scispace - formally typeset
S

Steve Milan

Researcher at University of Leicester

Publications -  235
Citations -  7503

Steve Milan is an academic researcher from University of Leicester. The author has contributed to research in topics: Magnetosphere & Ionosphere. The author has an hindex of 43, co-authored 222 publications receiving 6536 citations. Previous affiliations of Steve Milan include University of Bergen.

Papers
More filters
Journal ArticleDOI

Variations in the polar cap area during two substorm cycles

TL;DR: In this article, the authors employed observations from several sources to determine the location of the polar cap bound-ary, or open/closed field line boundary, at all local times, allowing the amount of open flux in the magnetosphere to be quantified.
Journal ArticleDOI

Reconnection in a rotation-dominated magnetosphere and its relation to Saturn's auroral dynamics

TL;DR: The first extended series of observations of Saturn's auroral emissions, undertaken by the Hubble Space Telescope in January 2004 in conjunction with measurements of the upstream solar wind and interplanetary magnetic field (IMF) by the Cassini spacecraft, have revealed a strong auroral response to the inter-planetary medium as discussed by the authors.
Journal ArticleDOI

Convection and auroral response to a southward turning of the IMF : Polar UVI, CUTLASS, and IMAGE signatures of transient magnetic flux transfer at the magnetopause

TL;DR: In this article, the first spacecraft-borne imager observations of the auroral manifestation of transient magnetic flux transfer at the magnetopause were presented, during an interval of interplanetary magnetic field Bz ≈ −10 nT and By ≈ 10 nT, and solar wind dynamic pressure and velocity Psw ≈ 5 nPa and vsw vw ≈ 650 km s−1, Polar Ultraviolet Imager (UVI) images show a sequence of events, each of which begins as a bifurcation of the main auroral oval in
Journal ArticleDOI

Magnetic flux transport in the Dungey cycle: A survey of dayside and nightside reconnection rates

TL;DR: In this paper, changes in the open flux content of the ionospheric polar cap, estimated from auroral, radar, and low-Earth orbit particle measurements, are used to determine dayside and nightside reconnection rates during 73 hours of observation spread over nine intervals.