https://nova.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:46908 Tue 06 Dec 2022 16:07:23 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:33746 Tue 03 Sep 2019 17:56:42 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:7804 Thu 28 Jun 2018 13:53:29 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:51197 Thu 24 Aug 2023 14:51:17 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:35056 Thu 09 Dec 2021 11:01:32 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:32640 Thu 02 Aug 2018 14:54:38 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:31496 I_Total, and the distribution of radial current density, Jr, for all models are compared with AMPERE results. While the total currents are well correlated, the quantitative agreement varies considerably. The J_r distributions reveal discrepancies between the models and observations related to the latitude distribution, morphologies, and lack of nightside current systems in the models. The results motivate enhancing the simulations first by increasing the simulation resolution and then by examining the relative merits of implementing more sophisticated ionospheric conductance models, including ionospheric outflows or other omitted physical processes. Some aspects of the system, including substorm timing and location, may remain challenging to simulate, implying a continuing need for real-time specification.]]> Sat 24 Mar 2018 08:43:39 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:27636 Sat 24 Mar 2018 07:34:06 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:29480 E region can reduce the chance of F region and increase the chance of E region backscatter. It was also shown that reduction in backscatter cannot be explained by D region absorption. Using a normalized SYM-H value, percentage time through recovery phase can be estimated during storm progression which allows a prediction of backscatter return in real time that accounts for varying storm recovery phase duration.]]> Sat 24 Mar 2018 07:29:45 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:23150 Sat 24 Mar 2018 07:10:34 AEDT ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:41575 Fri 05 Aug 2022 14:44:23 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:41537 aer nullius, dismissing or downplaying prior relationships, belongings and becomings with/as weather and the power relations that mediate what weather means and does. In this article, we aim to speak back to aer nullius and consider weathers' many diverse sovereignties. We engage with weather in ways led by Indigenous scholars and their allies and trace our own positionalities and responsibilities through what it means to weather on unceded Indigenous land. Our focus is brought to power and weather, to the enrolment of weathers' beings and becomings to differentially discipline and empower. Entwining its way through these accounts, but in ways not generally acknowledged, are the sovereignties of weather knowledges and the sovereignties of weather itself. The beings and becomings of weather have their own Law/s, their own knowledges, their own survivances, their own sovereignties. We end the article with a consideration of academic positionalities and responsibilities as we weather and are weathered in entangled, more-than-human ways.]]> Fri 05 Aug 2022 13:55:18 AEST ]]> https://nova.newcastle.edu.au/vital/access/ /manager/Repository/uon:41426 Fri 02 Sep 2022 09:26:02 AEST ]]>