experience periodic heating at the HF modulation. = (4) frequency. Since the ionospheric conductivity is electron temperature dependent, the conductivity This current is a source of -frequency radiation, under oes a similar periodic variation. Natura
For perfectly localized orbitals, the basins of ELF are the domains in which ... Electron localization function (ELF); maximum probability; localized orbitals; basins.
Nov 16, 1998 - Abstract. This paper describes the results of a prelim- inary study to determine the effective heating and cooling time constants of ionospheric ...
and if we introduce dÎ¾=[Î´ Î¸]T the following relationship holds. 0. = +. + Î» Î¾ Î» Î¾ dg. dVg dg. V ..... and Controlâ, Draft, North American Electric Reliability Council,.
the solar wind often cause communication disruptions as well as observable phenomena such as the .... sensor boom deployment and spacecraft spin-up. ..... The authors wish to thank Dr. Jan J. Sojka for his contributions to the research.
Jan 12, 1987 - approximately one chord length the wing tip. ... 0.005 inch diameter tungsten wire and located 18" two-dimensional ... negative 16 m movie film was exposed via a 50 mm ..... coherent vortex is extended to 580 for a+ - 0.b.
... firms could improve their efficiency by such a way that it replicates the input combinations of the ... main interest in this study is to estimate the technical efficiency of the .... and large, and estimate efficiency scores for each of the cate
Nov 9, 2016 - Global Navigation Satellite System (GNSS) satellite-receiver links traveling through the ..... from a synchronous satellite would be less than 5â¦.
[PDF] The Shelf Elf [EBOOK]
Oct 24, 2016 - labeling proteins on the cell surface15 because of cross-reactivity ... Chapman and co-workers to label the bacterial cytoskeletal protein FtsZ ...
been set up to comply with the requirement of ISO/IEC 17025 and covers the ... types of measurement (electric and magnetic field) which are described in IEC 61786 ... The AC source provided the required value of the current free of harmonics.
locity filter effect (Rosenbauer et al., 1975). If the dayside reconnection is ..... S. W. H., and Lühr, H.: Ionospheric signatures of pulsed dayside reconnection at the ...
For determining the lower heating value, LHV, calculation is needed to deduct the heat of condensation from the HHV. In US engineering practice, HHV is generally used for steam plants, while in the European practice, efficiency calculations are based
solidearth.jpl.nasa.gov/GESS/3123_GESS_Rep_ 2003.pdf.  HU ... ISBN: 978-3-8007-4228-8 /ISSN: ... Qilei ZHANG was born in 1984 and received the B.S..
time behaviour by using the latest SWACI TEC maps, the TEC gradient estimated by the regional. NTCM model, and the sub-sequent correction for geomagnetic / ionospheric storm influence. (Stankov and Jakowski, 2006). The storm correction assumes that t
Jun 16, 2016 - Improving Power Generation Efficiency using Deep Neural Networks. Stefan Hosein. [email protected] Patrick Hosein. [email protected] The University of the West Indies, St. Augustine, Trinidad and Tobago. Abstract. Re
Dec 1, 2014 - the two new DEA models to evaluate the performance of the biomass power plants in. China and find that the efficiency of biomass power ...
[READ] The Shelf Elf [EBOOK]
compare amplitude modulation, geometric modulation, and a previously proposed technique ... Due to the temperatureâdependent conductivity of the lower.
Aug 13, 2011 - Engineering and Physical Sciences Research Council (EPSRC), the ionospheric scintillation effects (abrupt power fades and phase variations in the ... error variance at the PLL and DLL outputs were calculated from the formulae in ; a
Mar 24, 2012 - Pulinets, 2009], (2) the study of other earthquakes for sim- ... 3Department of Earth and Space Sciences, University of ... 5Jet Propulsion Laboratory, NASA, Pasadena, California, USA. Copyright ... with the JPL Global Ionosphere Map (
Oct 8, 1985 - r +1 each z, fi. )2_ 2E(fs(j)fs(j_1))- 2E(fs(j+1)fs(j+2)). It follows fromthe theorem of R. V. Erickson  that for. IE(exp izTo. I) exp(-z2/2)l < a31zlme3.
