Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0

A measurement intensive campaign was carried out in Barrow, Alaska in spring 2009 as part of the Ocean Atmosphere Sea Ice Snowpack (OASIS) program. This dataset contains three-dimensional wind velocities measured at 2 heights (~ 2 m agl and 6 m agl) using sonic anemometers (Applied Technologies, Son...

Full description

Bibliographic Details
Main Author: Guenther, A.
Format: Dataset
Language:English
Published: UCAR/NCAR - Earth Observing Laboratory 2012
Subjects:
Online Access:https://dx.doi.org/10.5065/d62j6902
https://arcticdata.io/catalog/#view/doi:10.5065/D62J6902
id ftdatacite:10.5065/d62j6902
record_format openpolar
spelling ftdatacite:10.5065/d62j6902 2023-05-15T14:51:35+02:00 Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0 Guenther, A. 2012 XLS: Excel (application/vnd.ms-excel) https://dx.doi.org/10.5065/d62j6902 https://arcticdata.io/catalog/#view/doi:10.5065/D62J6902 en eng UCAR/NCAR - Earth Observing Laboratory http://data.eol.ucar.edu/codiac/dss/id=106.370 http://oasishome.net/barrow2009_investigators.php These data are available to be used subject to the University Corporation for Atmospheric Research ("UCAR") terms and conditions. http://www2.ucar.edu/terms-of-use climatologyMeteorologyAtmosphere Arctic Chemistry Manned Field Station ARCSS NSF Arctic System Science ACADIS Advanced Cooperative Arctic Data and Information Service dataset Dataset scientific data 2012 ftdatacite https://doi.org/10.5065/d62j6902 2021-11-05T12:55:41Z A measurement intensive campaign was carried out in Barrow, Alaska in spring 2009 as part of the Ocean Atmosphere Sea Ice Snowpack (OASIS) program. This dataset contains three-dimensional wind velocities measured at 2 heights (~ 2 m agl and 6 m agl) using sonic anemometers (Applied Technologies, Sonic Anemometer/Thermometer model (SATI/3K)). Also, from the measured speed of sound, virtual potential temperature was also obtained. Wind velocities and virtual potential temperature were acquired at 10 Hz. Meteorological variables such as wind speed and direction were obtained from vector-averaging the horizontal wind velocities over 1 minute intervals. Turbulent fluxes, such as friction velocities and sensible heat flux, were obtained from covariances of wind velocities and temperature over 15 minute averages. The longer time scale allows for adequate sampling of larger atmospheric eddies that contribute to the measured flux. Wind speeds and direction are accurate to +/- 0.03 m/s and +/- 0.1 degrees, respectively, according to the manufacturer's specifications. Turbulent fluxes are estimated to be accurate to +/- 10-15% due to statistical sampling issues. Dataset Arctic Barrow Sea ice Alaska DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic climatologyMeteorologyAtmosphere
Arctic
Chemistry
Manned Field Station
ARCSS
NSF Arctic System Science
ACADIS
Advanced Cooperative Arctic Data and Information Service
spellingShingle climatologyMeteorologyAtmosphere
Arctic
Chemistry
Manned Field Station
ARCSS
NSF Arctic System Science
ACADIS
Advanced Cooperative Arctic Data and Information Service
Guenther, A.
Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
topic_facet climatologyMeteorologyAtmosphere
Arctic
Chemistry
Manned Field Station
ARCSS
NSF Arctic System Science
ACADIS
Advanced Cooperative Arctic Data and Information Service
description A measurement intensive campaign was carried out in Barrow, Alaska in spring 2009 as part of the Ocean Atmosphere Sea Ice Snowpack (OASIS) program. This dataset contains three-dimensional wind velocities measured at 2 heights (~ 2 m agl and 6 m agl) using sonic anemometers (Applied Technologies, Sonic Anemometer/Thermometer model (SATI/3K)). Also, from the measured speed of sound, virtual potential temperature was also obtained. Wind velocities and virtual potential temperature were acquired at 10 Hz. Meteorological variables such as wind speed and direction were obtained from vector-averaging the horizontal wind velocities over 1 minute intervals. Turbulent fluxes, such as friction velocities and sensible heat flux, were obtained from covariances of wind velocities and temperature over 15 minute averages. The longer time scale allows for adequate sampling of larger atmospheric eddies that contribute to the measured flux. Wind speeds and direction are accurate to +/- 0.03 m/s and +/- 0.1 degrees, respectively, according to the manufacturer's specifications. Turbulent fluxes are estimated to be accurate to +/- 10-15% due to statistical sampling issues.
format Dataset
author Guenther, A.
author_facet Guenther, A.
author_sort Guenther, A.
title Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
title_short Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
title_full Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
title_fullStr Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
title_full_unstemmed Meteorology measurements during OASIS Barrow field intensive Spring 2009, Version 1.0
title_sort meteorology measurements during oasis barrow field intensive spring 2009, version 1.0
publisher UCAR/NCAR - Earth Observing Laboratory
publishDate 2012
url https://dx.doi.org/10.5065/d62j6902
https://arcticdata.io/catalog/#view/doi:10.5065/D62J6902
geographic Arctic
geographic_facet Arctic
genre Arctic
Barrow
Sea ice
Alaska
genre_facet Arctic
Barrow
Sea ice
Alaska
op_relation http://data.eol.ucar.edu/codiac/dss/id=106.370
http://oasishome.net/barrow2009_investigators.php
op_rights These data are available to be used subject to the University Corporation for Atmospheric Research ("UCAR") terms and conditions.
http://www2.ucar.edu/terms-of-use
op_doi https://doi.org/10.5065/d62j6902
_version_ 1766322710602842112