published in WGN, the Journal of IMO 26:6 (December 1998), pp. 239-248
Ghazalaha Al-Abed (ABEGH, 5.95h), Iyad Ahmad (AHMIY, 1.83h), Ahmad Al-Niamat (ALNAH, 5.00h), Rainer Arlt (ARLRA, 0.63h), Joseph D. Assmus (ASSJO, 3.11h), Zaid Ata (ATAZA, 5.00h), Juan Alberto Aveledo (AVEJU, 1.20h), Jlia Babina (BABJL, 3.28h), Halim Baituk (BAIHA, 2.30h), Ana Bankovic (BANAN, 4.12h), Rony Barry (BARRO, 0.54h), Luc Bastiaens (BASLU, 1.66h), Rizlane Bechar (BECRI, 1.67h), Sanae Bechar (BECSA, 1.67h), Luis R. Bellot Rubio (BELLU, 4.97h), Mahjoub Belfahim (BELMA, 6.83h), Pavel Belov (BELPA, 2.15h), Vladimir Belchenko (BELVL, 2.55h), Abdelaziz Bennouna (BENAB, 1.08h), Felix Bettonvil (BETFE, 4.39h), Neil Bone (BONNE, 1.97h), Mark Borg (BORMR, 6.25h), Michael Boschat (BOSMI, 4.00h), Joana M. Brunet (BRUJO, 5.30h), Marija Cajetinac (CAJMA, 5.75h), Arturo Carvajal R. (CARAR, 0.50h), Tal Carmon (CARTA, 0.04h), Andrew Casely (CASAN, 1.00h), Matthew Collier (COLMA, 0.24h), Tim Cooper (COOTI, 1.00h), Uros Cotar (COTUR, 1.03h), Stefano Crivello (CRIST, 5.78h), Hani Dalee (DALHA, 4.00h), Luigi d'Argliano (DARLU, 1.41h), Mark Davis (DAVMA, 7.50h), Goedele Deconinck (DECGO, 1.71h), Benoit Dejust (DEJBE, 2.00h), Marc de Lignie (DE MA, 15.23h), Vincent Desmarais (DESVI, 2.20h), Peter Detterline (DETPE, 5.06h), Asdai Diaz Rodriguez (DIAAS, 2.00h), Anton Dimitrov (DIMAN, 2.14h), Elena Dimovski (DIMEL, 6.08h), John Drummond (DRUJO, 2.50h), Tonis Eenmae (EENTO, 3.07h), Maurizio Eltri (ELTMA, 2.75h), Frank Enzlein (ENZFR, 2.69h), Tamás Fodor (FODTA, 1.93h), Keiiti Fukui (FUKKE, 11.73h), Nobuyuki Fukuda (FUKNO, 4.15h), Ofer Gabzo (GABOF, 0.25h), Christoph Gerber (GERCH, 15.18h), Jaroslav Gerbos (GERJA, 8.50h), Ivanka Getsova (GETIV, 3.52h), George W. Gliba (GLIGE, 3.25h), Orly Gnat (GNAOR, 0.17h), Shelagh Godwin (GODSH, 0.66h), Amit Gokhale (GOKAM, 2.05h), Sagar Gokhale (GOKSA, 1.03h), Yeshodhan Gokhle (GOKYE, 3.68h), Alexandra Golova (GOLAL, 3.28h), Prerana Gore (GORPA, 2.67h), Roberto Gorelli (GORRO, 8.20h), Valentin Grigore (GRIVA, 4.45h), Monica de la Guardia (GUAMO, 4.36h), Michal Haltuf (HALMI, 1.41h), Torsten Hansen (HANTO, 1.98h), Takema Hashimoto (HASTA, 10.50h), Roberto Haver (HAVRO, 5.12h), Kim Hay (HAYKI, 2.37h), Amera Hemsy (HEMAM, 5.33h), Kamil Hornoch (HORKM, 3.39h), Daiyu Ito (ITODA, 4.97h), Kiyoshi Izumi (IZUKI, 7.23h), Helle Jaaniste (JAAHE, 3.35h), Jan Janssens (JANJA, 12.50h), Vibor Jelic (JELVI, 4.52h), Ilhame Jemmah (JEMIL, 0.50h), Carl Johannink (JOHCA, 16.35h), Ivan Jokic (JOKIV, 2.20h), Kevin Jones (JONKE, 6.24h), Javor Kac (KACJA, 5.87h), Primoz Kajdic (KAJPR, 2.09h), D. Kalayda (KALDU, 3.33h), Dmitrij Karkach (KARDM, 3.28h), Niladri Kar (KARNI, 3.72h), Kenya Kawabata (KAWKE, 3.71h), Srdjan Keca (KECSR, 3.70h), Akos Kereszturi (KERAK, 3.53h), Katarina Kerekesova (KERKT, 8.78h), Noor Al-Khateeb (KHANO, 4.44h), Mark Kidger (KIDMA, 1.50h), Kevin Kilkenny (KILKE, 3.09h), André Knöfel (KNOAN, 7.68h), Daniel Köhn (KOHDA, 1.46h), Khalil Konsul (KONKH, 5.50h), Marija Kotur (KOTMA, 0.91h), Jakub Koukal (KOUJA, 11.36h), Zoran Kraljevic (KRAZO, 3.47h), Nikola Kresojevic (KRENI, 5.55h), Gary W. Kronk (KROGA, 6.50h), Tom Kucharski (KUCTO, 2.42h), Brigitte Kuneth (KUNBR, 2.00h), Werfried Kuneth (KUNWE, 1.00h), Zsolt Lantos (LANZS, 2.96h), Anne-Laure Lebacq (LEBAN, 1.71h), Adrian Lelyen (LELAD, 1.00h), Anna S. Levina (LEVAN, 3.33h), Mihir Limaye (LIMMH, 1.18h), Alister Ling (LINAL, 1.38h), Vladimir Lukic (LUKVL, 6.02h), Robert Lunsford (LUNRO, 5.00h), Hartwig Luthen (LUTHA, 9.20h), Mirjana Malaric (MALMR, 5.00h), Katuhiko Mameta (MAMKA, 1.50h), David Martinez Delgado (MARDA, 2.01h), José Alfonso dos Reis Martins (MARJO, 2.88h), Khalid Marwat (MARKH, 2.48h), Pierre Martin (MARPI, 4.65h), Takuya Maruyama (MARTA, 0.67h), Antonio Martinez (MARTI, 4.42h), Yukihisa Matumoto (MATYU, 1.50h), Alastair McBeath (MCBAL, 7.05h), Stephen McCann (MCCST, 0.23h), Bruce McCurdy (MCCBR, 1.38h), Kevin McKeown (MCKKE, 1.00h), Lukas Mecir (MECLU, 0.13h), Mark Mikutis (MIKMR, 12.20h), Ana Milovanovic (MILAA, 6.42h), Dragan Milisavljevic (MILDR, 1.02h), Iris Miljacki (MILIR, 2.65h), Hidekatu Mizoguchi (MIZHI, 2.41h), Amruta Modani (MODAM, 2.66h), Sirko Molau (MOLSI, 14.17h), William Morgan (MORWI, 1.84h), Erick Mota Perez (MOTER, 2.90h), Darshan Mundada (MUNDA, 3.86h), Sin Nakayama (NAKSI, 3.76h), Koji Naniwada (NANKO, 4.33h), Sven Näther (NATSV, 12.35h), Dalibor Nikolic (NIKDA, 2.46h), Prakash Nitsure (NITPR, 4.05h), Mohammad Odeh (ODEMO, 4.15h), Ibrahim Odwan (ODWIB, 4.75h), Eran Ofek (OFEER, 