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Lüers, Johannes; Barrais, Jörg (2013): Modeled turbulent atmospheric heat fluxes for time series site ARCTEX in 2006. PANGAEA, https://doi.org/10.1594/PANGAEA.811062, In: Lüers, Johannes; Bareiss, Jörg (2013): Turbulent flux and meteorological measurements during ARCTEX-2006 campaign. PANGAEA, https://doi.org/10.1594/PANGAEA.811066

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Related to:
Lüers, Johannes; Bareiss, Jörg (2010): The effect of misleading surface temperature estimations on the sensible heat fluxes at a high Arctic site – the Arctic Turbulence Experiment 2006 on Svalbard (ARCTEX-2006). Atmospheric Chemistry and Physics, 10(1), 157-168, https://doi.org/10.5194/acp-10-157-2010
Lüers, Johannes; Bareiss, Jörg (2011): Direct near-surface measurements of sensible heat fluxes in the Arctic tundra applying eddy covariance and laser scintillometry—the Arctic Turbulence Experiment 2006 on Svalbard (ARCTEX-2006). Theoretical and Applied Climatology, 105(3-4), 387-402, https://doi.org/10.1007/s00704-011-0400-5
Coverage:
Latitude: 78.921500 * Longitude: 11.929000
Date/Time Start: 2006-05-04T23:55:00 * Date/Time End: 2006-05-19T10:20:00
Minimum Elevation: 12.0 m * Maximum Elevation: 12.0 m
Event(s):
ARCTEX-Site * Latitude: 78.921500 * Longitude: 11.929000 * Date/Time Start: 2006-05-04T23:00:00 * Date/Time End: 2006-05-19T11:00:00 * Elevation: 12.0 m * Location: Ny-Ålesund, Spitsbergen * Campaign: ARCTEX-2006 * Basis: Monitoring station * Method/Device: Monitoring station (MONS)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DATE/TIMEDate/TimeGeocode
2Temperature, air, gradientTTT gradKLüers, JohannesCalculatedTemperature gradient between 10 m and 0 m above ground derived from infrared long-wave upward radiation
3Temperature, air, gradientTTT gradKLüers, JohannesCalculatedTemperature gradient between 10 m and 0 m above ground derived from hydrodynamic three-layer temperature-profile model (3LM)
4Wind speed, gradientff gradm/sLüers, JohannesCalculatedWind speed gradient between 10 m and 0.7 m above ground
5Richardson numberRiLüers, JohannesCalculatedwith T(0) derived from infrared long-wave upward radiation
6Richardson numberRiLüers, JohannesCalculatedwith T(0) derived from hydrodynamic three-layer temperature-profile model (3LM)
7Heat Flux, sensible, modeledQh modW/m2Lüers, Johannesmodelledwith the bulk parameters after Louis (1979, doi:10.1007/BF00117978) and Ebert & Curry (1993, doi:10.1029/93JC00656)
8Heat Flux, sensible, modeledQh modW/m2Lüers, Johannesmodelledsensible heat flux above snow-cover using IR-derived T(0) after Launiainen and Cheng (1995)
9Heat Flux, latent, modeledQe modW/m2Lüers, Johannesmodelledlatent heat flux above snow-cover using IR-derived T(0) after Launiainen and Cheng (1995)
10Heat Flux, sensible, modeledQh modW/m2Lüers, Johannesmodelledsensible heat flux above snow-cover using 3LM-derived T(0) after Launiainen and Cheng (1995)
11Heat Flux, latent, modeledQe modW/m2Lüers, Johannesmodelledlatent heat flux above snow-cover using 3LM-derived T(0) after Launiainen and Cheng (1995)
12Heat Flux, sensible, modeledQh modW/m2Lüers, Johannesmodelledsensible heat flux above snow-cover using IR-derived T(0) after Ebert and Curry (1993, doi:10.1029/93JC00656)
13Heat Flux, sensible, modeledQh modW/m2Lüers, Johannesmodelledsensible heat flux above snow-cover using 3LM-derived T(0) after Ebert and Curry (1993, doi:10.1029/93JC00656)
Size:
26799 data points

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