18

th Report:

The CMO/OAA Observations made during a fortnight period

 from

1 November 2003 (290°Ls)

to

15 November 2003 (299°Ls)

 


An OAA Mars Section article to be published in CMO #283 (25 November 2003 issue)


 Masatsugu MINAMI, Director of the OAA Mars Section


Japanese version here


W

E here deal with the period from 1 November 2003 (λ=290°Ls) to 15 November 2003 (λ=299°Ls). During the period the apparent diameter δ went down from 15.0" to 12.9".The central latitude φ was about 24°S to 25°S, and the southern hemisphere was well observed. The phase angle  ι went up from 38° to 41°. The eastern quadrature was quite ahead, but we were forced to quite observing before midnight.

 

T

he observers who contributed this period were as follows:

 

AKUTSU, Tomio (Ak)  Karasuyama, Tochigi, Japan

           13 Sets of CCD Images (1, 2, 4, 6, 11, 13, 14 November 2003)

                             f/33×32cm spec with a Bitran BJ-41L

    

IWASAKI, Tohru (Iw)  KitaKyushu, Fukuoka, Japan

        4 Drawings (13 November 2003) 400×21cm speculum

    

FRASSATI, Mario (MFr)  Crescentino (VC), Italia

            1 Drawing (13 November 2003)    250×20cm SCT

     

KUMAMORI, Teruaki (Km)  Sakai, Osaka, Japan 

           13 CCD Images (1#, 4, 7#, 8, 14# November 2003)

               f/50, 84×20cm Dall-Kirkham & f/40×60cm Cass# with a ToUcam

                                            #Sakai City Observatory

    

MASSÓ MILLEURO, Félix (FMr)  La Corña, Galicia, España

            1 CCD Image (1 November 2003) 25cm spec with a ToUcam

    

MELILLO, Frank J (FMl)  Holtsville, NY, USA

           8 Red CCD Images (1, 4, 9, 9/10 November 2003) 

                         20cm SCT with a Starlight Xpress MX5

    

MINAMI, Masatsugu (Mn)  Fukui, Fukui, Japan

           50 Drawings (1, 4, 6, 7, 11, 12, 14 November 2003)

                   480, 400, 340×20cm F/12 ED Goto refractor*

                           *Fukui City Observatory, Fukui

    

MIYAZAKI, Isao (My)  Gushikawa, Okinawa, Japan

            7 CCD Images (5, 8 November 2003)

 f/50×40cm speculum with ToUcam Pro

    

MORITA, Yukio (Mo)  Hatsuka-ichi, Hiroshima, Japan

            8 Sets of CCD Images (6, 7, 13 November 2003)

                          f/50×25cm spec equipped with an ST-5C

    

MURAKAMI, Masami (Mk)  Yokohama, Kanagawa, Japan

      20 Drawings (1, 2, 6, 7, 8, 14 November 2003)

 320, 400×20cm speculum

    

NAKAJIMA, Takashi (Nj)  Fukui, Fukui, Japan

           25 Drawings (1, 2, 11, ~14 November 2003) 

                        480, 400×20cm F/12 ED Goto refractor*

                                                  * Fukui City Observatory, Fukui

    

NARITA, Hiroshi (Nr)  Kawasaki, Kanagawa, Japan

           14 Drawings (1, 2, 6, 13, 14 November 2003)

 400×20cm refractor

    

PARKER, Donald C (DPk)  Miami, FL, USA

            6 Sets of CCD Images (7, 8, 14 November 2003)

               f/20, 59×41cm F/6 spec equipped with an ST-9XE or ToUcam

    

PEACH, Damian A (DPc)  Loudwater, Buckinghamshire, UK

            3 Sets of CCD Images (7, 12 November 2003) 

                               f/31×28cm SCT with a ToUcam

  

PELLIER, Christophe (CPl)  Bruz, Ille-et-Vilaine, France

            5 Sets of CCD Images (1, 3, 6 November 2003)

                       18cm spec with a modified B&W ToUcam Pro

    

ROEL SCHREURS, Eric (ERl)  Mexico

            2 CCD Images (7, 15 November 2003)

  f/50×25cm TEC Mak/MX70 with a ToUcam

    

SIEGEL, Elisabeth (ESg)  Malling, Danmark

            3 Drawings (3, 11, 12, November 2003)  270×20cm F/10 SCT

    

