General aspects of land and sea breezes in western Seto Inland Sea and surrounding areas

被引:6
|
作者
Mizuma, M [1 ]
机构
[1] Kyoto Univ, Inst Res Reactor, Kumatori, Osaka 5900494, Japan
关键词
D O I
10.2151/jmsj1965.76.3_403
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The general aspects of land and sea breezes in western Seto Inland Sea and the surrounding areas are revealed from an analysis of the wind data obtained from the AMeDAS. The study area consists of Kyushu, the western part of Chugoku, and the western end of Shikoku surrounded by the Pacific Ocean, the East China Sea and the Sea of Japan, and the study area contains inland seas both wide and narrow. The day of the land and sea breeze in the study area is specified from the day when the land and sea breeze appears on a coastal area in the middle of the study area. The appearance of unexpected wind directions in the sea breeze situation in that area and the presence or not of the sea breeze in a nearby coastal area of smaller water body are taken into account in the classification of types of the land and sea breeze; this classification results in eight types. The type of sea breeze in both coastal areas is characterized by the developed sea breezes all over the area, except for the northeastern half of the coast facing the Sea of Japan in Chugoku and the eastern end of the Seto Inland Sea. Meeting of the sea breezes in the central region from either side of Chugoku and Kyushu is clearly seen in the afternoon. The other types are discussed and characteristics are compared with this fundamental type. The location of a significant land breeze in northwestern Shikoku is noted in relation to the well-known local gale "Hijikawa-arashi." The results from the previous study of the relationship between the occurrence of the land and sea breezes and the general meteorological conditions in Osaka Bay and the surrounding areas are shown to hold also for the present area. By coupling the features of the sea breeze in the present study area and those in Osaka Bay and the surrounding areas, the typical features of the sea breeze for a wider area of western Japan are revealed. The interrelation of the behavior of the land and sea breezes in these two areas is also discussed.
引用
收藏
页码:403 / 418
页数:16
相关论文
共 50 条
  • [21] Four new dendrochirotid holothurians collected from the Seto Inland Sea and the western part of the Sea of Japan, western Japan
    Yamana, Yusuke
    Nakaguchi, Kazumitsu
    Yamaguchi, Shuhei
    Katoh, Mikio
    Ogawa, Akito
    Ohtsuka, Susumu
    ZOOTAXA, 2021, 5023 (01) : 1 - 43
  • [22] Dynamics of microphytobenthic biomass in a coastal area of western Seto Inland Sea, Japan
    Yamaguchi, Hitomi
    Montani, Shigeru
    Tsutsumi, Hiroaki
    Hamada, Ken-Ichiro
    Ueda, Naoko
    Tada, Kuninao
    ESTUARINE COASTAL AND SHELF SCIENCE, 2007, 75 (04) : 423 - 432
  • [23] ENVIRONMENTAL-MANAGEMENT OF THE SETO INLAND SEA
    YASUI, H
    KOBAYASHI, E
    MARINE POLLUTION BULLETIN, 1991, 23 : 485 - 488
  • [24] Recovery of fish stocks in the Seto Inland Sea
    Nagai, T
    MARINE POLLUTION BULLETIN, 2003, 47 (1-6) : 126 - 131
  • [25] On land and sea breezes in Bayonne.
    Rouch
    COMPTES RENDUS HEBDOMADAIRES DES SEANCES DE L ACADEMIE DES SCIENCES, 1919, 168 : 313 - 315
  • [26] The Attractive Port Facilities of the Seto Inland Sea
    Sega, Yasuhiro
    Uchida, Normasa
    Kurokawa, Shigetomo
    COASTAL STRUCTURES 2011, VOL 1 & 2, 2013, : 1467 - 1468
  • [27] Distribution and production of meiobenthos in the Seto Inland Sea
    Tsujino, Mutsumi
    NIPPON SUISAN GAKKAISHI, 2024, 90 (01) : 19 - 27
  • [28] Spawning grounds of red sea bream in the east Seto Inland Sea
    Zenitani, Hiromu
    Onishi, Yosuke
    Obata, Yasuhiro
    FISHERIES SCIENCE, 2014, 80 (03) : 499 - 504
  • [29] Spawning grounds of red sea bream in the east Seto Inland Sea
    Hiromu Zenitani
    Yosuke Onishi
    Yasuhiro Obata
    Fisheries Science, 2014, 80 : 499 - 504
  • [30] ACOUSTIC SOUNDING OF LAND AND SEA BREEZES
    BACCI, P
    GIRAUD, C
    LONGHETTO, A
    RICHIARDONE, R
    BOUNDARY-LAYER METEOROLOGY, 1984, 28 (1-2) : 187 - 192