VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE
A river has the effect of climate alleviation not only as a cool spot but also as a so called wind channel. Statistical analysis shows the penetration of sea breeze front over Kanto plane classified into two cases, East or South-wind, influenced of synoptic scale. In these two cases the characterist...
Gespeichert in:
Veröffentlicht in: | PROCEEDINGS OF HYDRAULIC ENGINEERING 1998/02/20, Vol.42, pp.49-54 |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 54 |
---|---|
container_issue | |
container_start_page | 49 |
container_title | PROCEEDINGS OF HYDRAULIC ENGINEERING |
container_volume | 42 |
creator | FUKUDA, Tadahiro KASIMA, Masahiko SUZUKI, Jo KANDA, Manabu |
description | A river has the effect of climate alleviation not only as a cool spot but also as a so called wind channel. Statistical analysis shows the penetration of sea breeze front over Kanto plane classified into two cases, East or South-wind, influenced of synoptic scale. In these two cases the characteristics of penetration of sea breeze front were investigate on three scales (1) wide area (Kanto plane), (2) urban (Tokyo), (3) river (Ara river). Especially, as a result of meteorological field observation conducted along Ara river in detail in this summer, a typical urban river lead the sea breeze front to inland as a wind channel when South-wind matched with river flow. Around secondary scale, Tokyo, the penetration of sea breeze front are blocked over urban area because of heat island, then the front may be surrounding there. |
doi_str_mv | 10.2208/prohe.42.49 |
format | Article |
fullrecord | <record><control><sourceid>jstage_cross</sourceid><recordid>TN_cdi_crossref_primary_10_2208_prohe_42_49</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>article_prohe1990_42_0_42_0_49_article_char_en</sourcerecordid><originalsourceid>FETCH-LOGICAL-c1919-a4d9b2ede47622e42cb98a4d9d51b3dd2528b323a9756c3ee8339e4c58f01a3a3</originalsourceid><addsrcrecordid>eNo9kF9LwzAUxYMoOOae_AJ5l87865o8dl1qCzWV2ikKEtI0c5PpRroXv72t073cC-f-zr2XA8A1RlNCEL_d-93aTRmZMnEGRphzFggckXMwQgLPgohG7BJMum7TIERCFs0iMQJvT7LK0zyJ67xUsEzhc64WMMlipWQBZZrKpIZxVS57NVZwWc37WuW9C85fYJ1JeB8_DL5HGcN5JeWrhGlVqhoWuZJX4GJltp2b_PUxWKayTrKgKO_6m0VgscAiMKwVDXGt658ixDFiG8EHsQ1xQ9uWhIQ3lFAjonBmqXOcUuGYDfkKYUMNHYOb417rd13n3Urv_ebT-G-NkR7C0b_haEY0Ez29ONIf3cG8uxNr_GFjt-7IYiHQwP8XcRrbtfHafdEf3k1oBw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE</title><source>Freely Accessible Japanese Titles - check A-Z of ejournals</source><source>Alma/SFX Local Collection</source><source>J-STAGE</source><creator>FUKUDA, Tadahiro ; KASIMA, Masahiko ; SUZUKI, Jo ; KANDA, Manabu</creator><creatorcontrib>FUKUDA, Tadahiro ; KASIMA, Masahiko ; SUZUKI, Jo ; KANDA, Manabu</creatorcontrib><description>A river has the effect of climate alleviation not only as a cool spot but also as a so called wind channel. Statistical analysis shows the penetration of sea breeze front over Kanto plane classified into two cases, East or South-wind, influenced of synoptic scale. In these two cases the characteristics of penetration of sea breeze front were investigate on three scales (1) wide area (Kanto plane), (2) urban (Tokyo), (3) river (Ara river). Especially, as a result of meteorological field observation conducted along Ara river in detail in this summer, a typical urban river lead the sea breeze front to inland as a wind channel when South-wind matched with river flow. Around secondary scale, Tokyo, the penetration of sea breeze front are blocked over urban area because of heat island, then the front may be surrounding there.</description><identifier>ISSN: 0916-7374</identifier><identifier>EISSN: 1884-9172</identifier><identifier>DOI: 10.2208/prohe.42.49</identifier><language>eng</language><publisher>Japan Society of Civil Engineers</publisher><subject>Heat island ; Sea breeze front ; T-temp analysis ; Urban river ; Wind channel effect</subject><ispartof>PROCEEDINGS OF HYDRAULIC ENGINEERING, 1998/02/20, Vol.42, pp.49-54</ispartof><rights>by Japan Society of Civil Engineers</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,1877,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>FUKUDA, Tadahiro</creatorcontrib><creatorcontrib>KASIMA, Masahiko</creatorcontrib><creatorcontrib>SUZUKI, Jo</creatorcontrib><creatorcontrib>KANDA, Manabu</creatorcontrib><title>VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE</title><title>PROCEEDINGS OF HYDRAULIC ENGINEERING</title><addtitle>PROCEEDINGS OF HYDRAULIC ENGINEERING</addtitle><description>A river has the effect of climate alleviation not only as a cool spot but also as a so called wind channel. Statistical analysis shows the penetration of sea breeze front over Kanto plane classified into two cases, East or South-wind, influenced of synoptic scale. In these two cases the characteristics of penetration of sea breeze front were investigate on three scales (1) wide area (Kanto plane), (2) urban (Tokyo), (3) river (Ara river). Especially, as a result of meteorological field observation conducted along Ara river in detail in this summer, a typical urban river lead the sea breeze front to inland as a wind channel when South-wind matched with river flow. Around secondary scale, Tokyo, the penetration of sea breeze front are blocked over urban area because of heat island, then the front may be surrounding there.