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“CONVECTIVE CLOUDS SPACE AND TIME
ORGANIZATION: THE REGIONAL
DIFFERENCES”
Wagner Flauber Araújo Lima
and
Luiz Augusto Toledo Machado
CHUVA International Workshop
CHUVA International Workshop
Objective
Investigate the space and time organization ofthe convective clouds and rain cells during theCHUVA campaigns.
CHUVA International Workshop
Methodology Fortracc Satellite set up
Minimum Size: 20 pixels = 320km²;
Field : Brightness Temperature Ch4 (K);
Spatial resolution = 4km;
Threshold BT = 235 K ;
Sites
Fortaleza;
Belém;
Vale;
Santa Maria;
Average Direction of Propagation and Speed of Convective Systems
FORTRACC SATELLITE
Frequencies of Convective Systems in (4 x 4) km area during CHUVA Campaigns
FORTRACC SATELLITE
Frequencies of Convective Systems in (4 x 4) km area during CHUVA-VALE Campaign
FORTRACC SATELLITE
Average Direction of Propagation and Speed of CS during CHUVA-VALE Campaign
FORTRACC SATELLITE
Histogram Size of the Convective System during CHUVA Campaigns
FORTRACC SATELLITE
0%
5%
10%
15%
20%
25%
30%
11 16 22 32 45 63 89 126 178 251 355 501 708 1000
Fre
qu
en
cy (%
)
Convective System Radius (km)
Histogram Size of the CS for CHUVA
Fortaleza Belém Vale Santa Maria
Histogram Life Cycle Duration of the Convective System during CHUVA Campaigns
FORTRACC SATELLITE
0%
2%
4%
6%
8%
10%
12%
14%
0.75 1.50 2.25 3.00 3.75 4.50 5.25 6.00 6.75 7.50
Fre
qu
en
cy (
%)
Life Cycle Duration (hours)
Histogram Life Cycle Duration of the CS in Site CHUVA
Fortaleza Belém Vale Santa Maria
CHUVA International Workshop
Conclusions MCSs in Santa Maria are faster than any other region;
The frequency of occurrence are normally associated with orography
or on the coast as in Fortaleza.
Size distribution for all regions are very close, Santa Maria presents
the larger , followed by Belém.;
The Life Time durations are also very close among all regions.
Further investigations with radar will give a better understand of the
physical processes associated to the regions.
CHUVA International Workshop
Studies Underway
Space-Time organization of the rain cells- XPOL Radar and
FORTRACC;
Reflectivity profiles as function of the Life Cycle – Regional differences;
0
2
4
6
8
10
12
14
16
18
20
0.0 5.0 10.0 15.0 20.0 25.0 30.0 35.0 40.0 45.0
Centróides Convectivo
G1
G2
G3
G4
G5
0
1
2
3
4
5
6
7
8
9
10
0.0 5.0 10.0 15.0 20.0 25.0
Centróides Nuvens Quentes
G1
G2
G3
0
2
4
6
8
10
12
14
16
18
20
0.0 5.0 10.0 15.0 20.0 25.0 30.0 35.0 40.0
Centróides Banda Brilhante
G1
G2
G3
G4
G5
Radar Banda-X :
Zdr;
R(dBZ);
Kdp;
Fortracc –Radar :
Cappi in 2km;
Threshold : Dbz > 1;
Size > 100 pixels ( 4 km²);
CHUVA International Workshop
Next Steps MCS Life cycle and convective cloud cover and theirs relations to the
dynamics and thermodynics properties (moisture convergene, upper level
divergence, CAPE, CINE, etc.). The regional differences.
Parameter;
CAPE;
CINE;
Div. Humidity ;
Div. Wind;
Variables;
Rain;
Clouds Cover;