| Item type |
紀要論文 / Departmental Bulletin Paper(1) |
| 公開日 |
2010-11-30 |
| タイトル |
|
|
タイトル |
The relationship between double thermal inversions and thermal belt in the mt. yatsugatake area, central japan |
| 言語 |
|
|
言語 |
eng |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
double thermal inversions |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
thermal belt |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
sonde observation |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
adiabatic warming by subsidence flow |
| キーワード |
|
|
主題Scheme |
Other |
|
主題 |
radiative surface cooling |
| 資源タイプ |
|
|
資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
|
資源タイプ |
departmental bulletin paper |
| 著者 |
Tanaka, Hiroharu
Tanimoto, Youichi
Mikami, Takehiko
|
| 著者(ヨミ) |
タナカ, ヒロハル
タニモト, ヨウイチ
ミカミ, タケヒコ
|
| 抄録 |
|
|
内容記述タイプ |
Abstract |
|
内容記述 |
We examined a thermal structure on the mountain slope over clean calm nights at the southern Mt. Yatsugatake, central Japan. Meteorological observations showed double thermal inversions over the slope. The upper one appeared between approximately 1800 m and 2000 m a.s.l. (1100 m and 1300 m from surface), and the lower one, between 700 m and 950 m a.s.l. (surface and 250 m from surface). Successive snapshots of a thermography showed horizontal bands of this upper inversion clearly. Radiosonde data in this field indicated that this thermal structure on the slope was associated with the thermo-dynamical processes in the atmospheric boundary layer: the upper inversion forced by the adiabatic warming by subsidence but the lower one forced by the radiative surface cooling. |
| 書誌情報 |
Geographical Reports of Tokyo Metropolitan University
号 33,
p. 21-31,
発行日 1998
|
| ISSN |
|
|
収録物識別子タイプ |
ISSN |
|
収録物識別子 |
03868710 |
| 書誌レコードID |
|
|
収録物識別子タイプ |
NCID |
|
収録物識別子 |
AA00200173 |
| 著者版フラグ |
|
|
出版タイプ |
VoR |
|
出版タイプResource |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
| 出版者 |
|
|
出版者 |
Department of Geography, Tokyo Metropolitan University |
20005-33-002.pdf (528.9 kB)
