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...
| Main Authors: | , |
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| Language: | unknown |
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2022
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| Subjects: | |
| Online Access: | http://www.osti.gov/servlets/purl/1843763 https://www.osti.gov/biblio/1843763 https://doi.org/10.5439/1843763 |
| Summary: | 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: 500 m, 1000 m, 2000 m, and 5000 m. Locations (latitudes and longitudes) for each hour of the trajectory were reported in the data files. |
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