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Journal articleOwens MJ, Horbury TS, Wicks RT, et al., 2014,
Ensemble downscaling in coupled solar wind-magnetosphere modeling for space weather forecasting
, Space Weather, Vol: 12, Pages: 395-405, ISSN: 1539-4956Advanced forecasting of space weather requires simulation of the whole Sun-to-Earth system, which necessitates driving magnetospheric models with the outputs from solar wind models. This presents a fundamental difficulty, as the magnetosphere is sensitive to both large-scale solar wind structures, which can be captured by solar wind models, and small-scale solar wind “noise,” which is far below typical solar wind model resolution and results primarily from stochastic processes. Following similar approaches in terrestrial climate modeling, we propose statistical “downscaling” of solar wind model results prior to their use as input to a magnetospheric model. As magnetospheric response can be highly nonlinear, this is preferable to downscaling the results of magnetospheric modeling. To demonstrate the benefit of this approach, we first approximate solar wind model output by smoothing solar wind observations with an 8 h filter, then add small-scale structure back in through the addition of random noise with the observed spectral characteristics. Here we use a very simple parameterization of noise based upon the observed probability distribution functions of solar wind parameters, but more sophisticated methods will be developed in the future. An ensemble of results from the simple downscaling scheme are tested using a model-independent method and shown to add value to the magnetospheric forecast, both improving the best estimate and quantifying the uncertainty. We suggest a number of features desirable in an operational solar wind downscaling scheme.
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Journal articleHietala H, Eastwood JP, Isavnin A, 2014,
Sequentially released tilted flux ropes in the Earth's magnetotail
, PLASMA PHYSICS AND CONTROLLED FUSION, Vol: 56, ISSN: 0741-3335- Author Web Link
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- Citations: 17
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Journal articleMiller RL, Schmidt GA, Nazarenko LS, et al., 2014,
CMIP5 historical simulations (1850-2012) with GISS ModelE2
, JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, Vol: 6, Pages: 441-477- Cite
- Citations: 136
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Journal articleMarlier ME, Voulgarakis A, Shindell DT, et al., 2014,
The role of temporal evolution in modeling atmospheric emissions from tropical fires
, ATMOSPHERIC ENVIRONMENT, Vol: 89, Pages: 158-168, ISSN: 1352-2310- Author Web Link
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- Citations: 12
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Journal articleGryspeerdt E, Stier P, Grandey BS, 2014,
Cloud fraction mediates the aerosol optical depth-cloud top height relationship
, GEOPHYSICAL RESEARCH LETTERS, Vol: 41, Pages: 3622-3627, ISSN: 0094-8276- Author Web Link
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- Citations: 44
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Journal articleNichols JD, Badman SV, Baines KH, et al., 2014,
Dynamic auroral storms on Saturn as observed by the Hubble Space Telescope
, Geophysical Research Letters, Vol: 41, Pages: 3323-3330, ISSN: 1944-8007We present observations of significant dynamics within two UV auroral storms observedon Saturn using the Hubble Space Telescope in April/May 2013. Specifically, we discuss bursts of auroralemission observed at the poleward boundary of a solar wind-induced auroral storm, propagating at ∼330%rigid corotation from near ∼01 h LT toward ∼08 h LT. We suggest that these are indicative of ongoing, burstyreconnection of lobe flux in the magnetotail, providing strong evidence that Saturn’s auroral storms arecaused by large-scale flux closure. We also discuss the later evolution of a similar storm and show that theemission maps to the trailing region of an energetic neutral atom enhancement. We thus identify the auroralform with the upward field-aligned continuity currents flowing into the associated partial ring current.
