REVIEW 4 major objections 5 minor 62 references
Evidence of potential thermospheric overcooling during the May 2024 geomagnetic superstorm
T0 review · 4 major / 5 minor · reviewed 2026-08-12 · deepseek-v4-flash
Pith's one-line read The May 2024 geomagnetic superstorm produced a rare post-storm thermospheric overcooling, with Swarm-C measuring a 23% density depletion on May 12 despite rising solar EUV, likely driven by record nitric-oxide infrared cooling.
desk verdict A real and well-documented density undershoot for the May 2024 superstorm, but the paper doesn't quantitatively close the case that NO radiative cooling caused it—Joule heating for this event is never computed. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The central mechanism is NO infrared radiative cooling: NO molecules, produced in abundance by auroral particle precipitation, are vibrationally excited by collisions with atomic oxygen and then emit $5.3\,\mu\mathrm{m}$ photons that escape to space, converting thermospheric thermal energy into radiation. The paper combines TIMED/SABER limb radiances in the $5.3\,\mu\mathrm{m}$ channel, integrated over 115--250 km to give NO infrared flux and then globally integrated to give daily radiative power, with Swarm accelerometer-derived mass densities normalized to a reference altitude via the NRLMSISE-00 model and referenced to pre-storm days (May 7, 8, or 9) to quantify the density undershoot.
What would settle it
A direct calculation or retrieval of Joule heating for May 10-12 using alternative magnetic-activity proxies (for example provisional AE, SuperMAG, or assimilated indices) that shows heating still above pre-storm levels on May 12 would undermine the overcooling attribution, as would a finding that NO cooling at the sampled local times and latitudes on May 12 was not actually elevated.
Extended reading notes
Core claim
The central claim is that the May 2024 superstorm produced a post-storm thermospheric density depletion of roughly $-23\%$ (Swarm-C, northern polar region, May 12) relative to the pre-storm day May 9, observable across Swarm-A, -B, and -C in the northern hemisphere but absent in the southern winter hemisphere. Because solar EUV flux kept increasing through the event, the expected density response was a rise, not a fall; the paper attributes the observed undershoot to NO $5.3\,\mu\mathrm{m}$ radiative cooling that remained 2--4 times above pre-storm levels through May 12, long after the storm's Joule heating had subsided. It also reports the largest NO infrared cooling flux on record, $11.84\ \mathrm{ergs\,cm^{-2}\,s^{-1}}$, slightly above the $11.74\ \mathrm{ergs\,cm^{-2}\,s^{-1}}$ peak of the 2003 Halloween storm, and a higher average NO radiative power (about $9.27\times10^{11}$ W) than in either phase of the Halloween storms.
Load-bearing premise
By May 12, the storm's heating sources—chiefly Joule heating and auroral particle precipitation—had returned to pre-storm levels, so the observed density undershoot can be attributed almost entirely to elevated NO infrared cooling; the paper did not directly calculate Joule heating for May 2024.
Editorial extensions
If this is right
- If correct, post-storm density forecasts for extreme geomagnetic storms must account for NO radiative cooling that persists 2--4 times above quiet levels for days, not just during the main phase.
- The May 2024 storm provides a second, well-observed case of thermospheric overcooling, strengthening the case that overcooling is a real phenomenon for storms of comparable strength and duration.
- The reported all-time-high NO cooling flux of $11.84\ \mathrm{ergs\,cm^{-2}\,s^{-1}}$ and daily radiative power exceeding 1 TW imply that NO cooling can dissipate more than a terawatt of storm energy in a single day.
- The hemispheric asymmetry—overcooling in the northern summer hemisphere but not the southern winter hemisphere—suggests that seasonal composition and dynamics modulate the net density response, a constraint for thermosphere-ionosphere circulation models.
- The recovery phase showed density returning to pre-storm levels by 2--4 UT on May 12 in northern polar regions while NO cooling stayed elevated, supporting a direct causal chain from persistent cooling to the density undershoot.
- These results imply that satellite drag models tuned to storm-time heating may systematically overestimate post-storm drag for severe storms, a practical concern for LEO operations.
Reading between the lines
- If the attribution holds, thermospheric density models used for satellite drag predictions should be checked for a systematic post-storm low bias after storms of Dst near $-412\ \mathrm{nT}$; overcooling could translate into roughly $23\%$ less drag in the northern hemisphere a day after storm peak.
- The paper did not compute Joule heating for May 2024 because definitive Dst and PCN indices were unavailable, so the claim that heating had returned to pre-storm levels by May 12 is inferred by analogy with Halloween 2003; a direct reconstruction using provisional indices or other magnetic-activity proxies would test whether the residual density deficit is truly all NO cooling.