3.47h), Hiroyuki Okayasu (OKAHI, 4.98h), Masayuki Oka (OKAMA, 5.59h), Dragana Okolic (OKODR, 3.91h), Kazuhiro Osada (OSAKA, 8.50h), Ketan Pendse (PENKE, 1.33h), Miroslav Penev (PENMI, 2.15h), Alfredo Pereira (PERAF, 5.71h), Dusan Perovic (PERDU, 5.01h), Radame Perez (PERRA, 1.00h), Suyin Perret-Gentil (PERSU, 1.52h), Furio Pieri (PIEFU, 4.73h), Mila Popovic (POPMI, 1.20h), Dubravko Potkrajac (POTDU, 1.08h), Tushar Purohit (PURTU, 2.85h), Daniela Rapava (RAPDA, 7.09h), Pavol Rapavy (RAPPA, 8.34h), Simona Rapava (RAPSI, 2.96h), Ina Rendtel (RENIN, 1.08h), Jürgen Rendtel (RENJU, 21.68h), Mileny Roche Lamas (ROCMI, 1.00h), Francisco Rodriguez Ramirez (RODFR, 5.05h), Juan Rodríguez (RODJU, 3.72h), Victor Ruiz Ruiz (RUIVI, 3.91h), K.V. Sankaranarayanan (SANKV, 2.50h), René Scurbecq (SCURE, 4.22h), Abderazak Sersouri (SERAB, 1.67h), Shashank Shalgar (SHASH, 4.03h), Brian Shulist (SHUBR, 3.10h), Hendrik Sielaff (SIEHE, 5.67h), Hiroyuki Sioi (SIOHI, 5.24h), Vesna Slavkovic (SLAVE, 2.65h), James N. Smith (SMIJN, 6.65h), Andrey Solodovnik (SOLAD, 3.05h), Manuel Solano Ruiz (SOLMA, 1.25h), George Spalding (SPAGE, 4.92h), Ulrich Sperberg (SPEUL, 3.90h), Mark Stafford (STAMA, 1.82h), Enrico Stomeo (STOEN, 1.19h), Niko Stritof (STRNI, 3.04h), Paul Sutherland (SUTPA, 1.39h), David Swann (SWADA, 6.10h), Eva Szabados (SZAEV, 0.90h), Richard Taibi (TAIRI, 4.42h), Masaaki Takanasi (TAKMA, 0.75h), Mika Takanasi (TAKMI, 4.49h), Khaled Tell (TELKH, 10.47h), István Tepliczky (TEPIS, 1.51h), Kazumi Terakubo (TERKA, 1.00h), Neelima Thatte (THANE, 5.90h), Danilo Tomic (TOMDA, 2.40h), Yasuhiro Tonomura (TONYA, 1.83h), Michael Toomey (TOOMI, 2.60h), Tamas Tordai (TORTA, 4.10h), Hamid Touma (TOUHA, 3.25h), Gabrijela Triglav (TRIGA, 0.93h), Josep M. Trigo Rodriguez (TRIJO, 1.07h), Mihaela Triglav (TRIMI, 5.31h), Arnold Tukkers (TUKAR, 15.41h), Anne van Weerden (VANAE, 5.10h), Erwin van Ballegoy (VANER, 4.92h), Jan Verbert (VERJN, 1.60h), Ivaylo Videv (VIDIV, 2.30h), Miquel A. Villalonga Vidal (VILMQ, 1.36h), Catarina Vitorino (VITCA, 3.35h), Marija Vlajic (VLAMA, 2.40h), Björn Voß (VOSBJ, 8.60h), Maja Vuckovic (VUCMJ, 1.17h), Barbara Wilson (WILBA, 5.15h), Larry Wood (WOOLA, 1.38h), Kim S. Youmans (YOUKI, 3.88h), George Zay (ZAYGE, 12.08h), Jin Zhu (ZHUJI, 1.75h).
