Report

The Global Morphology of Wave Poynting Flux: Powering the Aurora

See allHide authors and affiliations

Science  17 Jan 2003:
Vol. 299, Issue 5605, pp. 383-386
DOI: 10.1126/science.1080073

This article has a correction. Please see:

Abstract

Large-scale, electric currents flowing along magnetic field lines into the polar regions of Earth are thought to be the main contributors of the energy that powers the ionospheric aurora. However, we have found evidence for global contributions from electromagnetic waves (Alfvén waves). Data that were collected from the Polar spacecraft over the course of 1 year show that the flow of wave electromagnetic energy at altitudes of 25,000 to 38,000 kilometers delineates the statistical auroral oval. The Poynting flux of individual events distributed along the auroral oval was larger than 5 ergs per square centimeter per second, which is sufficient to power auroral acceleration processes. This evidence suggests that in addition to magnetic field-aligned currents, the dayside and nightside aurora is globally powered by the energy flow of these high-altitude Alfvén waves.

Earth's aurora occurs statistically and often simultaneously in an oval-shaped belt (Fig. 1A) around the magnetic poles (1). Magnetic field lines connect this auroral oval to the magnetosphere, the region above the atmosphere that is dominated by Earth's magnetic field and filled with plasma. The dayside and nightside auroras are associated with different magnetospheric phenomena (2). The nightside aurora is the result of the sudden release (over the time period of tens of minutes to hours) of large amounts of energy, which is periodically extracted from the solar wind and stored in the magnetic field of the magnetotail (3). Through an unknown sequence of energy transfer processes, a large fraction of this energy is transported to the auroral acceleration region (located at an altitude of 5000 to 15,000 km above the polar regions) (4), where electron energization processes occur to create the intense electron beams that cause the aurora. In contrast, the dayside aurora is connected to the cusp region and is driven by uncertain mechanisms. In either case, it is expected that the aurora is powered by energy flow along the magnetic field lines. However, the altitude away from the ionosphere at which the energy flow becomes dominantly field-aligned has not been determined. In addition, the form of energy that dominates is not known, considering that it could be either kinetic particle energy or electromagnetic energy carried by quasi-static field-aligned currents (FACs) [for a tutorial on FACs in space, see (5)] or Alfvén waves (6). To understand the auroral phenomenon, we need to identify all contributing energy carriers. Here, we determined the global morphology of the Poynting flux due to electromagnetic waves, which are also called Alfvén waves (6), on auroral field lines at altitudes of 25,000 to 38,000 km above ground by using electric and magnetic field data (7, 8) that were collected for one year by the Polar spacecraft (9).

Figure 1

Morphology of the aurora as seen from two cameras onboard the Polar satellite and as inferred from in situ, high-altitude Poynting flux measurements from Polar. (A) The aurora in the visible spectrum over the Northern Hemisphere [the image from the Visible Imaging System camera (26)]. This image shows the instant global morphology of auroral luminosity delineating an oval-shaped band. The dayside is to the left. Scattered sunlight during the day makes the aurora invisible to the human eye. (B) A map of average auroral intensity in the Northern Hemisphere recorded in the UV spectrum [Lyman-Birge-Hopfield (long)]. This map is composed of 17,372 images taken by the UVI (10) during four months of operation (1 April 1997 to 28 July 1997). This figure is slightly modified from Liou et al. (11). The numbers around the outside circle are the local times at the given locations. The numbers down the middle of the plot are magnetic latitudes. (C) Average wave Poynting flux flowing toward Earth as measured at high altitude (25,000 to 38,000 km) in the Northern Hemisphere obtained from 1 year of Polar measurements and then scaled along converging magnetic field lines to ionospheric altitudes (100 km). More intense downward Poynting flux (brown, red, and yellow) delineates the auroral oval. Blue indicates very little or no flux. (D) Similar to Fig. 1C but for upward Poynting flux (i.e., away from Earth). Very little return Poynting flux exists at high altitude.

