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  • Journal article
    Woolley T, Matteini L, Horbury TS, Laker R, Woodham LD, Bale SD, Stawarz JE, Beri L, McManus MD, Badman STet al., 2021,

    <jats:p>&amp;lt;p&amp;gt;The slow solar wind is thought to consist of a component originating close to the Heliospheric Current Sheet (HCS) in the streamer belt and a component from over-expanded coronal hole boundaries. In order to understand the roles of these contributions with different origin, it is important to separate and characterise them. By exploiting the fact that Parker Solar Probe&amp;amp;#8217;s fourth and fifth orbits were the same and the solar conditions were similar, we identify intervals of slow polar coronal hole wind sampled at approximately the same heliocentric distance and latitude. Here, solar wind properties are compared, highlighting typical conditions of the slow coronal hole wind closer to the Sun than ever before. We explore different properties of the plasma, including composition, spectra and microphysics, and discuss possible origins for the features that are observed.&amp;lt;/p&amp;gt;</jats:p>

  • Journal article
    Good S, Kilpua E, Ala-Lahti M, Osmane A, Bale S, Zhao Let al., 2021,

    <jats:p>&amp;lt;p&amp;gt;Magnetic clouds are large-scale transient structures in the solar wind with low plasma &amp;lt;em&amp;gt;&amp;amp;#946;&amp;lt;/em&amp;gt;, low-amplitude magnetic field fluctuations, and twisted field lines with both ends often connected to the Sun. We analyse the normalised cross helicity, &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt;, and residual energy, &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;r&amp;lt;/sub&amp;gt;, in magnetic clouds observed by Parker Solar Probe (PSP). In the November 2018 cloud observed at 0.25 au, a low value of &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt; was present in the cloud core, indicating that wave power parallel and anti-parallel to the mean field was approximately balanced, while the cloud&amp;amp;#8217;s outer layers displayed larger amplitude Alfv&amp;amp;#233;nic fluctuations with high &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt; values and &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;r&amp;lt;/sub&amp;gt; ~ 0. These properties are compared and contrasted to those found in clouds observed by PSP at larger heliocentric distances. We suggest that low &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt; is likely a common feature of magnetic clouds given their typically closed field structure, in contrast to the generally higher &amp;lt;em&amp;gt;&amp;amp;#963;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;c&amp;lt;/sub&amp;gt; found on the open field lines of the solar wind.&amp;lt;/p&amp

  • Conference paper
    Thomas C, Voulgarakis A, Lim G, Haigh J, Nowack Pet al., 2021,

    <jats:p>&amp;lt;p&amp;gt;Atmospheric blocking events are mid-latitude weather patterns, which obstruct the usual path of the polar jet stream. Several blocking indices (BIs) have been developed to study blocking patterns and their associated trends, but these show significant seasonal and regional differences. Despite being central features of mid-latitude synoptic-scale weather, there is no well-defined historical dataset of blocking events. Here, we introduce a new blocking index using self-organizing maps (SOMs), an unsupervised machine learning approach, and compare its detection skill to some of the most widely applied BIs. To enable this intercomparison, we first create a new ground truth time series classification of European blocking based on expert judgement. We then demonstrate that our method (SOM-BI) has several key advantages over previous BIs because it exploits all the spatial information provided in the input data and avoids the need for arbitrary thresholds. Using ERA5 reanalysis data (1979-2019), we find that the SOM-BI identifies blocking events with a higher precision and recall than other BIs. We present a case study of the 2003 European heat wave and highlight that well-defined groups of SOM nodes can be an effective tool to reliably and accurately diagnose such weather events. This contrasts with the way SOMs are commonly used, where an individual SOM node can be wrongly assumed to represent a weather pattern. We also evaluate the SOM-BI performance on about 100 years of climate model data from a preindustrial simulation with the new UK Earth System Model (UK-ESM1). For the model data, all blocking detection methods have lower skill than for the ERA5 reanalysis, but SOM-BI performs significantly better than the conventional indices. This shows that our method can be effectively applied to climate models to develop our understanding of how climate change will affect regional blocking characteristics. Overall, our results demonstra

  • Journal article
    Chen C, Chandran B, Woodham L, Jones S, Perez J, Bourouaine S, Bowen T, Klein K, Moncuquet M, Kasper J, Bale Set al., 2021,

