Environmental Data: CCN, hygroscopicity, predicted cloud droplet numbe...
Description
__Cloud Condensation Nuclei (CCN) data:__ A Droplet Measurement Technologies (DMT) single-column continuous-flow streamwise thermal gradient chamber (CFSTG...
Citation
Nenes, A., Georgakaki, P., Bougiatioti, A. (2020). CCN, hygroscopicity, predicted cloud droplet numbers Weissfluhjoch. EnviDat. https://www.doi.org/10.16904/envidat.198.
Resources
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CCN data Weissfluhjoch
In-situ CCN measurements were conducted between February 24 and March 8 2019 at Weissfluhjoch. The data file contains:
* Date and time (DD/MM/YYYY hh:mm:ss) in UTC
* Filtered CCN number concentrations (in cmˉ³) measured at 6 discrete supersaturations (SS) ranging from 0.09% to 0.74%. The name of each CCN column is indicative of the SS developed within the instrument.
* Instrument characteristics such as sample temperature (in °C) and pressure (in mbar)
* A code that refers to the reason of filtering.
Missing or filtered CCN values are indicated by "-999", while a declaration of each "Error_code" can be found in the following list:
_Error_code_:
__0000__: Measurements without error
__1000__: Period of transient operation after a supersaturation change
__2000__: Sharp change (decrease) in the room temperature housing the instrument, which induces a reset in column temperature
__3000__: Irregular values in the room temperature housing the instrument
__9999__: Missing data
CCN data Weissfluhjoch >
Hygroscopicity parameter Weissfluhjoch
The aerosol hygroscopicity parameter is derived combining the CCN and SMPS size distribution data collected between February 24 and March 8 2019 at Weissfluhjoch. The data file contains:
* Date and time (DD/MM/YYYY hh:mm:ss) in UTC
* The instrument supersaturation (SS%)
* The calculated hygroscopicity parameter (kappa)
* The calculated critical dry diameter of the particles (Dcr) in nm.
Missing values are indicated by "-999".
Hygroscopicity parameter Weissfluhjoch >
Predicted cloud droplet number concentrations Weissfluhjoch
In-situ measurements of aerosol size distributions along with updraft velocities collected from a wind Doppler Lidar are coupled with a state-of-the art droplet activation parameterization (Morales and Nenes, 2014) to determine the cloud droplet number and maximum in-cloud supersaturation that can potentially form over the Weissfluhjoch station between February 24 and March 8 2019. For this, a hygroscopicity parameter of 0.25 is assumed, according to the CCN-derived values. The data file contains:
* Date and time (DD/MM/YYYY hh:mm:ss) in UTC
* The wind-lidar derived standard deviation of updraft velocities (sigma-w) in m/s, used to apply the parameterization employing a single characteristic velocity (Morales and Nenes, 2010)
* The maximum predicted cloud parcel supersaturation (Smax%)
* The total in-situ aerosol number concentration (Naer) in cmˉ³, measured by the SMPS
* The predicted cloud droplet numbers (Nd) in cmˉ³
* The activation fraction (%)
Predicted cloud droplet number concentrations Weissfluhjoch