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Journal articleSimon S, Saur J, van Treeck SC, et al., 2014,
Discontinuities in the magnetic field near Enceladus
, GEOPHYSICAL RESEARCH LETTERS, Vol: 41, Pages: 3359-3366, ISSN: 0094-8276- Author Web Link
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- Citations: 14
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Journal articleCeppi P, Zelinka MD, Hartmann DL, 2014,
The response of the Southern Hemispheric eddy-driven jet to future changes in shortwave radiation in CMIP5
, Geophysical Research Letters, Vol: 41, Pages: 3244-3250, ISSN: 0094-8276A strong relationship is found between changes in the meridional gradient of absorbed shortwave radiation (ASR) and Southern Hemispheric jet shifts in 21st century climate simulations of CMIP5 (Coupled Model Intercomparison Project phase 5) coupled models. The relationship is such that models with increases in the meridional ASR gradient around the southern midlatitudes, and therefore increases in midlatitude baroclinicity, tend to produce a larger poleward jet shift. The ASR changes are shown to be dominated by changes in cloud properties, with sea ice declines playing a secondary role. We demonstrate that the ASR changes are the cause, and not the result, of the intermodel differences in jet response by comparing coupled simulations with experiments in which sea surface temperature increases are prescribed. Our results highlight the importance of reducing the uncertainty in cloud feedbacks in order to constrain future circulation changes.
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Book chapterGaland MIF, Coates A, Cravens T, et al., 2014,
Titan's Ionosphere
, Titan: Interior, Surface, Atmosphere, and Space Environment, Editors: Mueller-Wodarg, Griffith, Lellouch, Cravens, Publisher: Cambridge University Press, Pages: 376-418, ISBN: 9780521199926 -
Journal articleVigren E, Galand M, Shebanits O, et al., 2014,
INCREASING POSITIVE ION NUMBER DENSITIES BELOW THE PEAK OF ION-ELECTRON PAIR PRODUCTION IN TITAN'S IONOSPHERE
, ASTROPHYSICAL JOURNAL, Vol: 786, ISSN: 0004-637X- Cite
- Citations: 10
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Journal articleSouthwood D, 2014,
Crowded Orbits: Conflict and Cooperation in Space
, NATURE, Vol: 509, Pages: 32-32, ISSN: 0028-0836 -
Journal articleBunce EJ, Grodent DC, Jinks SL, et al., 2014,
Cassini nightside observations of the oscillatory motion of Saturn's northern auroral oval
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 3528-3543, ISSN: 2169-9380- Author Web Link
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- Citations: 17
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Journal articleAnsell C, Brindley HE, Pradhan Y, et al., 2014,
Mineral dust aerosol net direct radiative effect during GERBILS field campaign period derived from SEVIRI and GERB
, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, Vol: 119, Pages: 4070-4086, ISSN: 2169-897X- Author Web Link
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- Citations: 15
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Journal articleGoldman MV, Newman DL, Lapenta G, et al., 2014,
Cerenkov Emission of Quasiparallel Whistlers by Fast Electron Phase-Space Holes during Magnetic Reconnection
, PHYSICAL REVIEW LETTERS, Vol: 112, ISSN: 0031-9007- Author Web Link
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- Citations: 56
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Journal articleBadman SV, Branduardi-Raymont G, Galand M, et al., 2014,
Auroral Processes at the Giant Planets: Energy Deposition, Emission Mechanisms, Morphology and Spectra
, Space Science Reviews, Vol: 187, Pages: 99-179, ISSN: 1572-9672The ionospheric response to auroral precipitation at the giant planets is reviewed,using models and observations. The emission processes for aurorae at radio, infrared, visible,ultraviolet, and X-ray wavelengths are described, and exemplified using ground- andspace-based observations. Comparisons between the emissions at different wavelengths are made, where possible, and interpreted in terms of precipitating particle characteristics oratmospheric conditions. Finally, the spatial distributions and dynamics of the various componentsof the aurorae (moon footprints, low-latitude, main oval, polar) are related to magnetosphericprocesses and boundaries, using theory, in situ, and remote observations, withthe aim of distinguishing between those related to internally-driven dynamics, and thoserelated to the solar wind interaction.
