CLIMAS QUENTES CLIMA EQUATORIAL. CLIMA EQUATORIAL GRÁFICO TERMOPLUVIOMÉTRICO.
Global Distribution of Equatorial Plasma Bubbles in the Pre-midnight Sector 3 Mar. 2005 Jaeheung...
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Transcript of Global Distribution of Equatorial Plasma Bubbles in the Pre-midnight Sector 3 Mar. 2005 Jaeheung...
Global Distribution of Equatorial Plasma Bubbles in the Pre-
midnight Sector
3 Mar. 2005Jaeheung PARK
What is EPB?
• Equatorial Plasma Bubble : sharp decrease of plasma density in equatorial region
-40 -30 -20 -10 0 10 20 300.0
2.0x105
4.0x105
6.0x105
8.0x105
Space Physics Package, STSAT-1Nov. 19, 2003
geographic latitude (deg)
pla
sma
de
nsi
ty (
cm-3)
h Km 400 800 Altitude
B gauss 0.5 0.4 Total intensity of Earth’s magnetic induction
no cm-3 2108 2106 Concentration of neutral particles
n+ cm-3 106 105 Concentration of positive ions
n+/no cm-3 510-3 510-2 The ratio of n+ to no
Tn K 1400 1400 Temperature of neutral gas
T+ K 1600 2200 Temperature of positive ions
Te K 2800 3000 Temperature of electrons
D cm 0.4 1 Electron Debye length
o cm 2106 2108 The neutral particle mean free path
e+ cm 1105 1106 The electron-ion mean free path
+ cm·sec-1 1.3105
1.8105
Mean positive ion thermal velocity
e cm·sec-1 3107 3107 Mean electron thermal velocity
+ cm 5102 7102 Mean positive ion Larmor radius
e cm 3 4 Mean electron Larmor radius
+o sec-1 610-2 910-4 The positive ion-neutral gas collision frequency
eo sec-1 2.5 210-2 The electron-neutral gas collision frequency
e+ sec-1 3102 3101 The electron-positive ion collision frequency
+ sec-1 2102 3102 The positive ion angular gyro-frequency
e sec-1 9106 7106 The electron angular gyro-frequency
General Features of EPB
• Scale lengths : several meters ~ several hundred kilometers
• Local time : sunset to sunrise
• Field-aligned structure
• Forming a vertical channel
• Adverse effects on the radio communication
micro-structure wave scattering
Rayleigh-Taylor instability
• When heavy fluid sits above lighter fluid in a gravitational field
• Bubbles of light fluid rise into the heavier medium
1( - ) -
FFgz F NP V U L
e mE F F F zNP eff
Generalized Rayleigh-Taylor instability
F-region Pedersen conductivity
F-region plasma density
; Kil et al. [2004]
vertical drift speed
F-region dynamo
; Fejer et al. [1999]
Recombination loss
Observational Instruments
• date of launch : Dec. 21, 1999 (near the solar maximum)
• sun-synchronous orbit : fixed at 2250 LT
• altitude : 685 km
• plasma density and electron temperature
(1) KOMPSAT-I ( KOREA )
(2) DMSP F15 (U.S.)
• sun-synchronous orbit : fixed at 2130 LT
• altitude : 840 km
• electron density, electron temperature, ion fraction, and drift speed
DMSP F15
KOMPSAT-1
Seasonal-Longitudinal distribution of EPBs
① ②③ ④ ⑤
Sunset-node theory of Tsunoda (1985)
1( - ) -
FFgz F NP V U L
e mE F F F zNP eff
Generalized Rayleigh-Taylor instability
F-region Pedersen conductivity
F-region plasma density
; Kil et al. [2004]
vertical drift speed
F-region dynamo
; Fejer et al. [1999]
Global verification using in-situ measurements
Fig. GUVI disk-scan image in February and August, 2002.
