STCE Newsletter

20 Oct 2014 - 26 Oct 2014

Published by the STCE - this issue : 31 Oct 2014.
The Solar-Terrestrial Centre of Excellence (STCE) is a collaborative network of the Belgian Institute for Space Aeronomy, the Royal Observatory of Belgium and the Royal Meteorological Institute of Belgium.
Archive of the newsletters Subscribe to this newsletter by mail
1. NOAA 2192 in perspective
2. Review of solar and geomagnetic activity (20 Oct 2014 - 26 Oct 2014)
3. Noticeable Solar Events (20 Oct 2014 - 26 Oct 2014)
4. Geomagnetic Observations at Dourbes (20 Oct 2014 - 26 Oct 2014)
5. Review of ionospheric activity (20 Oct 2014 - 26 Oct 2014)
6. Future Events
7. New documents in the European Space Weather Portal Repository

NOAA 2192 in perspective


Much has already been written on the numerous X-class flares produced by NOAA 2192. In this news item, scientists from the STCE let their light shine on some of the other issues associated to this very active region:
- How does NOAA 2192 compare in size to other sunspot groups?
- How "old" is NOAA 2192?
- How exceptionnal was NOAA 2192's flaring activity?
- Why were there no obvious CMEs associated to these X-class flares?




How does NOAA 2192 compare in size to other sunspot groups?


According to the NOAA reports, NOAA 2192 reached a maximum sunspot area of 2750MH (see Note 1) on 26 October. This is comparable to 16 times the Earth's surface area. It is by far the biggest sunspot group of the current solar cycle, and even slightly bigger than the famous Halloween group NOAA 0486 (see Note 2), the largest sunspot region of the previous solar cycle (2610MH). We have to go back already to November 1990 to find the first region which was even bigger (NOAA 6368, 3080MH)!
NOAA 2192 currently ranks 12th in the Top-50 of largest sunspot groups observed since 1874. See http://users.telenet.be/j.janssens/Engzonnecyclus.html#Top50spot for an overview. The largest group appears to have been Greenwich 1488603 which started its transit of the solar disk late March 1947 and reached its maximum sunspot area on 8 April 1947. There are drawings of this sunspot group in the archives of the Kanzelhöhe Solar Observatory at http://cesar.kso.ac.at/synoptic/draw_days.php?year=1947 Amazingly, almost the entire NOAA 2192 group would fit in just the main spot of Greenwich 1488603! See image underneath for a comparison.




How "old" is NOAA 2192?


It is well known that big sunspot groups can survive for several solar rotations. So, it didn't take long before the blogs were speculating on the number of solar rotations NOAA 2192 had already survived. Some of them were going back till June this year, making NOAA 2192 almost 5 months old!
So, a preliminary analysis was performed of the positions and evolution of the sunspot groups that have appeared in this area starting June this year. As it turns out, most of these groups appeared several degrees to the north or the south of NOAA 2192. More importantly, quite a bit of these groups were decaying. This was for example the case early August when the groups NOAA 2127-2131 were rounding the west limb, and the entire area was nearly devoid of sunspots.
An STCE scientist concludes: "... Indeed, I only see one possible recurrence. There was already a big active region complex (NOAA 2172-2173) at that longitude one month ago, crossing the central meridian on 26 September. However, both active regions were decaying and were about to vanish when passing the west solar limb. Therefore, it may well be that this is the first appearance of NOAA 2192. ..."
He adds that "... Let us keep in mind that the past months marked a high peak in the current cycle, possibly the actual cycle maximum. For an active Sun, there is then always a rather large probability that an active region appears in any longitude "bin" simply because of the high overall density of active regions. ... Therefore, in my sense, all earlier cases before September are obviously due to the random location of emerging active regions."




How exceptional was NOAA 2192's flaring activity?


NOAA 2192 has produced already 6 X-class flares, and it has not rounded the west solar limb yet. Since systematic solar x-ray observations started in 1976, about 12000 groups have appeared on the solar disk and got a NOAA-number. Yet, only 13 of those sunspot groups managed to produce 6 or more X-class flares during their transit.
The table below shows this "wild bunch". NOAA 5395 (March 1989) and NOAA 0808 (September 2005) are well-known for their high number and particularly intense solar flares. Interesting is that there are a few groups with a relatively small area that also produced 6 X-class flares, such as NOAA 0649 (July 2004). It's also true that big groups not necessarily produce the most or the most intense X-class flares.




Why were there no obvious CMEs associated to these X-class flares?


