Precision measurement.
For every cloud.
For every community.

Next-generation atmospheric instruments for climate science.

Our first instrument

The HCCNC

The Horizontal Cloud Condensation Nuclei Counter is our first instrument — a device that generates supersaturation conditions at close to those found in real clouds. Developed at ETH Zurich, it addresses a measurement limitation that has been documented in the atmospheric science literature for over two decades.

The Measurement Gap

The conditions inside the instrument are not the conditions inside a cloud.

For over two decades, atmospheric researchers measuring cloud condensation nuclei have relied on essentially one commercially available instrument design. Its operating limitations are well documented and widely acknowledged in the peer-reviewed literature.

Limitation 1

The Heating Bias

Conventional cloud condensation nuclei counters, such as the Streamwise CCNC, use a heated column to generate supersaturation. With a sample drawn at 25 °C, the column operates at roughly 30–52 °C — well above the range in which real cloud droplets form. At these elevated temperatures, semi-volatile compounds evaporate from the particles, biasing the measured cloud condensation nuclei activity.1, 2, 3

Heating bias — temperature comparison between HCCNC and conventional CCN counters
Limitation 2

The Low-Supersaturation Blind Spot

Measurements below approximately 0.13 % supersaturation — and in some cases below 0.2 % — are widely considered unreliable on instruments of this design.4, 5, 6 This operating floor makes it difficult to study highly hygroscopic particles, such as Southern Ocean aerosols (κ ≈ 0.92) larger than 100 nm, which activate well below that threshold.

Limitation 3

Supersaturation stabilization bottlenecks

Because supersaturation is established with thermoelectric heaters, which respond slowly, thermal lag occurs when stepping between supersaturation levels or beginning a new supersaturation scan cycle. Data collected during these equilibration periods — up to the first three minutes of each step (could vary with different device) — must be excluded from analysis, that means discarding crucial data.

Supersaturation stabilization bottlenecks in streamwise-gradient CCNC instruments
The Solution

The Horizontal Cloud Condensation Nuclei Counter (HCCNC).

01Feature

Dynamic Temperature Range

The HCCNC generates supersaturation across a temperature range of 4 °C to 40 °C — the first cloud condensation nuclei counter validated to operate across this range.6 Development is underway to extend this further, which would allow researchers to study how temperature governs particle activation and gas–particle partitioning across a broader envelope.

02Feature

Low-Supersaturation Capability

Precise thermal control and a residence time of up to 24 seconds allow the HCCNC to generate supersaturation levels reliably down to 0.05 %.

03Feature

Speed Without Compromise

No data is lost during the supersaturation cycle. On top of that, the supersaturation cycle resets up to seven times faster than conventional cloud condensation nuclei counters. A new "flash scan" mode sweeps 0.05 % to 0.8 % supersaturation in under a minute.

04Feature

Modular Design

Opening the HCCNC chamber takes three steps. After a long campaign, clearing residual material is as simple as opening a water bottle: open the chamber, replace the filter paper, close it. No specialist required — which saves time and cost. So you can focus on research not repairs.

Three steps to change the filter paper in the HCCNC
Side-by-side analysis: Streamwise CCNC vs HCCNC
The Technology

How the HCCNC works.

The HCCNC operates on the principle of a parallel-plate thermal-gradient diffusion chamber.

Developed through computational fluid dynamics simulations, the design optimises laminar flow stability and precise temperature regulation to achieve stable, controllable supersaturation across a wide operating range.

Since temperature gradients drive supersaturation in a cloud condensation nuclei counter, each plate is controlled precisely and independently to provide stable and direct command over the internal supersaturation.

Technology · What It Enables

New science,
made measurable.

