Javascript must be enabled to continue!
A Kp‐based model of auroral boundaries
View through CrossRef
The auroral oval can serve as both a representation and a prediction of space weather on a global scale, so a competent model of the oval as a function of a geomagnetic index could conveniently appraise space weather itself. A simple model of the auroral boundaries is constructed by binning several months of images from the Polar Ultraviolet Imager by Kp index. The pixel intensities are first averaged into magnetic latitude–magnetic local time (MLT‐MLAT) and local time bins, and intensity profiles are then derived for each Kp level at 1 hour intervals of MLT. After background correction, the boundary latitudes of each profile are determined at a threshold of 4 photons cm−2 s1. The peak locations and peak intensities are also found. The boundary and peak locations vary linearly with Kp index, and the coefficients of the linear fits are tabulated for each MLT. As a general rule of thumb, the UV intensity peak shifts 1° in magnetic latitude for each increment in Kp. The fits are surprisingly good for Kp < 6 but begin to deteriorate at high Kp because of auroral boundary irregularities and poor statistics. The statistical model allows calculation of the auroral boundaries at most MLTs as a function of Kp and can serve as an approximation to the shape and extent of the statistical oval.
Title: A Kp‐based model of auroral boundaries
Description:
The auroral oval can serve as both a representation and a prediction of space weather on a global scale, so a competent model of the oval as a function of a geomagnetic index could conveniently appraise space weather itself.
A simple model of the auroral boundaries is constructed by binning several months of images from the Polar Ultraviolet Imager by Kp index.
The pixel intensities are first averaged into magnetic latitude–magnetic local time (MLT‐MLAT) and local time bins, and intensity profiles are then derived for each Kp level at 1 hour intervals of MLT.
After background correction, the boundary latitudes of each profile are determined at a threshold of 4 photons cm−2 s1.
The peak locations and peak intensities are also found.
The boundary and peak locations vary linearly with Kp index, and the coefficients of the linear fits are tabulated for each MLT.
As a general rule of thumb, the UV intensity peak shifts 1° in magnetic latitude for each increment in Kp.
The fits are surprisingly good for Kp < 6 but begin to deteriorate at high Kp because of auroral boundary irregularities and poor statistics.
The statistical model allows calculation of the auroral boundaries at most MLTs as a function of Kp and can serve as an approximation to the shape and extent of the statistical oval.
Related Results
Sporadic aurorae observed in East Asia
Sporadic aurorae observed in East Asia
Abstract. All the accessible auroral observations recorded in Chinese and Japanese histories during the interval AD 1840–1911 are investigated in detail. Most of these auroral reco...
Auroral and sub-auroral phenomena: an electrostatic picture
Auroral and sub-auroral phenomena: an electrostatic picture
Abstract. Many auroral and sub-auroral phenomena are manifestations of an underlying magnetosphere-ionosphere coupling. In the electrostatic perspective the associated auroral curr...
The Morphology of Poleward Moving Auroral Forms
The Morphology of Poleward Moving Auroral Forms
Abstract. We investigated the morphology of poleward moving auroral forms (PMAFs) qualitatively by visual inspection of all sky camera (ASC) images and quantitatively using the arc...
Longitudinal Gradients in Field-Aligned Currents as Observed by Swarm
Longitudinal Gradients in Field-Aligned Currents as Observed by Swarm
<p>Field-aligned currents (FACs) are closely related to aurora and a key component of the magnetosphere-ionosphere-thermosphere system. Large scale FAC structures, li...
THEMIS observation of a substorm event on 04:35, 22 February 2008
THEMIS observation of a substorm event on 04:35, 22 February 2008
Abstract. We report on THEMIS in-situ and ground-based observations during a substorm between 04:30~04:50 UT on 22 February 2008. The spacecraft (probes) were aligned along the tai...
DAY BY DAY BEHAVIOR OF GNNS POSITIONING ERRORS AND TEC FLUCTUATIONS ASSOCIATED AURORAL DISTURBANCES OVER MARCH 2015
DAY BY DAY BEHAVIOR OF GNNS POSITIONING ERRORS AND TEC FLUCTUATIONS ASSOCIATED AURORAL DISTURBANCES OVER MARCH 2015
We analyzed the occurrence of TEC fluctuations and an impact of auroral disturbances on the Precise Point Positioning (PPP) errors in European sector using GPS measurements of EPN ...
Filth, Incontinence and Border Protection
Filth, Incontinence and Border Protection
This paper investigates linkages between two apparently disparate government initiatives. Together they function symbolically to maintain Australia’s...
Relation of Offshore and Onshore Mineral Resources to Plate Tectonics
Relation of Offshore and Onshore Mineral Resources to Plate Tectonics
ABSTRACT
The Pacific and Atlantic are natural laboratories to study relations between mineral resources and plate tectonics. The distribution of mineral deposits ...