THE question of the week was probably why there were no obvious coronal mass ejections (CMEs) associated to all the X-class flares produced by NOAA 2192. Except for the brief HF radio black-outs resulting from the intense x-ray radiation, space weather forcasters were puzzled by the lack of geo-effective effects (no increase in high-energetic particles, no CMEs).
However, scientists of the STCE pointed out that "... Flares and CMEs are both consequences of a restructuring of the magnetic field in the corona. But there are no requirements that both signatures are present. ..." meaning that "... There's nothing in particular that says large flares need to be associated with CMEs. Any large magnetic reconnection event that frees stored ... energy can make a large flare, but the active region is not always in a favorable configuration to produce an eruption. ..."


In the case of NOAA 2192, "... This region appears to be dominated by very strong magnetic fields, which accounts for the strength of the flaring, but does not contain large, unstable prominences. So you can get the interaction of powerful fields and, thus, big flares without freeing a lot of built up field and plasma to erupt. ..." In particular, "... this region's magnetic configuration was close to bipolar on the large scale. So, though it was classified as beta-gamma-delta (see Note 3), the mixed polarities were small and not affecting too much the large-scale magnetic field above the photosphere. ..."
In conclusion, statistically, a big flare is usually associated to a CME, but it is certainly not physically required to have both together. In fact, "... confined X-class flares are not that uncommon (for one reason or another). What is uncommon is such a remarkable series of strong flares without a clear CME. ..." Peculiar cases like these perfectly illustrate the fact that there are still significant gaps in our understanding of the generation of CMEs and in predicting space weather in general.




Note 1 - MH: Millionths of a solar hemisphere, with 1MH corresponding to about 3 million km2. The total area of the Earth corresponds to about 167MH, which is a good reference when comparing big sunspot groups.


Note 2 - The NOAA numbering started in 1972, with currently more than 12000 sunspot groups numbered. Starting from group 10000, it is not uncommon to omit the first "1". Hence, in this text e.g. NOAA 0486 is used instead of NOAA 10486.


Note 3 - More on Beta-Gamma-Delta in this news item at http://stce.be/news/222/welcome.html


Credits - Data and imagery were taken from NOAA/SWPC (http://www.swpc.noaa.gov/today.html), NASA/MSFC (http://solarscience.msfc.nasa.gov/greenwch.shtml), SDO (http://sdo.gsfc.nasa.gov/data/aiahmi/), PROBA2 (http://proba2.oma.be/ssa), and Kanzelhöhe Observatory (http://cesar.kso.ac.at/).

Review of solar and geomagnetic activity (20 Oct 2014 - 26 Oct 2014)


Solar Activity

Nine sunspot groups were reported by NOAA during the week, with NOAA AR numbers 2186, 2187, 2191, 2192, 2193, 2194, 2195, 2196, and 2197. NOAA AR 2192 (Catania number 88) grew to become the biggest sunspot group during two solar cycles (since 1990) and produced the most of the solar activity during the week. This included four X-class flares, fourteen M-class flares, and numerous C-class flares. The only M-class flare produced by another region was the east-limb M1.4 flare peaking at 15:57 UT on October 22 in the future NOAA AR 2197.




The strongest flare of the week was the X3.1 flare peaking at 21:41 UT on October 24. Most of the flares in the NOAA AR 2192 were either confined (and not accompanied by a CME) or associated with weak and/or narrow CMEs that did not arrive at the Earth. The only exception was the M1.4 flare peaking at 19:02 UT on October 20. It was associated with a weak partial halo CME (angular width around 200 degrees) first seen in the SOHO/LASCO C2 field of view at 19:12 UT. The CME was very weak and disappeared before reaching the LASCO C3 field of view, so it did not arrive at the Earth.


The solar proton flux remained at the background level during the week.


Geomagnetic Activity


On October 20 the Earth was situated inside an interaction region between slow and fast solar wind flows. Due to elevated values of the interplanetary magnetic field (IMF) magnitude and predominantly southward IMF direction, the K index reached 5 during one interval in the evening of October 20 (according to Dourbes, IZMIRAN, and NOAA). On October 21 the fast flow arrived, and the geomagnetic conditions were quiet to active. The fast flow was associated with a narrow low-latitude coronal hole that passed the solar central meridian on October 17-18.




On October 22 the fast stream ended, and slow solar wind was observed until the end of the week. Several occasional intervals of active (K = 4) geomagnetic conditions were reported (IZMIRAN even reported one minor storm interval of K = 5 on October 22), but overall the geomagnetic conditions were quiet to unsettled.