- The SABER density enhancement at 105--110 km during the overcooling hints that the cooling may extend below the usual 115--250 km integration range, so a lower-altitude energy-budget analysis could refine the magnitude of of the overcooling.
- Comparing May 2024 with the Halloween storms suggests that peak NO cooling flux may scale more with storm duration or energy deposition geometry than with Dst magnitude alone, a relation that could be tested against other severe storms.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript reports an observational analysis of thermospheric neutral density (Swarm-A, -B, -C) and thermospheric NO infrared radiative flux (TIMED/SABER) during the May 2024 geomagnetic superstorm. The authors identify a post-storm density depletion in the northern polar region on May 12, reaching about -23% relative to May 9 in Swarm-C, despite rising solar EUV flux. They attribute this depletion to enhanced NO radiative cooling during the recovery phase, calling it a rare thermospheric overcooling event. The paper also reports an all-time high NO IRF of 11.84 ergs/cm2/s and compares the event with the Halloween 2003 storms.
Significance. If the attribution to NO radiative cooling is correct, this would be the first documented thermospheric overcooling event in solar cycle 25 and would strengthen the case that NO cooling plays a controlling role in the recovery of the thermosphere after extreme storms. The analysis uses publicly available, independent datasets, and the density depletion is internally consistent across Swarm-A and -C, which is a notable strength. The comparison with Halloween 2003 is useful for context. However, the central causal claim is not quantitatively supported because the paper does not compute Joule heating for May 2024, does not connect the NO cooling power on the depletion day to the observed density deficit, and provides no uncertainty estimates.
major comments (4)
- [3.4] The attribution of the May 12 density depletion to NO overcooling rests on the premise that Joule heating and particle precipitation had returned to prestorm levels by May 12. The paper itself states, 'The Joule heating rates were not calculated for the may 2024 geomagnetic superstorm because of the unavailability of definitive Dst-index and PCN-index.' Without a Joule heating estimate (or at least an upper bound) for 10-12 May, the density undershoot could equally reflect the normal recovery of thermospheric circulation and composition, or a temporary reduction in high-latitude energy input, rather than excess radiative cooling. The analogy to Halloween 2003, where Joule heating was computed and shown to decay, does not establish the premise for this event because storm morphology differs. Since 'overcooling' is fundamentally an energy-balance statement, this missing term is load-bearing for the central claim.
- [3.2-3.3] No quantitative link is made between the NO radiative cooling power and the magnitude of the observed density depletion. The daily NO radiated power of 12.35 x 10^11 W is quoted for May 11, while the density depletion is reported on May 12; for May 12 the text only states qualitatively that NO IRF remained 2-4 times prestorm. The authors should provide either a time-resolved energy budget (cooling power versus heating power over 10-12 May) or a scaling argument that relates the radiative energy loss to the density change. As written, the causal statement is unsupported by the data shown.
- [Abstract] The abstract claims that 'TIMED/SABER observed thermospheric density between 105 and 110 km altitude shows an enhancement during this thermospheric overcooling,' but this observation is not presented or analyzed anywhere in the main text, figures, or tables. If this SABER density measurement is intended as evidence for the overcooling mechanism, it must be added and discussed; otherwise, the claim should be removed from the abstract.
- [3.3] The reported depletion percentages (-23%, -22%, etc.) are given without uncertainties or significance testing. The density data are derived from accelerometer and precise orbit determination, which carry known errors, and the chosen reference day (May 7, 8, or 9) changes the depletion magnitude from about -9% to -23%. The authors should quantify the statistical significance of the depletion relative to natural variability (e.g., quiet-day density variation) to support the claim that this is a rare and notable event.
minor comments (5)
- [2] There is a typo in the data description: 'datasets ate utilized' should be 'datasets are utilized.' Also, 'Solar Heliospheric Observatory (SOHO) Solar EUV Monitor (SEM)' should likely be 'Solar and Heliospheric Observatory.'
- [3.1] The text states 'The high pressure solar wind of about 50 hPa' - the unit hPa is inconsistent with typical solar wind dynamic pressure values (nPa). Please correct the unit or the value, and ensure it matches Figure 1.
- [3.4] The sentence 'The Joule heating rates were not calculated for the may 2024 geomagnetic superstorm' contains a capitalization error ('may' should be 'May').
- [Abstract / 3.2] The claim of an 'all time high' NO radiative cooling flux of 11.84 ergs/cm2/s is compared only with the Halloween 2003 storms. Since SABER has been operating since 2002, the authors should verify this against the full SABER record or cite a study that does so, rather than relying on a single historical comparison.
- [Figure 1] In the Figure 1 caption, 'magneta' should be 'magenta.'