In addition to in situ measurements, the Ultraviolet Imager (UVI) (10) onboard Polar takes images of ionospheric auroral emissions. These images show the global morphology of auroras in the UV spectrum, but they can also be used to estimate energy depositions through electron beams into the ionosphere causing the auroral emissions. The average global distribution of auroral luminosity in the Northern Hemisphere derived from a large set of images taken over a period of 4 months coincides with the statistical location of the auroral oval with three distinct emission intensifications centered at 22:30, 15:00, and 09:00 local time (Fig. 1B) (11).

During the period from 1 January 1997 to 31 December 1997, the Polar spacecraft completed about 470 orbits. The wave Poynting fluxes (S = δE × δB0) were calculated for the entire database from the electric (δE) and magnetic (δB) wave perturbation fields in the period range from 6 to 180 s (12). This period range was chosen based on the results of previous Polar studies (13, 14) that showed the existence of large Alfvén waves in this range in the plasma sheet during auroral and substorm activity. This filtering removes any Poynting flux caused by large-scale FACs (Fig. 2). It also excludes any wave activity below 5.5 mHz, as previously reported (15). To obtain the component of the wave Poynting flux that flows along the background magnetic field, the wave Poynting flux, S, was projected onto the background magnetic field, B(S = S ·B/∣B∣). To reduce the effect of standing waves, which change their Poynting flux direction periodically (and, thus, do not contribute to a net energy transfer), we averaged the Poynting flux over 30-s intervals. All of the Poynting flux values were scaled along converging magnetic field lines to ionospheric altitudes (∼100 km) under the assumption of dissipationless propagation for the sake of comparing in situ values with ionospheric values (16). The database was then binned (2° × 0.75 hours per bin) according to magnetic latitude and local time. For each bin, two values were calculated: the average of all positive Poynting flux values (downward-directed Poynting flux) and the average of all negative values (upward- directed Poynting flux). The distribution of the downward-directed Poynting flux (Fig. 1C) delineates the auroral oval. Two regions of enhanced intensity occur at about 21:00 to 00:00 and at about 15:00 local time. The general location and intensity distribution of this high-altitude wave Poynting flux is very similar to the global auroral luminosity (Fig. 1B). Both ovals are displaced equally far (several degrees) antisunward from the magnetic north pole, and the two brightest regions in Fig. 1B nearly coincide with the two brightest regions in Fig. 1C. This similarity suggests a correlation between the global energy flow at Polar's altitude and the auroral oval in the ionosphere. In contrast, very little wave Poynting flux is flowing away from the ionosphere (Fig. 1D), which implies that the downward-directed wave Poynting flux (Fig. 1C) is not reflected back from the ionosphere but must be dissipated below the spacecraft's altitude, presumably in the auroral acceleration region.

Figure 2

Sketch of Polar's orbit and the two contributions of Poynting flux flowing along magnetic field lines into the polar region. Three distinct regions exist above the polar region and extend out into space: cusp, polar cap, and plasma sheet. The Polar spacecraft crosses these regions on an elliptical, polar orbit at altitudes between 25,000 and 38,000 km in the Northern Hemisphere. During the course of 1 year, the orbital plane precesses by 360°. The Poynting flux is carried by static fields (convection electric fields and magnetic fields associated with FACs) and Alfvén waves. It is mostly dissipated by Joule heating in the ionosphere and particle acceleration in the auroral acceleration region. The in situ wave Poynting flux measured by Polar delineates the statistical location of auroras.