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Journal articleMessori G, Czaja A, 2014,
Some considerations on the spectral features of meridional heat transport by transient eddies
, QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, Vol: 140, Pages: 1377-1386, ISSN: 0035-9009- Author Web Link
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- Citations: 8
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Journal articleShen C, Yang YY, Rong ZJ, et al., 2014,
Direct calculation of the ring current distribution and magnetic structure seen by Cluster during geomagnetic storms
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 2458-2465, ISSN: 2169-9380- Cite
- Citations: 36
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Journal articleFuselier SA, Frahm R, Lewis WS, et al., 2014,
The location of magnetic reconnection at Saturn's magnetopause: A comparison with Earth
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 2563-2578, ISSN: 2169-9380- Author Web Link
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- Citations: 55
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Journal articlePilkington NM, Achilleos N, Arridge CS, et al., 2014,
Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 2858-2875, ISSN: 2169-9380- Author Web Link
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- Citations: 20
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Journal articleKriegel H, Simon S, Meier P, et al., 2014,
Ion densities and magnetic signatures of dust pickup at Enceladus
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 2740-2774, ISSN: 2169-9380- Author Web Link
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- Citations: 39
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Journal articleMeredith CJ, Alexeev II, Badman SV, et al., 2014,
Saturn's dayside ultraviolet auroras: Evidence for morphological dependence on the direction of the upstream interplanetary magnetic field
, Journal of Geophysical Research: Space Physics, Vol: 119, Pages: 1994-2008, ISSN: 2169-9402We examine a unique data set from seven Hubble Space Telescope (HST) “visits” that imagedSaturn’s northern dayside ultraviolet emissions exhibiting usual circumpolar “auroral oval” morphologies,during which Cassini measured the interplanetary magnetic field (IMF) upstream of Saturn’s bow shock overintervals of several hours. The auroras generally consist of a dawn arc extending toward noon centered near~15° colatitude, together with intermittent patchy forms at ~10° colatitude and poleward thereof, locatedbetween noon and dusk. The dawn arc is a persistent feature, but exhibits variations in position, width, andintensity, which have no clear relationship with the concurrent IMF. However, the patchy postnoon aurorasare found to relate to the (suitably lagged and averaged) IMF Bz, being present during all four visits withpositive Bz and absent during all three visits with negative Bz. The most continuous such forms occur in thecase of strongest positive Bz. These results suggest that the postnoon forms are associated with reconnectionand open flux production at Saturn’s magnetopause, related to the similarly interpreted bifurcated auroral arcstructures previously observed in this local time sector in Cassini Ultraviolet Imaging Spectrograph data,whose details remain unresolved in these HST images. One of the intervals with negative IMF Bz howeverexhibits a prenoon patch of very high latitude emission extending poleward of the dawn arc to the magnetic/spin pole, suggestive of the occurrence of lobe reconnection. Overall, these data provide evidence ofsignificant IMF dependence in the morphology of Saturn’s dayside auroras.
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Journal articleMasters A, Fujimoto M, Hasegawa H, et al., 2014,
Can magnetopause reconnection drive Saturn's magnetosphere?
, GEOPHYSICAL RESEARCH LETTERS, Vol: 41, Pages: 1862-1868, ISSN: 0094-8276- Cite
- Citations: 23
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Journal articleCargill PJ, 2014,
ACTIVE REGION EMISSION MEASURE DISTRIBUTIONS AND IMPLICATIONS FOR NANOFLARE HEATING
, ASTROPHYSICAL JOURNAL, Vol: 784, ISSN: 0004-637X- Author Web Link
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- Citations: 73
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Journal articleJasinski JM, Arridge CS, Lamy L, et al., 2014,
Cusp observation at Saturn's high-latitude magnetosphere by the Cassini spacecraft
, Geophysical Research Letters, Vol: 41, Pages: 1382-1388, ISSN: 1944-8007We report on the first analysis of magnetospheric cusp observations at Saturn by multiple insitu instruments onboard the Cassini spacecraft. Using this we infer the process of reconnection wasoccurring at Saturn’s magnetopause. This agrees with remote observations that showed the associatedauroral signatures of reconnection. Cassini crossed the northern cusp around noon local time along apoleward trajectory. The spacecraft observed ion energy-latitude dispersions—a characteristic signature ofthe terrestrial cusp. This ion dispersion is “stepped,” which shows that the reconnection is pulsed. The ionenergy-pitch angle dispersions suggest that the field-aligned distance from the cusp to the reconnectionsite varies between ∼27 and 51 RS. An intensification of lower frequencies of the Saturn kilometricradiation emissions suggests the prior arrival of a solar wind shock front, compressing the magnetosphereand providing more favorable conditions for magnetopause reconnection.