Status of development of thermoelectric element materials. With the growing public interest in environmental problems in recent years, the importance of thermoelectric power generation â an energy conversion technology â is being re-recognized. I
Oct 20, 2016 - Here, a few-layer anisotropic metasurface is presented ...... Ni, X., Kildishev, A. V. & Shalaev, V. M. Metasurface holograms for visible light. Nat.
Radio Science, Volume 25, Number 6, Pages 1311-1320, November-December 1990
On the efficiencyof ionospheric ELF generation K. Papadopoulos, C. L. Chang, P. Vitello, and A. Drobot Science Applications International Corporation, McLean, Virginia
(Received June 1, 1988; revised February 21, 1989; accepted November 9, 1989.)
The scalinglaws that control the efficiencyof convertingground-basedHF power to ELF power by using modulationof the polar electrojetcurrent is discussed.The analysisis based on kinetic calculationsof the modificationof the ionosphericconductivityby HF waves in conjunctionwith the experimentalresults reported from the Tromso Max Planck and the Alaska high power auroral simulation(HIPAS) facilities. It is shownthat the efficiencycan be increasedby more than a factor
of 104 by (1) usingphasingto sweepthe antennabeamoveran areaspanned by a maximumtilt of 35ø, on a time scale faster than the cooling rate at the heating altitude (<100/•s) and (2) localization of the heating at the E region (90-100 km) where electron runaway can be induced resulting in substantial modification of the Pederson conductivity.
Generation of ULF/ELF/VLF
waves by modu-
lating ionospheric currents has been confirmed for Generating ULF/VLF/ELF waves by utilizing both the equatorial and the auroral electrojet in the ionosphereas an active medium is an exciting experiments conducted in the U SSR [Migulin and prospect. The techniqueprovidesfrequency agility Gurevich, 1985; Belyaev et al., 1987], the Maxand avoids many of the geopolitical and economic Planck Tromso facility [Stubbe et al., 1982a, b; difficulties associated with large and inefficient Barr and Stubbe, 1984a, b; James et al., 1984; Barr ground-based facilities. By adjusting the HF beam et al., 1985], and the United States [Ferraro et al., geometry, the low-frequency waves can be made to 1982; Ferraro and Lee, this issue]. Most of the propagate upward in the magnetospherefor use in active magnetospheric stimulation experiments or experiments were performed using HF frequencies downward into the Earth's ionosphere waveguide in the range of 2-5 MHz, while the power density at regionvariedbetween10-4 and for communication and geological-probing pur- the interaction poses. One of the mechanismsdiscussedfor down- 10-3 W/m 2. The most exhaustive studies were converting HF power to ULF/ELF/VLF power by performed at the Tromso Max-Planck facility and interactioning with the ionosphere requires the the typical results are summarized in Figure 1. presence of ambient ionospheric currents, such as These results are in general terms consistent with the auroral or equatorial electrojets [Germantsev et results produced at other facilities, [Ferraro and al., 1974; Kotik and Trakhtengerts, 1975; Stubbe Lee, this issue; Belyaev et al., 1987] although the and Kopka, 1977; Chang et al., 1981;Ferraro et al., precise values of the detected field amplitudes de1982], while another relies on pure plasma nonlin- pend on local conditions, characteristicsof the HF earities and does not require the presence of iono- facility, and other specific factors. The purpose of spheric currents [Papadopoulos et al., 1982, 1983; this paper is to explore the potential and the limitaPapadopoulos and Chang, 1985; Ko et al., 1986; tions of the ionospheric generation of ULF/ELF/ Ganguli et al., 1986]. Although both mechanisms VLF waves using as a guide the current experimenhave been verified experimentally, the predom- tal results in conjunction with theoretical inance of the experimentsdealt with the modulation extrapolations. Namely, starting from the current of ionospheric currents because this technique de- experimental and theoretical status, we develop mands lower HF transmitter power and antenna scalinglaws and use them to explore the efficiency directionality. with which HF power can be converted to the desired low-frequency range. It is expected that the Copyright 1990 by the American Geophysical Union. conclusionswill be useful in guidingfuture facilities and experiments. For specificity we selectedfor our Paper number 89RS03537. 0048-6604/90/89RS-03537508.00 study the ELF frequency range (i.e., 50-500 Hz), 1311