TATUM, Randy (RTm)  Richmond,VA, USA

            1 CCD Image (4 November 2003)

  f/12×25 cm spec with a ToUcam

    

TEICHERT, Gérard (GTc)  Hattstatt, France

            3 Drawings (4, 7, 10 November 2003) 330×28cm SCT

  

VALIMBERTI, Maurice P (MVl)  Melbourne, Australia

            7 CCD Images (7, 8, 10, 13 November 2003)

 f/34×35cm SCT with a ToUcam Pro

  

Van Der VELDEN, Erwin (EVl)  Brisbane, Australia

            3 CCD Images (2, 9, 12 November 2003)

 f/31×20cm SCT with a Vesta Pro modified

    

WARELL, Johan (JWr)  Tcuson, AZ, USA

       4 Sets of CCD Images (2, 3, 6, 10 November 2003)

 f/24×25cm SCT with a ToUcam

   

WILLIAMSON, Thomas E (TWs)  Alburquerque, NM, USA

            1 Set of CCD Images (6 November 2003)

 f/50×20cm spec with a Philips ToUcam

 

 

Morning Mist: Still the terminator morning side was observed thickly covered by the morning mist. From the Oriental hemisphere the mist was watched over the areas to the east of Hellas and Syrtis Mj: See for instance KUMAMORI (Km)’s images on 1 Nov (λ=290°Ls) at ω=219°W, and on 4 Nov (λ=292°Ls) at ω=215°W, 233°W, AKUTSU (Ak)’s images on 2 Nov (λ=291°Ls) at ω=216°W, 234°W, 259°W, Van der VELDEN (EVl)’s on 2 Nov (λ=291°Ls) at ω=238°W, MIYAZAKI (My)’s on 5 Nov (λ=293°Ls) at ω=232°W, MORITA (Mo)’s on 6 Nov (λ=293°Ls) at ω=234°W, 244°W and so on. In particular, Ak’s images show how the mist enters inside deeply. The morning mist over the Margaritifer S and S Sabaeus was watched from Europe: PELLIER (CPl)’s images on 1 Nov (λ=291°Ls) at ω=346°W, 008°W, and on 3 Nov (λ=292°Ls) at ω=348°W, 010°W clearly show the mist. The morning mist over the Solis L area was caught from the US: See TATUM (RTm)’s on 4 Nov (λ=293°Ls) at ω=046°W, and PARKER (DPk)’s on 8 Nov (λ=295°Ls) at ω=026°W, 029°W, and 037°W. WARELL (JWr)’s images on 6 Nov (λ=293°Ls) at ω=113°W, and Km’s on 7 Nov (λ=294°Ls) at ω=170°W show an uneven distribution of the mist and prove the presence of de-concentration like LAU’s (see below).

The mist was also visually strong: MURAKAMI (Mk) described it having a tint of weak violet when Syrtis Mj was coming on 1 Nov (λ=291°Ls) at ω=251°W, 261°W, 270°W. The same scene was observed by SIEGEL (ESg) on 11 Nov (λ=296°Ls) at ω=266°W, and on 12 Nov (λ=207°Ls) at ω=245°W where the strong mist covered the morning Hellas and Syrtis Mj while Hellas showed a detail. The present writer observed that grossly the morning side was whitish, while the afternoon side was yellowish (eg on 4 Nov (λ=292°Ls) at ω=242°W et al), but even then the evening side sometimes also showed a whitish limb (eg on 1 Nov (λ=291°Ls) at ω=262°W, 11 Nov (λ=297°Ls) at ω=175°W~192°W et al: See also below for the cases of the evening Arsia Mons).

 

 LAU Phenomenon: The de-concentration of the mist showing a big hole has been known since the observation by Canon LAU (CLa) on 9 Sept (λ=257°Ls) at ω=088°W, 096°W and since then it was frequently observed. Still the phenomenon was seen at this season as were caught by Km on 8 Nov (λ=295°Ls) at ω=154°W→219°W and also its deformed form on 9 Nov (λ=295°Ls) at ω=155°W: See also Mo’s images on 13 Nov (λ=298°Ls) at ω=152°W, and VALIMBERTI (MVl)’s images on the same day at ω=138°W.