Circularity Check
Observational study with no circular derivation; the NO-overcooling attribution is an interpretive gap, not a circular step.
full rationale
No circularity is present. The paper compares independent public datasets: Swarm-A/B/C thermospheric densities from POD/accelerometer retrievals, TIMED/SABER NO infrared radiance and derived cooling fluxes, SOHO/SEM and TIMED/SEE solar EUV fluxes, and geomagnetic indices from OMNIWeb/ISGI. The -23% post-storm density depletion on May 12 is computed directly as a percentage difference relative to observed prestorm daily-mean densities, not from any fitted parameter or model inversion. The NO cooling values are likewise direct SABER retrievals and are not constructed from the density data. The paper never derives density from NO cooling or NO cooling from density, so there is no equation-level equivalence. The principal weakness is interpretive: attributing the undershoot to elevated NO radiative cooling requires that storm-time heating sources (Joule heating and particle precipitation) had returned to prestorm levels by May 12, yet the paper states in Section 3.4 that 'The Joule heating rates were not calculated for the May 2024 geomagnetic superstorm because of the unavailability of definitive Dst-index and PCN-index.' This is an evidentiary gap in the energy-balance argument, not a circular reduction. The comparison to Halloween 2003 and citations to prior work, including the authors' own papers, provide context and mechanism but are not load-bearing in the sense of defining the target result into existence. Accordingly, the circularity score is low: the central observations are self-contained and independently falsifiable, while the causal attribution rests on analogy rather than on circular logic.
Assumptions & free parameters
free parameters (2)
- Reference prestorm day for reported depletion =
May 9, 2024 (also May 7 and May 8 reported)
- Latitude and local-solar-time analysis window =
e.g., >45N and 07:00-09:00 LST for Swarm-A; analogous windows for Swarm-B/C
assumptions (5)
- domain assumption NRLMSISE-00 model density ratios provide a valid altitude normalization for Swarm densities across 7-13 May 2024.
- domain assumption TIMED/SABER 5.3 micron limb radiance and Abel inversion yield accurate NO volume emission rates, and integrating 115-250 km captures the thermospheric NO cooling flux.
- domain assumption SABER latitude coverage (53S to 83N) and 10-degree by 180-degree binning give a representative global daily NO radiative power.
- ad hoc to paper Joule heating and particle precipitation had subsided to prestorm levels by May 12, so the residual density deficit is attributable to NO cooling.
- domain assumption The EUV increase between May 9 and May 12 would have raised thermospheric density absent cooling, making the observed decrease a genuine overcooling signal.
Cite this review
Pith. "Pith review of Evidence of potential thermospheric overcooling during the May 2024 geomagnetic superstorm." pith.science (2026). https://pith.science/paper/R2RC3SIW
@misc{pith2026241114071,
author = {Pith},
title = {Pith review of: Evidence of potential thermospheric overcooling during the May 2024 geomagnetic superstorm},
year = {2026},
howpublished = {\url{https://pith.science/paper/R2RC3SIW}},
note = {Machine review of arXiv:2411.14071}
}
read the original abstract
During intense geomagnetic storms, the rapid and significant production of NO followed by its associated infrared radiative emission in lower thermosphere contributes crucially to the energetics of the upper atmosphere. This makes NO infrared radiative cooling a very important phenomenon which needs to be considered for accurate density forecasting in thermosphere. This study reports the investigation of variations in thermospheric density, and NO radiative cooling during the recent geomagnetic superstorm of May 2024. A very rare post-storm thermospheric density depletion of about -23% on May 12 was observed by Swarm-C in northern hemisphere in comparison to the prestorm condition on May 9. This overcooling was observed despite the continuous enhancement in solar EUV (24-36 nm) flux throughout the event. The thermospheric NO infrared radiative emission in the recovery phase of the storm seems to be the plausible cause for this observed post-storm density depletion. The TIMED/SABER observed thermospheric density between 105 and 110 km altitude shows an enhancement during this thermospheric overcooling. Our analysis also suggests an all time high thermospheric NO radiative cooling flux up to 11.84 ergs/cm2/sec during May 2024 geomagnetic superstorm, which has also been compared with famous Halloween storms of October 2003.
Figures
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Reference graph
Works this paper leans on
-
[1]
apacite url apacite =6pt Acknowledgments. 6pt 1sp \@dates Received \@recvdate\@empty\@rcvaccrule \@recvdate \@revisedate\@empty ; revised \@revisedate; \@accptdate\@empty \@revisedate\@empty; accepted \@accptdate \@pubdate\@empty. ; published \@pubdate. -2pt \@authaddrs @list\@empty =.15in @list 1sp @list =9pt plus 2pt minus 6pt \@sluginfo width 4pc =3000...