ET AL.: ON THE EFFICIENCY
of the modulated
profile, for any specifiedambient ionosphericelectric field (assumed or measured). This calculation
involves computation of the primary current, the polarization currents required to set up quasineu••E 1 oo trality, and the induction currents caused by the time dependence of the magnetic field. Finally, from the modulated current profile the excitation and propagationof the ULF/ELF/VLF waves in the Earth's ionosphericwaveguide can be computedby 10 2 10 3 1 04 using either the extended source technique [TripModulation Frequency [Hz] athi et al., 1982] or with an equivalent ULF/ELF/ Fig. 1. Typical experimental results in the ELF region gener- VLF moment in the ionosphere the reciprocity principle [Galejs, 1968, 1971; Barr and Stubbe, ated by the Max Planck Tromso facility [Stubbe et al., 1982]. 1984a, b]. A comprehensive analysis of these factors lies beyond the scopeof this paper. Within the sincein this rangethe interpretationof the resultsis experimental and theoretical uncertainties our purnot complicated by waveguide resonances, high- pose can be accomplished by starting from the order modes, and skin layer thickness. The plan of current experimental results in the frequency range the paper is as follows. The next section summa- of 50-500 Hz and analyzing them under the assumprizes the statusof understandingof ELF generation tion that the power generated is proportional to the by current modulation and the resulting scaling square of the dipole moment laws. Section 3 discussesthe level of conductivity M = IL (1) modification as a function of the incident power density and altitude. Contrary to previous studies which used fluid analysis to calculate the electron where I is the total modulated current contributing heating, a completely kinetic treatment is used to the ELF field on the ground and L is the linear here. Such a treatment is required for power densi- size of the modulated region. All other factors tiesexceeding 10-3 W/m2. Basedontheanalysis of entering the efficiency calculation will be taken sections2 and 3, section4 discussestechniquesfor from the available experimental data base. For increasing the HF to ELF conversion efficiency. concretenessthe measurementsand analysis of the The final section summarizesthe results and pin- Tromso results [Barr and Stubbe, 1984a] are used as our baseline input. These results are in general points high-leverage research issues. agreement to the ones reported from high power 2.
Relating the amplitude of the ELF waves on the
auroral simulation (HIPAS) [Ferraro and Lee, this issue]. The range of 50-500 Hz has been selected in
order to avoid effects associated with waveguide resonances which arise for frequencies above 1
ground to the extent and characteristics of the
modified region in the ionosphereand to the design characteristicsof the HF transmitter is a complex problem. Aspects of the problem have been examined by many authors [Kotik and Trakhtengerts, 1975;Bellyustin and Polyakov, 1977; Tripathi et al., 1982; Fejer and Krenzien, 1982; Bart and Stubbe, 1984a, b]. It involves the following seriesof sequential steps. Based on the transmitter characteristics (power, gain, HF frequency, and modulation frequency) and the applicable model of the ambient ionosphere the conductivity modulation is first
The experimental results indicate that when the heating transmitter operated at a power level of 150 MW ERP the amplitude of the ELF field measured on the ground is -100 tzV/m or 1 pT. These correspond to about 10-100 mW of radiated ELF power in the 200-500 Hz range [Bart and Stubbe, 1984a]. The equivalent radiating horizontal dipole at 75-80 km altitude in the ionosphere is IL • 3-5 x
computed as a function of altitude. This allows for
104 A-m which corresponds to an equivalent ground-based electric vertical dipole with IL •
2-4 x 103A-m.Thepolarization is consistent with predominanceof Hall current modulation. Compu-
ET AL ß ON THE EFFICIENCY
For instance, if we increase the peak conductivity modulationby a factor of 10 while keeping L = 20 km, the radiated power at 500 Hz would increase from 100 mW to about 10 W. Similarly, if we increasethe size L by a factor of 5 while keepingAo-
• 3-4 x 103 s-! theradiated powerwouldincrease by a factorof (5)4 ---6 x 102.
