SuperDARN is a network of HF radars (8-20 MHz) used to study the convection in the Earth's ionosphere at altitudes between 90 and 400 km and at magnetic.

Slides:



Advertisements
Similar presentations
Wave-particles interaction in radiation belt region Hanna Rothkaehl Space Research Center, PAS Bartycka 18 A Warsaw, Poland,
Advertisements

“Rates of occurrence of TIGER HF radar echo parameters sorted according to the K p index and the IMF - early results” M. L. Parkinson 1, J. C. Devlin 2,
“Simultaneous measurements of convection changes in the high-latitude day- and night- side ionosphere with the Halley and TIGER HF backscatter radars -
Earth Science Chapter 7 Atmosphere.
Generation of the transpolar potential Ramon E. Lopez Dept. of Physics UT Arlington.
Statistical study of non-reconnection plasma jets as observed by the DOUBLE STAR spacecraft E. Amata 1, S. Savin 2, D. Ambrosino 1, L. Trenchi 1, M.F.
Aim: What are some of Earth’s wind patterns? I. Winds and Pressure Belts A. Convection cell – when air circulates by rising in one place and sinking at.
E. Amata M. Candidi (1), M.F. Marcucci (1), S. Massetti (1), P. Francia (3), U. Villante (3) (1) Istituto di Fisica dello Spazio Interplanetario (IFSI),
VT SuperDARN Group2011 SuperDARN WorkshopJoseph Baker Testing the Equipotential Magnetic Field Line Assumption Using Interhemispheric.
SuperDARN interhemispheric observations of reconnection signatures: a case study. Coco, I. (1), S. Massetti (1), E. Amata (1), M. F. Marcucci (1), and.
Anti-parallel versus Component Reconnection at the Magnetopause K.J. Trattner Lockheed Martin Advanced Technology Center Palo Alto, CA, USA and the Polar/TIMAS,
Peter Boakes 1, Steve Milan 2, Adrian Grocott 2, Mervyn Freeman 3, Gareth Chisham 3, Gary Abel 3, Benoit Hubert 4, Victor Sergeev 5 Rumi Nakamura 1, Wolfgang.
Figure 4: Overview of the geometry of the Rankin Inlet and Inuvik radar in MLT coordinates on Aug 08 th Merged vectors are shown in black. AMPERE.
Modelling the Thermosphere-Ionosphere Response to Space Weather Effects: the Problem with the Inputs Alan Aylward, George Millward, Alex Lotinga Atmospheric.
Ionospheric Convection and Field-Aligned Currents During Strong Magnetospheric Driving: A SuperDARN/AMPERE Case Study L. B. N. Clausen (1), J. B. H. Baker.
Phase Coherence on Open Field Lines Associated with FLRs Abiyu Nedie, Frances Fenrich & Robert Rankin University of Alberta Edmonton, Alberta, Canada 2011.
On the relationship between polar cap flows and the IMF W.A. Bristow, R.T. Parris, J. Spaleta, T. Theurer Geophysical Institute, University of Alaska.
State Key Laboratory of Space Weather An inter-hemisphere asymmetry of the cusp region against the geomagnetic dipole tilt Jiankui Shi Center for Space.
Reinisch_ Solar Terrestrial Relations (Cravens, Physics of Solar Systems Plasmas, Cambridge U.P.) Lecture 1- Space Environment –Matter in.
31 May 2011SuperDARN Workshop, 29 May - 3June 2011, Hanover, US 1 Short-period Doppler shift variations in the polar cap: ULF waves or something else?
& Atmospheric StudiesPhysics & Engineering Physics, University of Saskatchewan Hemispheric Comparison of Signatures of.
Tracing Geomagnetic Conjugate Points by means of Extremely Similar Interhemispheric Auroras N. Sato (1), A. Kadokura (1), Y. Ebihara (1), H. Deguchi (1),
Ionospheric Convection Response to High-Latitude Reconnection and Electrodynamics of a Split-Transpolar Aurora S. Eriksson 1, G. Provan 2, F. J. Rich 3,
What DMSP Data Tell us About the Thermosphere Response to Solar Wind Forcing Delores Knipp CU Aerospace Engineering Sciences and NCAR HAO With Assistance.
On the importance of IMF |B Y | on polar cap patch formation Qinghe Zhang 1, Beichen Zhang 1, Ruiyuan Liu 1, M. W. Dunlop 2, M. Lockwood 2, 3, J. Moen.
Radio and Space Plasma Physics Group The formation of transpolar arcs R. C. Fear and S. E. Milan University of Leicester.
SuperDARN real time products for Space Weather Ermanno Amata INAF Istituto di Fisica dello Spazio Interplanetario Roma ESWW5, Bruxelles, 20 November 2008.
Global Wind Patterns Science Lesson Objectives ► using scientific theory, describe and explain heat transfer and its consequences in both the atmosphere.
Figure 1: show a causal chain for how Joule heating occurs in the earth’s ionosphere Figure 5: Is of the same format as figure four but the left panels.
Magnetospheric ULF wave activity monitoring based on the ULF-index OLGA KOZYREVA and N. Kleimenova Institute of the Earth Physics, RAS.
