Scheduling the Upper Atmospheric Facilities for World Day Coordinated Experiments
(Final Report)
Convener:
Wes Swartz (wes@ece.cornell.edu)
2005 Thursday 30 June 0400 - 0600 PM
Establishing "World Day" (WD) schedules to coordinate experiments at all the incoherent scatter radars and
associated instrumentation is one of the activities of the URSI Incoherent Scatter Working Group (ISWG).
The CEDAR meeting provided a timely forum for working on the schedule for the following year. The link to the
current schedule (as well as those for previous years) may be found at:
Objectives of the current year were reviewed and included the following:
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LTCS (Lower Thermosphere Coupling Study): Tidal Variability
With a number of years of ISR data from the lower thermosphere under the LTCS program, the basic structure
of tides seems to be relatively well understood with the most striking single property of atmospheric
tides being the very large variability of tidal amplitudes. Possible sources for this variability include
non-migrating tides, planetary waves, and geomagnetic influences. Now efforts must focus on the sources of this
tidal variability.
LTCS Contact: Larisa P. Goncharenko
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M-I Coupling (Magnetosphere-Ionosphere Coupling): Storm and Substorm Effects on the
Middle- and Low-Latitude Ionosphere
Magnetic storms and substorms are fundamental disturbances in the magnetosphere and can significantly
increase, or decrease ionospheric electron densities. Outstanding questions concerning the effects of
storms and substorms on the middle- and low-latitude ionosphere include
- How much do magnetic storms affect the low-latitude ionosphere?
- How significant are the changes in TEC and F-region densities that result from penetrating
magnetospheric substorm electric fields?
- How are changes in the low-latitude ionosphere coupled with the variations in the magnetosphere and
solar wind?
- What processes are responsible for the ionospheric electron density disturbances?
- How do the disturbances in the electron density profiles and TEC vary with longitude and latitude?
- What are the atmospheric and dynamic processes at low latitudes during magnetic storms?
MI-Coupling Contact: Chaosong Huang
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GPS-Radar (Global Plasma Structuring-Radar Experiment): Thermal plasma coupling between
low, mid, and high latitudes
Recent multi-technique observations have shown that the equatorial ionosphere and inner plasmasphere
are coupled from low to auroral latitudes by electric fields and plumes of storm enhanced electron
densities which feed tongues of ionization into the polar caps. This global mechanism carries
low-latitude dayside plasma into the nightside auroral ionosphere and can cause significant space weather
effects during major magnetic storms, as well as during less-disturbed conditions. Wide latitude
coverage is used to study these events and include
- Measurements of plasma perturbations due to inner magnetospheric electric fields (Sonderstrom,
EISCAT, Millstone Hill, SuperDARN)
- Topside observations (Arecibo and Jicamarca)
- Mid-latitude profiles (Kharkov and Irkutsk)
- Global GPS TEC imagery
- Particle precipitation and electric fields (DMSP)
- Plasmaspheric imagery (IMAGE)
GPS-Radar Contact: John Foster
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Meteoric Ions (Global observations of ionization created by the Perseids and Leonids)
During the 2002 Leonids, the EISCAT UHF radar detected enhanced ionization between 90 and 180 km
with densities up to 3.3 x 10^11 m-3. Systematic studies of these enhancements are planned during
three-day runs for the Perseids (starting on August 10 at 0900 UT) and for the Leonids (starting on
November 17 at 1600 UT) are suggested.
Meteoric Ions Contact: Ingemar Haggstrom
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Synoptic
Synoptic experiments are intended to emphasize wide coverage of the F-region, with some augmented
coverage of the topside or E-region to fill in areas of the databases that have relatively little data.
Synoptic Contact: Wes Swartz
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C/NOFS (Communications / Navigation Outage Forecasting System)
The primary purpose of C/NOFS is to forecast the presence of ionospheric irregularities that adversely
impact communication and navigation systems. The satellite launch has been delayed until next year and
the UAF component will be rescheduled.
C/NOFS Contacts: Odile de La Bedaujardiere, David Hysell, Wes Swartz
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CPEA (Coupling Processes in the Equatorial Atmosphere)
This is an initiative for studying the coupling of dynamical coupling processes in the equatorial atmosphere
from the troposphere up through the thermosphere and ionosphere centered around the Indonesian
Equatorial Atmospheric Radar (EAR). The original plans have been refocused and the UAF component deleted
for this year.
CPEA Contacts: Shoichiro Fukao, Project Leader, Sunanda Basu, Janet Kozyra
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MST (Studies of the Mesosphere, Stratosphere, and Troposphere)
Coordinated D- and E-region campaigns focus the ISR's and supporting instrument capabilities on the lower
altitudes. JRO uses a high resolution MST mode, while Arecibo uses a dual mode of D- and E-region drifts
(with accompanying lidar & imaging measurements). The main interest is in obtaining gravity wave
momentum fluxes. Data for these studies may also be obtained during the LTCS World Day periods.
MST Contacts: Gerald Lehmacher, Erhan Kudeki, Jorge L. Chau
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World Month (Searching for Long Period Effects)
Studies of long period waves and tides require measurements over many sequential days. The 30-day run
in September should provide an unprecedented data set for such studies. Not all of the ISRs will provide
data for the full 30-day period and only a "best effort" is asked for. The Arecibo Observatory is to observe
for about 10 of the 30 days. Labor or power saving modes were to be adapted at some sites.
WM Contacts: Larisa P. Goncharenko, and Wes Swartz
The "World Month" scheduled for September 2005 was discussed with some fervor and anticipated by many
as a prime resource of data for very long period waves of the LTCS program and for driving and verifying
assimilative models of the upper atmosphere and ionosphere. Although a concern was expressed that
having a second "World Month" would limit the number of separate World Days that could be scattered throughout
out the calendar year, and that perhaps a second should not be scheduled in 2006, the consensus from the
modeling community has consistently been that short runs just are not useful to them. We were informed
that the ESR would run for a month in 2006 even independently of the other UAFs if necessary. After concerns
were expressed about the resources required for that many days, Bob Robinson of the Facilities Program
at NSF said that some accommodation should be possible and that a lack of incremental resources
should not be the reason for not doing the long runs. It was decided to again schedule the second "World
Month" in the March-April time frame and do so on a "best effort" within available resources at each of the
UAFs.
Two other World Day periods were placed on the 2006 schedule available at the above URL.