the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
29 Sep 2021
29 Sep 2021
Exceptional middle latitude electron precipitation detected by balloon observations: implications for atmospheric composition
- 1St. Petersburg State University, St. Petersburg, Russia
- 2Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
- 3Lebedev Physical Institute, Russian Academy of Sciences, Moscow, Russia
- 4British Antarctic Survey, Cambridge, United Kingdom
- 5Instituto de Astrofisica de Andalucia, CSIC, Granada, Spain
- 6Moscow Institute of Physics and Technology, Moscow, Russia
- 7PMOD/WRC and IAC ETHZ, Davos, Switzerland
- 8Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA USA
- 1St. Petersburg State University, St. Petersburg, Russia
- 2Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
- 3Lebedev Physical Institute, Russian Academy of Sciences, Moscow, Russia
- 4British Antarctic Survey, Cambridge, United Kingdom
- 5Instituto de Astrofisica de Andalucia, CSIC, Granada, Spain
- 6Moscow Institute of Physics and Technology, Moscow, Russia
- 7PMOD/WRC and IAC ETHZ, Davos, Switzerland
- 8Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA USA
Abstract. Energetic particle precipitation leads to ionization in the Earth's atmosphere, initiating the formation of active chemical species which destroy ozone and have the potential to impact atmospheric composition and dynamics down to the troposphere. We report on one exceptionally strong high-energy electron precipitation event detected by balloon measurements in middle latitudes on 14 December 2009 with ionization rates locally comparable to strong solar proton events. This electron precipitation was likely caused by wave-particle interactions in the slot region between the inner and outer radiation belts, connected with still not well understood natural phenomena in the magnetosphere. Satellite observations of odd nitrogen and nitric acid are consistent with wide-spread electron precipitation into magnetic midlatitudes. Simulations with a 3D chemistry-climate model indicate almost complete destruction of ozone in the upper mesosphere over the region where high-energy electron precipitation occurred. Such an extraordinary type of energetic particle precipitation can have major implications for the atmosphere, and their frequency and strength should be carefully studied.
Irina Mironova et al.
Status: final response (author comments only)
-
RC1: 'Comment on acp-2021-737', Anonymous Referee #1, 03 Oct 2021
Review of “Exceptional middle latitude electron precipitation detected by balloon observations: implications for atmospheric composition” by Mironova, Sinnhuber, Bazilevskaya, Clilverd, Funke, Makhmutov, Rozanov, Santee and Sukhodolov
The electron precipitation event is quite intriguing and should be published. However contrary to what has been stated in the paper, the interplanetary and geomagnetic conditions are quite ordinary and are not an obvious cause. I will comment in more detail about that. I would say that the event is more of a mystery than one that can be explained. I think the authors will agree with this point of view?
Main Comments
Please provide a blow up of the solar wind parameters and the geomagnetic activity before and after your event. A better geomagnetic index now commonly used is the SME index. It involves many more ground stations and is a better index than AE. The SYM-H index is essentially a one minute average of Dst and therefore with better time resolution is superior to Dst. I recommend that you use this index as well.
I have made such a plot to see what was going on in interplanetary space and on the ground for your event. I agree that I have found nothing exceptional for your exceptional electron precipitation event. A ~200 nT substorm is very common and is a weak event. If you look at JGR, 95, A3, 2241-2252, 1990 in their Figure 2, 200 nT is quite weak in comparison to a general distribution. If you look at a distribution of SME values you will find the same results. The same goes for the interplanetary Bz component. A value of ~-5 nT is quite common. Look at the above paper’s Figure 1.
Your comment that there is not a magnetic storm is correct. But I take exception to your ascribing your event to a 200 nT substorm. I think this should be toned down since the substorm is so weak.
Abstract, line 5. “This event was likely caused…”. Perhaps “possibly” rather than “likely”? Soften things a bit. I will later point out that this is a double substorm event. This may possibly be the cause?
The readership should know that your event is one of precipitation of relativistic electrons that are already trapped in the magnetosphere and were accelerated by other mechanisms. The precipitation event does not have anything to do with the acceleration of the electrons to such high energies. This is not clear in the present version of the text. Please correct the text so that the readership will not be misled. Acceleration mechanisms are described in Nature, 437, 227, doi:10.1038/nature03939; JGR, 115, A00F01, 2010. doi:10.1029/2010JA015870; ApJ, 799:39, 2015, doi:10.1088/0004-637X/799/1/39. You may wish to add a short discussion of this for the readership?
Minor Comments
Line 17. A good reference to add here is JGRSP, 121, 2016. doi:10.1002/2016JA022499.
Line 117. “AE index larger than 200 nT”. In my plot I find two substorms, one with an SME of ~500 nT and a second with ~400 nT. It would be best if you quote exact numbers. And of course show the plot in high resolution.
Same line. A Dst of -12 nT is not thought of as a magnetic storm. I suggest that you state this here. A good reference for this is JGR, 99, A4, 5771-5792, 1994. They quote a Dst level which they consider a threshold for a magnetic storm. Most space weather people use this value.
