Direct and Indirect Thermospheric Heating Sources for Solar Cycles 21-23

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Direct and Indirect Thermospheric Heating Sources
Daily Average Power Values for Solar Cycles 21-23
for Solar Cycles 21-23
Academy Department of Physics
2Space
Weather Technologies
Mar
1989
NORAD
Space
Tracking
Disrupted
SKYLAB
Reenters
ABSTRACT: We use a trio of empirical models to estimate the
relative contributions of solar extreme ultraviolet (EUV) heating,
Joule heating and particle heating to the global energy budget of the
earth’s upper atmosphere over the last three solar cycles. Daily
power values are derived from models of three sources. The
SOLAR2000 solar irradiance specification model provides estimates
of the daily extreme EUV solar power input. Geomagnetic power
comes from a combination of satellite-derived particle precipitation
power and an empirical model of Joule power derived from
hemispherically-integrated estimates of high-latitude heating, which
we discuss in this paper. Since 1975 the average daily contributions
from the three sources have been: particles ~36 GW, Joule ~95 GW
and solar ~464 GW. Joule and particle heating combine to provide
more than 22% of the total global upper atmospheric heating and
more than one third of the variability in the heating. During solar
minimum the variability of the Joule power dominates total
variability. During solar maximum the variability in the Joule power
is approximately that of the solar power variability. In the top 15
heating events geomagnetic power contributed more than 66% of the
total power budget. During all of these events the Joule power alone
exceeded solar power. We will briefly discuss our methods of deriving
the power estimates. We will also provide quantitative comparisons
with the largest storms of the last three solar cycles in terms of total
values and temporal profiles of estimated heating.
Acknowledgements: NOAA Space Environment Center,
NASA OMNIWEB Danish Meteorological Institute,
World Data Center, Kyoto University
Ref: Knipp et al., Solar Physics, In Press, Oct 2004
Power (GW)
Altitude Observatory
•Electrons from
•POES 50 eV - 20 keV,
•DMSP 30 eV- 30 keV
•Low energy ions from POES also
included
6 Nov
2000
2001
30
2003
AMIE JH
900
predicted JH
800
Solar Power
1500
Total
Power
700
600
Slow Flow
High Speed Stream
Magnetic Cloud
South
North
500
400
300
200
0
18.0
500
Joule
Power
18.5
19.0
19.5
Particle
Power
0
1973 1975 1977 1979 1981 1983 1985 1987 1989 1991 1993 1995 1997 1999 2001 2003 2005
Year
Daily Average Power Values for Solar Cycles 21-23
2500
20.0
20.5
21.0
21.5
22.0
22.5
23.0
Day of Month
Table 1. Fit Coefficients for Joule Power
Fit Season Months
Fit Using Absolute Values of PC and Dst
R2
Annual
Jan-Dec
JH(GW)=24.89*PC + 3.41*PC2 +.41*Dst + .0015*Dst2
0.76
Winter
21 Oct-20 Feb
JH(GW)=13.36*PC + 5.08*PC2 +.47*Dst + .0011*Dst2 0.84
Summer
21Apr-20 Aug JH(GW)=29.27*PC + 8.18*PC2 -.04*Dst + .0126*Dst2
0.78
Equinox
21Feb-20Apr,
21Aug-20Oct
JH(GW)=29.14*PC + 2.54*PC2 +.21*Dst + .0023*Dst2
0.74
14 Jul 1982
2000
Summary of Average Power and Variability
13 Mar 1989
6 Nov 2001
10 May 1992
Power Category:
1500
30 Oct 2003
Power Category:
Solar Min: 75-77,
83-87, 93-98
Solar Cycles
21-23
Solar Max: 78-82,
88-92, 99-03
Top 5% of
power events
Top 1% of
power events
1000
Joule
Power
500
0
1973
1975
1977
1979
1981
1983
Avg
St Dev
Avg
St Dev
Avg
St Dev
Avg
St Dev
Avg
St Dev
1985
Particle
(GW)
38 (8%)
21
36 (6%)
24
35 (5%)
23
73 (7%)
36
104 (7%)
44
1987
1989
Joule
(GW)
77 (16%)
63
95 (16%)
93