 

 Wine Coloured Dark Areas: We have hitherto paid attention to the areas which showed a tint of dark wine colour since they must have been made free from the covering by the atmospheric matters mingled of the air-borne dusts and thick water vapour condensates (maybe since #14). This time also Mare Chronium and its vicinity showed the colour as shown on the images by My on 5 Nov (λ=293°Ls) at ω=232°W, by MVl on 7 Nov (λ=294°Ls) at ω=194°W, 222°W, and also by Mo on 7 Nov at ω=214°W. My’s image was sharp and also proved the surrounding of the spc to show the wine colour. At the region to the south of Solis L, DPk showed on 7 Nov (λ=294°Ls) at ω=092°W that the area preceding the morning mist patch at Aonius S was wine-coloured. This was also caught again by Km on 14 Nov (λ=298°Ls) at ω=086°W, while Km also took the image at ω=150°W on the same day and hence it well shows a similarity with LAU’s case.

 

 Description of the Evening Limb: We here note that the description of the limb side of CPl on 3 Nov (λ=292°Ls) at ω=346°W, 008°W is superb: Since its B shows a brightness there, the evening haze must be made of water vapour but the images show that it is mingled still with the airborne dusts. Visually SIEGEL (ESg)’s drawing on 3 Nov (λ=292°Ls) at ω=340°W also shows that the Hellas was very bright. Mk also recorded the brightness of the evening haze on 6 Nov (λ=294°Ls) at ω=186°W.

 

  Arsia Mons: Already the phase angle ι was augmented to 40°, it was hard to observe the evening cloud over the summits of Tharsis Montes. The B image by Ak on 6 Nov (λ=293°Ls) at ω=195°W seems to reproduced the evening cloud over Arsia Mons. Km also took images on 8 Nov, but his processing of the limb was not pertinent to the observation of the Tharsis area. Visually, the present writer (Mn) noticed the remaining Arsia cloud on 6 Nov (λ=294°Ls) at ω=194°W, and on 7 Nov (λ=294°Ls) at ω=194°W near the limb, and also saw it on 12 Nov (λ=298°Ls) at ω=192°W. The observation on 7 Nov showed the white area still remained near the limb at ω=223°W. At ω=194°W, the summit of Arsia Mons geographically is quite near the limb (by just 6°), but since ι=39° on 7 Nov, it was still before the sunset by three hours. Olympus Mons’ cloud already ceased its activity, while the Arsia cloud was near the second peak.

 

 SPC and Its Surroundings: The white spc was small but clearly seen during the period. As to the splitting or vanishing of the isolated fragment as suggested by BARNARD’s drawing in 1894 at λ=296°Ls (see Report #17 in CMO#282) DPk’s images on 14 Nov(λ=298°Ls) at ω=342°W  suggests, though the angle was in short. Otherwise EVl’s images on 9 Nov and 12 Nov suggest some projections from the spc, but look ghost-like. At the vicinity of the spc, Thyle was interesting. Mn saw it as if composed of several light spots on 6 Nov (λ=294°Ls) at ω=194°W, and it was largely roundish evident though not so whitish on 7 Nov (λ=294°Ls) at ω=184°W, 194°W.

 

NPH: At the arctic region, we should also be concerned with the activity of the nph, especially at the regions of M Acidalium and Utopia, though it is believed the regions are however rather calm in this season. ROEL (ERl)’s image on 7 Nov (λ=294°Ls) at ω=038°W features well the nph, and its details were shown by DPk on 8 Nov (λ=295°Ls) at ω=026°W~037°W. Also the nph at Utopia was inactive as suggested by the images of Ak on 2 Nov (λ=291°Ls) at ω=259°W(B), of My on 5 Nov (λ=293°Ls) at ω=232°W, and of Mo on 6 Nov (λ=293°Ls) at ω=232°W, 242°W(B).