2001
-
[2]
\@ifstar \@figbox \@figbox \@figbox#1#2#3 to !#1! #3 [#1][c] !#2!#3 \@tempdima#2 \@tempdima by2 \@tempdima by- \@tempdima by- \@height\@tempdima\@depth\@tempdima\@width @ to @ #3 Bib ??? ??? ??? =0 =0 = @figure=0 @table=0 #1 --#1 -24pt -2ex #1 0= #1 to 0 #1 I NDEX T ERMS: #1 #1 Citation: #1 Feb 9, 2009 Changed name and references to name from agu2001 to a...
work page 2009
-
[3]
araki1994physical APACrefauthors Araki, T. APACrefauthors \ 1994 . A physical model of the geomagnetic sudden commencement A physical model of the geomagnetic sudden commencement . Geophysical Monograph-American Geophysical Union 81 183--183 . APACrefDOI doi:https://doi.org/10.1029/GM081p0183 APACrefDOI
-
[4]
bag2024thermospheric APACrefauthors Bag, T. , Kataoka, R. , Ogawa, Y. , Fujiwara, H. , Li, Z. , Singh, V. Tourgaidis, T. APACrefauthors \ 2024a . Thermospheric nitric oxide energy budget during extreme geomagnetic storms: a comparative study Thermospheric nitric oxide energy budget during extreme geomagnetic storms: a comparative study . Frontiers in Astr...
-
[5]
bag2024thermospherica APACrefauthors Bag, T. , Ogawa, Y. \ Sivakumar, V. APACrefauthors \ 2024b . Thermospheric NO Cooling During 2003 October “Halloween Storm”: Revisited Thermospheric no cooling during 2003 october “halloween storm”: Revisited . Journal of Geophysical Research: Space Physics 129 7 e2024JA032805 . APACrefDOI doi:https://doi.org/10.1029/2...
-
[6]
barth2009joule APACrefauthors Barth, C. , Lu, G. \ Roble, R. APACrefauthors \ 2009 . Joule heating and nitric oxide in the thermosphere Joule heating and nitric oxide in the thermosphere . Journal of Geophysical Research: Space Physics 114 A5 . APACrefDOI doi:https://doi.org/10.1029/2008JA013765 APACrefDOI
-
[7]
barth2003global APACrefauthors Barth, C. , Mankoff, K D. , Bailey, S. \ Solomon, S. APACrefauthors \ 2003 . Global observations of nitric oxide in the thermosphere Global observations of nitric oxide in the thermosphere . Journal of Geophysical Research: Space Physics 108 A1 . APACrefDOI doi:https://doi.org/10.1029/2002JA009458 APACrefDOI
-
[8]
bergeot2011impact APACrefauthors Bergeot, N. , Bruyninx, C. , Defraigne, P. , Pireaux, S. , Legrand, J. , Pottiaux, E. \ Baire, Q. APACrefauthors \ 2011 . Impact of the Halloween 2003 ionospheric storm on kinematic GPS positioning in Europe Impact of the halloween 2003 ionospheric storm on kinematic gps positioning in europe . GPS solutions 15 171--180 . ...
Show all 62 references
-
[9]
, Sunil Krishna, M
bharti2018storm APACrefauthors Bharti, G. , Sunil Krishna, M. , Bag, T. \ Jain, P. APACrefauthors \ 2018 . Storm time variation of radiative cooling by nitric oxide as observed by TIMED-SABER and GUVI Storm time variation of radiative cooling by nitric oxide as observed by tim...
2018 doi
-
[10]
\ Lei, J
chen2018numerical APACrefauthors Chen, X. \ Lei, J. APACrefauthors \ 2018 . A numerical study of the thermospheric overcooling during the recovery phases of the October 2003 storms A numerical study of the thermospheric overcooling during the recovery phases of the october 200...
2018 doi
-
[11]
, Codrescu, S M
codrescu2022storm APACrefauthors Codrescu, M V. , Codrescu, S M. \ Fedrizzi, M. APACrefauthors \ 2022 . Storm time neutral density assimilation in the thermosphere ionosphere with TIDA Storm time neutral density assimilation in the thermosphere ionosphere with tida . Journal o...
2022
-
[12]
\ Bruinsma, S
dudok2011determination APACrefauthors Dudok de Wit, T. \ Bruinsma, S. APACrefauthors \ 2011 . Determination of the most pertinent EUV proxy for use in thermosphere modeling Determination of the most pertinent euv proxy for use in thermosphere modeling . Geophysical research le...