A critical input needed for the determination of
the factors that optimize PELF is the scalingof the conductivity modification Ao-on the HF power
density S at the modified height,
S = PHF/L2
Fig. 2. ELF power versusfrequencyfor the Tromsofacility as determined by the analysesof Bart and Stubbe [1984a]. The
where PHF is the ground HF power and L is the kin/L)4 to emphasize the scaling withsizeL andconductivityspot size at the appropriate height. Of course this Air. For the Tromso results this factor is unity (i.e., Air • 3 x neglectsabsorptionat lower heights,a point that we 103/s,L • 20 km). will return later on. Assumingthat ELF powerscalehasbeenmultipliedby (3 x 103s-I/Act) x (20
Act --- [PHF/L2]a tations based on a fluid model indicate that for an
we find from (3)-(5) that
assumedambientionosphericelectricfield E, - 25 mV/m the peak values of the modulated current
densityare in the rangeof 10-8 A/m2 and are located between 75 and 80 km in altitude. The effective horizontal radiated current moment M can
2a L4(i - a) PELF "' PHF
For a = I we find that PELF is independent of the antenna gain and scales as
be estimated by height integration as
M = IL = AjAzL2 = AcrAzEa L2
(2) Namely, the HF to ELF conversion increases as
where Aj is the modulatedcurrent density, Az is the extent of the effective radiating layer in altitude, and Ao-is the modulated conductivity. For the typical experimental conditions L = 20 km (i.e., at a heaterbeam width of 15ø),Az • 10 km, and E a •
the square of the HF power. For a >> I the ELF conversion efficiency increases enormously by in-
creasingthe ground-basedHF power PHF while maintaining the same antenna gain (i.e., L - constant). For a << 1, more efficient conversion re-
25 mV/m, the value of IL = 3-5 x 104 A-m quires large spot sizes. A computationof the value corresponds to a peakvalueof Ao-= 3-4 x 103s-l. of a for various altitudes and HF power densities is
This is achievedwith an incidentHF power density performed in the next section.
of 2 mW/m2 at 75-80kmheight.Finally,it should be noted that the value of IL is independent of
'frequencyand the frequencydependencein the ELF power is attributed to the scaling of the excitation efficiency [Galejs, 1971]. Since the quantities that can be controlled from the groundare the value (and possiblythe altitude location) of the conductivity modulation Ao-and the size L, it is instructive to cast the experimentaldata as interpreted by Bart and Stubbe [1984a] in the form of Figure 2. Notice the importantscalingvalid for each ELF frequency, i.e.,
PELF '•' M2 "' (Acr)2L4
DEPENDENCE OF CONDUCTIVITY ON ALTITUDE AND POWER
In this section we evaluate the level of cop.duc-
tivity modulationat variousionosphericheightsas a function of the incident HF power density S. The calculation is "local" and neglectstransport. From the modulated conductivity we can easily evaluate the modulatedcurrent for a given ionosphericelectric field. Contrary to previous studies [Stubbe and Kopka, 1977; Tomko, 1981; Chang et al., 1981; James, 1985] which used fluid equations to compute (3) the variation of the electron temperature Te as a
ET AL.' ON THE EFFICIENCY
linear approximation, the present study uses the complete time dependent kinetic equation for the electron energy distribution function f(e). For an HF electric field of peak amplitude E o and frequency •oo at the chosenheight,f(e) is given by [Gurevich, 1978]
where v(e) is the energy dependentelectron-neutral altitude (km) collisionfrequency at the chosenheight and 12is the Fig. 3. Ionosphericprofile used in the Fokker-Planckruns. electron cyclotron frequency. The _+ signs correspond to o(+) and x(-) mode heating correspondingly. The term L(e) is an operator that represents the energy loss due to various inelastic processes. and high altitude is obvious from the distribution Its form is discussedin the appendix and includes function shownin Figure 4. Figures 4a-4 c show the excitation of rotational, vibrational, and optical initial and steady state distribution functions for levels as well as ionization and attachment for N 2 ionosphericheating at 75, 90, and 100 km altitude and at valuesof S - 10-3 W/m 2 10-2 W/m 2 and and02. Note that the latter processis not important 10-2 W/m2 correspondingly Thetimerequiredto for the power densitiesanalyzed here. Equation (8) reach steady state was in all cases much shorter was solved numerically for f(e, t) at various altithan 10 -4 s. This implies that steadystate is tudes, HF power density values S and modulation reached at times much shorter than the relevant frequencies•o. The form of v(e) and the numerical method for solving (8) are given in the appendix. modulation frequencies. It is seen that at lowandlow-power density(i.e., 75 km, 10-3 The time dependenceof the conductivity is found altitude
and the fluid descriptionis a reasonableapproxima-
m2 e2(e)f(e, t)e de ne • •Q2+p(e) m2/ ,0,2 +D /x2(e)f(e, t)e1/2 de ne
tion. This, however, is not true for the'other two caseswhere the high-energytails of the distribution functions become the dominant part.
