m s-1) and radial wind (contour, m s-1) for Doppler and HWRF-x
20:08Z 8/27
19:23Z 8/28
00Z 8/28
03Z 8/29
00Z 8/28
03Z 8/29
27:9 km 9:3 kmDoppler
27:9 km 9:3 kmDoppler
Vortex-scale diagnostics: Vertical structure of axisymmetric vortex
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20
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2005
-08-
27_0
0:00
:00
2005
-08-
27_0
6:00
:00
2005
-08-
27_1
2:00
:00
2005
-08-
27_1
8:00
:00
2005
-08-
28_0
0:00
:00
2005
-08-
28_0
6:00
:00
2005
-08-
28_1
2:00
:00
2005
-08-
28_1
8:00
:00
2005
-08-
29_0
0:00
:00
2005
-08-
29_0
6:00
:00
2005
-08-
29_1
2:00
:00
2-km
RM
W (k
m)
RMW (27-9 km)RMW (9-3 km)RMW (Dop)
20
30
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60
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80
90
100
110
obs 9:3 km 27:9 km
Time series of radius of peak axisymmetric tangential wind at 2 km altitude (km) from Doppler and HWRF-x
Vortex-scale diagnostics: Time evolution of vortex size
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50 100 150 200
radius (km)
25 75 125 17550 100 150 200
radius (km)
25 75 125 175
50 100 150 200
radius (km)
25 75 125 17550 100 150 200
radius (km)
25 75 125 175
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
RI RI
RI RI
Time-radius Hovmoller of axisymmetric tangential wind and vertical velocity at 5.1 km altitude
27:9 km
9:3 km
27:9 km
9:3 km
ut
ut
w
w
Vortex-scale diagnostics: Time evolution of axisymmetric vortex size
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50 100 150 200
radius (km)
25 75 125 17550 100 150 200
radius (km)
25 75 125 175
50 100 150 200
radius (km)
25 75 125 17550 100 150 200
radius (km)
25 75 125 175
2
4
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16
hei
gh
t (k
m)
18
2
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6
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12
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hei
gh
t (k
m)
18
2
4
6
8
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14
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hei
gh
t (k
m)
18
2
4
6
8
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16
hei
gh
t (k
m)
18
Axisymmetric tangential wind (shaded, m s-1) and vertical velocity (contour, m s-1)
27:9 km
27:9 km
9:3 km
9:3 km
00Z 8/28
03Z 8/29
00Z 8/28
03Z 8/29
Vortex-scale diagnostics: Vertical structure of axisymmetric vortex
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-3
-2
-1
0
1
2
3
4
5
6
2005
-08-
27_0
0:00
:00
2005
-08-
27_0
6:00
:00
2005
-08-
27_1
2:00
:00
2005
-08-
27_1
8:00
:00
2005
-08-
28_0
0:00
:00
2005
-08-
28_0
6:00
:00
2005
-08-
28_1
2:00
:00
2005
-08-
28_1
8:00
:00
2005
-08-
29_0
0:00
:00
2005
-08-
29_0
6:00
:00
2005
-08-
29_1
2:00
:00
eyew
all s
lope
(km
/km
)2-8 km slope (27-9 km)2-8 km slope (9-3 km)2-8 km slope (Dop)
-3
-2
-1
0
1
2
3
4
5
6
obs 9:3 km 27:9 km
Time series of 2-8 km altitude eyewall slope (km km-1) from Doppler and HWRF-x
Vortex-scale diagnostics: Time evolution of vortex vertical structure
Outward slope with height
Inward slope with height
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Wind speed (m/s) at 2-km altitude
Vorticity (shaded, x 10-3 s-1) and w
(contour, m/s) at 4-km altitude
Doppler 27:9 km HWRF-x 9:3 km HWRF-x
5010
015
00
5010
015
00
5010
015
00
5010
015
00
5010
015
00
500
0
-2
-1
1
3
5
7
2
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6
35
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60
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45
55
65
distance (km)
dis
tan
ce (
km)
distance (km)
dis
tan
ce (
km)
distance (km)
dis
tan
ce (
km)
distance (km)
dis
tan
ce (
km)
distance (km)
dis
tan
ce (
km)
distance (km)
dis
tan
ce (
km)
2038-2231 UTC 8/28 0000 UTC 8/29 0000 UTC 8/29
Vortex- and convective-scale diagnostics: Wind speed, vertical motion, and vorticity
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Time series of mean updraft/downdraft velocity (m s-1) profiles in 4° box with maskingh
eig
ht
(km
)
2
4
6
8
10
12
14 Updraft 27:9 kmRI
hei
gh
t (k
m)
2
4
6
8
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12
14 Updraft 9:3 kmRI
hei
gh
t (k
m)
2
4
6
8
10
12
14 Downdraft 27:9 kmRI
hei
gh
t (k
m)
2
4
6
8
10
12
14 Downdraft 9:3 kmRI
Convective-scale diagnostics: Time evolution of vertical profiles
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Time series of aggregate updraft/downdraft vertical mass flux (x 1010 kg s-1) profiles in 4° box with masking