2011 doi
-
[13]
, Dothe, H
duff2003rate APACrefauthors Duff, J. , Dothe, H. \ Sharma, R. APACrefauthors \ 2003 . On the rate coefficient of the N ( ^2 D)+ O _2 → NO+ O reaction in the terrestrial thermosphere On the rate coefficient of the n ( ^2 d)+ o _2 → no+ o reaction in the terrestrial thermosphere...
2003 doi
-
[14]
, Mlynczak, M G
esplin2023sounding APACrefauthors Esplin, R. , Mlynczak, M G. , Russell, J. , Gordley, L. \ Team, S. APACrefauthors \ 2023 . Sounding of the Atmosphere using Broadband Emission Radiometry (SABER): Instrument and science measurement description Sounding of the atmosphere using ...
2023 doi
-
[15]
, Gonzalez, R
forbes1996magnetic APACrefauthors Forbes, J. , Gonzalez, R. , Marcos, F. , Revelle, D. \ Parish, H. APACrefauthors \ 1996 . Magnetic storm response of lower thermosphere density Magnetic storm response of lower thermosphere density . Journal of Geophysical Research: Space Phys...
1996 doi
-
[16]
, Codrescu, M
fuller1994response APACrefauthors Fuller-Rowell, T. , Codrescu, M. , Moffett, R. \ Quegan, S. APACrefauthors \ 1994 . Response of the thermosphere and ionosphere to geomagnetic storms Response of the thermosphere and ionosphere to geomagnetic storms . Journal of Geophysical Re...
1994 doi
-
[17]
, Joselyn, J A
gonzalez1994geomagnetic APACrefauthors Gonzalez, W. , Joselyn, J A. , Kamide, Y. , Kroehl, H W. , Rostoker, G. , Tsurutani, B. \ Vasyliunas, V. APACrefauthors \ 1994 . What is a geomagnetic storm? What is a geomagnetic storm? Journal of Geophysical Research: Space Physics 99 A...
1994 doi
-
[18]
, Castle, K J
hwang2003vibrational APACrefauthors Hwang, E S. , Castle, K J. \ Dodd, J A. APACrefauthors \ 2003 . Vibrational relaxation of NO (v= 1) by oxygen atoms between 295 and 825 K Vibrational relaxation of no (v= 1) by oxygen atoms between 295 and 825 k . Journal of Geophysical Rese...
2003 doi
-
[19]
, Daras, I
iorfida2023swarm APACrefauthors Iorfida, E. , Daras, I. , Haagmans, R. \ Str mme, A. APACrefauthors \ 2023 . Swarm A and C accelerometers: Data validation and scientific interpretation Swarm a and c accelerometers: Data validation and scientific interpretation . Earth and Spac...
2023 doi
-
[20]
, Kilcommons, L
knipp2013thermospheric APACrefauthors Knipp, D. , Kilcommons, L. , Hunt, L. , Mlynczak, M. , Pilipenko, V. , Bowman, B. Drake, K. APACrefauthors \ 2013 . Thermospheric damping response to sheath-enhanced geospace storms Thermospheric damping response to sheath-enhanced geospac...
2013 doi
-
[21]
, Tobiska, W K
knipp2004direct APACrefauthors Knipp, D. , Tobiska, W K. \ Emery, B. APACrefauthors \ 2004 . Direct and indirect thermospheric heating sources for solar cycles 21-23 Direct and indirect thermospheric heating sources for solar cycles 21-23 . Solar Physics 224 495-505 . APACrefD...
2004 doi
-
[22]
APACrefauthors \ 1980
kockarts1980nitric APACrefauthors Kockarts, G. APACrefauthors \ 1980 . Nitric oxide cooling in the terrestrial thermosphere Nitric oxide cooling in the terrestrial thermosphere . Geophysical Research Letters 7 2 137--140 . APACrefDOI doi:https://doi.org/10.1029/GL007i002p00137...
1980 doi
-
[23]
, Krishna, M S
kumar2024influence APACrefauthors Kumar, A. , Krishna, M S. , Ranjan, A K. , Bender, S. , Sinnhuber, M. \ Sarkhel, S. APACrefauthors \ 2024 . Influence of temperature changes and vertically transported trace species on the structure of MLT region during major SSW events Influe...
2024
-
[24]
, Burns, A G
lei2012overcooling APACrefauthors Lei, J. , Burns, A G. , Thayer, J P. , Wang, W. , Mlynczak, M G. , Hunt, L A. Sutton, E. APACrefauthors \ 2012 . Overcooling in the upper thermosphere during the recovery phase of the 2003 October storms Overcooling in the upper thermosphere d...