We would also like to encourage all those meteor observers to continue their efforts in meteor astronomy, whose reports did not go in the analysis because of insufficient data:
Andras Adrovicz, Farrahzadi Azzadeh, Joshi Bhargav, Bozorgi Behnaz, Worachate Boonplod, Ravi Brahmavar, Chun Byung-hun, Diadina Cotte, Szillard Csizmadia, Kunal Dhande, Marc de Lignie, David Dickinson, Zha Dong-yan, Alipour Elnaz, Kin Enriquez, David Farkas, Azeemlu Fatemeh, Alap Ghosh, Michael Gorshechnikov, Katalin Hidasi, Brujerdi Hoda, Peter Horvath, Hyabanyan Hossein, Aftab Husain, Mustafa Husain, Yu Ji-hong, He Jing-yang, Amaya Kaloti, Usha Kasinadhuni, Timo Kinnunen, D. Kothawala, Nanda Kumar, Csaba Lendvai, Doug Little, Keith Little, Y.L. Malathi Latha, Paul Maley, Maleki Mania, Fred Mason, Dan McIntosh, Karoly Mikics, Masjedi Morad, Pathak Mukesh, Chun Myung-in, Adam Nemeth, Shigemi Numazawa, Andras Petyus, Adam Pozsik, Raj Purohit, P. Radhika, L. Ramesh, Anand Rao, Rezaai Reza, Qi Rui, J. Rukmini, Khoeini Saloumeh, Moghimi Saman, Debasis Sarkar, Lamei Sepideh, Jang Seong-hwan, Kharrazi Sharmin, Amy Shelton, Ghassemi Sima, Szandor Szabo, Darren Tabbot, Hezareh Talayeh, Zoltan Tarnoki, Zoltan Toth, Kim Won-tag, Zoltan Zelko, Sajjadi Zeynab, Wang Zhen-shi, Wu Zhi-wei.
The list of residence countries of the observers is extensive; however, many of them were not observing from home:
Aruba, Austria, Bulgaria, Canada, China, Croatia, Cuba, Czech Republic, Ecuador, Estonia, Finland, Germany, Hungary, India, Iran, Israel, Italy, Japan, Jordan, Korea, Malta, Marocco, the Netherlands, New Zealand, Pakistan, Philippines, Portugal, Russia, Slovakia, Slovenia, South Africa, Spain, UK, Ukraine, USA, Venezuela, Yugoslavia.
with additional observing sites in Cyprus and Mongolia. We would like to acknowledge the great efforts of several amateur groups here, who popularized meteor observations and sent in their results quickly for the analysis, in particular the Jordanian Astronomical Society with reporter Mohammad Odeh, the Israeli Astronomical Association and Ilan Manulis, the Spanish Sociedad de Meteoros y Cometas de España and Luis Bellot Rubio, the North American Meteor Network and Mark Davis, and the Association of Meteor Observers in and around Tokyo Area from whose internet homepage a number of records were taken; a list which is certainly far from complete and without a ranking by its order. The list of contributors is so impressive, that we can say for sure the 1998 Leonids were the most successful observing campaign ever carried out. Thank you for all the observing reports!
The beginning of the whole activity period is covered by few data; the earliest r-value of 2.4 in the graph was derived from 4 magnitude distributions, and it indicates that the population index resembles values of other major showers off their maximum. The r-value starts to increase quickly after lambda=235.3° ending up at values of about 2.1 on November 19.
Figure 1: Population index profile of the 1998 Leonids.
The lowest r-value of 1.19±0.02 at lambda=234.43° (November 16, 23h 30m UT) coincides quite well with the highest ZHRs observed in 1998 (see below). Such a low population index is very rare even among major meteor showers. A value of r=1.0 means that no faint meteors are appearing at all. Because of the excitement of the observers and the abundance of meteors, we should bear in mind that the population index as well as the activity are lower limits for the true values. A considerable number of faint meteors may have been missed during the impressive show of fireballs. When operating with r-values, we should not forget that the population index as a power law may not be valid at all for a magnitude range as wide as in the bright-meteor component of the Leonids stream, and r may not be a suitable measure to define the mass distribution within the stream.