 

  Auroral Protrusion Phenomenon from Ausonia-Hellas: There was observed from Japan an unusual specific phenomenon which might deserve special mention: It lasted for a few days at the beginning of November and checked by naked eyes as well as by the ccd images. First we should report in what follows chronologically how we observed the phenomenon:

 

On 4 November (λ=292°Ls), a fine day, the present writer (Mn) started his routine observation from 07:50 GMT (16:50 JST, sunset time) at the Fukui City Observatory by the use of the 20cm refractor as usual: The Martian surface showed ω=183°W at 08:00 GMT. The seeing was poor or very poor. The second observation was made at 08:40 GMT (ω=193°W): Since Mn noted here that the morning neighbour of the spc was light wine-coloured, the morning mist was rather white, and the morning Electra-Eridania was usually bright and so on, it must have been such that he was attentive to the morning terminator. Then the third observation was made at 9:20 GMT (ω=203°W) (started from 9:10 and ended at 9:30 GMT): The se eing was slightly improved, and, after checking that M Chronium was in a wine colour and Thyle was quite faded to the south of it, and the mist at the morning side was so thick that M Cimmerium was bluish, he became aware that the terminator following Ausonia looked strange. Apparently from the terminator stood there a convex protrusion which was not so vivid, nor cloud-like but just like a broad brush protruded from the terminator, or a silent broad steam. It was constantly visible .The width was about 10°. The height is low compared with the width, and the upper boundary was not obvious because it gradually faded. However he was sure that it was a real phenomenon on Mars, while thought that it was a kind of phenomenon he had never experienced or heard in his long observational life. Since it looked not conspicuous, it was possible it meant just nobody had never been aware of it if any. So to record or discard, it was the question. After that, the seeing did not improve, and at ω=213°W he could not detect the protrusion. It remained the same at the following observations at 222°W, 232°W, 242°W, and 252°W (12:40 GMT). Just the area around Ausonia was thickly covered by the mist and showed different colour than the preceding reddish Eridania at ω=232°W. At ω=242°W, Hellas was coming covered by the morning mist, and while he watched until 13:20 GMT (at ω=261°W), Hellas was not particularly bright nor showed any particularity.

 

On 5 November, the sky was not preferable at Fukui. On 6 November, he could first observe at 8:00 GMT (at ω=164°W): The seeing was better than the condition on 4 Nov, and observed successively at ω=174°W, 184°W, and at 194°W, but then unfortunately it was clouded. At the final stage Mn was not able to be aware of the protrusion.

 

On 7 November (λ=294°Ls, δ=13.8"), though the sky was haunted by cloud patches, and the seeing was unstable, Mn started from 7:50 GMT and made the first observation at 8:00GMT (ω=155°W). At 8:40, it was cloudy. Then he restarted from ω=174°W (at 9:20GMT), and observed also at 184°W, 194°W, and reached ω=203°W. At ω=194°W, the seeing was rather good and used 600× in addition to 480×, but Mn was not aware of the protrusion. At ω=203°W (at 11:20 GMT), the seeing was not bettered but the protrusion proved to be clearly seen! To tell the truth, since he had rather discarded the phenomenon on 4 Nov in his mind, he awaked at this moment to it knowing the present LCM pinned down the same angle as on 4 Nov. Ausonia was not particularly bright, and the protrusion looked quite plain but reminded him of the 4 Nov case. How does anybody do in such a case? Using several eyepieces, and moving the image at every corner of the ocular-field, he was thus determined not to discard the phenomenon. This session ended at 11:30 GMT, but he remained chasing the image, and started the next session slightly earlier from 11:46 (at ω=209°W). The protrusion was still evident. So at 11:55 GMT (8:55 PM JST) Mn tried to ring up Isao MIYAZAKI (My) at Okinawa away by 1300 km from Fukui by the use of mobile telephone (My’s phone number being recorded in Mn’s mobile). He replied, and Mn, watching the image at the eyepiece, described about the protrusion and asked him to readily observe and check it. My agreed to go up to his observatory. Unfortunately however Mn heard later that though My waited at his observatory, the sky at his place remained unfavourable on the night of 7 Nov (MIYAZAKI emailed to Mn at 14:10 GMT (23:10 JST)).

At Mn’s observing time 12:05 (ω=214°W), the protrusion was still visible. At 12:09 (ω=215°W) it looked slightly weaker. But at 12:15 (ω=217°W) it was still caught by 400× though weak. At 12:17 (ω=217°W) it was seen still by 480×. Even at 12:20 (ω=218°W), the convex form was noticed, but looked disappearing. At 12:23 (ω=218°W), he could detect, but from around 12:30 GMT, the seeing was broken. At the next routine observation time at 12:40 (ω=223°W), it was no longer seen, and no remnant was detected. Before that Mn contacted MURAKAMI (Mk) at Yokohama by the mobile. The sky seemed to be unfavourable there in the evening, but he was persuaded to come up to his observation site and at least at around 12:30 GMT he could catch the planet inside the ocular-field and could take a glimpse of the convex protrusion by his (Saheki made) 20cm spec: He recorded it as his observation on 7 Nov at 12:30 GMT (ω=220°W) and its note says he was talking with Mn on the phone at the eyepiece at that moment. Unfortunately the sky was then clouded again there.