2012 doi
-
[25]
, Thayer, J P
lei2010wind APACrefauthors Lei, J. , Thayer, J P. , Burns, A G. , Lu, G. \ Deng, Y. APACrefauthors \ 2010 . Wind and temperature effects on thermosphere mass density response to the November 2004 geomagnetic storm Wind and temperature effects on thermosphere mass density respo...
2010 doi
-
[26]
, Thayer, J P
lei2011rapid APACrefauthors Lei, J. , Thayer, J P. , Lu, G. , Burns, A G. , Wang, W. , Sutton, E K. \ Emery, B A. APACrefauthors \ 2011 . Rapid recovery of thermosphere density during the October 2003 geomagnetic storms Rapid recovery of thermosphere density during the october...
2011 doi
-
[27]
, Knipp, D
li2019understanding APACrefauthors Li, Z. , Knipp, D. \ Wang, W. APACrefauthors \ 2019 . Understanding the behaviors of thermospheric nitric oxide cooling during the 15 May 2005 geomagnetic storm Understanding the behaviors of thermospheric nitric oxide cooling during the 15 m...
2019 doi
-
[28]
, Mlynczak, M
lu2010relationship APACrefauthors Lu, G. , Mlynczak, M. , Hunt, L. , Woods, T. \ Roble, R. APACrefauthors \ 2010 . On the relationship of Joule heating and nitric oxide radiative cooling in the thermosphere On the relationship of joule heating and nitric oxide radiative coolin...
2010 doi
-
[29]
, Fuller-Rowell, T
maeda1992heat APACrefauthors Maeda, S. , Fuller-Rowell, T. \ Evans, D. APACrefauthors \ 1992 . Heat budget of the thermosphere and temperature variations during the recovery phase of a geomagnetic storm Heat budget of the thermosphere and temperature variations during the reco...
1992 doi
-
[30]
Halloween Storms
mannucci2005dayside APACrefauthors Mannucci, A. , Tsurutani, B. , Iijima, B. , Komjathy, A. , Saito, A. , Gonzalez, W. Skoug, R. APACrefauthors \ 2005 . Dayside global ionospheric response to the major interplanetary events of October 29--30, 2003 “Halloween Storms” Dayside gl...
2005 doi
-
[31]
, Harris, I
mayr1978some APACrefauthors Mayr, H. , Harris, I. \ Spencer, N. APACrefauthors \ 1978 . Some properties of upper atmosphere dynamics Some properties of upper atmosphere dynamics . Reviews of Geophysics 16 4 539--565 . APACrefDOI doi:https://doi.org/10.1029/RG016i004p00539 APACrefDOI
1978 doi
-
[32]
APACrefauthors \ 1997
mlynczak1997energetics APACrefauthors Mlynczak, M G. APACrefauthors \ 1997 . Energetics of the mesosphere and lower thermosphere and the SABER experiment Energetics of the mesosphere and lower thermosphere and the saber experiment . Advances in Space Research 20 6 1177--1183 ....
1997 doi
-
[33]
, Hunt, L A
mlynczak2021spectroscopy APACrefauthors Mlynczak, M G. , Hunt, L A. , Lopez-Puertas, M. , Funke, B. , Emmert, J. , Solomon, S. Mertens, C. APACrefauthors \ 2021 . Spectroscopy, gas kinetics, and opacity of thermospheric nitric oxide and implications for analysis of SABER infra...
2021
-
[34]
, Hunt, L A
mlynczak2024global APACrefauthors Mlynczak, M G. , Hunt, L A. , Nowak, N. , Marshall, B T. \ Mertens, C J. APACrefauthors \ 2024 . Global thermospheric infrared response to the Mother's day weekend extreme storm of 2024 Global thermospheric infrared response to the mother's da...
2024 doi
-
[35]
, Hunt, L A
mlynczak2010observations APACrefauthors Mlynczak, M G. , Hunt, L A. , Thomas Marshall, B. , Martin-Torres, F J. , Mertens, C J. , Russell III, J M. others APACrefauthors \ 2010 . Observations of infrared radiative cooling in the thermosphere on daily to multiyear timescales fr...
2010
-
[36]
, Martin-Torres, F J
mlynczak2005energy APACrefauthors Mlynczak, M G. , Martin-Torres, F J. , Crowley, G. , Kratz, D P. , Funke, B. , Lu, G. others APACrefauthors \ 2005 . Energy transport in the thermosphere during the solar storms of April 2002 Energy transport in the thermosphere during the sol...
2005 doi
-
[37]
, Martin-Torres, F J
mlynczak2003natural APACrefauthors Mlynczak, M G. , Martin-Torres, F J. , Russell, J. , Beaumont, K. , Jacobson, S. , Kozyra, J. others APACrefauthors \ 2003 . The natural thermostat of nitric oxide emission at 5.3 m in the thermosphere observed during the solar storms of Apri...