Figure 2: Small-scale variation of the population index of the 1998 Leonids around the faint-meteor component. The magnitude distributions were binned in 0.05 classes shifted by 0.025.
First impressions of the Leonid fireball night November 16-17 gave higher values for the hourly rate. The very low population index is probably the main reason for the ZHR being so much lower. First calculations with a major-shower r-value of 2.0 give rates which are 1.5 times higher at lm=5.5mag than with r=1.3. Again, the activity might be underestimated by some of the observers, since less attention may have been paid to faint meteors under the fireball display. A selection of those observations which report no meteors fainter than +2mag gives no preference to either high-rate or low-rate observers. Video records will tell us more objective numbers, though they will not cover the whole activity period.
Figure 3: ZHR profile of the 1998 Leonids. The radiant elevation is corrected for by the geometrical factor sin-1hR, which may underestimate low-elevation ZHRs. See the details in Figures 4 and 5 and the discussion in the text for final values of a maximum ZHR.
Figure 4: Small-scale ZHR profile of the 1998 Leonids around the time of highest activity. Only observations with radiant elevation hR>50° were used to avoid any influence of non-geometrical zenith corrections. The obervations were binned in 0.05 classes shifted by 0.025.
The ZHR may be subject to deviations of the zenithal correction from the geometric value sin-1hR with hR being the radiant elevation. The exponent may be altered to values higher or lower than unity. A general value of 1.4 was adopted in [3], and a re-calculation of the ZHR profile with a zenithal exponent of gamma=1.4 shifts the whole graph up with a maximum ZHR near 300, which is simply a consequence of gamma increasing the corrections at all elevations. The abundance of observations allowed a restriction to observations with hR>50°, reducing the set of rates to those which are not strongly affected by the uncertainty in the zenith correction; the results for the broad component and the `storm' component are given in Figures 4 and 5. The ZHR appears to be significantly higher than the average of all elevations hR>20°. The indications for gamma>1.0 contradict the finding in [4] that gamma is not larger than unity for the Leonids.
Another difficulty at very low population indices is the change in effective field of view. Usually, about 98% of all observed meteors appear within a field of 105° diameter. This will hardly be true for an abundance of fireballs. Future analyses should scrutinize the influence of a low r on the actual activity measure and on the spatial number density (flux density) in particular.
Despite the clear maximum near lambda=234.5°, we should pay attention to the additional activity enhancement which is close to the prediction for the storm component. This secondary peak was hardly detectable by the observers in the field, but the significant increase of the population index makes the enhancement more prominent. The ZHRs are far below even pessimistic predictions - no meteor storm was observed. Very fine temporal binning of ZHRs in windows of 0.02 length (about 30 min), shifted by 0.01, reveals a short peak at lambda=235.308°±0.010°, (November 17, 20h 30m UT) as shown in Figure 5. The set of observations was restricted to those with hR>50° in order to find the actual peak ZHR being less affected by zenithal-correction uncertainties. Since systematical errors are involved additionally to the statistical uncertainty, we are well advised if we double the errors and fix the sharp peak at ZHR=180±20. The same rule gives a Leonid maximum of ZHR=340±20 for the bright-meteor component.
The extremely short period cut out in Figure 5 allows us to subtract a roughly linear decrease of the background component from the ZHR values, such as ZHRback~ 40288-170.9 lambda. The full width at half maximum of the remaining component is 0.031° corresponding to about 45 minutes or B~20 in terms of [3] which is quite similar to B~30 for the Leonid outbursts in 1866, 1867, 1966, 1969. A first detection of the short-lived peak in this Leonid epoch (which has produced enhanced activity since 1994) was found in 1996 data in [5] with B~30.
Figure 5: Small-scale ZHR profile of the 1998 Leonids around the time of storm prediction. Again, only observations with hR>50° were used. The obervations were binned in 0.02 classes shifted by 0.01.
