Summer Ionic Pollution of Easterly Cold Wind (Yamase) Fog at the Hachimantai Mountain Range in Northern Japan
To make clarify the pollution mechanism of the fog which occurs in Yamase, which is a local weather phenomenon in summer of cold wind blown from the edge of the Okhotsk Sea high-pressure region to the northern Pacific coast ofJapan, fog water samples were collected at Akita Hachimantai in 2003. The...
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| Veröffentlicht in: | INTERNATIONAL JOURNAL OF THE SOCIETY OF MATERIALS ENGINEERING FOR RESOURCES 2009, Vol.16 (1_2), p.1-4 |
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| container_title | INTERNATIONAL JOURNAL OF THE SOCIETY OF MATERIALS ENGINEERING FOR RESOURCES |
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| creator | Kikuchi, Ryoei Oba, Mahiro Yoshimura, Keiji Ozeki, Toru Kajikawa, Masahiro Ogawa, Nobuaki |
| description | To make clarify the pollution mechanism of the fog which occurs in Yamase, which is a local weather phenomenon in summer of cold wind blown from the edge of the Okhotsk Sea high-pressure region to the northern Pacific coast ofJapan, fog water samples were collected at Akita Hachimantai in 2003. The Yamase fog pollution level is lower than that of usual weather conditions. The total ion, nss-SO sub(4) super(2-) and NO sub(3) super(-) concentrations of fog water in Yamase are lower than those of other wind directions. Therefore the pH of fog water in Yamase is higher than other cases and the Yamase fog is not acidified. The component ratio of NH sub(4) super(+) of fog water in Yamase is higher than that of nss-SO sub(4) super(2-) because fog droplets would take up gaseous NH sub(3) generated from the ground surface, rather than (NH sub(4)) sub(2)SO sub(4). |
| doi_str_mv | 10.5188/ijsmer.16.1 |
| format | Article |
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The Yamase fog pollution level is lower than that of usual weather conditions. The total ion, nss-SO sub(4) super(2-) and NO sub(3) super(-) concentrations of fog water in Yamase are lower than those of other wind directions. Therefore the pH of fog water in Yamase is higher than other cases and the Yamase fog is not acidified. The component ratio of NH sub(4) super(+) of fog water in Yamase is higher than that of nss-SO sub(4) super(2-) because fog droplets would take up gaseous NH sub(3) generated from the ground surface, rather than (NH sub(4)) sub(2)SO sub(4).</description><identifier>ISSN: 1347-9725</identifier><identifier>EISSN: 1884-6629</identifier><identifier>DOI: 10.5188/ijsmer.16.1</identifier><language>eng</language><subject>Climatology ; Droplets ; Fog ; Materials engineering ; Mountains ; Pollution abatement ; Water pollution ; Weather</subject><ispartof>INTERNATIONAL JOURNAL OF THE SOCIETY OF MATERIALS ENGINEERING FOR RESOURCES, 2009, Vol.16 (1_2), p.1-4</ispartof><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c4991-977db63d9caeb3752cad20d05af38e8d7a580a3ad7f58aaf380fb9d89e1416213</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>Kikuchi, Ryoei</creatorcontrib><creatorcontrib>Oba, Mahiro</creatorcontrib><creatorcontrib>Yoshimura, Keiji</creatorcontrib><creatorcontrib>Ozeki, Toru</creatorcontrib><creatorcontrib>Kajikawa, Masahiro</creatorcontrib><creatorcontrib>Ogawa, Nobuaki</creatorcontrib><title>Summer Ionic Pollution of Easterly Cold Wind (Yamase) Fog at the Hachimantai Mountain Range in Northern Japan</title><title>INTERNATIONAL JOURNAL OF THE SOCIETY OF MATERIALS ENGINEERING FOR RESOURCES</title><description>To make clarify the pollution mechanism of the fog which occurs in Yamase, which is a local weather phenomenon in summer of cold wind blown from the edge of the Okhotsk Sea high-pressure region to the northern Pacific coast ofJapan, fog water samples were collected at Akita Hachimantai in 2003. The Yamase fog pollution level is lower than that of usual weather conditions. The total ion, nss-SO sub(4) super(2-) and NO sub(3) super(-) concentrations of fog water in Yamase are lower than those of other wind directions. Therefore the pH of fog water in Yamase is higher than other cases and the Yamase fog is not acidified. 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| source | J-STAGE Free; Open Access Titles of Japan; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Climatology Droplets Fog Materials engineering Mountains Pollution abatement Water pollution Weather |
| title | Summer Ionic Pollution of Easterly Cold Wind (Yamase) Fog at the Hachimantai Mountain Range in Northern Japan |
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