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Ions and Highly Charged Particles in the Atmosphere. Thomas Leisner, Technische Universiät Ilmenau, Germany. - The global electrical circuit. - The Role of Charges in the Climate System. - Laboratory Experiments on Charged Levitated Droplets. - The Stability of Highly Charged Droplets.
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Ions and Highly Charged Particles in the Atmosphere Thomas Leisner, Technische Universiät Ilmenau, Germany - The global electrical circuit - The Role of Charges in the Climate System - Laboratory Experiments on Charged Levitated Droplets - The Stability of Highly Charged Droplets www.physik.tu-ilmenau.de/exp2/home.htm
Anthropogenic climate change ? www.physik.tu-ilmenau.de/exp2/home.htm
The 11 year sunspot cycle www.physik.tu-ilmenau.de/exp2/home.htm
Correlation between cosmic rays and cloud coverage symbols : cloud coverage solid line: cosmic rays adapted from H. Svensmark, Phys. Rev. Lett. 81, 5027, (1998) www.physik.tu-ilmenau.de/exp2/home.htm
Simplified global electrical circuit E~100V/m www.physik.tu-ilmenau.de/exp2/home.htm
A connection between solar wind activity and climate? solar wind activity magnetosph. particles cosmic rays space weather and atmospheric electricity atmospheric current density cloud space charge observed correlations cloud microphysics highly charged evaporation residues (good ice nulei) electroscavenging enhances ice formation radiation transport and cloud albedo precipitation and latent heat release atmosphericphysics atmospheric temperature and dynamics www.physik.tu-ilmenau.de/exp2/home.htm
Cloud microphysics in the laboratory feedback control W CCDarray www.physik.tu-ilmenau.de/exp2/home.htm
Experimental www.physik.tu-ilmenau.de/exp2/home.htm
Climate chamber and levitator periphery www.physik.tu-ilmenau.de/exp2/home.htm
Connection to the Raman microscope (Yobin Yvon) www.physik.tu-ilmenau.de/exp2/home.htm
Connection to the Bruker IFS 66 FTIR with IRscope II www.physik.tu-ilmenau.de/exp2/home.htm
Determination of size and index of refraction r= 19.973 µm, n=1.4087 www.physik.tu-ilmenau.de/exp2/home.htm
Freezing phase transitions in droplets www.physik.tu-ilmenau.de/exp2/home.htm
Determination of the nucleation rate www.physik.tu-ilmenau.de/exp2/home.htm
Homogeneous nucleation rates of water Journal of Chemical Physics, 111, 6521, (1999) Journal of Molecular Liquids 96-97, 153(2002) www.physik.tu-ilmenau.de/exp2/home.htm
Dynamics of highly charged droplets + + + + + + 100 kV/m - ~100 V/m 10 kV/m - - - thunderstorms are the generators of free charges in the atmosphere most of the mechanisms for charge separation include collisionsbetween droplets or ice crystals www.physik.tu-ilmenau.de/exp2/home.htm
A mechanism of charge separation in thunderstorm clouds Supercooled cloud droplet nucleation starts on surface Theromodiffusion leads to charge separation Outer shell splinters carry postitive charge upward www.physik.tu-ilmenau.de/exp2/home.htm
Is homogeneous freezing of water a surface or bulk process? www.physik.tu-ilmenau.de/exp2/home.htm
Stability of highly charged droplets The quadrupole oscillation (l=2) is unstable if the fissillity: stability is determined by interplaybetween surface energy and coulombenergy. Lord Rayleigh 1882: the frequency of mode l is given by: Though a quadrupole deformation would ultimately lead to symmetric fission, LordRayleigh did predict an asymmetric disintegration of the droplet: If ... (X>>1)... the liquid is thrown out in fine jets, whose fineness however has a limit" Philosophical Magazine, XIV, 184, (1882) (Rayleigh did not mention the X=1 case) www.physik.tu-ilmenau.de/exp2/home.htm
Coulomb- instability of an evaporating droplet www.physik.tu-ilmenau.de/exp2/home.htm
Fast microscopy of the disintegration process Photo-multiplier cw laser beam Trigger and delay unit Long working distance microscope CCDcamera Fast flashlamp injector phase function measurement Image processor www.physik.tu-ilmenau.de/exp2/home.htm
Rayleigh jets www.physik.tu-ilmenau.de/exp2/home.htm Nature, Jan. 9, 2003