2003 doi
-
[38]
, Oberheide, J
nischal2019solar APACrefauthors Nischal, N. , Oberheide, J. , Mlynczak, M. , Marsh, D. \ Gan, Q. APACrefauthors \ 2019 . Solar Cycle Variability of Nonmigrating Tides in the 5.3 and 15 m Infrared Cooling of the Thermosphere (100--150 km) from SABER Solar cycle variability of n...
2019 doi
-
[39]
, Mlynczak, M
oberheide2013impact APACrefauthors Oberheide, J. , Mlynczak, M. , Mosso, C. , Schroeder, B. , Funke, B. \ Maute, A. APACrefauthors \ 2013 . Impact of tropospheric tides on the nitric oxide 5.3 m infrared cooling of the low-latitude thermosphere during solar minimum conditions ...
2013
-
[40]
\ Zesta, E
oliveira2019satellite APACrefauthors Oliveira, D M. \ Zesta, E. APACrefauthors \ 2019 . Satellite orbital drag during magnetic storms Satellite orbital drag during magnetic storms . Space Weather 17 11 1510--1533 . APACrefDOI doi:https://doi.org/10.1029/2019SW002287 APACrefDOI
2019 doi
-
[41]
APACrefauthors \ 2016
pedatella2016impact APACrefauthors Pedatella, N M. APACrefauthors \ 2016 . Impact of the lower atmosphere on the ionosphere response to a geomagnetic superstorm Impact of the lower atmosphere on the ionosphere response to a geomagnetic superstorm . Geophysical Research Letters...
2016 doi
-
[42]
, Hedin, A
picone2002nrlmsise APACrefauthors Picone, J. , Hedin, A. , Drob, D P. \ Aikin, A. APACrefauthors \ 2002 . NRLMSISE-00 empirical model of the atmosphere: Statistical comparisons and scientific issues Nrlmsise-00 empirical model of the atmosphere: Statistical comparisons and sci...
2002 doi
-
[43]
APACrefauthors \ 1980
prolss1980magnetic APACrefauthors Pr \"o lss, G. APACrefauthors \ 1980 . Magnetic storm associated perturbations of the upper atmosphere: Recent results obtained by satellite-borne gas analyzers Magnetic storm associated perturbations of the upper atmosphere: Recent results ob...
1980 doi
-
[44]
APACrefauthors \ 2011
prolss2011density APACrefauthors Pr \"o lss, G W. APACrefauthors \ 2011 . Density perturbations in the upper atmosphere caused by the dissipation of solar wind energy Density perturbations in the upper atmosphere caused by the dissipation of solar wind energy . Surveys in Geop...
2011 doi
-
[45]
, Krishna, M S
ranjan2023aspects APACrefauthors Ranjan, A K. , Krishna, M S. , Kumar, A. , Sarkhel, S. , Bharti, G. , Bender, S. \ Sinnhuber, M. APACrefauthors \ 2023a . Aspects related to variability of radiative cooling by NO in lower thermosphere, TEC and O/N2 correlation, and diffusion o...
-
[46]
, Sunil Krishna, M
ranjan2023no APACrefauthors Ranjan, A K. , Sunil Krishna, M. , Kumar, A. , Sarkhel, S. , Chakrabarty, D. \ Reeves, G. APACrefauthors \ 2023b . NO Radiative Cooling and Ionospheric Response to the HILDCAA Events Following Geomagnetic Storms No radiative cooling and ionospheric ...
-
[47]
richmond2000upper APACrefauthors Richmond, A. \ Lu, G. APACrefauthors \ 2000 . Upper-atmospheric effects of magnetic storms: a brief tutorial Upper-atmospheric effects of magnetic storms: a brief tutorial . Journal of Atmospheric and Solar-Terrestrial Physics 62 12 1115--1127 ...
2000 doi
-
[48]
APACrefauthors \ 2021
richmond2021joule APACrefauthors Richmond, A D. APACrefauthors \ 2021 . Joule heating in the thermosphere Joule heating in the thermosphere . Upper atmosphere dynamics and energetics 1--18 . APACrefDOI doi:https://doi.org/10.1002/9781119815631.ch1 APACrefDOI
2021 doi
-
[49]
, Ridley, E
roble1987global APACrefauthors Roble, R. , Ridley, E. \ Dickinson, R. APACrefauthors \ 1987 . On the global mean structure of the thermosphere On the global mean structure of the thermosphere . Journal of Geophysical Research: Space Physics 92 A8 8745--8758 . APACrefDOI doi:ht...
