Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport
A nomogram was prepared by [Golder, 1972. Boundary Layer Meteorology 3, 47–58] to compute the surface layer parameters in stable conditions. This note revisits the Golder’s curves and examines the methodology underlying their derivation in stable conditions. The inherent limitation in...
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sg-ntu-dr.10356-940642023-02-28T19:38:19Z Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport Maithili Sharan. S. G. Gopalakrishnan. Jagabandhu Panda. School of Physical and Mathematical Sciences DRNTU::Science::Physics::Meteorology and climatology A nomogram was prepared by [Golder, 1972. Boundary Layer Meteorology 3, 47–58] to compute the surface layer parameters in stable conditions. This note revisits the Golder’s curves and examines the methodology underlying their derivation in stable conditions. The inherent limitation in the methodology used for construction of Golder’s curves was also noticed by Trombetti et al. (1986). Surface layer fluxes computed using the parameters derived from modified curves are found to be closer to the turbulence measurements from CASES-99 experiment for stable conditions than those calculated from the [Golder, 1972. Boundary Layer Meteorology 3, 47–58] curves. Accepted version 2011-10-19T02:53:33Z 2019-12-06T18:50:13Z 2011-10-19T02:53:33Z 2019-12-06T18:50:13Z 2009 2009 Journal Article 1558-8432 https://hdl.handle.net/10356/94064 http://hdl.handle.net/10220/7306 10.1016/j.atmosenv.2005.05.034 161465 en Journal of applied meteorology and climatology 6 p. application/pdf |
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DRNTU::Science::Physics::Meteorology and climatology Maithili Sharan. S. G. Gopalakrishnan. Jagabandhu Panda. Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
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A nomogram was prepared by [Golder, 1972. Boundary Layer Meteorology 3, 47–58] to compute the surface layer
parameters in stable conditions. This note revisits the Golder’s curves and examines the methodology underlying their
derivation in stable conditions. The inherent limitation in the methodology used for construction of Golder’s curves was
also noticed by Trombetti et al. (1986). Surface layer fluxes computed using the parameters derived from modified
curves are found to be closer to the turbulence measurements from CASES-99 experiment for stable conditions than
those calculated from the [Golder, 1972. Boundary Layer Meteorology 3, 47–58] curves. |
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School of Physical and Mathematical Sciences |
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School of Physical and Mathematical Sciences Maithili Sharan. S. G. Gopalakrishnan. Jagabandhu Panda. |
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Article |
author |
Maithili Sharan. S. G. Gopalakrishnan. Jagabandhu Panda. |
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Maithili Sharan. |
title |
Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
title_short |
Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
title_full |
Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
title_fullStr |
Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
title_full_unstemmed |
Study of regional-scale boundary layer characteristics over Northern India with a special reference to the role of the Thar Desert in regional-scale transport |
title_sort |
study of regional-scale boundary layer characteristics over northern india with a special reference to the role of the thar desert in regional-scale transport |
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2011 |
url |
https://hdl.handle.net/10356/94064 http://hdl.handle.net/10220/7306 |
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1759855814901760000 |