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PINE - Portable Ice Nucleation Experiment
Instrument

Developed in Cooporation with:

Developed in collaboration with:
KIT & University of Leeds

PINE - Accurate Measurement of INP Concentration

Ice nucleating particles (INP) are the source for primary ice formation in clouds, hence their concentration has a critical impact on the temporal and spatial distribution of precipitation as well as a major impact on climate. PINE enables the accurate measurement of INP concentration, thus providing researchers and meteorologists with a unique and valuable insight on the temporal evolution of INP. Alternative technologies do not offer minimal user input automation or the sensitivity to the huge range of atmospheric INP concentrations over a broad temperature range at high time resolution and at conditions relevant for a range of clouds types. In addition, PINE provides information on the overall aerosol concentration.

Applications

  • Ice nucleating particle concentration measurement for atmospheric and climatic observation
  • Cloud physics research

PINE:

the first instrument to automatically measure long-term series of INP concentrations at high sensitivity, time resolution and in a wide range of temperatures.

How it works
 

The core element of PINE is an air tight vessel, which can be cooled to a specified temperature.

Air is drawn into the chamber through a valve at the top, and pulled through by a pump below.

The pressure within the chamber is then reduced,

causing the temperature to drop and an adiabatic expansion to occur.

The chamber is temperature controlled, allowing for measurements to be taken between 0 and −60°C.

The frost point within the chamber is measured,

and the humidity within is controlled to ensure that frost build up does not

occur on the walls of the chamber.

Detection occurs by particles being drawn through an Optical Particle Counter (OPC) which records the particle

count and aerodynamic particle diameter.

 

Operation modes
 

Immersion mode: 

this will form a cloud within the chamber, as liquid cloud droplets form on the aerosol.

If the aerosol is an INP, the water droplet will nucleate and an ice crystal

will form and grow to much larger sizes

than water droplets.

 

Super saturation mode: 

will induce deposition freezing, water vapor will freeze directly onto aerosol particles

as the temperature within the chamber decreases.

These particles will again be distinct in size from the aerosol particles and hence detectable.

 

Downloads

Links & Downloads 

Links

Measurement activities and campaigns can be followed online at this link:

KIT - IMK-AAF - Competences - Ice Nucleating Particle Measurement - PINE INP monitoring

For detailed information about the capabilities of PINE and the science case see Möhler et al., Atmos. Meas. Tech., 14, 1143–1166, 2021.

AMT - The Portable Ice Nucleation Experiment (PINE): a new online instrument for laboratory studies and automated long-term field observations of ice-nucleating particles (copernicus.org)

Kontakt
Kontakt
Michael Gehring
Leiter Vertrieb Magnettechnik
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