Lines 120-122. I suggest that you reword this. I see two dips in the IMF Bz. These cause the two substorms as mentioned above. You should refer to this when you show your blow up of the solar wind parameters and geomagnetic activity. It is possible that the TWO substorms may have caused your unusual event. Concerning a good reference for IMF bz and substorms, see JGR, 77, 16, 2964-2970, 1972. The event in Figure 3 has some similarities to your event.
Lines 245-6. New results show that plasmaspheric hiss is most intense near the slot region, not near the plasmapause boundary. The new results show that plasmaspheric hiss is quasi-coherent leading to orders of magnitude faster pitch angle scattering. This paper hypothesizes that the slot is formed much faster than previously believed. See JGRSP, 124, 10063-10084. 2019. https://doi.org/10.1029/2019JA027102 and references therein.
Lines 263-264. It might be possible that it is not substorm intensity that led to your event, but the double substorm. For example here is a scenario. The first southward IMF Bz led to the first substorm through magnetic reconnection (reference Phys. Rev. Lett, 6, 2, 47-48, 1961). This led to the injection of ~10-100 keV electrons in the midnight sector (reference JGR 76, 16, 3587-3611, 1971). The electrons gradient drift to the noon sector (taking ~ 1 hr see JGR82, 32, 5112-5128, 1977) and there create electromagnetic outer zone chorus through the temperature anisotropy instability (reference JGR, 71, 1, 1-28, 1966). The chorus propagates into the plasmasphere (reference Nature, 452, 2008. Doi:10.1038/nature06741). Now a second southward IMF creates a second substorm and the injected 10 to 100 keV electrons drift from the midnight sector to the noon sector. When these electrons get there they enhance the preexisting hiss in the slot region leading to the parasitic loss of relativistic electrons.
-
RC2: 'Comment on acp-2021-737', Anonymous Referee #2, 22 Oct 2021
The authors use a number of observations and simulations to investigate the atmospheric impact of an EEP event identified by a ballon borne experiment. The study is very interesting, but I find that some of the necessary supporting information is not included and it is not always clear why things were done the way they were. Detailed comments and questions are included below and I recommend that these are addressed in a revision before the paper can be accepted for publication.
Major comments:
- Why is some data not shown? For example, the VLF data is used to justify the extend and occurrence of the EEP event, but is not shown in the paper. Similarly, the POES data is only presented with a daily resolution. Both datasets are used to explain that the event lasted for a few hours and motivate the model simulations. This is even explicitly mentioned in the discussion so it seems important that you present more of these observations.
- With predicted ozone loss at 90% level, I was left wondering why are you not using MLS and MIPAS ozone observations to check for ozone impacts as predicted by the model simulations, as you already use other measurements from both instruments.
- It is not clear what the reason for using two separate models is. Why do you need to use the HAMMONIA model? The event is short-lived, and any model results are only presented for a period of four days. Why not use only the ExoTIC ion chemistry model so that the particle impact can be simulated as accurately as possible? This would also mean not needing to account for horizontal transport effects. The balloon measurements are from one point so most accurate ionisation rates are for one location only. Presently only the NOy partitioning from the ion chemistry model are shown. Could you show the density/VMR results from the ExoTIC ion chemistry model?
- The HAMMONIA model results in Figure 5 are presented in a format that is difficult to assess (spatial extreme statistics). If the impact is limited to within the polar vortex you could use a vortex average, or present the results as maps for example. Also, since you have observations to contrast the model results directly to, I suggest presenting the results in a way that allows the reader to make those comparisons.
- For the ionisation rates, balloon rates and AIMOS rates are used. AIMOS uses POES observations and you show that POES measured enhanced EEP on the 14 December, as also observed by the balloon. What is not clear presently is how this does not lead to “double counting” EEP ionisation in the simulations where AIMOS + balloon rates are used. This need to be clarified. Can you include an example of representative AIMOS ionisation rated in Figure 4a) along with the balloon rates for comparison?
Further comments:
- Level of radiation belt information and referencing. For example in the Introduction, line 18: I would not expect most ACP readers to know about adiabatic invariants in the radiation belts. There are no references to help the reader, but, actually, this is not even needed to understand the study (from the atmospheric point of view, the precipitation side is a different story!). Similar situation happens again in the first paragraph of section 5, where you have a lot of detailed information about radiation belt processes that are not really needed in the context. For example, discussing inward radial diffusion does not seem necessary for the results presented in the manuscript, which are focused on the atmospheric impact. I suggest the authors look at these sections critically and revise the text so that it best supports the understanding needed for this work. Whether this is to dial the radiation belt side down, or provide much more context (in which case please include more references) I think is up to the authors.
- Since you show data from both, you need explain what the difference and significance between the two POES telescopes (0° and 90°) is.
- With the instrumentation relying on X-ray absorption, did you check for any changes in solar X-ray flux during the time of investigation?
