9,940 research outputs found
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A numerical model of the ionospheric signatures of time-varying magnetic reconnection: III. Quasi-instantaneous convection responses in the Cowley-Lockwood paradigm
Using a numerical implementation of the Cowley and Lockwood (1992) model of flow excitation in the magnetosphereâionosphere (MI) system, we show that both an expanding (on a _12-min timescale) and a quasiinstantaneous response in ionospheric convection to the onset of magnetopause reconnection can be accommodated by the CowleyâLockwood conceptual framework. This model has a key feature of time dependence, necessarily considering the history of the coupled MI system. We show that a residual flow, driven by prior magnetopause reconnection, can produce a quasi-instantaneous global ionospheric convection response; perturbations from an equilibrium state may also be present from tail reconnection, which will superpose constructively to give a similar effect. On the other hand, when the MI system is relatively free of pre-existing flow, we can most clearly see the expanding nature of the response. As the open-closed field line boundary will frequently be in motion from such prior reconnection (both at the dayside magnetopause and in the cross-tail current sheet), it is expected that there will usually be some level of combined response to dayside reconnection
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A numerical model of the ionospheric signatures of time-varying magnetic reconnection: II. Measuring expansions in the ionospheric flow response
A numerical model embodying the concepts of the Cowley-Lockwood (Cowley and Lockwood, 1992, 1997) paradigm has been used to produce a simple Cowleyâ Lockwood type expanding flow pattern and to calculate the resulting change in ion temperature. Cross-correlation, fixed threshold analysis and threshold relative to peak are used to determine the phase speed of the change in convection pattern, in response to a change in applied reconnection. Each of these methods fails to fully recover the expansion of the onset of the convection response that is inherent in the simulations. The results of this study indicate that any expansion of the convection pattern will be best observed in time-series data using a threshold which is a fixed fraction of the peak response. We show that these methods used to determine the expansion velocity can be used to discriminate between the two main models for the convection response to a change in reconnection
Quantitative assessment of Earthâs radiation belt modeling
The âQuantitative Assessment of Radiation Belt Modelingâ focus group was in place at Geospace Environment Modeling from 2014 to 2018. The overarching goals of this focus group were to bring together the current stateâofâtheâart models for the acceleration, transport, and loss processes in Earth's radiation belts; develop eventâspecific and global inputs of wave, plasma, and magnetic field to drive these models; and combine all these components to achieve a quantitative assessment of radiation belt modeling by validating against contemporary radiation belt measurements. This article briefly reviews the current understanding of radiation belt dynamics and related modeling efforts, summarizes the activities and accomplishments of the focus group, and discusses future directions.Accepted manuscrip
Quantitative assessment of radiation belt modeling
The âQuantitative Assessment of Radiation Belt Modelingâ focus group was in place at Geospace Environment Modeling from 2014 to 2018. The overarching goals of this focus group were to bring together the current stateâofâtheâart models for the acceleration, transport, and loss processes in Earth's radiation belts; develop eventâspecific and global inputs of wave, plasma, and magnetic field to drive these models; and combine all these components to achieve a quantitative assessment of radiation belt modeling by validating against contemporary radiation belt measurements. This article briefly reviews the current understanding of radiation belt dynamics and related modeling efforts, summarizes the activities and accomplishments of the focus group, and discusses future directions.Accepted manuscrip
A Comparison of Near-Infrared Photometry and Spectra for Y Dwarfs with a New Generation of Cool Cloudy Models
We present YJHK photometry, or a subset, for the six Y dwarfs discovered in
WISE data by Cushing et al.. The data were obtained using NIRI on the Gemini
North telescope. We also present a far-red spectrum obtained using GMOS-North
for WISEPC J205628.90+145953.3. We compare the data to Morley et al. (2012)