The HCCNC's operating range opens measurement regimes that have not been accessible with instruments of the conventional streamwise design. A few examples:

Low-Temperature Capability

Köhler theory confirmation: critical supersaturation scales inversely with temperature
Variable Temperature CCN Activation Generating supersaturation between 4 °C and 40 °C opens new possibilities in temperature-dependent cloud condensation nuclei activation studies. For example, this temperature control has enabled first experimental confirmation that critical supersaturation scales inversely with temperature (Scrit ∝ 1/T) for particles of the same size and composition, consistent with Köhler theory.6
Semi-volatile bias reduction & co-condensation Lower operating temperatures reduce the evaporation of semi-volatile compounds that biases measurements on conventional instruments. They also enable the study of co-condensation, particularly at low temperatures where Henry's-law uptake and gas–particle partitioning favour the condensed phase. Because the HCCNC is highly modular, the sheath flow can be supplied as a chosen gas phase — further reducing gas–particle partitioning while the low temperature supports direct co-condensation studies.

Low-Supersaturation Capability

Low SS capability size comparison — HCCNC vs conventional instruments
Larger particle characterisation Reaching supersaturation as low as 0.05 % allows the HCCNC to characterise particles roughly twice the size accessible to conventional instruments, whose reliable limit sits near 0.13 %. Methodology & technical details (PDF)
Radiation fog measurement Radiation fog can form at supersaturation as low as 0.043 %.7 The HCCNC's low-supersaturation capability brings this regime within reach. Work is ongoing to extend the lower operating limit further.
Cloud-seeding material study Silver iodide — widely used for cloud seeding — is produced by burning flares that also contain highly hygroscopic material. On conventional instruments, this material activates at the lowest achievable supersaturation levels, making reliable characterisation difficult. The HCCNC's low-supersaturation capability allows these particles to be studied across a wider range of activation conditions.

High-Supersaturation & Dynamic Residence Time

High-supersaturation capability The current instrument is validated up to 2 % supersaturation. Development is underway to raise this ceiling alongside increased residence time, to enable the study of weakly hygroscopic particles.
Dynamic residence time Residence time can be varied from 8 to 24 seconds simply by adjusting the injector position. This makes it possible to study particle growth kinetics, including size-resolved droplet growth.
Traction

Validated by science.
Recognised by the field.

Peer-Reviewed Publication

Published in Atmospheric Measurement Techniques (EGU), 2025 — a full instrument characterisation validated against Köhler theory.6 A second publication demonstrating the HCCNC's capabilities in analysing complex organic compounds (such as levoglucosan) is currently in preparation.

Patent Filed

The patent for HCCNC has already been filed.

ETH Pioneer Fellowship

Awarded the prestigious ETH Zurich Social Impact Pioneer Fellowship to develop the instrument toward a deployable device.

Industry Recognition

An unsolicited licensing inquiry received from established industry incumbents, acknowledging the HCCNC's demonstrated performance advantage.

Active Customer Interest

Two researchers are in active discussions to purchase the instrument. Two research groups — one in Asia, one in Europe — are collaborating with us on scientific projects.

The Team

The people behind the instrument.

Meet the full team
Dr. Mayur G. Sapkal
Dr. Mayur G. Sapkal
Project Lead
Dr. Zamin A. Kanji
Dr. Zamin A. Kanji
Scientific Advisor
Prof. Ulrike Lohmann
Prof. Ulrike Lohmann
Scientific Advisor
Dr. Michael Rösch
Dr. Michael Rösch
Technical Advisor
For Researchers

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Our principles

The principles behind RepliClouds.

References
1 Romakkaniemi et al., Atmos. Meas. Tech., 7, 1377–1384, doi:10.5194/amt-7-1377-2014, 2014.
2 Hu et al., Atmos. Chem. Phys., 18, 14925–14937, doi:10.5194/acp-18-14925-2018, 2018.
3 Asa-Awuku et al., Atmos. Chem. Phys., 9, 795–812, doi:10.5194/acp-9-795-2009, 2009.
4 Rose et al., Atmos. Chem. Phys., 8, 1153–1179, doi:10.5194/acp-8-1153-2008, 2008.
5 Tao et al., Geophys. Res. Lett., 50, e2022GL101603, doi:10.1029/2022GL101603, 2023.
6 Sapkal et al., Atmos. Meas. Tech., 18, 5649–5667, doi:10.5194/amt-18-5649-2025, 2025.
7 Mazoyer et al., Atmos. Chem. Phys., 19, 4323–4344, doi:10.5194/acp-19-4323-2019, 2019.