112 (16%)
111
331 (30%)
226
638 (45%)
306
1991
1993
Solar
(GW)
359Power
(76%)
Solar
46
464 (78%)
135
562 (79%)
116
687 (63%)
116
691 (48%)
113
1995
1997
Total
(GW)
474
101
596
190
710
182
1090
226
1433
313
1999
2001
Partic
Powe
2003
200
Year
Solar Min: 75-77,
83-87, 93-98
Solar Cycles
21-23
Solar Max: 78-82,
88-92, 99-03
Top 5% of
power events
Top 1% of
power events
Year
Daily Average Power Values for Max of Solar Cycle 23
Joule Power*2
Electron Pcp Power*2
Sum
Solar Power
3000
Jul 15&16
2000
Aug 12
2000
Mar 31
2001
Nov 6 Nov 24
2001 2001
Oct 29 &30
2003
Nov 20
2003
2500
2000
1500
1000
0
2000
2001
2002
Year
2003
2004
Avg
St Dev
Avg
St Dev
Avg
St Dev
Avg
St Dev
Avg
St Dev
Particle
(GW)
38 (8%)
21
36 (6%)
24
35 (5%)
23
73 (7%)
36
104 (7%)
44
Joule
(GW)
77 (16%)
63
95 (16%)
93
112 (16%)
111
331 (30%)
226
638 (45%)
306
Solar
(GW)
359 (76%)
46
464 (78%)
135
562 (79%)
116
687 (63%)
116
691 (48%)
113
Total
(GW)
474
101
596
190
710
182
1090
226
1433
313
Top 15 power events of the last 3 solar cycles
1979
1982
1982
1982
1989
1989
1991
1992
2000
2000
2000
2001
2001
2003
2003
500
•NOAA TIROS southern hemisphere
particle data used in particle power
calculation
AMIE Joule Heating Compared to Predicted Joule Heating for
October 1995
1000
100
Power (GW)
of F10.7 for coronal emission and
the Magnesium II (Mg II) core to
wing ratio for chromospheric
emission and irradiance
measurements from TIMED
•Thermospherically effective
irradiances (Wm-2) modeled at 1 nm
resolution between 1 and 106 nm at
one AU
•Model energy deposition is in the
150-200 km range for almost all
levels of solar activity, integrated
over the dayside
14 Jul
Oct
Japanese
Satellite
Malfunction
Attributed
to Satellite
Drag
2000
1000
Procedure:
•Estimate solar EUV input using daily power estimates from
SOLAR2000 Research Grade version 2.22a
1975-2003
•Estimate Joule heating from ground indice proxies
1975-2003 (see box at top right)
•Estimate particle heating from NOAA TIROS and DMSP data
1979-2003
•Uses solar irradiance proxy inputs
•SOLAR2000 Research Grade
version 2.22a spectral irradiance
used in solar power calculation
Jul
1982
2500
Power (GW)
3High
3000
Joule Heating (GW)
D. J. Knipp1, W. Kent Tobiska2 and B. Emery3
1USAF
Joule Power Estimate Procedure
Multiple Linear Regression Fit of Polar Cap Index and Dst
hourly values to 13,000+ estimates of integrated
hemispheric Joule heating rates from the AMIE procedure
3500
Month/
Particle
Day
Pwr (GW)
25-Apr
152
13-Jul
183
14-Jul
159
6-Sep
267
13-Mar
290
21-Oct
147
5-Jun
126
10-May
162
15-Jul
173
16-Jul
51
12-Aug
129
31-Mar
144
6-Nov
122
29-Oct
185
30-Oct
156
Avg
163
Joule
Pwr (GW)
1154
900
2035
941
1576
1059
1082
1484
1083
1144
1040
878
1518
918
1214
1202
Solar
Pwr (GW)
502
690
739
609
732
668
717
459
652
676
612
805
754
760
758
675
Total
Pwr (GW)
1808
1772
2932
1817
2599
1874
1924
2105
1909
1871
1781
1826
2394
1863
2128
2038
Rank % Joule
Pwr
13
64
15
51
1
69
12
52
2
61
8
56
6
56
5
71
7
57
9
61
14
58
11
48
3
63
10
49
4
57
59
% Joule
+ Particle Pwr
72
61
75
66
72
64
63
78
66
62
66
64
74
59
64
67
Summary:
Solar wind forcing competes with and at times exceeds
solar radiative forcing; thereby adding a significant
component of variability to the solar cycle impressed upon
the upper atmosphere. When geomagnetic sources are
accounted for, the peak upper atmospheric heating events
are more extreme than those from solar EUV input only.
Further, the solar maxima intervals expand to include
broad shoulders of solar wind-driven heating from
geomagnetic storms.
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