</description><subject>Heat island</subject><subject>Sea breeze front</subject><subject>T-temp analysis</subject><subject>Urban river</subject><subject>Wind channel effect</subject><issn>0916-7374</issn><issn>1884-9172</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><recordid>eNo9kF9LwzAUxYMoOOae_AJ5l87865o8dl1qCzWV2ikKEtI0c5PpRroXv72t073cC-f-zr2XA8A1RlNCEL_d-93aTRmZMnEGRphzFggckXMwQgLPgohG7BJMum7TIERCFs0iMQJvT7LK0zyJ67xUsEzhc64WMMlipWQBZZrKpIZxVS57NVZwWc37WuW9C85fYJ1JeB8_DL5HGcN5JeWrhGlVqhoWuZJX4GJltp2b_PUxWKayTrKgKO_6m0VgscAiMKwVDXGt658ixDFiG8EHsQ1xQ9uWhIQ3lFAjonBmqXOcUuGYDfkKYUMNHYOb417rd13n3Urv_ebT-G-NkR7C0b_haEY0Ez29ONIf3cG8uxNr_GFjt-7IYiHQwP8XcRrbtfHafdEf3k1oBw</recordid><startdate>1998</startdate><enddate>1998</enddate><creator>FUKUDA, Tadahiro</creator><creator>KASIMA, Masahiko</creator><creator>SUZUKI, Jo</creator><creator>KANDA, Manabu</creator><general>Japan Society of Civil Engineers</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>1998</creationdate><title>VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE</title><author>FUKUDA, Tadahiro ; KASIMA, Masahiko ; SUZUKI, Jo ; KANDA, Manabu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1919-a4d9b2ede47622e42cb98a4d9d51b3dd2528b323a9756c3ee8339e4c58f01a3a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Heat island</topic><topic>Sea breeze front</topic><topic>T-temp analysis</topic><topic>Urban river</topic><topic>Wind channel effect</topic><toplevel>online_resources</toplevel><creatorcontrib>FUKUDA, Tadahiro</creatorcontrib><creatorcontrib>KASIMA, Masahiko</creatorcontrib><creatorcontrib>SUZUKI, Jo</creatorcontrib><creatorcontrib>KANDA, Manabu</creatorcontrib><collection>CrossRef</collection><jtitle>PROCEEDINGS OF HYDRAULIC ENGINEERING</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>FUKUDA, Tadahiro</au><au>KASIMA, Masahiko</au><au>SUZUKI, Jo</au><au>KANDA, Manabu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE</atitle><jtitle>PROCEEDINGS OF HYDRAULIC ENGINEERING</jtitle><addtitle>PROCEEDINGS OF HYDRAULIC ENGINEERING</addtitle><date>1998</date><risdate>1998</risdate><volume>42</volume><spage>49</spage><epage>54</epage><pages>49-54</pages><issn>0916-7374</issn><eissn>1884-9172</eissn><abstract>A river has the effect of climate alleviation not only as a cool spot but also as a so called wind channel. Statistical analysis shows the penetration of sea breeze front over Kanto plane classified into two cases, East or South-wind, influenced of synoptic scale. In these two cases the characteristics of penetration of sea breeze front were investigate on three scales (1) wide area (Kanto plane), (2) urban (Tokyo), (3) river (Ara river). Especially, as a result of meteorological field observation conducted along Ara river in detail in this summer, a typical urban river lead the sea breeze front to inland as a wind channel when South-wind matched with river flow. Around secondary scale, Tokyo, the penetration of sea breeze front are blocked over urban area because of heat island, then the front may be surrounding there.</abstract><pub>Japan Society of Civil Engineers</pub><doi>10.2208/prohe.42.49</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0916-7374 |
ispartof | PROCEEDINGS OF HYDRAULIC ENGINEERING, 1998/02/20, Vol.42, pp.49-54 |
issn | 0916-7374 1884-9172 |
language | eng |
recordid | cdi_crossref_primary_10_2208_prohe_42_49 |
source | Freely Accessible Japanese Titles - check A-Z of ejournals; Alma/SFX Local Collection; J-STAGE |
subjects | Heat island Sea breeze front T-temp analysis Urban river Wind channel effect |
title | VERIFICATION OF WIND CHANNEL EFFECT AROUND AN URBAN RIVER BY THE MAP OF SEA BREEZE FRONT LINE |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-11T18%3A32%3A08IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstage_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=VERIFICATION%20OF%20WIND%20CHANNEL%20EFFECT%20AROUND%20AN%20URBAN%20RIVER%20BY%20THE%20MAP%20OF%20SEA%20BREEZE%20FRONT%20LINE&rft.jtitle=PROCEEDINGS%20OF%20HYDRAULIC%20ENGINEERING&rft.au=FUKUDA,%20Tadahiro&rft.date=1998&rft.volume=42&rft.spage=49&rft.epage=54&rft.pages=49-54&rft.issn=0916-7374&rft.eissn=1884-9172&rft_id=info:doi/10.2208/prohe.42.49&rft_dat=%3Cjstage_cross%3Earticle_prohe1990_42_0_42_0_49_article_char_en%3C/jstage_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |