DOE Data Explorer title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: 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:
;
  1. ORNL
Publication Date:
DOE Contract Number:  
AC05-00OR22725
Research Org.:
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)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Collaborations:
PNNL, BNL, ANL, ORNL
Subject:
54 ENVIRONMENTAL SCIENCES; 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:Sat Nov 30 23:00:00 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 = {Sat Nov 30 23:00:00 EST 2019},
month = {Sat Nov 30 23:00:00 EST 2019}
}