Evaluating aerosol influence on cloud models using in-situ measurements during the INUPIAQ campaign

Robert Farrington1, Paul Connolly2, Tom Choularton3, Keith Bower3, Gary Lloyd3, Michael Flynn4, Jonathan Crosier3 and Paul Field5, (1)University of Manchester, Manchester, M13, United Kingdom, (2)Centre for Atmospheric Science, University of Manchester, Manchester, United Kingdom, (3)University of Manchester, Manchester, United Kingdom, (4)University of Manchester, Department of Earth and Environmental Sciences, Manchester, United Kingdom, (5)United Kingdom Met Office, Exeter, United Kingdom
Abstract:
At temperatures between -35°C and 0°C, the presence of insoluble aerosols acting as ice nuclei (IN) initiate the nucleation of ice under atmospheric conditions. Previous field and laboratory campaigns have suggested that mineral dust present in the atmosphere act as IN at temperatures around -20°C (e.g. Sassen et al. 2003), however the cause of ice nucleation at temperatures of around -5°C is less certain. Coupled with the limited representation of aerosol and cloud processes in large-scale weather and climate models, the need for improved in-situ measurements of aerosol properties and cloud micro-physical processes to drive the improvement of aerosol-clouds processes in models is evident.

As part of the Ice NUcleation Process Investigation and Quantification (INUPIAQ) project, two field campaigns were conducted in early 2013 and early 2014. Both campaigns included measurements of cloud micro-physical properties at the summit of Jungfraujoch in Switzerland (3580m asl). Using data from the 2013 campaign and modelling simulations from the Weather Research and Forecasting model (WRF), an upwind site, located at Schilthorn (2970m asl), was determined for measuring aerosol properties out of cloud during the 2014 campaign. Further measurements of the cloud and aerosols properties were taken remotely using a doppler LiDAR located at Kleine Scheidegg (2061m asl).

The aim of this project is to determine whether detailed aerosol information is important to determining cloud and precipitation properties downwind. To this end WRF was run using the aerosol number concentrations and size distributions measured at the Schilthorn site to compare modelled ice number concentrations with measurements taken at Jungfraujoch using state of the science cloud ice probes, including the Three-View Cloud Particle Imager (3V-CPI) and the Cloud Aerosol Spectrometer with Depolarization (CAS-DPOL), with the results of the comparison presented and discussed at this meeting.

References

Sassen, K., et al, 2003: Saharan dust storms and indirect aerosol effects on clouds: Crystal-face results. Geophys. Res. Lett., 30(12), 1633–1636.

Back to: Atmospheric Ice Nuclei and Ice Cloud Formation: Field, Laboratory, and Modeling Studies II Posters