Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica

The measurements of profiles of wind speed and air temperature in the atmospheric surface layer above bare ice surface in the circumference of the Yamato Mountains were carried out under neutral and unstable conditions in December, 1973. The results are summarized as follows: 1) The value of aerodyn...

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Main Author: Shun'ichi KOBAYASHI
Format: Article
Language:English
Published: National Institute of Polar Research 1978-03-01
Series:Antarctic Record
Online Access:https://doi.org/10.15094/00007979
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author Shun'ichi KOBAYASHI
author_facet Shun'ichi KOBAYASHI
author_sort Shun'ichi KOBAYASHI
collection DOAJ
description The measurements of profiles of wind speed and air temperature in the atmospheric surface layer above bare ice surface in the circumference of the Yamato Mountains were carried out under neutral and unstable conditions in December, 1973. The results are summarized as follows: 1) The value of aerodynamic roughness parameter (Z_0) was constantly 0.085 cm independent on wind speed, and this value corresponded to the depth of spoon-cut features (2-3 cm) on the bare ice surface. 2) The relation between the friction velocity (U_*) and the wind speed at 1 m height (U_1) is expressed by U_*=0.057 U_1. 3) Atmosphere showed an unstable condition (negative Richardson number) with the decrease of wind speed, as the bare ice surface was heated by radiation. 4) Eddy diffusivity obtained on the bare ice surface in neutral condition was larger than that of sea ice around Syowa Station.
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spelling doaj.art-06b424144e0f44e7aee972a34c59bcd32022-12-22T00:03:05ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1978-03-0161112210.15094/00007979Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, AntarcticaShun'ichi KOBAYASHI0The Institute of Low Temperature Science, Hokkaido UniversityThe measurements of profiles of wind speed and air temperature in the atmospheric surface layer above bare ice surface in the circumference of the Yamato Mountains were carried out under neutral and unstable conditions in December, 1973. The results are summarized as follows: 1) The value of aerodynamic roughness parameter (Z_0) was constantly 0.085 cm independent on wind speed, and this value corresponded to the depth of spoon-cut features (2-3 cm) on the bare ice surface. 2) The relation between the friction velocity (U_*) and the wind speed at 1 m height (U_1) is expressed by U_*=0.057 U_1. 3) Atmosphere showed an unstable condition (negative Richardson number) with the decrease of wind speed, as the bare ice surface was heated by radiation. 4) Eddy diffusivity obtained on the bare ice surface in neutral condition was larger than that of sea ice around Syowa Station.https://doi.org/10.15094/00007979
spellingShingle Shun'ichi KOBAYASHI
Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
Antarctic Record
title Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
title_full Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
title_fullStr Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
title_full_unstemmed Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
title_short Observation of the Atmospheric Surface Layer on Bare Ice in the Circumference of the Yamato Mountains, Antarctica
title_sort observation of the atmospheric surface layer on bare ice in the circumference of the yamato mountains antarctica
url https://doi.org/10.15094/00007979
work_keys_str_mv AT shunichikobayashi observationoftheatmosphericsurfacelayeronbareiceinthecircumferenceoftheyamatomountainsantarctica