Noticeable Solar Events (20 Oct 2014 - 26 Oct 2014)


DAY BEGIN MAX END LOC XRAY OP 10CM TYPE Cat NOAA
20 0900 0911 0920 S14E42 M3.9 1N 47 88 2192
20 1600 1637 1655 S14E37 M4.5 2N 190 88 2192
20 1855 1902 1904 M1.4 120 88 2192
20 1953 2004 2013 M1.7 88 2192
20 2243 2255 2313 S14E36 M1.2 1N 88 2192
21 1335 1338 1340 M1.2 510 III/2II/2
22 0116 0159 0228 M8.7 580 IV/1 88 2192
22 0511 0517 0521 M2.7 88 2192
22 1402 1428 1450 S14E13 X1.6 2B 200 88 2192
22 1551 1557 1603 M1.4 II/1
23 0944 0950 0956 S16E3 M1.1 1F 88 2192
24 0737 0748 0753 M4.0 150 V/2II/1IV/1 88 2192
24 2107 2141 2213 S16W21 X3.1 3B 210 88 2192
25 1655 1708 1811 S16W31 X1.0 3B 160 88 2192
26 1004 1056 1118 S18W40 X2.0 2B 200 88 2192
26 1708 1717 1730 M1.0 110 88 2192
26 1807 1815 1820 M4.2 88 2192
26 1843 1849 1856 M1.9 88 2192
26 1959 2021 2045 M2.4 III/2 88 2192


LOC: approximate heliographic location TYPE: radio burst type
XRAY: X-ray flare class Cat: Catania sunspot group number
OP: optical flare class NOAA: NOAA active region number
10CM: peak 10 cm radio flux

Geomagnetic Observations at Dourbes (20 Oct 2014 - 26 Oct 2014)



Review of ionospheric activity (20 Oct 2014 - 26 Oct 2014)




The figure shows the time evolution of the Vertical Total Electron Content (VTEC) (in red) during the last week at three locations:
a) in the northern part of Europe(N61°, 5°E)
b) above Brussels(N50.5°, 4.5°E)
c) in the southern part of Europe(N36°, 5°E)
This figure also shows (in grey) the normal ionospheric behaviour expected based on the median VTEC from the 15 previous days.


The VTEC is expressed in TECu (with TECu=10^16 electrons per square meter) and is directly related to the signal propagation delay due to the ionosphere (in figure: delay on GPS L1 frequency).
The Sun's radiation ionizes the Earth's upper atmosphere, the ionosphere, located from about 60km to 1000km above the Earth's surface.The ionization process in the ionosphere produces ions and free electrons. These electrons perturb the propagation of the GNSS (Global Navigation Satellite System) signals by inducing a so-called ionospheric delay.


See http://stce.be/newsletter/GNSS_final.pdf for some more explanations ; for detailed information, see http://gnss.be/ionosphere_tutorial.php

Future Events


For more details, see http://www.spaceweather.eu/en/event/future


2014 Conference on Big Data from Space (BiDS '14) in Frascati, Italie

Start : 2014-11-12
This conference aims to bring together researchers, engineers, users in the area of Big Data in the Space sector.
The focus is on the whole data lifecycle, ranging from data acquisition by spaceborne and ground-based sensors to data management, analysis and exploitation in the domains of Earth Observation, Space Science, Space Engineering, Space Weather, etc.
Special emphasis will be put on highlighting synergies and cross-fertilization opportunities from domains like Climate Change, Solid Earth Science, Planetary Sciences, Life Science, Astrophysics, High Energy Physics, Social Sciences, etc.
We expect this conference to:
* contribute towards a common "Big Data from Space" scientific and programmatic framework
* widen competences and expertise of universities, labs and industrial actors
* foster networking of experts and users towards better access and sharing of data, tools and resources
* leverage innovation, spin-in, spin off of technologies, and business development arising from research and industry progress
Website:
http://congrexprojects.com/2014-events/BigDatafromSpace/objectives


European Space Weather Week in Liège, Belgium

Start : 2014-11-17 - End : 2014-11-21
The 11th Edition of the European Space Weather Week will take place on 17-21nd November 2014 in Liège, Belgium.
The ESWW will again adopt the central aim of bringing together the diverse groups in Europe working on different aspects of Space Weather. This includes but isn't limited to the scientific community, the engineering community, applications developers, service providers and service end users.
The meeting organisation is coordinated by the Belgian Solar-Terrestrial Centre of Excellence (STCE), ESA and the Space Weather Working Team. The local organisation is done by the STCE.
Website:
http://www.stce.be/esww11/


AGU 2014 Fall Meeting in San Fransisco, USA

Start : 2014-12-15 - End : 2014-12-19
Join nearly 24,000 Earth and space scientists, educators, students, and other leaders in San Francisco, California, 15-19 December, as they gather to present groundbreaking research and connect with colleagues. The abstract submission site is now closed. The housing and registration tools are now open; pre-registration deadline: 14 November, 11:59 P.M. EST. Note: letters of notification regarding abstract submissions have now been electronically distributed.
Website:
http://fallmeeting.agu.org/2014/