Section 3: Atmospheric Circulation Objectives ◦ Explain the Coriolis effect. ◦ Describe the global patterns of air circulation, and name three global wind.
EISCAT Svalbard Radar studies of meso-scale plasma flow channels in the polar cusp ionosphere Y. Dåbakk et al.
University of Colorado 1 ; Delft University of Technology 2 ; University of Alaska 3 ; Centre National d’Etudes Spatiales 4 ; National Center for Atmospheric.
Magnetosphere-Ionosphere coupling processes reflected in
Space Science MO&DA Programs - September Page 1 SS It is known that the aurora is created by intense electron beams which impact the upper atmosphere.
Localized Thermospheric Energy Deposition Observed by DMSP Spacecraft D. J. Knipp 1,2, 1 Unversity of Colorado, Boulder, CO, USA 2 High Altitude Observatory,
Distributed Radar Networks Ray Greenwald JHU/APL.
Introduction to Space Weather Jie Zhang CSI 662 / PHYS 660 Spring, 2012 Copyright © Ionosphere II: Radio Waves April 19, 2012.
Preview Section 1 Characteristics of the Atmosphere
Ionospheric Current and Aurora CSI 662 / ASTR 769 Lect. 12 Spring 2007 April 24, 2007 References: Prolss: Chap , P (main) Tascione: Chap.
Response of the Magnetosphere and Ionosphere to Solar Wind Dynamic Pressure Pulse KYUNG SUN PARK 1, TATSUKI OGINO 2, and DAE-YOUNG LEE 3 1 School of Space.
Coupling of the Magnetosphere and Ionosphere by Alfvén Waves at High and Mid-Latitudes Bob Lysak, Yan Song, University of Minnesota, MN, USA Murray Sciffer,
Intense Poynting flux at very high latitudes during magnetic storms: GITM simulation results Yue Deng 1 Cheng Sheng 1, Manqi Shi 1, Yanshi Huang 2, Cheryl.
University of Saskatchewan PHYSICS AND ENGINEERING PHYSICS Spectral widths of F-region PolarDARN echoes, a statistical assessment A.V. Koustov, S. Toderian.
Testing the Equipotential Magnetic Field Line Assumption Using SuperDARN Measurements and the Cluster Electron Drift Instrument (EDI) Joseph B. H. Baker.
Ionospheric Convection during an extended period of Northward IMF
Cluster and SuperDARN observations during a positive B y period D. Ambrosino, E. Amata, M.F. Marcucci, I. Coco Istituto di Fisica dello Spazio Interplanetario,
New Science Opportunities with a Mid-Latitude SuperDARN Radar Raymond A. Greenwald Johns Hopkins University Applied Physics Laboratory.
© Research Section for Plasma and Space Physics UNIVERSITY OF OSLO Daytime Aurora Jøran Moen.
SuperDARN:Looking ahead to RBSP Jim Wild Physics Department, Lancaster University, UK Tim Yeoman & Robert Fear Department of Physics & Astronomy, University.
Mike Ruohoniemi 2012VT SuperDARN Remote Sensing of the Ionosphere and Earth’s Surface with HF Radar J. Michael Ruohoniemi and Joseph Baker.
Energy inputs from Magnetosphere to the Ionosphere/Thermosphere ASP research review Yue Deng April 12 nd, 2007.
Postmidnight ionospheric trough in summer and link to solar wind: how, when and why? Mirela Voiculescu (1), T. Nygrén (2), A. Aikio(2), H. Vanhamäki (2)
VT SuperDARN Group Joseph Baker Ground-Based Observations of the Plasmapause Boundary Layer (PBL) Region with.
Baker Tech SuperDARN Large-Scale Observations of the Sub-Auroral Polarization Stream (SAPS) From.
near-Space Environment
SuperDARN data and ionosphere modelling perspectives at IRAP
Challenges The topological status of the magnetosphere: open or closed? Driver(s) of ionospheric sunward flow Source(s) of NBZ currents Key problem: are.
Visit for more Learning Resources
Paul Song Center for Atmospheric Research
The Ionosphere and Thermosphere GEM 2013 Student Tutorial
High-latitude Neutral Density Maxima
Night-side effects on the plasma convection in the polar ionosphere due to a Sudden Impulse (SI) of solar wind dynamic pressure Coco, I.(1,2,3); Amata,
Evidence for Dayside Interhemispheric Field-Aligned Currents During Strong IMF By Conditions Seen by SuperDARN Radars Joseph B.H. Baker, Bharat Kunduri.
The ionosphere is much more structured and variable than ever predicted. Solar Driven Model Since 2000, we have seen more, very clear evidence that the.
The Physics of Space Plasmas
Subauroral heliosphere-geosphere coupling during November 2004 ionospheric storms: F2-region, North-East Asia Chelpanov M. A., Zolotukhina N.A. Institute.
Title: Atmosphere in Motion; Wind Bands Page #: 75 Date: 2/25/2013
Fig. 5 Morphology of in situ peak Poynting flux during storm periods.
by Andreas Keiling, Scott Thaller, John Wygant, and John Dombeck
Presentation transcript:

SuperDARN is a network of HF radars (8-20 MHz) used to study the convection in the Earth's ionosphere at altitudes between 90 and 400 km and at magnetic latitudes between 60° and 90° (each radar has 16 azimuthal beams and 75 ranges). SuperDARN developed in the last 12 years. and 7 in the southern hemisphere. At present, 10 radars operate in the northern hemisphere

Temporal Response of Ionospheric Convection to Solar Wind Transitions SuperDARN Science highlights. Imaging High-Latitude Ionospheric Convection Determination of Global Poynting Flux and Joule Heating Global Detection of Atmospheric Gravity Waves and Planetary Waves Measurement of Cross-Polar-Cap Potential Drop Magnetic Reconnection Science Flow Transients and Variability Conjugate Studies of Ionospheric and Magnetospheric Convection Ionospheric Plasma Instabilities ULF Pulsations Magnetic Conjugacy

B z < 0 B z > 0 Magnetic reconnection in the magnetosphere. 12 MLT

Imaging High-Latitude Ionospheric Convection Spherical harmonics JHUAPL model for CPC potential 12 MLT

Counter-rotating convection cells in the dayside high-latitude polar cap [From Huang et al., 2000]. These patterns had been postulated to occur under northward IMF conditions. SuperDARN was the first instrument network to confirm their existence. Imaging High-Latitude Ionospheric Convection

Near midnight MLT. Equinox Equatorward moving bands of scatter Low spectral width well defined speeds. Coincident in UT and magnetic latitude. Several cases found. Origin unknown.

SuperDARN potential maps Istituto di Fisica dello Spazio Interplanetario, INAF, Roma.

SuperDARN potential maps

Istituto di Fisica dello Spazio Interplanetario, INAF, Roma. SuperDARN potential maps