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  • 1
    Online Resource
    Online Resource
    American Meteorological Society ; 2013
    In:  Journal of Atmospheric and Oceanic Technology Vol. 30, No. 2 ( 2013-02-01), p. 161-181
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 30, No. 2 ( 2013-02-01), p. 161-181
    Abstract: Small environmental research aircraft (ERA) are becoming more common for detailed studies of air–surface interactions. The Sky Arrow 650 ERA, used by multiple groups, is designed to minimize the complexity of high-precision airborne turbulent wind measurement. Its relative wind probe, of a nine-port design, is furthermore used with several other airplanes. This paper gives an overview of 1) calibration of the model that converts the probe’s raw measurements to meteorological quantities; 2) quality control and assurance (QC–QA) in postprocessing of these quantities to compute fluxes; and 3) sensitivity of fluxes to errors in calibration parameters. The model, an adapted version of standard models of potential flow and aerodynamic upwash, is calibrated using an integrated method to derive a globally optimum set of parameters from in-flight maneuvers. Methods of QC–QA from the tower flux community are adopted for use with airborne flux data to provide more objective selection criteria for large datasets. Last, measurements taken from a standard operational flight are used to show fluxes to be most sensitive to calibration parameters that directly affect the vertical wind component. In another test with the same data, varying all calibration parameters simultaneously by ±10% of their optimum values, the model computes a response in the fluxes smaller than 10%, though a larger response may occur if only a subset of parameters is perturbed. A MATLAB toolbox has been developed that facilitates the procedures presented here.
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2013
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    detail.hit.zdb_id: 48441-6
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  • 2
    Online Resource
    Online Resource
    American Meteorological Society ; 2012
    In:  Journal of Applied Meteorology and Climatology Vol. 51, No. 2 ( 2012-02), p. 205-218
    In: Journal of Applied Meteorology and Climatology, American Meteorological Society, Vol. 51, No. 2 ( 2012-02), p. 205-218
    Abstract: The utility of aggregating data from near-surface meteorological networks for initiating dispersion models is examined by using data from the “WeatherBug” network that is operated by Earth Networks, Inc. WeatherBug instruments are typically mounted 2–3 m above the eaves of buildings and thus are more representative of the immediate surroundings than of conditions over the broader area. This study focuses on subnetworks of WeatherBug sites that are within circles of varying radius about selected stations of the DCNet program. DCNet is a Washington, D.C., research program of the NOAA Air Resources Laboratory. The aggregation of data within varying-sized circles of 3–10-km radius yields average velocities and velocity-component standard deviations that are largely independent of the number of stations reporting—provided that number exceeds about 10. Given this finding, variances of wind components are aggregated from arrays of WeatherBug stations within a 5-km radius of selected central DCNet locations, with on average 11 WeatherBug stations per array. The total variance of wind components from the surface (WeatherBug) subnetworks is taken to be the sum of two parts: the temporal variance is the average of the conventional wind-component variances at each site and the spatial variance is based on the velocity-component averages of the individual sites. These two variances (and the standard deviations derived from them) are found to be similar. Moreover, the total wind-component variance is comparable to that observed at the DCNet reference stations. The near-surface rooftop wind velocities are about 35% of the magnitudes of the DCNet measurements. Limited additional data indicate that these results can be extended to New York City.
    Type of Medium: Online Resource
    ISSN: 1558-8424 , 1558-8432
    RVK:
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2012
    detail.hit.zdb_id: 2227779-1
    detail.hit.zdb_id: 2227759-6
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 1996
    In:  Boundary-Layer Meteorology Vol. 80, No. 1-2 ( 1996-7), p. 79-94
    In: Boundary-Layer Meteorology, Springer Science and Business Media LLC, Vol. 80, No. 1-2 ( 1996-7), p. 79-94
    Type of Medium: Online Resource
    ISSN: 0006-8314 , 1573-1472
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 1996
    detail.hit.zdb_id: 242879-9
    detail.hit.zdb_id: 1477639-X
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 4
    Online Resource
    Online Resource
    American Meteorological Society ; 2013
    In:  Journal of Applied Meteorology and Climatology Vol. 52, No. 3 ( 2013-03), p. 668-681
    In: Journal of Applied Meteorology and Climatology, American Meteorological Society, Vol. 52, No. 3 ( 2013-03), p. 668-681
    Abstract: Data from six urban areas in a nationwide network of sites within the surface roughness layer are examined. It is found that the average velocity variances in time, derived by averaging the conventional variances from a network of n stations, are nearly equal to the velocity variances in space, derived as the variances among the n average velocities. This similarity is modified during sunlit hours, when convection appears to elevate the former. The data show little dependence of the ratio of these two variances on wind speed. It is concluded that the average state of the surface roughness layer in urban and suburban areas like those considered here tends toward an approximate equality of these two measures of variance, much as has been observed elsewhere for the case of forests.
