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    Comments on “Wind and Temperature Profiles in the Radix Layer: The Bottom Fifth of the Convective Boundary Layer” 

    Source: Journal of Applied Meteorology:;1999:;volume( 038 ):;issue: 004:;page 493
    Author(s): Arya, S. Pal
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Modeling and Parameterization of Near-Source Diffusion in Weak Winds 

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 005:;page 1112
    Author(s): Arya, S. Pal
    Publisher: American Meteorological Society
    Abstract: A critical assessment is made of several different approaches that can be used for modeling near-source diffusion in weak winds, including the calm condition. For the convective boundary layer, the statistical theory ...
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    Finite-Difference Errors in Estimation of Gradients in the Atmospheric Surface Layer 

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 002:;page 251
    Author(s): Arya, S. Pal
    Publisher: American Meteorological Society
    Abstract: Errors associated with the linear and the logarithmic finite-difference approximations of gradients in the surface layer are computed using the well-known Monin-Obukhov flux-profile relations. It is shown that while the ...
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    Comments on “MARIAH-A Similarity-Based Method for Determining Wind, Temperature, and Humidity Profile Structure In the Atmospheric Surface Layer” 

    Source: Journal of Applied Meteorology:;1996:;volume( 035 ):;issue: 004:;page 610
    Author(s): Arya, S. Pal
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    Vertical Dispersion from Surface and Elevated Releases: An Investigation of a Non-Gaussian Plume Model 

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 003:;page 490
    Author(s): Brown, Michael J.; Arya, S. Pal; Snyder, William H.
    Publisher: American Meteorological Society
    Abstract: The vertical diffusion of a passive tracer released from surface and elevated sources in a neutrally stratified boundary layer has been studied by comparing field and laboratory experiments with a non-Gaussian K-theory ...
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    A Laboratory Study of the Urban Heat Island in a Calm and Stably Stratified Environment. Part I: Temperature Field 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 010:;page 1377
    Author(s): Lu, Jie; Arya, S. Pal; Snyder, William H.; Lawson, Robert E.
    Publisher: American Meteorological Society
    Abstract: An extensive and systematic water-tank study was performed to simulate the urban heat island under a calm and stably stratified environment. The objective was to examine the mean-temperature field, mixing height, and ...
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    A Laboratory Study of the Urban Heat Island in a Calm and Stably Stratified Environment. Part II: Velocity Field 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 010:;page 1392
    Author(s): Lu, Jie; Arya, S. Pal; Snyder, William H.; Lawson, Robert E.
    Publisher: American Meteorological Society
    Abstract: A fully turbulent, low-aspect-ratio buoyant plume with no initial momentum under calm and stably stratified conditions is produced in a convection tank. The plume is generated by a circular heat island at the bottom of the ...
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    Urban Modification of Thunderstorms: An Observational Storm Climatology and Model Case Study for the Indianapolis Urban Region 

    Source: Journal of Applied Meteorology and Climatology:;2010:;volume( 050 ):;issue: 005:;page 1129
    Author(s): Niyogi, Dev; Pyle, Patrick; Lei, Ming; Arya, S. Pal; Kishtawal, Chandra M.; Shepherd, Marshall; Chen, Fei; Wolfe, Brian
    Publisher: American Meteorological Society
    Abstract: radar-based climatology of 91 unique summertime (May 2000?August 2009) thunderstorm cases was examined over the Indianapolis, Indiana, urban area. The study hypothesis is that urban regions alter the intensity and ...
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