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Journal articleDavis N, Chandran BDG, Bowen TA, et al., 2023,
The Evolution of the 1/<i>f</i> Range within a Single Fast-solar-wind Stream between 17.4 and 45.7 Solar Radii
, ASTROPHYSICAL JOURNAL, Vol: 950, ISSN: 0004-637X -
Journal articlePerri S, Prete G, Zimbardo G, et al., 2023,
Interpretation of Flat Energy Spectra Upstream of Fast Interplanetary Shocks
, ASTROPHYSICAL JOURNAL, Vol: 950, ISSN: 0004-637X -
Journal articleBaker D, Demoulin P, Yardley SL, et al., 2023,
Observational Evidence of S-web Source of the Slow Solar Wind
, ASTROPHYSICAL JOURNAL, Vol: 950, ISSN: 0004-637X- Author Web Link
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- Citations: 1
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Journal articleHuang Z, Sioulas N, Shi C, et al., 2023,
New Observations of Solar Wind 1/<i>f</i> Turbulence Spectrum from Parker Solar Probe
, ASTROPHYSICAL JOURNAL LETTERS, Vol: 950, ISSN: 2041-8205- Author Web Link
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- Citations: 1
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Journal articleHall RJ, Mitchell DM, Seviour WJM, et al., 2023,
Surface hazards in North-west Europe following sudden stratospheric warming events
, ENVIRONMENTAL RESEARCH LETTERS, Vol: 18, ISSN: 1748-9326 -
Journal articleMalaspina DMM, Toma A, Szalay JRR, et al., 2023,
A Dust Detection Database for the Inner Heliosphere Using the Parker Solar Probe Spacecraft
, ASTROPHYSICAL JOURNAL SUPPLEMENT SERIES, Vol: 266, ISSN: 0067-0049 -
Journal articlede Moortel I, Eastwood J, Bridges J, et al., 2023,
Future UK solar system science
, Astronomy and Geophysics, Vol: 64, Pages: 3.34-3.38, ISSN: 0035-8738 -
Journal articleMozer F, Bale S, Kellogg P, et al., 2023,
Arguments for the physical nature of the triggered ion-acoustic waves observed on the Parker Solar Probe
, PHYSICS OF PLASMAS, Vol: 30, ISSN: 1070-664X -
Journal articleFargette N, Lavraud B, Rouillard AP, et al., 2023,
Clustering of magnetic reconnection exhausts in the solar wind: An automated detection study
, Astronomy and Astrophysics: a European journal, Vol: 674, Pages: 1-15, ISSN: 0004-6361Context. Magnetic reconnection is a fundamental process in astrophysical plasmas that enables the dissipation of magnetic energy at kinetic scales. Detecting this process in situ is therefore key to furthering our understanding of energy conversion in space plasmas. However, reconnection jets typically scale from seconds to minutes in situ, and as such, finding them in the decades of data provided by solar wind missions since the beginning of the space era is an onerous task.Aims. In this work, we present a new approach for automatically identifying reconnection exhausts in situ in the solar wind. We apply the algorithm to Solar Orbiter data obtained while the spacecraft was positioned at between 0.6 and 0.8 AU and perform a statistical study on the jets we detect.Methods. The method for automatic detection is inspired by the visual identification process and strongly relies on the Walén relation. It is enhanced through the use of Bayesian inference and physical considerations to detect reconnection jets with a consistent approach.Results. Applying the detection algorithm to one month of Solar Orbiter data near 0.7 AU, we find an occurrence rate of seven jets per day, which is significantly higher than in previous studies performed at 1 AU. We show that they tend to cluster in the solar wind and are less likely to occur in the tenuous solar wind (< 10 cm−3 near 0.7 AU). We discuss why the source and the degree of Alfvénicity of the solar wind might have an impact on magnetic reconnection occurrence.Conclusions. By providing a tool to quickly identify potential magnetic reconnection exhausts in situ, we pave the way for broader statistical studies on magnetic reconnection in diverse plasma environments.
