Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway
Abstract
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.
- Authors:
- Publication Date:
- DOE Contract Number:
- DE-AC05-00OR22725
- Research Org.:
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Atmospheric Radiation Measurement (ARM) Archive; Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Atmospheric Radiation Measurement (ARM) Data Center
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- Collaborations:
- PNNL, BNL, ANL, ORNL
- Subject:
- 54 Environmental Sciences
- Keywords:
- Weather balloons,Wind_from_direction, air_temperature, ARM, DOE.
- OSTI Identifier:
- 1843763
- DOI:
- https://doi.org/10.5439/1843763
Citation Formats
Wu, Peng, and Ovchinnikov, Mikhail. Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway. United States: N. p., 2019.
Web. doi:10.5439/1843763.
Wu, Peng, & Ovchinnikov, Mikhail. Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway. United States. doi:https://doi.org/10.5439/1843763
Wu, Peng, and Ovchinnikov, Mikhail. 2019.
"Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway". United States. doi:https://doi.org/10.5439/1843763. https://www.osti.gov/servlets/purl/1843763. Pub date:Sun Dec 01 00:00:00 EST 2019
@article{osti_1843763,
title = {Air mass back trajectories during cold-air outbreaks (CAOs) at Andenes and Bear Island, Norway},
author = {Wu, Peng and Ovchinnikov, Mikhail},
abstractNote = {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.},
doi = {10.5439/1843763},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2019},
month = {12}
}
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