    <jats:p>&amp;lt;p&amp;gt;The fourth orbit of Parker Solar Probe (PSP) reached heliocentric distances down to 27.9 Rs, allowing solar wind turbulence and acceleration mechanisms to be studied in situ closer to the Sun than previously possible. The turbulence properties were found to be significantly different in the inbound and outbound portions of PSP's fourth solar encounter, likely due to the proximity to the heliospheric current sheet (HCS) in the outbound period. Near the HCS, in the streamer belt wind, the turbulence was found to have lower amplitudes, higher magnetic compressibility, a steeper magnetic field spectrum (with spectral index close to -5/3 rather than -3/2), a lower Alfvenicity, and a &amp;quot;1/f&amp;quot; break at much lower frequencies. These are also features of slow wind at 1 au, suggesting the near-Sun streamer belt wind to be the prototypical slow solar wind. The transition in properties occurs at a predicted angular distance of ~4 degrees from the HCS, suggesting ~8 degrees as the full-width of the streamer belt wind at these distances. While the majority of the Alfvenic turbulence energy fluxes measured by PSP are consistent with those required for reflection-driven turbulence models of solar wind acceleration, the fluxes in the streamer belt are significantly lower than the model predictions, suggesting that additional mechanisms are necessary to explain the acceleration of the streamer belt solar wind.&amp;lt;/p&amp;gt;</jats:p>

  • Journal article
    Schwartz SJ, Ergun RE, Harald K, Wilson LB, Chen L-J, Goodrich KA, Turner DL, Gingell I, Madanian H, Gershman DJ, Strangeway RJet al., 2021,

    <jats:p>Shock waves are common in the heliosphere and beyond. The collisionlessnature of most astrophysical plasmas allows for the energy processed byshocks to be partitioned amongst particle sub-populations andelectromagnetic fields via physical mechanisms that are not wellunderstood. The electrostatic potential across such shocks is framedependent. In a frame where the incident bulk velocity is parallel tothe magnetic field, the deHoffmann-Teller frame, the potential is linkeddirectly to the ambipolar electric field established by the electronpressure gradient. Thus measuring and understanding this potentialsolves the electron partition problem, and gives insight into othercompeting shock processes. Integrating measured electric fields is spaceis problematic since the measurements can have offsets that change withplasma conditions. The offsets, once integrated, can be as large orlarger than the shock potential. Here we exploit the high-quality fieldand plasma measurements from NASA's Magnetospheric Multiscale mission toattempt this calculation. We investigate recent adaptations of thedeHoffmann-Teller frame transformation to include time variability, andconclude that in practise these face difficulties inherent in the 3Dtime-dependent nature of real shocks by comparison to 1D simulations.Potential estimates based on electron fluid and kinetic analyses providethe most robust measures of the deHoffmann-Teller potential, but withsome care direct integration of the electric fields can be made toagree. These results suggest that it will be difficult to independentlyassess the role of other processes, such as scattering by shockturbulence, in accounting for the electron heating.</jats:p>

  • Journal article
    Voigt A, Albern N, Ceppi P, Grise K, Li Y, Medeiros Bet al., 2021,

    , Wiley Interdisciplinary Reviews: WIREs Climate Change, Vol: 12, Pages: 1-22, ISSN: 1757-7780

    By interacting with radiation, clouds modulate the flow of energy through the Earth system, the circulation of the atmosphere, and regional climate. We review the impact of cloudradiation interactions for the atmospheric circulation in the presentday climate, its internal variability and its response to climate change. After summarizing cloudcontrolling factors and cloudradiative effects, we clarify the scope and limits of the Clouds OnOff Klimate Model Intercomparison Experiment (COOKIE) and cloudlocking modeling methods. COOKIE showed that the presence of cloudradiative effects shapes the circulation in the presentday climate in many important ways, including the width of the tropical rain belts and the position of the extratropical storm tracks. Cloud locking, in contrast, identified how clouds affect internal variability and the circulation response to global warming. This includes strong, but modeldependent, shortwave and longwave cloud impacts on the ElNino Southern Oscillation, and the finding that most of the poleward circulation expansion in response to global warming can be attributed to radiative changes in clouds. We highlight the circulation impact of shortwave changes from lowlevel clouds and longwave changes from rising highlevel clouds, and the contribution of these cloud changes to model differences in the circulation response to global warming. The review in particular draws attention to the role of cloudradiative heating within the atmosphere. We close by raising some open questions which, among others, concern the need for studying the cloud impact on regional scales and opportunities created by the next generation of global stormresolving models.