At 19:02 GMT (at 04:02JST on 8 Nov), Mn sent an email to the Japanese observers to check their observations at the beginning of November as well as to be on the alert on this phenomenon. Since AKUTSU (Ak) took images on 6 Nov at ω=195°W, it was possible for him to have met the phenomenon.

 On 8 November, it was cloudy at Fukui. However very fortunately MIYAZAKI (My) at Okinawa was endowed with a fine sky, and detected successfully the phenomenon by his 40 cm spec both visually and by the ToUcam. He readily processed a few images with a rush and sent it to us on 8 Nov at 15:17 GMT (midnight at 00:17 JST): Visually, he wrote, he could not detect any at around 10:00GMT (ω=174°W), but at 11:00 GMT (ω=189°W) the projection was very obvious to his eye which was clearly standing from the terminator, and it was perfectly visible until 12:50 GMT (ω=215°W) when it became cloudy. The attached file (here cited) showed the images by ToUcam at 11:41GMT (ω=199°W). The projection looked quite the same as Mn watched on 4 Nov and 7 Nov, and the images gave Mn the impression which he held on 4 and 7 Nov. The B image was the one taken at 11:16 GMT (ω=193°W), and this proves the convex projection was much weaker than the nph, and so never made of the white cloud or had no brightness of the white cloud. By the afternoon of the following day, My completed the processing of all images and sent a full file out at 05:10 GMT (14:10) on 9 Nov. He also noted the one taken earlier at 9:33 GMT (ω=168°W) also showed a weak convex. This final file readily replaced the previous provisional one on the CMO Mars Gallery, and the window at the façade of the CMO Web noticed as follows within the day:

8 November 2003 (λ=295°Ls) : A prominent protrusion from the terminator is visible: On 4 November at the session of ω=203°W, MINAMI was visually aware of a light protrusion at the morning terminator around the lat 40 - 50°S, and again on 7 November at ω=203°W, he noticed the same protrusion. It was explicit until around ω=220°W. During the session, MINAMI communicated with MIYAZAKI on mobile, while it was cloudy at Okinawa. Isao MIYAZAKI however confirmed visually the phenomenon on the following day. It was not seen before 10h GMT on 8 November at ω=170°W yet, but very explicit at 11h GMT (ω=188°W) and visible until ω=215°W when it became cloudy. See the CMO Gallery for MIYAZAKI's ToUcam images. The blue image does not show any prominent cloud. The auroral matter looks to cover the higher skies of the area from 260°W to 285°W (so the west of Ausonia to the eastern Hellas across M Hadiacum). Further observations are welcome.

My’s images run nearly every 20 minutes as follows: at ω=190°W (11:05 GMT), ω=195°W (11:23 GMT), ω=199°W (11:41 GMT), ω=204°W (12:00 GMT), and ω=209°W (12:20 GMT): these all show the projection clearly but similarly and do not look to say about the peak. The image at ω=199°W may be most excellent, but the one at ω=190°W also shows Caralis Fons clearly. His first shot shows the projection seems to be weakly seen at ω=170°W (power difference of 40cm from 20cm and the latitude or altitude difference by 10 degrees of Okinawa from Fukui cannot be overcome), but we should say his observation might have implied the projection became quite obvious around from ω=190°W up around to ω=215°W (quitted by the clouding). If the phenomenon repeated on 7 Nov as well as on 8 Nov in the same way, since Mn did not catch it at ω=194°W, the projection must be perfectly obvious from around ω=200°W to around ω=220°W, and the peak must be at the beginning of the period.