100µm Fast microscopy of the disintegration process t=0 t=130µs t=135µs t=140µs t=145µs t=150µs t=152µs t=153µs t=154 µs t=155 µs t=158 µs t=160µs t=165µs t=170µs t=180µs t=200µs
Droplet geometry during instability 4.0 180 3.5 160 3.0 140 / degree 120 2.5 100 aspect ratio 2.0 80 tip angle 1.5 60 1.0 40 jet visible 0.5 20 0.0 0 140 160 180 200 220 time (µs) www.physik.tu-ilmenau.de/exp2/home.htm
Summary of Observations • initially the droplets deform ellipsoidally (X=1, l=2 is unstable) • when an aspect ratio of 3.5 is reached, two sharp tips are formed at the poles • when the tip angle drops below 60° a fine jet is emitted from each tip • the jet is emitted within 5µs, with speed up to 50m/s • each jet disintegrates into roughly 50 small daughter droplets, 1.5 µm in diameter • in one event the total charge loss is 30%, mass loss about 0.3% • the dynamics is remarkably independent of size and surface tension www.physik.tu-ilmenau.de/exp2/home.htm
Acknowledgement TU Ilmenau Klaus Hemmelmann Andreas Richter Denis Duft Rene Müller Tobias Achtzehn Collaboration: Claude Guet, CEA Paris Bernd Huber,CEA Caen Ilmenau www.physik.tu-ilmenau.de/exp2/home.htm
Simulation of the jet breakup v0= 5m/s v0= 50m/s www.physik.tu-ilmenau.de/exp2/home.htm
Light scattering from an oscillating droplet: Laser www.physik.tu-ilmenau.de/exp2/home.htm Phys. Rev. Lett., (accepted)
Correlation between solar wind activity and cosmic rays adapted from H. Svensmark, Phys. Rev. Lett. 81, 5027, (1998) www.physik.tu-ilmenau.de/exp2/home.htm
Terrestrial Effects of Space Weather Aurorae Geomagnetical storms effect communication and navigation Satellite damage Radiation hazards to flight personnel Climate effects? www.physik.tu-ilmenau.de/exp2/home.htm
A connection between solar wind activity and climate? solar wind activity magnetosph. particles cosmic rays atmospheric current density cloud space charge observed correlations highly charged evaporation residues are good ice nulei electroscavenging enhances ice formation radiation transport and cloud albedo precipitation and latent heat release atmospheric temperature and dynamics adapted from B.A. Tinsley, Space Science Review 94 , 215, (2000) www.physik.tu-ilmenau.de/exp2/home.htm
Light scattering from an oscillating droplet Laser www.physik.tu-ilmenau.de/exp2/home.htm Phys. Rev. Lett., (accepted)
The instability occurs at X=1 ! experiment theory PRL 89, 084503, 2002 www.physik.tu-ilmenau.de/exp2/home.htm
Light scattering during Coulomb instability www.physik.tu-ilmenau.de/exp2/home.htm
An anayltical shape class for spindle like objects V: spindle volume: aspect ratio: relative displacement of the generating ellipse (tippedness of the shape) with: www.physik.tu-ilmenau.de/exp2/home.htm
Droplet geometry during instability 4.0 180 3.5 160 3.0 140 / degree 120 2.5 100 aspect ratio 2.0 80 tip angle 1.5 60 1.0 40 jet visible 0.5 20 0.0 0 140 160 180 200 220 time (µs) www.physik.tu-ilmenau.de/exp2/home.htm
Open questions • How universal is the phenomenon (temperature, size, surface tension, viscosity) ? • Is this process a relevant source of atmospheric nuclei ? • Is the ejected material from the droplet surface ? • Is it possible to induce the instability below X=1 ? www.physik.tu-ilmenau.de/exp2/home.htm
Forced oscillations of incompressible viscous droplets Vibration of mode l is governded by: With the effective dynamic parameters: nach R. W. Hasse, Annals of Physics, 1975, 93, 68 www.physik.tu-ilmenau.de/exp2/home.htm
Does the solar activity cycle influence the earth climate? www.physik.tu-ilmenau.de/exp2/home.htm
Types of solar activity Solar Wind: Quiet particle stream Flare: Explosion on Sun surface Protuberance: Ejection of particles from the sun surface CME: Coronal mass ejection: Ejection of plasma from the corona www.physik.tu-ilmenau.de/exp2/home.htm
Ions and Highly Charged Particles in the Atmosphere Thomas Leisner, Technische Universiät Ilmenau, Germany - The Electrical State of the Atmosphere - The Role of Charges in the Climate System - Experiments on Single Levitated Droplets - The Stability of Highly Charged Droplets www.physik.tu-ilmenau.de/exp2/home.htm