ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク

P(論文) The atmospheric turbulence in stable stratification was observed at Syowa Station in Antarctica during the period from February to December in 1970. Characteristics of atmospheric turbulence are analyzed in relation to the stability or the wind speed at the height of 20 m in surface air layer....

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Main Authors: 真木, 太一, マキ, タイチ, MAKI, Taichi
Language:Japanese
Published: 国立極地研究所 1974
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/7729/files/KJ00002476729.pdf
https://doi.org/10.15094/00007729
https://nipr.repo.nii.ac.jp/records/7729
_version_ 1829301236924416000
author 真木, 太一
マキ, タイチ
MAKI, Taichi
author_facet 真木, 太一
マキ, タイチ
MAKI, Taichi
author_sort 真木, 太一
collection National Institute of Polar Research Repository, Japan
description P(論文) The atmospheric turbulence in stable stratification was observed at Syowa Station in Antarctica during the period from February to December in 1970. Characteristics of atmospheric turbulence are analyzed in relation to the stability or the wind speed at the height of 20 m in surface air layer. Obtained results are as follows: U_<20> (horizontal mean wind speed at the height of 20m) is proportional to about -0.56 power of Ri (Richardson number). W_<20>/U_<20> (ratio of the vertical mean wind speed to U_<20> at the height of 20m) is independent of Ri. The standard deviation of the longitudinal wind speed (σ_U) is in direct proportion to the standard deviation of the lateral wind speed (σ_v). The relations between σ_U and σ_w (standard deviation of vertical wind speed) and between σ_v and σ_w are expressed with the two different equations, which have each transition point. Gustiness decreases with the increase of U_<20> below 8.5 m/s (U_<20>) and has a constant value above 8.5 m/s. Gust factor for five minutes decreases with the increase of U_<20>. The characteristic frequency distributions of three-dimensional wind components were made clear in comparison with the three typical weather condition. The Monin- Obukhov length and the energy dissipation rate increases in proportion to about -1.4 power of Ri and to about 2.7 power of U_<20> respectively in stable stratification. The characteristic time scales of longitudinal, lateral and vertical wind components increase with the increase of Ri and decrease with the increase of U_<20>, and the ratios of proportional components represent the cubic vortex, i.e., length:breadth:height = 6.3 : 1.9 : 1. The value of m obtained from Eq. (7) increases with the increase of Ri. departmental bulletin paper
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
geographic Syowa Station
geographic_facet Syowa Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00007729
institution Open Polar
language Japanese
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00007729
op_relation 南極資料
48
37
51
AN00181831
00857289
https://nipr.repo.nii.ac.jp/record/7729/files/KJ00002476729.pdf
https://doi.org/10.15094/00007729
https://nipr.repo.nii.ac.jp/records/7729
publishDate 1974
publisher 国立極地研究所
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00007729 2025-04-13T14:09:21+00:00 ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク 南極昭和基地での超音波風速温度計による大気乱流観測 Atmospheric Turbulence Measurements with the Sonic Anemometer-Thermometer at Syowa Station in Antarctica 真木, 太一 マキ, タイチ MAKI, Taichi 1974-01 application/pdf https://nipr.repo.nii.ac.jp/record/7729/files/KJ00002476729.pdf https://doi.org/10.15094/00007729 https://nipr.repo.nii.ac.jp/records/7729 jpn jpn 国立極地研究所 南極資料 48 37 51 AN00181831 00857289 https://nipr.repo.nii.ac.jp/record/7729/files/KJ00002476729.pdf https://doi.org/10.15094/00007729 https://nipr.repo.nii.ac.jp/records/7729 551.5 1974 ftnipr https://doi.org/10.15094/00007729 2025-03-19T10:19:57Z P(論文) The atmospheric turbulence in stable stratification was observed at Syowa Station in Antarctica during the period from February to December in 1970. Characteristics of atmospheric turbulence are analyzed in relation to the stability or the wind speed at the height of 20 m in surface air layer. Obtained results are as follows: U_<20> (horizontal mean wind speed at the height of 20m) is proportional to about -0.56 power of Ri (Richardson number). W_<20>/U_<20> (ratio of the vertical mean wind speed to U_<20> at the height of 20m) is independent of Ri. The standard deviation of the longitudinal wind speed (σ_U) is in direct proportion to the standard deviation of the lateral wind speed (σ_v). The relations between σ_U and σ_w (standard deviation of vertical wind speed) and between σ_v and σ_w are expressed with the two different equations, which have each transition point. Gustiness decreases with the increase of U_<20> below 8.5 m/s (U_<20>) and has a constant value above 8.5 m/s. Gust factor for five minutes decreases with the increase of U_<20>. The characteristic frequency distributions of three-dimensional wind components were made clear in comparison with the three typical weather condition. The Monin- Obukhov length and the energy dissipation rate increases in proportion to about -1.4 power of Ri and to about 2.7 power of U_<20> respectively in stable stratification. The characteristic time scales of longitudinal, lateral and vertical wind components increase with the increase of Ri and decrease with the increase of U_<20>, and the ratios of proportional components represent the cubic vortex, i.e., length:breadth:height = 6.3 : 1.9 : 1. The value of m obtained from Eq. (7) increases with the increase of Ri. departmental bulletin paper Other/Unknown Material Antarc* Antarctica National Institute of Polar Research Repository, Japan Syowa Station
spellingShingle 551.5
真木, 太一
マキ, タイチ
MAKI, Taichi
ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title_full ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title_fullStr ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title_full_unstemmed ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title_short ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
title_sort ナンキョク ショウワ キチ デノ チョウオンパ フウソク オンドケイ ニヨル タイキ ランリュウ カンソク
topic 551.5
topic_facet 551.5
url https://nipr.repo.nii.ac.jp/record/7729/files/KJ00002476729.pdf
https://doi.org/10.15094/00007729
https://nipr.repo.nii.ac.jp/records/7729