 The convex area looked to cover the angles around 40°S~50°S (and so about 300km wide). The difference of the longitude from the LCM to the terminator at 40°S is 70°W, and at 50°S is 80°W so that at ω=170°W the terminator is located at Ω=240°W~250°W, and at ω=220°W it is located at Ω=290°W~300°W. This implies the area spans from Ausonia to Hellas (about 1300km long). At ω=200°W, the terminator is situated at around Ω=270°W~280°W, and so it means a area between Hellas and Ausonia, maybe near M Hadriacum or the eastern cliff of the Hellas basin.

 

After 9 November, no explicit observation was made. It was cloudy in Fukui and also drizzled at Okinawa. Next opportunity came at Fukui on 11 Nov, but it was windy, and full of cloudy: NAKAJIMA (Nj) and Mn observed only at ω=170°W~180°W and failed to give any explicit results. It was the same on 12 Nov. On 11 Nov, Ak shot only at ω=151°W, and on 13 Nov Mo also gave images at ω=148°W, 156°W, 163°W, but we did not hear how he processed. On 14 Nov, the present writer (Mn) chased up until 13:10 GMT at ω=163°W, and just before the seeing was broken at ω=134°W, he did not see any protrusion on the terminator at 40°S~50°S.

We also asked the observers in Australia. VALIMBERTI (MVl) took images on 7 November at ω=194°W, 204°W, 222°W, and on 8 November at on ω=194°W, but his reply was: “Unfortunately, due to a change in camera settings for some recent solar work (with the 15cm refractor), my Mars data has suffered with low signal over the past couple of days. I have not had the opportunity to 'fine-tune' the camera for Mars and the C14 again. The regions near to the terminator rapidly fade to black so I have not succeeded in extracting useful information from these image areas.” (LtE)

Really at that time, the Sun was active (as reported in some details below), and there is a speculation that the protrusion phenomenon may be related with the enormous activity of the Sun, it was really unfortunate (both to us and to him). Km also made several images on 8 Nov, but we did not hear the detection. MIYAZAKI says the usual mind to treat the images did not produce the projection on the monitor. We finally add that on 8 Nov, Mk also pointed to the planet through the light cloud at ω=199°W, but failed to detect.

 

  So, the phenomenon was very apparent to the naked eyes, but those who had a chance to see really the convex complex were no more than MIYAZAKI, MURAKAMI (just a glance) and the present writer (Mn). To elucidate what it was or how it was given rise to, we need much more observations of exactly the same phenomenon. Just this was not the instantaneous one like the case where a steep topography passes the terminator, but it lasted long and further repeated for a few days so that if it is reproduced again it is quite possible for the observers on the alert to be able to witness the appearance and give some details. However it will be limited with a region on the Earth, and quality observations are needed under a good network communication. If the phenomenon was a rare one though spontaneous, we may not be able to meet it again for more than a decade or so.

 

MIYAZAKI (My) recalled from its sight it looked just something like the aurora spread at a higher altitude. This was also an impression the preset writer (Mn) conceived. However our colleague Kanehiro OSA (Oa), who is otherwise interested in the aurora phenomena, says it must have never been the genuine aurora since the planet has not much magnetic fields, and furthermore the images of the auroral matter made by My are rather too distinct. Oa also pointed out that My’s continual images might show a moving of the convex along the latitude also. Oa also suggested several possible causes of the projections: Usual suppositions of volcanic activity or a clash of an asteroid are possible, and furthermore if the dust is composed of a lot of irons oxide the charged particles there may cause a long standing spark like thunder if all dusts happen to be charged; since the atmospheric pressure is low, the cathode is easily accumulated. There is also a speculation that it was like a tail of a comet since the Sun activity was strong at that time, and from the end of October, the proton wind must have caused a plasma layer which could show a lightening.

In fact, as will be reported below, the flares on the Sun was quite extraordinary at the period, and we were on the alert if some usual events might happen. As was noted by MURAKAMI (Mk) and TSUNEMACHI (Ts), in the Director’s Note window in the Façade,

25 October 2003 (λ=286°Ls) : The Sun looks now active these days. MURAKAMI and TSUNEMACHI informed us that an X5.4 flare was erupted from AR#0486 on 23 October at 8:19 GMT.
 See http://sidc.oma.be/index.php3 and http://www.lmsal.com/solarsoft/latest_events/gev_20031023_0819.html A strong interplanetary shock wave passed us on 24 October at 14:50 GMT. Don PARKER's image of AR#0486 on 24 October at 17:17 GMT is found in
 http://science.nasa.gov/spaceweather/swpod2003/25oct03a/Parker1.jpg As to a possible importance of X flares in relation with the planet Mars atmosphere, see http://www.kwasan.kyoto-u.ac.jp/~cmo/cmohk/270Note17/index.html