The lowest population index of r=1.19 occurred about 0.09 earlier than the ZHR maximum in solar longitude (2.2 hours) which is not exceptionally much given the broad shape of the background component. The faint-meteor component peaks also at the end of the high population index period.
rho6.5 = ZHR c(r) / (Ared vinfinity).
The factor c(r) is the correction of the observed ZHR to a true ZHR in the observing field, taking into account that the probability to detect meteors of various magnitudes is less than 100%. ZHR measurements have to be reduced to a standard collection area Ared which depends on the population index r and the elevation of the field of view hfield. The so-called `reduced area' Ared depends only weakly on the field elevation between r=2.0 and r=3.5. The area Ared is thus a function of just r in that range. For very low population indices, however, the graphs for different elevations diverge strongly. The reduced area for 50° field height will be 2-3 times higher than for a field in the zenith when using r=1.3 as observed in 1998.
New numerical integrations of the standard collection area
Ared = INTEGRALfield of view r5 log(100 km / d) - epsilon dA
were carried out, where d is the distance to the infinitesimal area dA and epsilon is the extinction. As in [1], meteors appearing lower then 4° above the horizon are excluded, the curvature of the Earth is taken into account. An approximate function
epsilon = 0.002 e0.00785 z
was used for the extinction at zenith distance z (here given for degrees). A look-up table of Ared(r,hfield) was created to compute the flux densities. The function c(r), which corrects the observed ZHR to the true ZHR using the perception probabilities of a human observer, is also re-calculated. The linear function given in [1] is perfectly valid within the usual range of r=2--3. However, for a population index of 1.0, which means that there are only infinitely bright meteors, the factor c(r) should become unity. A better approximative function is
c(r) = 0.987 - 5.918r + 6.637r2 - 0.7540r3,
which is perfectly valid between r=1.1 and r=4.4. The flux density profile is given in Figure 6 and exhibits a completely different shape than the ZHR profile. The maximum of the ZHR curve has no equivalent in the flux density graph - at best, a maximum 4 hours later near lambda=234.7°. A high ZHR made of mostly bright meteors does not mean a high spatial density of particles within the stream, since the observer misses very few meteors due to perception limitations (represented by c(r) ), and the magnitude loss of meteors at greater distances (elevations lower than 90°) is more than compensated by the slow decrease of meteor numbers towards bright magnitudes seen in a larger volume (represented by Ared).
The relatively high population index and the activity enhancement at roughly lambda=235.3° reveal the young component of the Leonid stream very distinctly. The flux of about 0.02 particles per km2 and per hour is higher than that of 1996 with 0.012 km-2h-1 as derived in [6,7] and comparable to that of 1997 from [8], the latter being, however, highly uncertain.
It must be underlined here that only observations which report a center of the field view were used for the spatial number density profile. Otherwise, no accurate collection area determination is possible. The observers are encouraged to care for complete observational reports. In this analysis, the missing fields may a matter of preliminary reports, which will be updated soon.
Figure 6: Flux density profile of the 1998 Leonids. Individual data points of observers giving the center of their field of view are plotted along with an average flux density graph with maximum between lambda=235.1° and 235.3°.
The second component is called `the background component' of the stream. The large fraction of bright meteors is a typical feature of such a stream component which is several revolutions around the Sun old. Gravitational perturbations and solar radiation pressure have affected the motion of smaller particles more than that of large particles, resulting in lower mass and population indices. Since orbital dispersion has taken place for a considerable time, the background component is broad.
The 1998 Leonids are characterized by a strong background component with a maximum ZHR~340 centered at lambda=234.5°. The `storm-component' exhibited a relatively weak enhancement of activity of ZHR~180 at lambda=235.308°. In contrast to popular information spread quickly after the Leonid maximum, astronomers have not miscalculated the Leonid peak, since they all referred to the faint-meteor component observed in 1998, very close to the prediction.