evening prereversal enhancement (EPE)
vertical drift speed
F-region dynamo
; Fejer et al. [1999]
0 60 120 180 240 300 3600
10
20
30
40
50
geographic longitude (deg)
0
1x105
2x105
3x105
correlation coefficient : 0.79
0.0
0.2
0.4
0.6
0.8
1.0
correlation coefficient : 0.15
vz (
m/s
)ni
(cm
-3)
frac
tiona
l en
coun
ter
of E
PB
s
vernal equinoxKOMPSAT-1
0 60 120 180 240 300 3600
10
20
30
40
50
geographic longitude (deg)
0
1x105
2x105
3x105
0.0
0.2
0.4
0.6
0.8
1.0
vz (
m/s
)ni
(cm
-3)
frac
tiona
l en
coun
ter
of E
PB
s
vernal equinoxDMSP F15
correlation coefficient : 0.59
correlation coefficient : 0.86
0 60 120 180 240 300 3600
10
20
30
40
50
0
1x105
2x105
3x105
0.0
0.2
0.4
0.6
0.8
1.0
geographic longitude (deg)
June solsticeKOMPSAT-1
correlation coefficient : 0.78
correlation coefficient : 0.52
frac
tiona
l en
coun
ter
of E
PB
sni
(cm
-3)
vz (
m/s
)
0 60 120 180 240 300 3600
10
20
30
40
50
0
1x105
2x105
3x105
0.0
0.2
0.4
0.6
0.8
1.0
geographic longitude (deg)
June solsticeDMSP F15
frac
tiona
l en
coun
ter
of E
PB
sni
(cm
-3)
vz (
m/s
)
correlation coefficient : 0.85
correlation coefficient : 0.77
0 60 120 180 240 300 3600
10
20
30
40
50
0
1x105
2x105
3x105
frac
tiona
l en
coun
ter
of E
PB
sni
(cm
-3)
vz (
m/s
)
geographic longitude (deg)
0.0
0.2
0.4
0.6
0.8
1.0
December solsticeKOMPSAT-1
correlation coefficient : 0.27
correlation coefficient : 0.55
0 60 120 180 240 300 3600
10
20
30
40
50
0
1x105
2x105
3x105
frac
tiona
l en
coun
ter
of E
PB
sni
(cm
-3)
vz (
m/s
)
geographic longitude (deg)
0.0
0.2
0.4
0.6
0.8
1.0
December solsticeDMSP F15
correlation coefficient : 0.45
correlation coefficient : 0.66
American
Atlantic American
Atlantic
Magnetic declination angle?
Fig. Composite GUVI 135.6-nm scan image at 2150 LT on Jan. 29, 2002.
The background plasma density is higher in the south
But the northern anomaly is stronger than the southern anomaly
TIMED/GUVI disk-scan images at nighttime show large longitudinal and seasonal variations in the OI 135.6-nm radiance. The intensity of the anomaly does not precisely conform to the intensity of the background. The GUVI observations indicate that the F-region morphology near the F peak can be different from the morphology on the topside that has been extensively studied using DMSP data.
0.0 0.2 0.4 0.6 0.8 1.0
1x105
2x105
3x105
correlation coefficient: 0.58
pla
sma
de
nsi
ty (
cm-3)
fractional EPB encounter
DMSP F15
green : vernal equinoxred : June solsticeblue : December solstice
0.0 0.2 0.4 0.6 0.8 1.010
20
30
40
50
DMSP F15
green : vernal equinoxred : June solsticeblue : December solstice
fractional EPB encounterve
rtic
al d
rift
sp
ee
d (
m/s
)
correlation coefficient: 0.69
Conclusions
1. The S/L distribution of EPBs was common to both KOMPSAT-1 and DMSP F15, whose orbits have different local times and altitudes.
2. The importance of ambient plasma density and vertical drift speed was verified globally.
3. Their relative influences were proved to be dependent on the season.
1. March equinox : drift-dominated2. June solstice : density-dominated3. December solstice : possible dominated by bottomside
phenomena
Plasma blobs?
-40 -30 -20 -10 0 10 20-1
0
1
2
3
1000
1200
1400
1600
1800
ele
ctro
n te
mp
era
ture
(K
)
pla
sma
de
nsi
ty (
105
/cc)
geographic latitude (deg)26 Feb 2001
plasma blob
-40 -30 -20 -10 0 10 20-100000
0
100000
200000
300000
1000
1200
1400
1600
1800
10 Feb 2001
plasma blob
ele
ctro
n te
mp
era
ture
(K
)
pla
sma
de
nsi
ty (
/cc)
geographic latitude (deg)
KOMPSAT-1 DMSP-F15
S/L distribution