hei
gh
t (k
m)
2
4
6
8
10
12
14 Downdraft 9:3 km
hei
gh
t (k
m)
2
4
6
8
10
12
14 Updraft 27:9 kmRI
hei
gh
t (k
m)
2
4
6
8
10
12
14 Downdraft 27:9 kmRI
hei
gh
t (k
m)
2
4
6
8
10
12
14 Updraft 9:3 kmRI
RI
Convective-scale diagnostics: Time evolution of vertical profiles
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hei
gh
t (k
m)
2
4
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18
-6 -4 -2 0 2 4 6 8 10
vertical velocity (m/s)
12
1 km
-2 -1 0 1 2 3 4 5
vertical velocity (m/s)
6
10
20
30
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0
per
cen
tag
e
14 km
-2 -1 0 1 2 3 4 5 6vertical velocity (m/s)
5
10
15
20
25
30
35
40
0
per
cen
tag
e
vertical velocity
Convective-scale diagnostics: Contoured frequency by altitude diagram (CFAD)
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hei
gh
t (k
m)
hei
gh
t (k
m)
12
2
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-6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s)
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-6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s)
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-6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s)
2
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-6 -4 -2 0 2 4 6 8 10
vertical velocity (m/s)
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-6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s)
2
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-6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s)
Vertical velocity CFADs for Doppler radar and HWRF-x with masking
20:08Z 8/27
22:31Z 8/28
12Z 8/27
12Z 8/28
12Z 8/27
12Z 8/28
27:9 km
27:9 km
9:3 km
9:3 km
Doppler
Doppler
Convective-scale diagnostics: Contoured frequency by altitude diagram (CFAD)
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00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 30
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 30
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 30
00Z Aug 27
12Z Aug 27
00Z Aug 28
12Z Aug 28
00Z Aug 29
12Z Aug 29
00Z Aug 30
-6 -4 -2 0 2 4 6 8 10 12 -6 -4 -2 0 2 4 6 8 10 12
-6 -4 -2 0 2 4 6 8 10 12 -6 -4 -2 0 2 4 6 8 10 12
vertical velocity (m/s) vertical velocity (m/s)
vertical velocity (m/s) vertical velocity (m/s)
14 km alt 27:9 km
5 km alt 27:9 km
14 km alt 9:3 km
5 km alt 9:3 km
Time series of vertical velocity distribution (%) at 5- and 14-km altitudes with masking
RI
RI
RI
RI
Convective-scale diagnostics: Time evolution of distributions
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0
0.5
1
1.5
2
2.5
3
3.5
4
0
0.5
1
1.5
2
2.5
3
3.5
4
area
(x
104 k
m2)
area
(x
104 k
m2)
Time series of areal coverage (x 104 km2) of threshold values of 3-7 km vertical velocity in 4x4 deg box with masking
27:9 km 9:3 km1 m s-1
2 m s-1
3 m s-1
1 m s-1
2 m s-1
3 m s-1RI RI
Convective-scale diagnostics: Time evolution of convective coverage
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Summary• convective- and vortex-scale diagnostics can reveal much about inner-core structure and evolution from model and observations
• RMW, size of wind field at various thresholds, integrated kinetic energy• secondary eyewall, outer rainband evolution, eyewall slope• vertical velocity and mass flux profiles• vertical structure of vertical velocity distributions• time evolution of vertical velocity distributions
• differences between HWRF-x and observations for Katrina case• both resolutions produced RI, but both were delayed. 9:3 km was sooner, stronger than 27:9 km • vortex-scale
• RMW broader, outer wind field smaller in model compared to observations• both resolutions produced outer updraft maxima, 9:3 km produced hint of
contracting secondary eyewall• eyewall slope generally less for 9:3 km than 27:9 km, more time evolution
• convective-scale • mean updraft profiles peaked at higher altitude, downdrafts stronger in 9:3 km• stronger updraft and downdraft mass flux in 9:3 km• stronger updraft/downdraft, vorticity cores in 9:3 km
• all these quantities readily calculated from HWRF-x, airborne Doppler, and H*Wind analyses
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Future work
• include azimuthal asymmetries
• partition into precipitation structure regimes (eyewall/rainband/stratiform)
• finer-scale diagnostics (turbulent, microphysical) from model and observations
• broaden to multi-case diagnostics – normalization issues?
• ensemble-based diagnostics