  • Journal article
    Provan G, Bradley TJ, Bunce EJ, Cowley SWH, Cao H, Dougherty M, Hunt GJ, Roussos E, Staniland NR, Tao Cet al., 2021,

    , JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 126, ISSN: 2169-9380
  • Journal article
    Morimoto S, Goto D, Murayama S, Fujita R, Tohjima Y, Ishidoya S, Machida T, Inai Y, Patra PK, Maksyutov S, Ito A, Aoki Set al., 2021,

    , POLAR SCIENCE, Vol: 27, ISSN: 1873-9652
  • Journal article
    Xu S, Schwartz SJ, Mitchell DL, Horaites K, Andersson L, Halekas J, Mazelle C, Gruesbeck JRet al., 2021,

    , JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 126, ISSN: 2169-9380
  • Journal article
    He J, Cui B, Yang L, Hou C, Zhang L, Ip W-H, Jia Y-D, Dong C, Duan D, Zong Q, Bale SD, Pulupa M, Bonnell JW, Dudok De Wit T, Goetz K, Harvey PR, MacDowall RJ, Malaspina DMet al., 2021,

    , ASTROPHYSICAL JOURNAL, Vol: 910, ISSN: 0004-637X
  • Journal article
    Wang L, Zong Q, Shi Q, Wimmer-Schweingruber RF, Bale SDet al., 2021,

    , ASTROPHYSICAL JOURNAL, Vol: 910, ISSN: 0004-637X
  • Journal article
    Klein KG, Verniero JL, Alterman B, Bale S, Case A, Kasper JC, Korreck K, Larson D, Lichko E, Livi R, McManus M, Martinovic M, Rahmati A, Stevens M, Whittlesey Pet al., 2021,

    , ASTROPHYSICAL JOURNAL, Vol: 909, ISSN: 0004-637X
  • Journal article
    Huang SY, Sahraoui F, Andres N, Hadid LZ, Yuan ZG, He JS, Zhao JS, Galtier S, Zhang J, Deng XH, Jiang K, Yu L, Xu SB, Xiong QY, Wei YY, Dudok de Wit T, Bale SD, Kasper JCet al., 2021,

    , ASTROPHYSICAL JOURNAL LETTERS, Vol: 909, ISSN: 2041-8205
  • Journal article
    Schwartz SJ, Kucharek H, Farrugia CJ, Trattner K, Gingell I, Ergun RE, Strangeway R, Gershman Det al., 2021,

    , GEOPHYSICAL RESEARCH LETTERS, Vol: 48, ISSN: 0094-8276
  • Journal article
    Archer MO, Day N, Barnes S, 2021,

    , Geoscience Communication, Vol: 4, Pages: 57-67, ISSN: 2569-7110

    Impact evaluation in public engagement necessarily requires measuring change. However, this is extremely challenging for drop-in activities due to their very nature. We present a novel method of impact evaluation which integrates graffiti walls into the experience both before and after the main drop-in activity. The activity in question was a soundscape exhibit, where young families experienced the usually inaudible sounds of near-Earth space in an immersive and accessible way. We apply two analysis techniques to the captured before and after data – quantitative linguistics and thematic analysis. These analyses reveal significant changes in participants' responses after the activity compared to before, namely an increased diversity in language used to describe space and altered conceptions of what space is like. The results demonstrate that the soundscape was surprisingly effective at innately communicating key aspects of the underlying science simply through the act of listening. The impacts also highlight the power of sonification in stimulating public engagement, which, through reflection, can lead to altered associations, perceptions, and understanding. Therefore, we show that this novel approach to drop-in activity evaluation, using graffiti walls both before and after the activity and applying rigorous analysis to this data, has the power to capture change and, thus, have a short-term impact. We suggest that commonly used evaluation tools suitable for drop-in activities, such as graffiti walls, should be integrated both before and after the main activity in general, rather than only using them afterwards as is typically the case.

  • Journal article
    Heyns MJ, Lotz SI, Gaunt CT, 2021,

    , Space Weather, Vol: 19, ISSN: 1542-7390

    <jats:title>Abstract</jats:title> <jats:p> Geomagnetically induced currents (GICs) are driven by the geoelectric field induced by fluctuations of Earth's magnetic field. Drivers of intense GICs are often associated with large impulsive events such as coronal mass ejections. To a lesser extent fluctuations from regular oscillations of the geomagnetic field, or geomagnetic pulsations, have also been identified as possible drivers of GICs. In this work we show that these lowfrequency pulsations are directly observed in measured GIC data from power networks. Due to the lowpass nature of GICs, Pc5 and lowerfrequency pulsations drive significant GICs for an extended duration even at midlatitudes. Longerperiod Ps6type disturbances apparently not typical of midlatitudes are seen with GIC amplitudes comparable to the peak GIC at storm sudden commencement. The quasiac (alternating current) nature of the sustained pulsation driving affects the power system response and cannot be properly modeled using only direct current (dc) models. A further consideration is that the often used <jats:styled-content> <jats:italic>d</jats:italic> <jats:italic>B</jats:italic> / <jats:italic>d</jats:italic> <jats:italic>t</jats:italic> </jats:styled-content> GIC proxy is biased to the sampling rate of the geomagnetic field measurements used. The <jats:styled-content> <jats:italic>d</jats:italic> <jats:italic>B</jats:italic> / <jats:italic>d</jats:italic> <jats:italic>t</jats:italic> </jats:styled-content>

  • Journal article
    Archer M, DeWitt J, Davenport C, Keenan O, Coghill L, Christodoulou A, Durbin S, Campbell H, Hou Let al., 2021,

    , Research for All, Vol: 5, Pages: 67-85, ISSN: 2399-8121

    A major focus in the STEM public engagement sector concerns engaging withyoung people, typically through schools. The aims of these interventions areoften to positively affect students' aspirations towards continuing STEMeducation and ultimately into STEM-related careers. Most schools engagementactivities take the form of short one-off interventions that, while able toachieve positive outcomes, are limited in the extent to which they can havelasting impacts on aspirations. In this paper we discuss various differentemerging programmes of repeated interventions with young people, assessing whatimpacts can realistically be expected. Short series of interventions appearalso to suffer some limitations in the types of impacts achievable. However,deeper programmes that interact with both young people and those that influencethem over significant periods of time (months to years) seem to be moreeffective in influencing aspirations. We discuss how developing a Theory ofChange and considering young people's wider learning ecologies are required inenabling lasting impacts in a range of areas. Finally, we raise severalsector-wide challenges to implementing and evaluating these emergingapproaches.

  • Journal article
    Allen RC, Ho GC, Mason GM, Li G, Jian LK, Vines SK, Schwadron NA, Joyce CJ, Bale SD, Bonnell JW, Case AW, Christian ER, Cohen CMS, Desai M, Filwett R, Goetz K, Harvey PR, Hill ME, Kasper JC, Korreck KE, Lario D, Larson D, Livi R, MacDowall RJ, Malaspina DM, McComas DJ, McNutt R, Mitchell DG, Paulson KW, Pulupa M, Raouafi N, Stevens ML, Whittlesey PL, Wiedenbeck Met al., 2021,

    , GEOPHYSICAL RESEARCH LETTERS, Vol: 48, ISSN: 0094-8276
  • Journal article
    Liou K, Paranicas C, Vines S, Kollmann P, Allen R, Clark G, Mitchell D, Jackman C, Masters A, Achilleos N, Roussos E, Krupp Net al., 2021,

    , Journal of Geophysical Research: Space Physics, Vol: 126, ISSN: 2169-9380

    Energetic particles (>∼25 keV) have been observed routinely in the terrestrial magnetosheath, but have not been well studied at the magnetosheaths of the outer planets. Here we analyze energetic electrons and ions (mostly protons) in the vicinity (±1 RS) of Saturn's magnetopause, using particle data acquired with the lowenergy magnetosphere measurements system, one of the three sensors of the magnetosphere imaging instrument on board the Cassini spacecraft, during a period of ∼14 years (2004–2017). It is found that energetic particles, especially ions, are also common in Saturn's magnetosheath. A clear inward (toward Saturn) gradient in the electron differential flux is identified, suggestive of magnetospheric sources. Such an inward gradient does not appear in some of the ion channels. We conclude that Saturn's magnetopause acts as a porous barrier for energetic electrons and, to a lesser extent, for energetic ions. A dawndusk asymmetry in the gradient of particle flux across the magnetopause is also identified, with a gradual decrease at the dawn and a sharp decrease at the dusk magnetopause. It is also found that magnetic reconnection enhanced flux levels just outside of the magnetopause, with evidence suggesting that these particles are from magnetospheric sources. These findings strongly suggest that Saturn's magnetosphere is most likely the main source of energetic particles in Saturn's magnetosheath and magnetosphere leakage is an important process responsible for the presence of the energetic particles in Saturn's magnetosheath.