Figures5-6 showthe time dependenceof the Hall and Pedersen modulation
•h(t) = •
for the above three cases.
At 75 km and 10-3 W/m2 the Hall conductivity
modulationis about7 x 103s-] which is consistent with the value quoted in section 2 for the Tromso o'z(t)= • f(e t)e de (10c) experiments.The Pedersonconductivity modulam •-• ' tion is significantlysmaller.This is reversedfor the 90 and 100 km cases at 10-2 W/m2. The Hall whereO-p,o-h, ando-z arethePederson, Hall, and parallel conductivities and n is the electron density. conductivity modulation becomes progressively As noted in the introduction a kinetic analysis is an smaller and is negligible at 100 km. Furthermore, absoluterequirement for exploring high-power den- the level of the Pedersonconductivity modulationis sities. The initial f(e, t = 0) was taken as Max- about3 x 104s- 1 at 90 km and 6 x 104 s- 1 at 100 wellian at Te • 0.025 eV. For the studiesreported km. It is clear that if the size L, which is controlled belowwo = 1.8x 107rad/swhichcorresponds toa by the antennagain was the samefor all three cases and the increasein the power density was entirely heater frequency of 2.8 MHz. We report below resultsfor daytimeionospheric due to an increasein PHF by a factor of 10, the conditions corresponding to altitudes between 70 radiatedPELF would increaseby a factor of 20 and
ne 2j. 1
and 100 km. The ionospheric model used is shown in Figure 3. The need for a kinetic description at high power
100 for the 90 and 100 km cases over the 75 km case.
Notice that since steady state is established for all cases much earlier than the low-frequency oscilla-
(a) -I •% Initial
'-" O.O 0.3
Energy(eV) Fig. 4.
10-4-W/m 2. The resultsfor the Hall and Pederson conductivities are shown in Figures 7 and 8. The boundary altitudes were chosen in a way that they reflect the range of variation of the Pedersen and
analysis of the consequencesof the results shown in Figures 7 and 8 and of the efficiency optimization at intermediate altitudes will be presented elsewhere. We restrict our discussionhere to the consequences of the general trends derived from Figures 7 and 8.
1. For low altitudes (---70-75 km) the Hall conductivity provides the dominant contribution. The 0.0
Energy (eV) Fig. 4.
Initial and steady state electron distribution œor(a) 75
km, S = 10-3 W/m2' (b) 90km, S = 10-2 W/m2' and(c) 100kin, S = 10-2 W/m2.
tion period, the values of Art are independentof the ELF frequency. In order to determine the scalingof the conductivity modification with power density and altitude we conducted a survey of the level of steady conductivity modification for altitudes (70 and 100 km) and values of S in the range of
value of Ao-h increases very weakly with power density (a < 1/2) and saturates at a value of S about
10-3 W/m2. Furtherincrease in thepowerdensity does not produce any increase in the modulated current density. According to the discussion after (7), optimization of the conversion efficiency requires increase in L under constant S. 2. For high altitude (>90 km) heating the modification of the Pederson conductivity dominates.
Thevalue of/kO'p increases asS2(i.e.,a = 2),upto
powerdensityof 10-2 W/m2 andsaturates slowly afterward. There is an obvious premium in increas-
ing PHF, sincein this casePELF'" P•F, while keepingS - 10-2 W/m2.
o.ooom.do,s o.dozoo.do•so.4or, o o.,3• o.4o•oo.b,oso.b,2o o.b,•s o.o,so
interesting feature is a direct result of using the kinetic approach to estimate Hall conductivity. Specifically, at high-altitude and high heating power, the energy integral in (10b) gives an overall positive contributionto rrh as the electron distribution shifts toward the high energy end. In contrast, the conventional fluid approach always predict a decreasein o-h since the collision frequency •,(Te) increases with the fluid temperature Te. Before closingthis section we should caution the reader in the interpretation of the above results. In order to have uniformity in the results and be close to the benchmark case, the survey shown in Figure 4 was performed using the same frequency o•o = o.oom•.do,s 0.4030o.do4so.dor, o o.b•
Time (sec) Fig. 5.