We should compare the 1998 results with those of 1965. The number of observational data is very small for 1965; a good summary is given in [10], but this mainly covers Northern American observations. The actual ZHRs deriving from these records are lower than in 1998; the maxiumum was probably ZHR~100 near lambda=234.5°. The abundance of bright meteors was noted, particularly from sites in Hawaii and Australia. An average magnitude from the (moderate) Leonid number of 38 in three hours was -3 [11]. Radar data from the Springhill device as described in [12] and re-analyzed and compared with radar data from Ondrejov in [13] indicate a very broad maximum at lambda~234.5° (1965 November 16, 15h UT), coinciding exactly with the visual and photographic records. A population index of r=1.7 was derived from the echo duration distribution (>1 s). A most interesting feature in the 1965 radar data is a short-lived peak present in both the Springhill and Ondrejov data at lambda=235.16° (1965 November 17, 6h UT).
Figure 7: Comparison between the 1965 and 1998 Leonids from visual observations. The high value of ZHR=125 and those two left and right of it, are estimates from satellite-tracking cameras.
The few visual observations of 1965 are compared with the 1998 ZHR profile in Figure 7. The 1965 data are individual values, and there is no global coverage of the profile; the comparison should be treated with care, particularly as the high value of ZHR=125 was derived from the records of a Baker-Nunn satellite-tracking camera. Nevertheless, the radar, visual, and photographic records of the 1965 Leonids indicate an activity pofile which resembles that of the 1998 Leonids. Even the low population index seems comparable. Judging from these phenomenological facts, we may expect 1999 to show a similar shape of activity as in 1966. The actual maximum meteor numbers are hardly predictable.
I would like to encourage all friends of IMO to tackle these items and many more taking advantage of the data pool gathered after the Leonids. It is certainly the Leonid shower which brings us a wide step forward in all aspects of meteor astronomy.
[1] R. Koschack, J. Rendtel: Determination of Spatial Number Density and Mass Index from Visual Meteor Observations (I). WGN 18:2 (April 1990), pp. 44-58
[2] R. Koschack, J. Rendtel: Determination of Spatial Number Density and Mass Index from Visual Meteor Observations (II). WGN 18:4 (August 1990), pp. 119-140
[3] P. Jenniskens: Meteor stream activity. I. The annual streams. Astron. Astrophys. 287 (1994), pp. 990-1013
[4] R. Arlt, J. Rendtel, P. Brown: ILW Bulletin 9: Results of the 1996 Leonid Maximum. WGN 24:6 (December 1996), pp. 203-206
[5] M. Langbroek: Observation of a Narrow Component of Faint Leonids 1996. WGN 24:6 (December 1996), pp. 207-208
[6] P. Brown, M. Simek, J. Jones, R. Arlt, W.K. Hocking, M. Beech: Observations of the 1996 Leonid meteor shower by radar, visual and video techniques. Mon. Not. Roy. Astr. Soc. 300 (1998), pp. 244-250
[7] P. Brown, R. Arlt: Bulletin 10 of the International Leonid Watch: Final Results of the 1996 Leonid Maximum. WGN 25:5 (October 1997), pp. 210
[8] R. Arlt, P. Brown: Bulletin 12 of the International Leonid Watch: Final Results of the 1997 Leonids and Prospects for 1998. WGN 26:4 (August 1998), pp. 161-165
[9] P. Jenniskens: Meteor stream activity. II. Meteor outbursts. Astron. Astrophys. 295 (1995), pp. 206-235}
[10] L.J.R.: Observer's Page: Observations of Three Meteor Showers. Sky & Telescope 31 (1966), pp. 112-115
[11] anonymous: Many Leonids observed. Sky & Telescope 31 (1966), pp. 58-59
[12] B.A. MacIntosh, P.M. Millman: The Leonids by Radar - 1957 to 1968. Meteoritics 5 (1970), p. 1
[13] P. Brown, M. Simek, J. Jones: Radar observations of the Leonids: 1964-1995. Astron. Astrophys. 322 (1997), pp. 687-695