- You state that the Apatity balloon didn’t observe EEP 5h before the Moscow balloon, but at some point in the three overpasses over Apatity POES (0° telescope) did. Moscow balloon observed EEP, but POES 0° telescope did not, however, POES 90° telescope did. You should explain in the text what the significance of these is. It is not clear at present why the Apatity observations are included, or why the 0° and 90° telescopes provide such different results. The Apatity observations do not seem to be discussed any further in the manuscript.
- Section 3.1. Can you provide some context for the observed Dst and AE values representing moderate levels of geomagnetic activity? These seem rather low values to me. You should also include a reference for southward IMF being needed to enable electron precipitation.
- Section 3.2 the first paragraph should be moved/merged in the introduction section.
- What do you mean in section 3.2 about HNO3 controlling stratospheric ozone depletion? Do you mean as a reservoir for NOx, in PSCs, or its role in denitrification? It would be good to explain this already in the introduction as you go on to present both observations and simulation of HNO3. Please include references. As you mention its importance for stratosphere, could you elaborate on the potential contribution of mesospheric HNO3 (since these are presented) to stratospheric HNO3?
- In the context of fast horizontal transport, rather than try to see a localised impact, why not utilise observations of tracers and/or include illustration of the edge of the polar vortex? I understand this could be possible from MIPAS observations.
- For the averaged MIPAS and MLS observations at latitudes 10-55 geomagnetic, geographically this includes the equatorial region. This seems concerning, why include geomagnetic latitudes as low as 10°?
- Section 3.2, line 157. Substorm activity has not been mentioned before this. Some further explanation is necessary.
- line 164. What do you mean here by fast horizontal transport? Do you mean that the polar night jet extends to these low latitudes (what about horizontal mixing within the vortex)? If we assume a 70 m/s zonal wind speed, and take a simple zonally symmetric vortex, at latitudes of 40°-50° it would take 4-5 days to circle the Earth. I don’t quite see how the hotspot would have move such a large distance within the same day, even if the vortex is likely not zonally symmetric. Perhaps this just need a little bit more clarification. If anything, the MIPAS maps seem to suggest to me that there could have been a precipitation hotspot over the North-America/North-Atlantic sector on 14th Dec (more analysis would be needed to show this of course)!
- Figure 3 caption: What is the rhombi mark? Diamond?
- Are the models forced with ionisation for 6h or 8h? There seem to be conflicting numbers in the manuscript. On this topic: the balloon was only up for a very short period of time: 13:26-13:45 UT. How does this justify 6h/8h of forcing? POES observations supporting the use of 6h/8h are not presented.
- Is constant ionisation used for the whole 6h/8h? If yes, you should provide some justification for this.
- Relating to one of the major comments: Why use different ionisation rates in the HAMMONIA model? How much do these differ from the balloon ionisation rates? From reading section 4.3, it really seems like there could be double counting of EEP, with AIMOS representing medium energy electron precipitation using POES and adding on the balloon ionisation rates (also representing medium energy electron precipitation!).
- I find Figure 5 confusing: These are simply NH maximum of minimum values, without any regional restriction. The contour labels are too small (one can not see the powers clearly).
- Figure 5 and section 4.3: There doesn’t seem to be clear evidence for residual circulation in these figures. The timescale of 4 days is not really enough to see vertical transport clearly. I suggest carefully revising the text regarding residual circulation or showing more supporting evidence.
- Line 238: You are not presenting model simulations over Moscow, so you do not show ozone loss over Moscow during the event. Consider the use of the extreme statistics not tied to a specific location, or revise here.
- Section 5: "Both POES and VLF data on 14 December, as well as NOx and HNO3 observations throughout December, suggest that events indeed lasted for a few hours…” It seems critical that you present the POES and VLF observations in high enough a temporal resolution to support this statement.
- “Complete destruction of ozone in the upper mesosphere over the region where high-energy electron precipitation occurred is also shown by HAMMONIA numerical experiments.” Statement like this is conflicting when you present the results not tied to a location. I can see why you many want to present the maximum impact possible (in which case the ExoTIC model may have been sufficient, rather than HAMMONIA). On the other hand as you state, horizontal transport is relative rapid and these effects may be mixed in quickly and in this context also zonal averaged may be justified. I strongly recommend you consider presenting the HAMMONIA results in a different format (perhaps a time series of horizontal maps with a selected time resolution). I would also very much like to see the ExoTIC model results.
- Conclusions “This conclusion inspires further studies involving a wider network of the balloon-based instruments.” I think for a commend such as this, it is important to show how different the balloon ionisation rate is to the AIMOS ionisation rates.
- Please pay attention to the varied used of “middle latitudes” and “midlatitudes”. It is confusing, I suggest using just “midlatitudes”.
Irina Mironova et al.
Irina Mironova et al.
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 360 | 70 | 7 | 437 | 4 | 2 |
- HTML: 360
- PDF: 70
- XML: 7
- Total: 437
- BibTeX: 4
- EndNote: 2
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1