Hall conductivity modification for the cases of Figure 4.
1.8 x 107for all the threealtitudesexamined(75, 90, 100 km). This frequency corresponds to a criti-
calelectron density n•.= 105electrons/cm 3 which correspondsto an altitude of 105 km for the model ionosphereused here. The electron densitiesat 75,
90, and100km (Figure3) are 3 x 102electrons/ 3. Maximum value of Air is achieved for highaltitude heating.
cm3 8 x 103electrons/cm3 and 8 x 104 electrons/ cm3. Since the code does not include collective effects, the 100 km results are close but within the
Note that in Figure7, the IAo-•lcurveat 100km validity range of the model. Furthermore, as long as
shows a dipnearthepowerlevelof 0.4W/m2.This
the half width of the heater is smaller than 26ø,
implies a sign changeof Air h from minus to plus as the heating power increases at high altitude. This
effects of resonance absorption can also be neglected even for the 100 km case. However, we
ON THE EFFICIENCY
•.oa:•.•o•s o.•o•o o.•o,s o.,•or, o o.•s
o.hos o.h2o o.h•s o.o•so
o.ooo•.•otso.•o•o o.•o,s o.•or, o o.•,s o.;•o o.hos o.•2o o.&•s o.o•so
Time (sec) Fig. 6.
where b is the quiver energy of the electrons in the high-frequency field, with an effective frequency
Weft= Wo +- f•, definedas
• m(eEo/mw elf)2 Our resultscan be generalizedto any frequency by noting that the solution of (8) is self-similar with respectto the value of b. Thus for a frequency o) > wo a power density is higher by a factor (w _+
fi) 2/(wo +-1•)2 thanfor w = wo willberequired.
,.oa•.•ots o.,•o•oo.•,s o.•,o o.,•
o.•,o o.,hoso.,h2oo.h•s o.o,so
Same as Figure 5 for the Pedersonconductivity.
laOhl 10 (1/sec) 103 2
should note that for the high altitude cases(>90 cm)
the resultsare applicableto frequencieshigherthan the 2.8 MHz by a simple scalinglaw based on (8) and (9). Note that for Wo > 2.8 MHz and h > 90 km, + f•)2 >> v(e). Therefore (0)o -1
D(e) = • gv(e)
S (wattsire 2)
Hall conductivity modulationversus S for 70 and 100 km.
mW/m2, theresultant conductivity modification ac-
cording to Figures 7 and 8 increases by a factor of 100 over that for low-altitude heating. According to
(3), thiswill producea factorof 104 morepower
than the 5-10 roW, which results in 50-100 W in
ELF even in the absence of sweeping. The system
efficiency increases by a factorof 103givingan overallconversion efficiency of 10-5. Incorporating
S (watts/m 2)
Pederson conductivity modulation versus S for 70 and
OF HF TO ELF
In this section we combine
a similar sweep as for the low-altitude heating will result in further increase of the efficiency by a factor of 400 giving an overall efficiency better than 4 x
10-3 . The practicaldifficultyin realizingthe highaltitude scheme, especially under day time conditions, is the fact that self absorption at lower heights could prevent the achievement of power densities
achieved with power density of the order of 10
the results of Bart and
Stubbe [1984a] as shown in Figure 2 with the results reported in section 3 and use them to determine the HF to ELF conversion efficiency and techniquesby which it can be optimized. On the basis of Hall conductivity modulation of the polar electrojet at 70-75 km altitude, Bart and Stubbe [1984a] estimate a power conversion efficiency of 5-10 mW per MW of HF at 200 Hz. This implies an overall
conversion efficiency of about10-8 , compared with 10-6 conversion achievedby the Wisconsin Test Facility. For low-altitude heating the results of section 3 indicate that increasing the power does not have any significant effect in the ELF power. However, as shown in (3) for constant power den-
of 10mW/m2 at 95-100km altitudefor frequencies of 2.8 MHz used in our calculations. Such heating can be achieved by using higher frequencies, beating two HF waves at the local plasma frequency, or using short pulses that allow the power to "sneak through" to high altitudes. These possibilities are currently under study. The enormous increase in efficiency achieved in high-altitude heating places a large premium in realizing them even if their efficiency is by an order of magnitude lower. 5.