1987 doi
-
[50]
, Mlynczak, M G
russell1999overview APACrefauthors Russell III, J M. , Mlynczak, M G. , Gordley, L L. , Tansock Jr, J J. \ Esplin, R W. APACrefauthors \ 1999 . Overview of the SABER experiment and preliminary calibration results Overview of the saber experiment and preliminary calibration res...
1999 doi
-
[51]
, Borries, C
siemes2023new APACrefauthors Siemes, C. , Borries, C. , Bruinsma, S. , Fernandez-Gomez, I. , H adczuk, N. , den IJssel, J. Visser, P. APACrefauthors \ 2023 . New thermosphere neutral mass density and crosswind datasets from CHAMP, GRACE, and GRACE-FO New thermosphere neutral m...
2023
-
[52]
\ Bahr, K
simpson2020estimating APACrefauthors Simpson, F. \ Bahr, K. APACrefauthors \ 2020 . Estimating the electric field response to the Halloween 2003 and September 2017 magnetic storms across Scotland using observed geomagnetic fields, magnetotelluric impedances and perturbation te...
2020
-
[53]
, Picone, J
siskind2004middle APACrefauthors Siskind, D E. , Picone, J. , Stevens, M. \ Minschwaner, K. APACrefauthors \ 2004 . Middle and upper thermospheric odd nitrogen: 1. A new analysis of rocket data Middle and upper thermospheric odd nitrogen: 1. a new analysis of rocket data . Jou...
2004 doi
-
[54]
, Barth, C A
solomon1999auroral APACrefauthors Solomon, S C. , Barth, C A. \ Bailey, S M. APACrefauthors \ 1999 . Auroral production of nitric oxide measured by the SNOE satellite Auroral production of nitric oxide measured by the snoe satellite . Geophysical research letters 26 9 1259--12...
1999 doi
-
[55]
, Forbes, J
sutton2009rapid APACrefauthors Sutton, E. , Forbes, J. \ Knipp, D. APACrefauthors \ 2009 . Rapid response of the thermosphere to variations in Joule heating Rapid response of the thermosphere to variations in joule heating . Journal of Geophysical Research: Space Physics 114 A...
2009 doi
-
[56]
, Judge, D
tsurutani2005october APACrefauthors Tsurutani, B. , Judge, D. , Guarnieri, F. , Gangopadhyay, P. , Jones, A. , Nuttall, J. others APACrefauthors \ 2005 . The October 28, 2003 extreme EUV solar flare and resultant extreme ionospheric effects: Comparison to other Halloween event...
2005
-
[57]
, Doornbos, E
van2020thermosphere APACrefauthors van den IJssel, J. , Doornbos, E. , Iorfida, E. , March, G. , Siemes, C. \ Montenbruck, O. APACrefauthors \ 2020 . Thermosphere densities derived from Swarm GPS observations Thermosphere densities derived from swarm gps observations . Advance...
2020 doi
-
[58]
, Tsurutani, B
verkhoglyadova2011ionospheric APACrefauthors Verkhoglyadova, O. , Tsurutani, B. , Mannucci, A. , Mlynczak, M. , Hunt, L. , Komjathy, A. \ Runge, T. APACrefauthors \ 2011 . Ionospheric VTEC and thermospheric infrared emission dynamics during corotating interaction region and hi...
2011
-
[59]
, Doornbos, E
visser2013thermospheric APACrefauthors Visser, P. , Doornbos, E. , Van Den Ijssel, J. \ Teixeira da Encarna c \ a o, J. APACrefauthors \ 2013 . Thermospheric density and wind retrieval from Swarm observations Thermospheric density and wind retrieval from swarm observations . E...
2013 doi
-
[60]
\ Bruinsma, S
vourlidas2018euv APACrefauthors Vourlidas, A. \ Bruinsma, S. APACrefauthors \ 2018 . EUV irradiance inputs to thermospheric density models: Open issues and path forward Euv irradiance inputs to thermospheric density models: Open issues and path forward . Space Weather 16 1 5--...
2018 doi
-
[61]
, Paxton, L
zhang2014storm APACrefauthors Zhang, Y. , Paxton, L. , Morrison, D. , Marsh, D. \ Kil, H. APACrefauthors \ 2014 . Storm-time behaviors of O/N2 and NO variations Storm-time behaviors of o/n2 and no variations . Journal of Atmospheric and Solar-Terrestrial Physics 114 42--49 . A...
2014 doi
-
[62]
, Paxton, L J
zhang2019impact APACrefauthors Zhang, Y. , Paxton, L J. , Lu, G. \ Yee, S. APACrefauthors \ 2019 . Impact of nitric oxide, solar EUV and particle precipitation on thermospheric density decrease Impact of nitric oxide, solar euv and particle precipitation on thermospheric densi...
2019 doi
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