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Journal articleConcepcion F, Clear CP, Ding M, et al., 2023,
The Laboratory Astrophysics Programme at Imperial College London
, EUROPEAN PHYSICAL JOURNAL D, Vol: 77, ISSN: 1434-6060 -
Journal articleStjern CW, Forster PM, Jia H, et al., 2023,
The Time Scales of Climate Responses to Carbon Dioxide and Aerosols
, JOURNAL OF CLIMATE, Vol: 36, Pages: 3537-3551, ISSN: 0894-8755- Author Web Link
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- Citations: 2
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Journal articleLiu M, Issautier K, Moncuquet M, et al., 2023,
Total electron temperature derived from quasi-thermal noise spectroscopy in the pristine solar wind from Parker Solar Probe observations
, ASTRONOMY & ASTROPHYSICS, Vol: 674, ISSN: 0004-6361- Author Web Link
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- Citations: 3
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Journal articleZhong C, Cheng S, Kasoar M, et al., 2023,
Reduced-order digital twin and latent data assimilation for global wildfire prediction
, NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, Vol: 23, Pages: 1755-1768, ISSN: 1561-8633- Author Web Link
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- Citations: 1
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Journal articlePyakurel PS, Phan TD, Drake JF, et al., 2023,
On the Short-scale Spatial Variability of Electron Inflows in Electron-only Magnetic Reconnection in the Turbulent Magnetosheath Observed by MMS
, ASTROPHYSICAL JOURNAL, Vol: 948, ISSN: 0004-637X -
Journal articleRodenkirchen C, Ackerman AK, Mignanelli PM, et al., 2023,
Effect of Alloying on the Microstructure, Phase Stability, Hardness, and Partitioning Behavior of a New Dual-Superlattice Nickel-Based Superalloy
, METALLURGICAL AND MATERIALS TRANSACTIONS A-PHYSICAL METALLURGY AND MATERIALS SCIENCE, Vol: 54, Pages: 1902-1923, ISSN: 1073-5623 -
Journal articleMadanian H, Omidi N, Sibeck DG, et al., 2023,
Transient Foreshock Structures Upstream of Mars: Implications of the Small Martian Bow Shock
, GEOPHYSICAL RESEARCH LETTERS, Vol: 50, ISSN: 0094-8276 -
Journal articleCael BB, Bloch-Johnson J, Ceppi P, et al., 2023,
Energy budget diagnosis of changing climate feedback
, Science Advances, Vol: 9<jats:p> The climate feedback determines how Earth’s climate responds to anthropogenic forcing. It is thought to have been more negative in recent decades due to a sea surface temperature “pattern effect,” whereby warming is concentrated in the western tropical Pacific, where nonlocal radiative feedbacks are very negative. This phenomenon has however primarily been studied within climate models. We diagnose a pattern effect from historical records as an evolution of the climate feedback over the past five decades. Our analysis assumes a constant rate of change of the climate feedback, which is justified post hoc. We find a decrease in climate feedback by 0.8 ± 0.5 W m <jats:sup>−2</jats:sup> K <jats:sup>−1</jats:sup> over the past 50 years, corresponding to a reduction in climate sensitivity. Earth system models’ climate feedbacks instead increase over this period. Understanding and simulating this historical trend and its future evolution are critical for reliable climate projections. </jats:p>
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Journal articleJensen EA, Gopalswamy N, Wilson LB, et al., 2023,
The Faraday Effect Tracker of Coronal and Heliospheric Structures (FETCH) instrument
, FRONTIERS IN ASTRONOMY AND SPACE SCIENCES, Vol: 10, ISSN: 2296-987X- Author Web Link
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- Citations: 2
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Journal articleFroment C, Agapitov OV, Krasnoselskikh V, et al., 2023,
Whistler waves generated inside magnetic dips in the young solar wind: Observations of the search-coil magnetometer on board Parker Solar Probe
, ASTRONOMY & ASTROPHYSICS, Vol: 672, ISSN: 0004-6361- Author Web Link
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- Citations: 2
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Journal articleGryspeerdt E, Povey AC, Grainger RG, et al., 2023,
Uncertainty in aerosol-cloud radiative forcing is driven by clean conditions
, Atmospheric Chemistry and Physics, Vol: 23, Pages: 4115-4122, ISSN: 1680-7316Atmospheric aerosols and their impact on cloud properties remain the largest uncertainty in the human forcing of theclimate system. By increasing the concentration of cloud droplets (Nd ), aerosols reduce droplet size and increase the reflectivity of clouds (a negative radiative forcing). Central to this climate impact is the susceptibility of cloud droplet number to aerosol (β ), the diversity of which explains much of the variation in the radiative forcing from aerosol-cloud interactions (RFaci) in global climate models. This has made measuring β a key target for developing observational constraints of the aerosol forcing. While the aerosol burden of the clean, pre-industrial atmosphere has been demonstrated as a key uncertainty for the aerosol forcing, here we show that the behaviour of clouds under these clean conditions is of equal importance for understanding the spread in radiative forcing estimates between models and observations. This means that the uncertainty in the aerosol impact on clouds is, counterintuitively, driven by situations with little aerosol. Discarding clean conditions produces a close agreement between different model and observational estimates of the cloud response to aerosol, but does not provide a strong constraint on the RFaci. This makes constraining aerosol behaviour in clean conditions an important goal for future observational studies.