28 October 2003 (λ=288°Ls) : MURAKAMI and TSUNEMACHI informed that an X17.2 flare was set off from AR#0486 on 28 October at 9:51 GMT and lasted until 17:54 GMT (maximal at around 11 hrs GMT). It caused a full halo CME, and at 12 hrs GMT a proton event started. See
 http://sohowww.nascom.nasa.gov/hotshots/2003_10_28/
 This X17 flare is nominated as the second largest flare observed by SoHO: The biggest flare was the one (X20) observed in April 2001 just before the 2001 Martian dust storm: see
 http://www.kwasan.kyoto-u.ac.jp/~cmo/cmohk/270Note17/index.html

 

Note that the Flare which occurred on 28 October at 9:51 GMT was announced to be as large as X17.2 and several flares followed. We were therefore more attentive to a rise of a serious dust disturbance as in 2001.

 

The present writer (Mn) has a tendency to loose interest in those phenomena which don’t repeat (so if the confirmation of MIYAZAKI did not follow, he does not write about it thus far long). Therefore Mn has not been so interested in nor ponder on the so-called “Gray Cloud.”  So unfortunately he is not well acquainted with the terminal phenomenon nor the other cloud than “Yellow” and “White” (furthermore he also does not believe in the Blue cloud). Here however an old but good review by Holger HEUSELER (WFS, Berlin) who wrote a review on some atmospheric phenomena which may be related with the volcanic activity in Die Sterne 45 (1969) 133 entitled “Betrachtungen zur Vulkanaktivität auf dem Planeten Mars sowie synoptische Studien atmosphärischer Trübungserscheinungen”:  In its first section "Beobachtungen von grauen Wolken in der Marsatmosphäre" (observations of grey clouds in the Mars atmosphere), HEUSELER picked out several observations including those the present writer is not acquainted. First, as usual, he alluded to ANTONIADI’s grey cloud at Deucalionis R observed in 1911 (in his final book ANTONIADI also suggested a possibility of a volcanic activity in Deucalionis R, but did not mention about the grey cloud, though he admitted the Region showed sometimes a greish tint). The HEUSELER picks out the famous “grey clouds” observed in 1950 by Sayeki and Ebizawa (so written, while we write SAHEKI and EBISAWA: Yes, somebody sometimes pronounces as Sayeki, but EBISAWA’s s is not like the s of Gesang or oiseau). Furthermore HEUSELER counts in the famous phenomenon on Tithonius L observed by “Sayeki” made on 8 December 1951 as an observation of the large grey cloud. The latter is well known as the case where SAHEKI observed a bright flare which lasted for 5 minutes, but HEUSELER pays attention to the fact that the area was originally covered by the large cloud. SAHEKI’s revised book just mentions the cloud was covered by a white cloud, but HEUSELER might have been based on some earlier literature, and writes "eine grauße graue Wolke" which lasted 40 minutes (he restates this Tithonium phenomenon in the part of flares). HEUSELER also reports that “Ebizawa” observed several grey clouds in March/April in 1962, and also picks out MIYAMOTO’s observation on 5 May 1967 and states that MIYAMOTO observed a strange grey matter over Amazonis and Arcadia. In fact one page of the bulky collections of Prof MIYAMOTO’s articles shows that he observed on 5 May 1967 at 14:07~25 GMT (λ=126°Ls, ω=158°W, φ=22°N, δ=15.1”) and left a note: "Bright and grey mosaic structures is visible in Amazonis and Arcadia. Dark spots in Propontis." Otherwise, HEUSELER includes C F CAPEN’s observations at the same period as Ebizawa in 1962 as well as the observation from 9 January to 12 January 1965 made at the Table Mountain Observatory, Kalifornien: These were checked by the B filter and had an aspect of “das dunkle atmosphärishe Band”. Since these were observed from the preceding terminator to the morning side, this must be very different from what we saw this time. HEUSELER finally cites an observation of a "Rauchsäuleneffekt" from an unknown literature (similarly unknown when it was made). If the Säule is broad, the smoky column may be attraction, but how can it be broad enough?