2014 AGU Fall Meeting in San Fransisco, USA

Start : 2014-12-15 - End : 2014-12-19
The AGU Fall Meeting is the largest worldwide conference in the geophysical sciences, attracting more than 22,000 Earth and space scientists, educators, students, and other leaders. For 46 years, energized and passionate Earth and space scientists from around the world gather at the AGU Fall Meeting to connect with colleagues, broaden their knowledge base, and embrace the joy of science. The 2014 meeting takes place Monday 15 - Friday 19 December 2014.
Several sessions about space weather are foreseen:
*
When and Why Does Space weather Forecasting Fail?
*
Addressing Operational Space Weather Needs
*
Near Real Time Data for Earth Science and Space Weather Applications
*
Understanding Hemispheric Asymmetry and Space Weather
*
Connection of Solar Events With the Variability of Space Environments
*
Bz from the Sun to the Earth: Observations and Modeling
*
Solar Sources and Heliospheric Consequences of Coronal Mass Ejections in Solar Cycle 24
*
Advances in Ionospheric Forecasting - Modeling, Observations, and Validation
Abstract Submission Deadline: August 6, 2014
Website:
http://fallmeeting.agu.org/2014/


EGU 2015 in Vienna, Austria

Start : 2015-04-12 - End : 2015-04-17
The EGU General Assembly 2015 will bring together geoscientists from all over the world to one meeting covering all disciplines of the Earth, planetary and space sciences. The EGU aims to provide a forum where scientists, especially early career researchers, can present their work and discuss their ideas with experts in all fields of geoscience. The EGU is looking forward to cordially welcoming you in Vienna!
Website:
http://www.egu2015.eu/


Measurement Techniques for Solar and Space Physics, in Boulder, CO, USA

Start : 2015-04-20 - End : 2015-04-24
This gathering was born out of the desire to collect in one place the latest technologies required for advancement of science in the discipline of Solar and Space Physics. In doing so, it was recognized that the two 1998 volumes of 'Measurement Techniques in Space Plasmas' (Particles and Fields) have been a valuable reference and resource for advanced students and scientists who wish to know the fundamentals of measurement techniques and technology.
Website:
https://mtssp.msfc.nasa.gov/


26th General Assembly of the International Union of Geodesy and Geophysics (IUGG) in Prague, Czech Republic

Start : 2015-06-22 - End : 2015-07-02
We invite contributions on novel inversion methods with application across the geosciences. Of particular interest are 3D imaging, joint inversion of geodetic, geophysical and geochemical datasets, and multi-disciplinary interpretation approaches such as integration of gravity, EM and seismic data or thermo-mechanical modelling studies constrained by physical parameters.
Modelling of Space Weather Effects: Solar, Magnetospheric and Earth Resistivity Constraints (IAGA, IAMAS)
In this symposium we welcome contributions on all aspects of the modelling of space weather and its effects, from the Sun to Earth. This includes the modelling of the various interactions between travelling solar storms and the solar wind, magnetosphere, ionosphere and solid Earth and the validation of models through measurements. Contributions on models developed to aid end-users, such as satellite and power grid operators, survive the impact of space weather are also encouraged.
Website:
http://www.iugg2015prague.com/joint-inter-association-symposia.htm#JA

New documents in the European Space Weather Portal Repository


See http://www.spaceweather.eu/en/repository


STCE - Pourquoi mesurer la pesanteur g?

Presentation, in French given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=542


STCE - Waarom meten we de valversnelling g?

Presentation, in Dutch given at the open doors of the Space Pole, Brussels, Belgium, 2013.
http://www.spaceweather.eu/en/repository/show?id=543


STCE - Pourquoi Vénus est-elle si différente de la Terre?

Presentation, in French given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=544


STCE - Pourquoi installer des stations GNSS en Antarctique?

Presentation, in French given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=545


STCE - L'exploration de la planète Mercure

Presentation, in French given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=546


STCE - De zon bestuderen met PROBA2, hoe ontwerp en lanceer je een satelliet?

Presentation, in Dutch given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=547


STCE - Les grands tremblements de terre de nos régions et leurs conséquences sur le bâti

Presentation, in French given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=549


STCE - Seismologie in België

Presentation, in Dutch given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=548


STCE - Ruimteweer: de impact van zonnestormen op aarde

Presentation, in Dutch given at the open doors of the Space Pole, Brussels, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=550


STCE - Seismologie in België

Presentation, in Dutch, given at the open doors of the Space Pole, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=551


STCE - Les éruptions solaires: quand notre astre se fâche

Presentation, in Dutch, given at the open doors of the Space Pole, Belgium, 2014
http://www.spaceweather.eu/en/repository/show?id=552