NSF/NCAR C-130 3V-CPI Raw 2D-S Imagery
The Three-View Cloud Particle Imager (3V-CPI) is a combination of three imaging instruments. Two of them comprise a 2D-S instrument, in which two 2D probes image particles as they pass through beams that are oriented orthogonally to each other and the airflow. If particles also lie in the intersection of the sensitive areas of the two beams, they are seen by both 2D probes. In that case, the CPI is triggered to take a high-resolution picture, via a briefly illuminated high-resolution imaging array, to provide a third image at high resolution. The probe is particularly suited to imaging ice crystals, but also provide good detection of other hydrometeors including large cloud droplets, drizzle and small rain drops, and precipitation particles. The 3V-CPI measures the size, shape and concentration of water drops and ice particles in clouds in the size range of 15-250 micrometers. This dataset contains 2D-S imagery collected by the 3V-CPI aboard the NSF/NCAR C-130 during the ARISTO2016 project. The 2DS puts all flight data into 3 files, and the size of these files depends on the amount of time in clouds.
- ORDER data for delivery by FTP
|Subscribe||Subscribe to receive email when new or updated data is available.|
|GCMD Science Keywords|
|Begin datetime||2016-08-08 14:49:27|
|End datetime||2016-08-17 05:59:59|
Map data from IBCSO, IBCAO, and Global Topography.
Maximum (North) Latitude:
Minimum (South) Latitude:
Minimum (West) Longitude: -126.00, Maximum (East) Longitude: -103.00
Additional contact information
- author: EOL Data Support
- publisher: EOL Data Support
- resourceProvider: Pavel Romashkin <email@example.com>
CitationExample citation following ESIP guidelines:
UCAR/NCAR - Earth Observing Laboratory. 2018. NSF/NCAR C-130 3V-CPI Raw 2D-S Imagery. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6K936BD. Accessed 01 Jun 2020.
Today's date is shown: please replace with the date of your most recent access.
Additional citation styles
The citation text below is from the DataCite Content Resolver service and may take a few seconds to load. The styles and locales are obtained from CrossCite, which also provides a citation formatter. See ReFindit for another alternative. Formatting is not perfect: please verify and edit before use. Today's date is shown: please replace with the date of your most recent access.
Note that your browser may not display the above metadata links, but automatically save them as files in a folder such as "