The wave Poynting flux at high altitude (Fig. 1C) can account for about 30 to 35% of the energy flux required to cause the global ionospheric auroral luminosity (Fig. 1B). This value is an estimate, because the time periods used to generate the two distributions are not the same and auroral activity varies throughout the year. Nevertheless, this result suggests that the wave Poynting flux is a substantial contributor of energy flux for auroral processes. Our data (Fig. 1, C and D) show the global morphology of wave Poynting flux averaged over many spacecraft passes, which include quiet (no aurora) and active (aurora) times. Similarly, the distribution derived from UV images (Fig. 1B) shows the average distribution. Therefore, the energy fluxes shown in all three figures do not show the instantaneous energy flux associated with an auroral display. To determine whether the energy flux for individual events observed by Polar is itself sufficient to power auroral emissions, we searched for all the events in the database that would have a Poynting flux larger than 5 ergs cm−2s−1 when scaled to 100-km altitude (i.e., data points were not averaged over the bin size, as was done for Fig. 1, C and D). We chose 5 ergs cm−2 s−1 as the threshold because the weakest electron beams that can produce visible auroral emissions have energy fluxes of ∼1 ergs cm−2s−1 at ionospheric altitudes (17). Thus, each such event would carry a sufficient Poynting flux to create auroral emissions. We found that all events are located approximately along the auroral oval and more events cluster in the postnoon and midnight sectors (Fig. 3), a pattern that is similar to Fig. 1C. This result shows that individual events distributed along the entire auroral oval carry sufficient energy flux to power ionospheric auroral emissions. In addition, many events had larger values (>30 ergs cm−2 s−1) of Poynting flux that can account for intense auroras as well.

Figure 3

Distribution of events with Poynting flux larger than 5 ergs cm−2 s−1 (mapped along converging magnetic field lines into the ionosphere, ∼100 km) recorded by Polar versus latitude and local time. The events approximately delineate the statistical location of auroras. Two long traces of large Poynting flux events (at about 18:20 and about 04:30 local time) occurred on 10 January 1997 and 3 August 1997. During both orbits, geomagnetic storms prevailed. Geomagnetic storms are periods of enhanced energy transfer over an extended period of time (from one to many days) compared with 30 min to 3 hours for auroral substorms. Polar recorded enhanced Poynting flux throughout the plasma sheet on these days, which accounts for the long traces.

Large-scale FACs have been considered the main carrier of the electromagnetic energy that powers auroral acceleration processes. Our observations modify the view that FACs are the only energy carrier globally providing electromagnetic energy to the auroral region. We found that Alfvén waves, which occur globally, play an important role in the creation of the aurora. Previous studies have reported wave Poynting flux in association with auroral phenomena in isolated events in different space regions: the inner edge of the plasma sheet (18), the cusp (19), the central plasma sheet (20, 21), and the plasma sheet boundary layer (13, 14). It has also been shown for about 20 to 25 events that the observed high-altitude wave Poynting flux was sufficient to power the magnetically conjugate auroral emissions (13, 22). Our statistical study indicates that these case studies are not isolated occurrences. Most important, we found that the global distribution of auroral luminosity is closely related to the global distribution of high-altitude Alfvén waves. This correlation shows that the ionosphere and the magnetosphere are electrodynamically coupled via Alfvén waves over the entire auroral region. Furthermore, the magnitude and the flow direction of the wave Poynting flux that is carried by the Alfvén waves suggest that this wave Poynting flux is a major energy contributor for auroral acceleration processes and, ultimately, for auroral emissions along the entire auroral oval. The globally occurring Alfvén waves thus provide an important link in the chain of energy transfer processes from the magnetosphereto the aurora. To increase our understanding of energy transfer processes in the magnetosphere, the next step is to compare the wave Poynting flux distribution reported here with corresponding global distributions of particle energy flux and Poynting flux associated with large-scale FACs at the same altitude. Such a comparison has only been made for one large-amplitude Poynting flux event. It was shown (23) that the enhanced wave Poynting flux coincided with a slightly smaller enhancement in the particle energy flux and that it was one to two orders of magnitude larger than the electromagnetic energy flux associated with local FACs.

  • * Present address: Centre d'Etude Spatiale des Rayonnements, Toulouse, France.

  • To whom correspondence should be addressed. E-mail: akeiling{at}ham.space.umn.edu

REFERENCES AND NOTES

View Abstract

Navigate This Article