    Type of Medium: Online Resource
    ISSN: 1558-8424 , 1558-8432
    RVK:
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2013
    detail.hit.zdb_id: 2227779-1
    detail.hit.zdb_id: 2227759-6
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  • 5
    Online Resource
    Online Resource
    American Meteorological Society ; 2010
    In:  Journal of the Atmospheric Sciences Vol. 67, No. 4 ( 2010-04-01), p. 1157-1170
    In: Journal of the Atmospheric Sciences, American Meteorological Society, Vol. 67, No. 4 ( 2010-04-01), p. 1157-1170
    Abstract: High-resolution measurements obtained from NOAA “best” atmospheric turbulence (BAT) probes mounted on an EGRETT high-altitude research aircraft were used to characterize turbulence in the upper troposphere and lower stratosphere at scales from 2 m to 20 km, focusing on three-dimensional behavior in the sub-kilometer-scale range. Data were analyzed for 129 separate level flight segments representing 41 h of flight time and 12 600 km of wind-relative flight distances. The majority of flights occurred near the tropopause layer of the winter subtropical jet stream in the Southern Hemisphere. Second-order structure functions for velocity and temperature were analyzed for the separate level-flight segments, individually and in various ensembles. A 3D scaling range was observed at scales less than about 100 m, with power-law exponents for the structure functions of the velocity component in the flight direction varying mostly between 0.4 and 0.75 for the separate flight segments, but close to ⅔ for the ensemble-averaged curves for all levels and for various subensembles. Structure functions in the 3D scaling range were decoupled from those at scales greater than 10 km, with the large-scale structure functions showing less variation than those at smaller scales. Weakly anisotropic behavior was observed in the 3D range, with structure parameters for the lateral and vertical velocities on the same order as those in the flight direction but deviating from the expected isotropic value. Anisotropy was correlated with turbulence intensity, with greater anisotropy associated with weaker turbulence.
    Type of Medium: Online Resource
    ISSN: 1520-0469 , 0022-4928
    RVK:
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2010
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    detail.hit.zdb_id: 2025890-2
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 6
    Online Resource
    Online Resource
    American Meteorological Society ; 1989
    In:  Journal of Applied Meteorology Vol. 28, No. 6 ( 1989-06), p. 467-476
    In: Journal of Applied Meteorology, American Meteorological Society, Vol. 28, No. 6 ( 1989-06), p. 467-476
    Type of Medium: Online Resource
    ISSN: 0894-8763 , 1520-0450
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1989
    detail.hit.zdb_id: 242493-9
    detail.hit.zdb_id: 2027356-3
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  • 7
    Online Resource
    Online Resource
    American Meteorological Society ; 2007
    In:  Journal of Atmospheric and Oceanic Technology Vol. 24, No. 6 ( 2007-06), p. 994-1007
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 24, No. 6 ( 2007-06), p. 994-1007
    Abstract: Turbulence and air-surface exchange are important factors throughout the life cycle of a tropical cyclone. Conventional turbulence instruments are not designed to function in the extreme environment encountered in such storms. A new instrument called the Extreme Turbulence (ET) probe has been developed specifically for measuring turbulence on a fixed tower in hurricane conditions. Although the probe is designed for surface deployment, it is based on the same pressure-sphere technology used for aircraft gust probes. The ET probe is designed around a 43-cm-diameter sphere with 30 pressure ports distributed over its surface. A major obstacle during development was finding a method to prevent water from fouling the pressure ports. Two approaches were investigated: a passive approach using gravity drainage and an active approach using an air pump to flush water from the ports. The probes were tested in both dry and wet conditions by mounting them on a vehicle side by side with more conventional instruments. In dry conditions, test data from the ET probes were in good agreement with the conventional instruments. In rain, probes using the passive rain defense performed about as well as in dry conditions, with the exception of some water intrusion into the temperature sensors. The active rain defense has received only limited attention so far, mainly because of the success and simplicity of the passive defense.
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 2007
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    detail.hit.zdb_id: 48441-6
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  • 8
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 1993
    In:  Boundary-Layer Meteorology Vol. 66, No. 3 ( 1993-11), p. 237-245
    In: Boundary-Layer Meteorology, Springer Science and Business Media LLC, Vol. 66, No. 3 ( 1993-11), p. 237-245
    Type of Medium: Online Resource
    ISSN: 0006-8314 , 1573-1472
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 1993
    detail.hit.zdb_id: 242879-9
    detail.hit.zdb_id: 1477639-X
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 9
    Online Resource
    Online Resource
    Elsevier BV ; 2009
    In:  Atmospheric Environment Vol. 43, No. 18 ( 2009-6), p. 3024-3028
    In: Atmospheric Environment, Elsevier BV, Vol. 43, No. 18 ( 2009-6), p. 3024-3028
    Type of Medium: Online Resource
    ISSN: 1352-2310
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2009
    detail.hit.zdb_id: 216368-8
    detail.hit.zdb_id: 1499889-0
    SSG: 14
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  • 10
    Online Resource
    Online Resource
    American Meteorological Society ; 1989
    In:  Journal of Applied Meteorology Vol. 28, No. 9 ( 1989-09), p. 936-947
    In: Journal of Applied Meteorology, American Meteorological Society, Vol. 28, No. 9 ( 1989-09), p. 936-947
    Type of Medium: Online Resource
    ISSN: 0894-8763 , 1520-0450
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1989
    detail.hit.zdb_id: 242493-9
    detail.hit.zdb_id: 2027356-3
    Location Call Number Limitation Availability
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