Cambridge 2004
1 / 21

Cambridge 2004 - PowerPoint PPT Presentation

  • Uploaded on

Cambridge 2004. Wolfgang Baumjohann IWF/ÖAW Graz, Austria With help from: R. Nakamura, A. Runov, Y. Asano & V.A. Sergeev. Magnetotail Transport and Substorms. Sun-Earth Connection. Standard Model. Magnetospheric convection is driven by solar wind.

I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
Download Presentation

PowerPoint Slideshow about 'Cambridge 2004' - isaiah

An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
Cambridge 2004
Cambridge 2004

Wolfgang Baumjohann

IWF/ÖAW Graz, Austria

With help from: R. Nakamura, A. Runov, Y. Asano & V.A. Sergeev

Magnetotail Transport and Substorms

Standard model
Standard Model

Magnetospheric convection is driven by solar wind.

  • Merging of dipolar field with southward IMF at MP

  • Open field lines move tailward over polar cap

  • Reconnection to dipolar & SW field lines in tail

  • Closed field lines move sunward in equatorial plane

Inner magnetosphere
Inner Magnetosphere

In inner magnetosphere quasi-static convection:

  • GEOS-2 Electron Beam Experiment measures "shift" of gyration circle of 1 keV electrons by electrical drift

  • Southward IMF: convection towards magnetopause

  • Northward IMF: only weak plasma flow

  • Mean values for southward IMF correspond to standard model

Lobe convection 1
Lobe Convection - 1

  • Cluster/EDI gives first direct measurements of convection in lobe (measuring electric field in extremely thin plasma over polar cap)

  • Dependence of convection velocity toward plasma sheet on polarity of IMF BZ clearly visible

  • Cluster Electron Drift Instrument (EDI) uses same principle as GEOS-2 Electron Beam Experiment

Lobe convection 2
Lobe Convection - 2

  • EDI data also show IMF BY effect

  • Shear flow in Y-Z plane


Pressure Catastrophe:

  • Adiabatic convection: d/dt PV g = 0, V = ò B-1ds

  • Flux tube volume strongly decreases toward Earth

  • Convection stops to avoid pressure catastrophe

Tail observations with IMP show:

  • Fast Earthward flow for 25-40 RE

  • Closer in, convection severely slows down

Near earth neutral line
Near-Earth Neutral Line

  • Tail-like field geometry weakens pressure gradient

  • Reconnection leads to smaller flux tube volume

  • Earthward convection by bursty bulk flows

  • Reversal of fast flow direction observed by Geotail

  • Near-Earth neutral line located ~25 RE

Flow curv b reversal
Flow & Curv B Reversal

  • Magnetic field components in Cluster barycentre: 4 current sheet traversals

  • Field line curvature:

    curv B = (b.grad)b

  • Flow and field line curvature reversal

  • X-line moves tailward over Cluster

Reconnection hall effect
Reconnection & Hall Effect

  • Ion Flow Reversal during 4 neutral sheet crossings

  • X-line moves tailward over Cluster

  • 500 km thin CS around X-line

  • bifurcated current sheet on both sides

  • Hall effect (By) during ‘outer’ crossings shows ion decoupling

Electron hall current
Electron Hall Current

  • Cluster 2003 tail passes can resolve fine structure of currents

  • JY shows very thin current sheet (triple peaks?)

  • JX consistent with electron Hall current in ion diffusion region

Currents at psbl and x line
Currents at PSBL and X-line

  • Strong flow shear (N-S electric field) and thin field aligned current layer (1500 km) during a substorm

  • Consequence of Hall-effects in reconnection region and closure of the Hall-electric current

Ion diffusion region

Braking dipolarization
Braking & Dipolarization

  • Intermittent high-speed Earthward flow bursts (~500 km/s)

  • Bursty fast flows accompanied by dipolarization

  • Fast flow braked near 10 RE by dipolar field

  • More dipolar flux added by flow

  • Pressure gradients lead to current wedge and aurora

Aurora electrojet
Aurora & Electrojet

Flow braking and flow shear generate:

  • Substorm electrojet (adds to convection electrojet)

  • Aurora (in upward field-aligned current region electrons are accelerated downward)

Flow channel width
Flow Channel Width

  • Cluster gives direct estimate of spatial scale of bursty bulk flows

  • Vertical: 1.5-2 RE, Azimuthal: 2-3 RE

  • Sharper gradient on duskside flank

Aurora and bursty bulk flow
Aurora and Bursty Bulk Flow

  • Isolated flow burstswith E>2mV/m (Geotail)alwayscorrespond toauroral activations(Polar).

  • Auroral activationsnear foot pointof satellite startwithin 1 minofflow burst onset.

Structure of flow bursts
Structure of Flow Bursts

Spatial scale of flows

Small expansion, pseudo-breakup 1.4 MLT  (4-5 RE)

Auroral streamer (N-S aurora) 0.7 MLT  (3-4 RE)

  • Flow bursts are centered 0.4 MLT east of aurora

Flow bursts and fac
Flow Bursts and FAC

  • Aurora corresponds to upward FAC in bubble model

  • Scale size consistent with ionospheric observations

Substorm recovery
Substorm Recovery

  • 45 min after onset dipolarization front meets neutral line

  • No reconnection in dipolar field; recovery phase begins

  • Neutral line retreating tailward

Fast flows transport dipolar field inward:

Summary scenario
Summary Scenario

  • Plasma energy dominant outside of 25 REFlow uninhibited

  • Magnetic energy increases near 20-25 REPending pressure catastrophe leads to NENL

  • Magnetic field dominant inside 15 REDipolar field brakes BBF: current wedge & aurora are generated

  • Dipolarization front travels downtail and meets NENL

     near-Earth reconnection stops