Consulting
Consulting
schnaiTEC can share their experience and know-how in the following fields:
-
Development of scientific instrumentation that is based on optical methods
-
Instrumentation for laboratory research, e.g. cloud chamber instrumentation
-
Instrumentation for field research, e.g. airborne instruments
-
-
Particle light scattering simulations
-
Expected signal of optical particle instruments, e.g. light scattering spectrometers
-
Mie calculations for spherical particles
-
Multiple-sphere clusters, e.g. absorption and light scattering by fractal soot particles
-
T-matrix calculations for spheroidal particles
-
Geometric optics for ice crystals
-
-
Image analysis
-
Processing of particle micrographs, e.g. from bright-field optical microscopy
-
Extraction of microphysical properties from particle images
-
Contact us for more information!
schnaiTEC can share their experience and know-how in the following fields:
-
Development of scientific instrumentation that is based on optical methods
-
Instrumentation for laboratory research, e.g. cloud chamber instrumentation
-
Instrumentation for field research, e.g. airborne instruments
-
-
Particle light scattering simulations
-
Expected signal of optical particle instruments, e.g. light scattering spectrometers
-
Mie calculations for spherical particles
-
Multiple-sphere clusters, e.g. absorption and light scattering by fractal soot particles
-
T-matrix calculations for spheroidal particles
-
Geometric optics for ice crystals
-
-
Image analysis
-
Processing of particle micrographs, e.g. from bright-field optical microscopy
-
Extraction of microphysical properties from particle images
-
Contact us for more information!
Do completely new research
Do completely new research
Eight months of PAAS-4λ deployment successfully completed
Martin Schnaiter
24.8.2022
Eight months of unattended particle light absorption measurements at the Pallas Sammaltunturi station successfully completed. So far the PAAS-4λ instrument has demonstrated excellent performance in terms of stability and reliability. This is an important step to prove the final technology readiness level in the target operational environment (TRL9).
Daily averages of the absorption coefficient in the visible spectral region are typically below 0.5 1/Mm for clean arctic background air. This corresponds to black carbon (BC) particle mass concentrations of less than 50 ng/m3. Episodes of long-range transported pollution from Central Europe and from wildfires in Eurasia are clearly distinct by absorption coefficients above 0.5 1/Mm. Interestingly, the spectral dependence of the particle absorption is rather flat and stable for pollution events from Central Europe while wildfire episodes seem to have a steeper wavelength dependence indicating contributions from Brown Carbon (BrC) in these plumes.