  • Journal article
    Zappa G, Ceppi P, Shepherd TG, 2021,

    , Nature Climate Change, Vol: 11, Pages: 106-108, ISSN: 1758-678X
  • Journal article
    Sparks N, Toumi R, 2021,

    , Atmospheric Science Letters, Vol: 22, Pages: 1-8, ISSN: 1530-261X

    To date it has proved difficult to make seasonal forecasts of tropical cyclones, particularly for landfall and in East China specifically. This study examines sources of predictability for the number of landfalling typhoons in East China on seasonal (June–October) and subseasonal time scales. East China landfall count is shown to be independent of basinscale properties of TC tracks, such the genesis location, duration, basin track direction and length, and basin total count. Largescale environmental climate indices which are potential basin scale drivers are also shown to be largely uncorrelated with landfall prior to and throughout the season. The most important factor is the steering in the final stages to landfall. The seasonal landfall is strongly anticorrelated with the more local zonal midtropospheric wind field over the East China sea (r = −.61, p < .001). It is proposed that geopotential height anomalies over Korea/Japan cause anomalous easterly winds in the East China Sea and enhance landfall rates by steering typhoons onto the coast. Early, peak, and late subseasonal landfall counts are shown to be independent of each other yet share this predictor. This local feature may be dynamically predictable allowing a potential hybrid dynamicalstatistical seasonal forecast of landfall.

  • Journal article
    Southwood DJ, Cao H, Shebanits O, Elsden T, Hunt GJ, Dougherty MKet al., 2021,

    , Journal of Geophysical Research: Space Physics, Vol: 126, Pages: 1-18, ISSN: 2169-9380

    Between April and September 2017 in the final stages of the Cassini Saturn Orbiter mission the spacecraft executed 22 orbits passing planetward of the innermost ring, the D-ring. During all periapsis passes oscillations were detected in the azimuthal magnetic field components on typical time scales of a few minutes. We argue that these time-varying magnetic signals detected on the spacecraft are also primarily time-varying in the plasma frame. Furthermore, we show that nearly all signals exhibit a spatial feature, namely a magnetic node near the effective field line equator. We propose that the oscillations are associated with Alfvén waves excited in local field line resonances, most likely driven from global sources.

  • Journal article
    Jannet G, de Wit TD, Krasnoselskikh V, Kretzschmar M, Fergeau P, Bergerard-Timofeeva M, Agrapart C, Brochot J-Y, Chalumeau G, Martin P, Revillet C, Bale SD, Maksimovic M, Bowen TA, Brysbaert C, Goetz K, Guilhem E, Harvey PR, Leray V, Lorfevre Eet al., 2021,

    , JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 126, ISSN: 2169-9380
  • Journal article
    Agiwal O, Cao H, Cowley SWH, Dougherty MK, Hunt GJ, Muller-Wodarg I, Achilleos Net al., 2021,

    , JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, Vol: 126, ISSN: 2169-9097
  • Journal article
    Madanian H, Desai M, Schwartz SJ, Wilson LB, Fuselier SA, Burch JL, Le Contel O, Turner DL, Ogasawara K, Brosius AL, Russell CT, Ergun RE, Ahmadi N, Gershman DJ, Lindqvist P-Aet al., 2021,

    , ASTROPHYSICAL JOURNAL, Vol: 908, ISSN: 0004-637X
  • Journal article
    Liggins FS, Pickering JC, Nave G, Kramida A, Gamrath S, Quinet Pet al., 2021,

    , ASTROPHYSICAL JOURNAL, Vol: 907, ISSN: 0004-637X
  • Journal article
    Shi C, Zhao J, Huang J, Wang T, Wu D, Chen Y, Hu Q, Kasper JC, Bale SDet al., 2021,

    , ASTROPHYSICAL JOURNAL LETTERS, Vol: 908, ISSN: 2041-8205
  • Journal article
    Lai T-K, Hendricks EA, Menelaou K, Yau MKet al., 2021,

    , JOURNAL OF THE ATMOSPHERIC SCIENCES, Vol: 78, Pages: 473-496, ISSN: 0022-4928
  • Journal article
    Chandler MO, Schwartz SJ, Avanov LA, Coffey VN, Giles BL, Moore TE, Pollock CJ, Burch JL, Russell CT, Torbert RBet al., 2021,

    , JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 126, ISSN: 2169-9380
  • Journal article
    Toumi R, Wang S, 2021,

    , Science, Vol: 371, Pages: 514-517, ISSN: 0036-8075

    Poleward migrations of tropical cyclones have been observed globally, but their impact on coastal areas remains unclear. We investigated the change in global tropical cyclone activity in coastal regions over the period 1982–2018. We found that the distance of tropical cyclone maximum intensity to land has decreased by about 30 kilometers per decade, and that the annual frequency of global tropical cyclones increases with proximity to land by about two additional cyclones per decade. Trend analysis reveals a robust migration of tropical cyclone activity toward coasts, concurrent with poleward migration of cyclone locations as well as a statistically significant westward shift. This zonal shift of tropical cyclone tracks may be mainly driven by global zonal changes in environmental steering flow.

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