Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)

The vertical profiles of the strong katabatic winds at Syowa Station, Antarctica, are studied. A numerical solution of the equations of the Ekman layer above the Antarctic coastal slope is obtained under the following assumptions, (a) The steady state condition (b) The wind component of normal direc...

Full description

Bibliographic Details
Main Author: Takashi ADACHI
Format: Article
Language:English
Published: National Institute of Polar Research 1979-10-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00008095
id doaj-1d189baf39204524b3def77b9bfe16b1
record_format Article
spelling doaj-1d189baf39204524b3def77b9bfe16b12020-11-24T21:59:00ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1979-10-0167647410.15094/00008095Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)Takashi ADACHI0Research Institute of Japan Weather AssociationThe vertical profiles of the strong katabatic winds at Syowa Station, Antarctica, are studied. A numerical solution of the equations of the Ekman layer above the Antarctic coastal slope is obtained under the following assumptions, (a) The steady state condition (b) The wind component of normal direction to the sloped plane is zero (c) The wind vectors are uniform along the slope at each height (d) Monin-Obukhov's similarity theory is valid in each thin layer of Ekman layer (e) Local value of Monin-Obukhov length is defined by the local heat flux and the local momentum flux (f) New non-dimensional wind shear function (φ) is presented in neutial or stable Ekman laver, φ=(1+12 z/L)^<1/2>https://doi.org/10.15094/00008095
collection DOAJ
language English
format Article
sources DOAJ
author Takashi ADACHI
spellingShingle Takashi ADACHI
Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
Antarctic Record
author_facet Takashi ADACHI
author_sort Takashi ADACHI
title Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_short Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_full Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_fullStr Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_full_unstemmed Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)
title_sort numerical simulation of katabatic wind profile at syowa station, antarctica (special issue of the proceedings of the first symposium on antarctic meteorology and glaciology)
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1979-10-01
description The vertical profiles of the strong katabatic winds at Syowa Station, Antarctica, are studied. A numerical solution of the equations of the Ekman layer above the Antarctic coastal slope is obtained under the following assumptions, (a) The steady state condition (b) The wind component of normal direction to the sloped plane is zero (c) The wind vectors are uniform along the slope at each height (d) Monin-Obukhov's similarity theory is valid in each thin layer of Ekman layer (e) Local value of Monin-Obukhov length is defined by the local heat flux and the local momentum flux (f) New non-dimensional wind shear function (φ) is presented in neutial or stable Ekman laver, φ=(1+12 z/L)^<1/2>
url https://doi.org/10.15094/00008095
work_keys_str_mv AT takashiadachi numericalsimulationofkatabaticwindprofileatsyowastationantarcticaspecialissueoftheproceedingsofthefirstsymposiumonantarcticmeteorologyandglaciology
_version_ 1725849764918984704