We presented a detailed kinetic study of local heating of the ionospheric plasma by modulated radiowaves, of the resultant conductivity modulation and of the associated
sity and thereforeconstantAo-,PELF'" L4. An sity in the presence of an ionospheric electric field increase in area while maintaining approximately in the ELF region (50-500 Hz). Regimes where the the same power density can be achieved by using conductivity modulation is a strong or weak funcphasing to sweep the antenna beam over an area tion of the incident HF power density were identispanned by a maximum tilt of 0•, in eachdirection fied. Combining these results with the recorded at a rate faster than the cooling rate, which for 80 observationsin this ELF region and assumingthat km is approximatelyfew microseconds.PELF will to zero order the ELF power density is proportional 4 we foundthatthe HF to ELF power increaseaccordingto (3) by a factor of (tan (Om + to (Ao')2L 0o)/tan00)4. Taking0o = 7.5øandOm= 35ø, we conversion efficiency can be increased by more find an increase on the ELF power by a factor of than 2 orders of magnitude if the heater could be 2 x 103.Thusa facilityof thetypeof Tromsoor swept over a 35øcone on timescalesfaster than the HIPAS equipped with fast sweeping over a cone of plasma cooling rate (---10/•s) for low-altitude heat35ø can produce 5-10 watts of ELF power and can ing. Heating techniquesthat can preferentially dehavean efficiency of 10-5 whichis betterthanthe posit their energy at higher altitude (---90-100 km) efficiency of the Navy ELF Wisconsin test facility. where the dominant modulated current is the PedAlternately, higher efficiency as well as higher erson current, can further increase the efficiencyby partof thisincrease canbe PELF can be produced by high-altitudeheating. If a factorof 104 although HF heatinglocalized in the 95-100 km region can be negatedby the potential inefficiency of high-altitude
heating as well as by a more inefficient coupling to the waveguide. We are currently examining these issues theoretically and expect to resolve them in combination with the Penn State HIPAS experimental campaigns.
where o-a is the attachmentcross sectionand N o is the 02 number density. Ionization
f(e, ep)epf(ep)Cri(ep) dt•p
The inelastic term •(e) in the Fokker-Planck equation (equation (8)) is a summation of the various inelastic
•(E) = Sr -3-Sv,o -3-Sa -3-Si
Detailed expressions of these inelastic contributions are given as follows [Gurevich, 1978]: Excitation
where e i is the ionization energy and •i is the ionization
The collision frequency P(e) used in (9) contains the elastic
of the electrons
tral molecules. As such, the P(e) can be written as
p(e)= • Nmv•m(e)
Sr =--• 2v20v v2Rr(v)
Rr(v) = 8Boo'oNm/mV
O'o= 8rrQ2ao2/15 ao = h2/me 2
Q = 1.04
Q = 1.80
Acknowledgments. The work was supported by the Office of Naval Research through Penn State subcontract ONR-TPSU-
Bo = 2.48 x 10-4 eV
Bo = 1.79x 10-4 eV
•'. [(e+ e/•)f(e+ e/•)o-/•(e + k
where k standsfor different levels, o-kisthe energy of the k state, and o-kis the cross section. Attachment
S. = -Novcraf
and Lee of Penn State
Excitation of vibrational and optical levels 2Nm
Discussions with Ferraro
and Ossakow of the Naval Research Laboratory are gratefully acknowledged.
N m is the number density of N 2 and 02, and Sr is summingover both N 2 and 02 species.
where N m is the neutral density at the chosen height, •m is the momentum transfer cross section, and the summationis carried over both O2 and N2 species. Numerically, a finite difference scheme for initial value problems of Fokker-Planck equations has been applied to solve the governing equation (equation (8)). Details of the numerical method can be found in the work by Chang et al. .
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PAPADOPOULOS ET AL.: ON THE EFFICIENCY
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