models, which include cloud decks of sulfide and chloride condensates. We find
that the models with these previously neglected clouds can reproduce the energy
distributions of T9 to Y0 dwarfs quite well, other than near 5um where the
models are too bright. This is thought to be because the models do not include
departures from chemical equilibrium caused by vertical mixing, which would
enhance the abundance of CO, decreasing the flux at 5um. Vertical mixing also
decreases the abundance of NH_3, which would otherwise have strong absorption
features at 1.03um and 1.52um that are not seen in the Y0 WISEPC
J205628.90+145953.3. We find that the five Y0 to Y0.5 dwarfs have 300 < T_eff K
< 450, 4.0 < log g < 4.5 and f_sed ~ 3. These temperatures and gravities imply
a mass range of 5 - 15 M_Jupiter and ages around 5 Gyr. We suggest that WISEP
J182831.08+265037.8 is a binary system, as this better explains its luminosity
and color. We find that the data can be made consistent with observed trends,
and generally consistent with the models, if the system is composed of a T_eff
= 325 K and log g ~ 4.0
secondary, corresponding to masses of 10 and 7 M_Jupiter and an age around 2
Gyr. If our deconvolution is correct, then the T_eff = 300 K cloud-free model
fluxes at K and W2 are too faint by 0.5 - 1.0 magnitudes. We will address this
discrepancy in our next generation of models, which will incorporate water
clouds and mixing.Comment: 39 pages, 10 Figures, 8 Tables. Accepted by ApJ. This revision
replaces Figures 9 and 10 with B & W versions, corrects figure captions for
color online only, corrects references. Text is unchanged. Tables 3, 4 and 8
are available at http://www.gemini.edu/staff/sleggett, other model data are
available at http://www.ucolick.org/~cmorley/cmorley/Data.htm
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The dependence of cusp ion signatures on the reconnection rate
The interpretation of structure in cusp ion dispersions is important for helping to understand the temporal and spatial structure of magnetopause reconnection. âSteppedâ and âsawtoothâ signatures have been shown to be caused by temporal variations in the reconnection rate under the same physical conditions for different satellite trajectories. The present paper shows that even for a single satellite path, a change in the amplitude of any reconnection pulses can alter the observed signature and even turn sawtooth into stepped forms and vice versa. On 20 August 1998, the Defense Meteorological Satellite Program (DMSP) craft F-14 crossed the cusp just to the south of Longyearbyen, returning on the following orbit. The two passes by the DMSP F-14 satellites have very similar trajectories and the open-closed field line boundary (OCB) crossings, as estimated from the SSJ/4 precipitating particle data and Polar UVI images, imply a similarly-shaped polar cap, yet the cusp ion dispersion signatures differ substantially. The cusp crossing at 08:54 UT displays a stepped ion dispersion previously considered to be typical of a meridional pass, whereas the crossing at 10:38 UT is a sawtooth form ion dispersion, previously considered typical of a satellite travelling longitudinally with respect to the OCB. It is shown that this change in dispersed ion signature is likely to be due to a change in the amplitude of the pulses in the reconnection rate, causing the stepped signature. Modelling of the low-energy ion cutoff under different conditions has reproduced the forms of signature observed
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A numerical model of the ionospheric signatures of time-varying magneticreconnection: I. ionospheric convection
This paper presents a numerical model for predicting the evolution of the pattern of ionospheric convection in response to general time-dependent magnetic reconnection at the dayside magnetopause and in the cross-tail current sheet of the geomagnetic tail. The model quantifies the concepts of ionospheric flow excitation by Cowley and Lockwood (1992), assuming a uniform spatial distribution of ionospheric conductivity. The model is demonstrated using an example in which travelling reconnection pulses commence near noon and then move across the dayside magnetopause towards both dawn and dusk. Two such pulses, 8 min apart, are used and each causes the reconnection to be active for 1 min at every MLT that they pass over. This example demonstrates how the convection response to a given change in the interplanetary magnetic field (via the reconnection rate) depends on the previous reconnection history. The causes of this effect are explained. The inherent assumptions and the potential applications of the model are discussed
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