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Journal articleHartmann DL, Ceppi P, 2014,
Trends in the CERES dataset, 2000-13: the effects of sea ice and jet shifts and comparison to climate models
, Journal of Climate, Vol: 27, Pages: 2444-2456, ISSN: 0894-8755The Clouds and the Earth’s Radiant Energy System (CERES) observations of global top-of-atmosphere radiative energy fluxes for the period March 2000–February 2013 are examined for robust trends and variability. The trend in Arctic ice is clearly evident in the time series of reflected shortwave radiation, which closely follows the record of ice extent. The data indicate that, for every 106 km2 decrease in September sea ice extent, annual-mean absorbed solar radiation averaged over 75°–90°N increases by 2.5 W m−2, or about 6 W m−2 between 2000 and 2012. CMIP5 models generally show a much smaller change in sea ice extent over the 1970–2012 period, but the relationship of sea ice extent to reflected shortwave is in good agreement with recent observations. Another robust trend during this period is an increase in reflected shortwave radiation in the zonal belt from 45° to 65°S. This trend is mostly related to increases in sea ice concentrations in the Southern Ocean and less directly related to cloudiness trends associated with the annular variability of the Southern Hemisphere. Models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) produce a scaling of cloud reflection to zonal wind increase that is similar to trend observations in regions separated from the direct effects of sea ice. Atmospheric Model Intercomparison Project (AMIP) model responses over the Southern Ocean are not consistent with each other or with the observed shortwave trends in regions removed from the direct effect of sea ice.
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Journal articleSouthwood DJ, Cowley SWH, 2014,
The origin of Saturn's magnetic periodicities: Northern and southern current systems
, Journal of Geophysical Research: Space Physics, Vol: 119, Pages: 1563-1571, ISSN: 2169-9380The recent survey by Andrews et al. (2012) of the separate northern and southern ~10.7 h periodic magnetic signals in Saturn's magnetosphere limits very much their governing current systems. The existence of signals with pure or close to pure northern or southern periods in respective polar caps taken with the relatively narrow bandwidth of the signals indicates that the actual periodicities are imposed independently from northern and southern polar regions, i.e., the open field line regions. Field‐aligned currents must flow on the boundaries of these regions to exclude signals from the other hemisphere. Equatorward of the polar cap, on closed magnetic shells, there are distinct north and south “cam” source currents, the distinction being made clear by a difference in polarization. We outline the consequences for the governing current systems and the implications for sustaining the energy and power dissipation in the system.
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Journal articleMistry R, Dougherty MK, Masters A, et al., 2014,
Separating drivers of Saturnian magnetopause motion
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 1514-1522, ISSN: 2169-9380- Author Web Link
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- Citations: 5
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Journal articleLiu YD, Luhmann JG, Kajdic P, et al., 2014,
Observations of an extreme storm in interplanetary space caused by successive coronal mass ejections
, NATURE COMMUNICATIONS, Vol: 5, ISSN: 2041-1723- Cite
- Citations: 251
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Journal articleSchwartz SJ, 2014,
Comment on "Electron demagnetization and heating in quasi-perpendicular shocks" by Mozer and Sundkvist
, JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, Vol: 119, Pages: 1507-1512, ISSN: 2169-9380- Author Web Link
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- Citations: 10
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Journal articleSchmidt GA, Kelley M, Nazarenko L, et al., 2014,
Configuration and assessment of the GISS ModelE2 contributions to the CMIP5 archive
, JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, Vol: 6, Pages: 141-184- Author Web Link
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- Citations: 539
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