We have followed HEUSELER as above, and we don’t know the list is exhaustive, but as far as we depend on his descriptions, none should be said to correspond to our case. Mn himself have never seen the grey cloud, but as far as if we depend on the descriptions by SAHEKI or EBISAWA (long ago in a book in 1954) the present one is not any “grey cloud”. MIYAZAKI is also of the same opinion. We should further emphasise it was never the case of a bright white cloud at the terminator which may otherwise make a delusion that the terminator is partly convex.

If the phenomenon repeats again in a near future, it may be also clear but never conspicuous, and so we must always prepare to reproduce the dim terminator side well.

 

Appendix: (Solar Activity from the end of October to the beginning of November): Since just before the great yellow cloud in 2001, it was known a very great unprecedented flare occurred on the solar surface, we were used to keep information of the solar activity in mind. In this respect, MURAKAMI (Mk) and TSUNEMACHI (Ts) have been checking real surface or the internet information (Ts also was receiving and forwarding information from the Hiraiso Solar Terrestrial Research Center). Thus from the end of October 2003, we began to hear the extraordinary activity of flares and CME: as aforementioned the one unleashed by AR#10486 on 28 October at 9:51 GMT was of the X17 scale: Since the one emitted by #AR9393 on 2 April 2001 was first announced X17, this was really big (the 2001 one was later classified as X20, and regarded the biggest ever since). As here shown by the graph made by Mk, AR #0486 also caused others on 23 Oct and on 29 Oct. On 30 Oct at 15:23 GMT, Mk sent an email to Mn speculating that the proton wind will reach Mars on the following day. He also reported it was supposed to reach the Earth earlier than expected, and the aurora was already witnessed at Hokkaido. He himself was making routine observations of the sun spots, and he observed #0486 on 30 Oct was not so different from the aspect on 27 Oct, but AR#0488 which started from 26 Oct looked to be rapidly developing (already caught by naked eyes). There were also several smaller groups which were rising, and he had an impression that the activity was increasing. In the evening he observed the Martian surfaces from ω=260°W to 309°W on 30 Oct (not yet ω=200°W). These ARs were also watched by DPk and MVl and the AR images were communicated to us as cited in #282. As cited, MVl tuned the ToUcam for the bright Sun, and so missed the dim projection from the Martian terminator. It is difficult to kill two birds by one stone.

Thus we were somewhat on the alert, but we thought the effect if any will appear one month or more later, and so did not so regard it as a pressing issue. In 2001, there was a separation of one month and half from the unleashing of the giant solar wind and the veiling of the yellow cloud. So if the phenomenon on 4 November is related with effect of the X17 flare, it should have been more direct. The yellow cloud covering is usually considered to be caused by a meteorological reason, but we may speculate that the expansion at the higher layers is promoted more physically by some kind of plasma if some accumulation and retardation is attained. This time if it was also the effect of the emitted matters of the Sun, we may say the razor thin atmosphere must have directly and effectively received it on the ground as a cathode layer.

The Sun activity continued. On 4 November at 19:29 GMT, AR#0486 emitted unprecedented big flare as reported on the Façade of the CMO Web:

5 November 2003 (λ=293°Ls) : TSUNEMACHI communicated to us that the out-going AR#0486 unleashed a mega X-whatsoever flare on 4 November at 19:29 GMT. It was temporarily classified as an X17.4 by the SEC, but expected to be revised as more powerful than X20: See
 http://sohowww.nascom.nasa.gov/hotshots/2003_11_04/
Note Added : The mega flare on 4 November has been revised by NOAA to be an X28, doing away with SEC's X17.4. The associated proton event showed its peak on 5 November at 6h GMT.

As seen from the graph here of Mk, it was emitted when the relative numbers very decreased, that is, the emission occurred quite near the solar limb, and so it must have been not so fatal to the Earth though there were reported several difficulties were brought, while the proton activity lasted at the peak at 6h GMT on 6 Nov. To Mars, it must have been a little more decisive due to an angle difference. It will be necessary and interesting to pursue the geometry of the proton path to the planet Mars in connection with the activity from the end of October to the beginning of November.

 


T

he next issue shall treat the observations made in the Second half of November 2003 from 15 November (λ=299°Ls, δ=12.8") to 30 November 2003 (λ=308°Ls, δ=11.2").


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