Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway
For each CAO hour identified from interpolated sounding, a 36-hour back trajectory was calculated using the NOAA HYSPLIT model. We used three different meteorological data as inputs to HYSPLIT: GFS 0.25 deg, GDSA 1deg, and NCEP/NCAR Reanalysis. The trajectories were calculated at four elevations: 50...
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Format: | Dataset |
Language: | English |
Published: |
Atmospheric Radiation Measurement (ARM) Archive, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (US); ARM Data Center, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
2019
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Online Access: | https://dx.doi.org/10.5439/1843763 https://www.osti.gov/servlets/purl/1843763/ |