Coordinated Measurements of Transient Luminous Events SPRITES from the Space Shuttle and Ground Stat - PowerPoint PPT Presentation

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Coordinated Measurements of Transient Luminous Events SPRITES from the Space Shuttle and Ground Stat

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Coordinated Measurements of Transient Luminous Events ... Zev Levin, Yoav Yair, Colin Price, Peter Israelevich, Adam Devir, Baruch Ziv, Joachim Joseph, ... – PowerPoint PPT presentation

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Title: Coordinated Measurements of Transient Luminous Events SPRITES from the Space Shuttle and Ground Stat


1
Coordinated Measurements of Transient
Luminous Events - SPRITES from the Space
Shuttle and Ground Stations during MEIDEX
  • Zev Levin, Yoav Yair, Colin Price,
  • Peter Israelevich, Adam Devir,
  • Baruch Ziv, Joachim Joseph,
  • Yuri Mekler, Meir Moalem

2
The Global Circuit 1
Ionosphere
Precipitation
Earth
Fair weather field
250kV
  • The atmosphere is like a spherical capacitor with
    the outside charged positively and the inside
    (ground) charge negatively.
  • The potential difference between these two
    electrodes is about 250,000 Volts. Its average
    value remains fairly constant with time.

3
The Global Circuit 2
  • Although the atmosphere is a poor conductor an
    electrical current is continuously discharging
    the capacitor.
  • The electric field starts at about 120 V/M near
    the ground and decreases exponentially with
    height. At heights above clouds it is normally as
    low as 1 mV/m.
  • Lightning flashes are the generators that
    maintain the atmospheric electric field.

4
The Charge Distribution in Thunderclouds
5
Global Lightning Distribution for June 1999
6
Lightning
  • Lightning are much more common over land than
    over the sea.
  • Most lightning strokes are inter cloud. They
    simply discharge the charge centers that have
    been developed.
  • About 40 of all flashes are cloud to ground and
    most of these are negative bringing negative
    charge to ground.
  • About 10-20 of the flashes to ground are
    positive positive charge to ground.
  • The reason for these positive flashes is not yet
    known, but its frequency of occurrence is
    related to either the tilt of the clouds
    and/or to the size of the storms (large mesoscale
    convective systems).

7
The ratio N PGF/NGF varies during the lifetime
of the storm. Sometimes N gt 1.
N0.3
Early part of the storm
8
N0.52
Mature part of the storm
9
N6.25
Decaying part of the storm
10
SPRITES
  • About 10 years ago, the Transient Luminous
    Emissions were first discovered and were given
    the names of Sprites (most common), Blue Jets and
    Elves.

11
Sprites etc.
12
Transient Luminous Events
13
Red Sprites
  • Usually associated with very strong PGFs (peak
    current gt 130kA, 77 probability).
  • Stratiform region of MCS
  • Initiate at 70-75 km, moves both up and down.
  • Terminal height 85-90 km. Lifetime few msec.
    500 kR.
  • Speed 107 m/sec.
  • Illuminated Volume gt 104 km3.

14
Blue Jets
  • Not associated with PGFs, but occur in T-storms
    with intense NGF hail strong updrafts
  • Terminal altitude 32-43 km, Speed 11224 km/sec.
    Ionized N2
  • Not so rare, but hard to observe from the ground.
    10 MR

15
Sprites from Space
17 events from payload-Bay cameras during the MLE
(Boeck et al, 1995) STS 34 (1989), STS 32
(1990), STS 31 (1990), STS 41 (1990)STS 43
(1991), STS 48 (1991), STS 46 (1991)
16
Sprites observations with the MEIDEX cameras
  • Primarily with the 665nm filter for Red Sprites
    and Elves and with the 380 and 470nm filters to
    record Blue Jets.
  • Continuous recording of the Earths limb from the
    direction of the dusk terminator towards the
    night side, preferably before midnight local time
    at the observed area.
  • The Astronaut will use the SEKAI LL-Video color
    camera to look for major thunderstorm centers.

17
On-Orbit Operations and Ground Stations for
Sprite Measurements
Chile
18
Configuration for Viewing Sprites
19
Forecast of Sprites --forecast of regions of
strong convection and cloud top temp. of around
70C
20
MEIDEX-Sprite ROIs
21
The atmosphere as a wave guide
22
Ground Observations Israel
  • During the 16-day flight, two field sites in the
    Negev Desert in Israel will be used to collect
    ELF (SR) and VLF data related to sprite activity.
  • Both are operated by TAU.

23
Global Ground Observations
  • Optical measurements Japan (Osaka, Sendai),
    Taiwan (Taipei), USA YRFS, Stanford (?)
  • ELF measurements Long Island, Hungary,
    Antarctica
  • VLF network Germany, S.Africa, Chile,
    California, New-Zealand, Japan USA (Duke)
  • Lightning Location Systems Japan, Brazil, NLDN

24
Summary
  • Unique opportunity for global coverage
  • Multi-sensor measurements
  • The first ever spectral Calibrated measurements
    from space
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