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Journal articleHuang J, Kasper JC, Larson DE, et al., 2023,
Parker Solar Probe Observations of High Plasma <i>β</i> Solar Wind from the Streamer Belt
, ASTROPHYSICAL JOURNAL SUPPLEMENT SERIES, Vol: 265, ISSN: 0067-0049- Author Web Link
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- Citations: 2
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Journal articleKarbashewski S, Agapitov OV, Kim HY, et al., 2023,
Whistler Wave Observations by Parker Solar Probe During Encounter 1: Counter-propagating Whistlers Collocated with Magnetic Field Inhomogeneities and their Application to Electric Field Measurement Calibration
, ASTROPHYSICAL JOURNAL, Vol: 947, ISSN: 0004-637X- Author Web Link
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- Citations: 2
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Journal articleSafrankova J, Nemecek Z, Nemec F, et al., 2023,
Evolution of Magnetic Field Fluctuations and Their Spectral Properties within the Heliosphere: Statistical Approach
, ASTROPHYSICAL JOURNAL LETTERS, Vol: 946, ISSN: 2041-8205- Author Web Link
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- Citations: 1
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Journal articleSeo H, Oneill LW, Bourassa MA, et al., 2023,
Ocean Mesoscale and Frontal-Scale Ocean-Atmosphere Interactions and Influence on Large-Scale Climate: A Review
, JOURNAL OF CLIMATE, Vol: 36, Pages: 1981-2013, ISSN: 0894-8755- Author Web Link
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- Citations: 10
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Journal articleShuster JR, Gershman DJ, Giles BL, et al., 2023,
Temporal, Spatial, and Velocity-Space Variations of Electron Phase Space Density Measurements at the Magnetopause
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 128, ISSN: 2169-9380 -
Journal articleStawarz JEE, Genestreti KJJ, 2023,
Preface to Special Topic: Plasma Physics from the Magnetospheric Multiscale Mission
, PHYSICS OF PLASMAS, Vol: 30, ISSN: 1070-664X -
Journal articleBadman ST, Riley P, Jones SI, et al., 2023,
Prediction and Verification of Parker Solar Probe Solar Wind Sources at 13.3 R<sub>⊙</sub>
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 128, ISSN: 2169-9380- Author Web Link
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- Citations: 8
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Journal articleWells C, Kasoar M, Bellouin N, et al., 2023,
Local and remote climate impacts of future African aerosol emissions
, Atmospheric Chemistry and Physics, Vol: 23, Pages: 3575-3593, ISSN: 1680-7316The potential future trend in African aerosol emissions is uncertain, with a large range found in future scenarios used to drive climate projections. The future climate impact of these emissions is therefore uncertain. Using the Shared Socioeconomic Pathway (SSP) scenarios, transient future experiments were performed with the UK Earth System Model (UKESM1) to investigate the effect of African emissions following the high emission SSP370 scenario as the rest of the world follows the more sustainable SSP119, relative to a global SSP119 control. This isolates the effect of Africa following a relatively more polluted future emissions pathway. Compared to SSP119, SSP370 projects higher non-biomass-burning (non-BB) aerosol emissions, but lower biomass burning emissions, over Africa. Increased shortwave (SW) absorption by black carbon aerosol leads to a global warming, but the reduction in the local incident surface radiation close to the emissions is larger, causing a local cooling effect. The local cooling persists even when including the higher African CO2 emissions under SSP370 than SSP119. The global warming is significantly higher by 0.07 K when including the non-BB aerosol increases and higher still (0.22 K) when including all aerosols and CO2. Precipitation also exhibits complex changes. Northward shifts in the Inter-tropical Convergence Zone (ITCZ) occur under relatively warm Northern Hemisphere land, and local rainfall is enhanced due to mid-tropospheric instability from black carbon absorption. These results highlight the importance of future African aerosol emissions for regional and global climate and the spatial complexity of this climate influence.
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Journal articleDandouras I, Taylor MGGT, De Keyser J, et al., 2023,
Space plasma physics science opportunities for the lunar orbital platform - Gateway
, Frontiers in Astronomy and Space Sciences, Vol: 10, Pages: 1-30, ISSN: 2296-987XThe Lunar Orbital Platform - Gateway (LOP - Gateway, or simply Gateway) is a crewed platform that will be assembled and operated in the vicinity of the Moon by NASA and international partner organizations, including ESA, starting from the mid-2020s. It will offer new opportunities for fundamental and applied scientific research. The Moon is a unique location to study the deep space plasma environment. Moreover, the lunar surface and the surface-bounded exosphere are interacting with this environment, constituting a complex multi-scale interacting system. This paper examines the opportunities provided by externally mounted payloads on the Gateway in the field of space plasma physics, heliophysics and space weather, and also examines the impact of the space environment on an inhabited platform in the vicinity of the Moon. It then presents the conceptual design of a model payload, required to perform these space plasma measurements and observations. It results that the Gateway is very well-suited for space plasma physics research. It allows a series of scientific objectives with a multi-disciplinary dimension to be addressed.
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Journal articleLai T-K, Toumi R, 2023,
Has there been a recent shallowing of tropical cyclones?
, Geophysical Research Letters, Vol: 50, Pages: 1-9, ISSN: 0094-8276Many aspects of tropical cyclone (TC) properties at the surface have been changing but any systematic vertical changes are unknown. Here, we document a recent trend of high thick clouds of TCs. The global inner-core high thick cloud fraction measured by satellite has decreased from 2002 to 2021 by about 10% per decade. The TC inner-core surface rain rate is also found to have decreased during the same period by a similar percentage. This suppression of high thick clouds and rain has been largest during the intensification phase of the strongest TCs. Hence, these two independent and consistent observations suggest that the TC inner-core convection has weakened and that TCs have become shallower recently at least. For this period, the lifetime maximum intensity of major TCs has not changed and this suggests an increased efficiency of the spin-up of TCs.
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