Title: Incoherent Scatter Radars Current Status and Future Plans
1Incoherent Scatter RadarsCurrent Status and
Future Plans
- Ian McCrea
- Space Science and Technology Department
- Rutherford Appleton Laboratory
- Chilton, Oxfordshire OX11 0QX
- United Kingdom
i.w.mccrea_at_rl.ac.uk
2An Idealised Radar System
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4ISR coverage at 500km
- EISCAT Svalbard Radar
- EISCAT UHF
- Poker Flat
- Resolute Bay
- Sondrestrom
- Millstone Hill
- Arecibo
- Jicamarca
- ALTAIR
- MU
- EISCAT VHF
- Kharkov
- Irkutsk
Courtesy Craig Heinselman, SRI
5EISCAT UHF VHF
6ISR Science Topics Understanding the Solar Wind
- AIMS
- Find the factors determining structure and
evolution with distance - Study transfer of energy between scale sizes in
solar wind - Study terrestrial response to fast solar wind
streams, CIRs, CMEs etc - METHOD
- Long-baseline observations e.g. EISCAT and MERLIN
- Opportunistic observations of solar wind events
arriving at Earth - Coordination with ground (e.g. GLORIA) space
(e.g. THEMIS) instruments
7ISR Science Topics Magnetosphere-Ionosphere
Coupling
- AIMS
- Understand the location and timing of substorm
initiation. - Understand extent of plasma loss to magnetosphere
- Test hypothesis of magnetic reconnection for
various IMF - Predict effects on ionospheric structure
- METHOD
- Coordination with Cluster, Double Star and THEMIS
space missions. - Coordination with THEMIS and SuperDARN
ground-based networks.
8ISR Science Topics Fundamental Plasma Physics
- AIMS
- Study particle acceleration within the ionosphere
- Probe the energy transfer between particles and
waves (and vice versa) - Study generation and effects of non-linear plasma
instability - Explain the structure of heater-stimulated
emissions - Study magnetospheric dynamics via artificial
striations. - METHOD
- Coordination with SPEAR, HAARP and space missions
(e.g. FAST). - Coordination with SuperDARN HF radar network.
9ISR Science Topics Auroral Physics
- AIMS
- Understand how aurora are generated and evolve.
- Understand small-scale structure and
electrodynamics. - Study plasma physics in aurora (e.g. NEIALs).
- Study the relationship between proton and
electron aurora. - Study meso-scale ion-neutral coupling.
- METHOD
- Coordination with all kinds of optical imagers
- Use of multi-wavelength/multi-scale data
- Sub-beamwidth interferometry
10ISR Science Topics Ionosphere-Atmosphere Coupling
- AIM
- Study vertical coupling of energy from upper to
lower atmosphere - Understand role of upper atmosphere in long-term
global change - Understand effects of long-term change on the
upper atmosphere - Study how upper atmosphere phenomena couple to
sub-mesopause heights. - Quantify low frequency oscillations (planetary
waves and tides). - Study vertical coupling and wave ducting in the
high-latitude mesosphere and lower thermosphere
and their dependence on solar variability. - METHOD
- Coordination with ground-based meteor radar
network and spacecraft instruments (e.g. TIMED.
AIM)
11ISR Science Topics Micrometeoroids and Solar
System Formation
- AIM
- Resolve source of meteor streams, i.e.
differentiate between solar system and
extra-solar system populations. - Study meteor smoke as source of condensation
nuclei for mesopause dust/ice layers (e.g. PMSE). - Understand how meteor dust phenomena respond to
global change - METHOD
- Synoptic observations at various
seasons/locations to determine MIF
12ISR Science Topics Applications
- AIMS
- Provide input and test data for ionospheric
modelling. - Test and refine communications prediction models
- Monitor the global space debris environment
- METHOD
- Synoptic observations at various
seasons/locations to determine MIF
13The Competition US AMISRs
14Europes Answer EISCAT-3D
15How is EISCAT_3D different, and why do we need
it?
EISCAT_3D will give accurate, large-scale, three
dimensional measurements of the ionosphere and
atmosphere for the first time and much else
besides EISCAT_3D will give us unprecedented
temporal and spatial information about the plasma
environment essential to understanding crucial
and societally relevant problems in the geospace
environment, in space weather, and in the global
energy budget and related climate change
16Test array
96 elements
17Module
The module (or sub-array) is the point where
the data is beam-formed In fact, we shall
beam-form rows first, and then beam form the
columns This keeps each beam-former managable
(24 inputs) The compromise is a square module
576 elements
18Central site
The central site will comprise 32 modules Each
module becomes an interferometric
element Packing arrangement to be determined!
13824 elements
19Multi-site, multi-beam, multi-static
- 5-10 electronically steered beams per site
- Near and far receiver sites (150, 300km),
selected for the sky view - near sites are too close for good tri-statics
at high altitudes - far sites cant see low altitude
- Note that Tx site also has receive ability
E-W
N-S
20Proposed locations
- Four Rx-only sites (Examples shown here)
- One dual-Tx/Rx site (Tromsø)
- N-S and E-W lines
- Uniform spacing
- 150 and300 km
21What are the next steps ?
- Next-generation ISRs represent large strategic
investments - Only possible with wide multi-national
collaboration - EU already funds EISCAT-3D design study under FP6
- Design study ends May 2009
- Bidding for build money 2010-2011
- EISCAT-3D build will require collaboration
between national councils (RCs) and
multi-national organisations (e.g. EU Framework
Programmes) - Hence importance of recognition by Roadmap
exercises such as ESFRI and AstroNet
22Summary
- ISRs are the most powerful instruments for
studies of the geospace environment - Science topics range from solar wind, to plasma
physics, to global change. - Significant applications benefits
- Europe already has a world-leading community (cf
EISCAT) and the state-of-the-art design for the
next generation radar (cf EISCAT-3D) - We have the potential (and the plan) to build and
exploit the best atmospheric radar in the world
hence our desire to be included in the
infrastructure roadmaps
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