Relationship between landslide size and rainfall conditions in Taiwan
This study analyzed the size of 172 rainfall-induced landslides in Taiwan during 2006–2012. Comparing the landslide size with rainfall conditions, this study found that large and deep landslides usually occurred due to long-duration and moderate-intensity rainfall (11.5–31.0 mm/h; 26.5–62.5 h), wher...
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Veröffentlicht in: | Landslides 2017-06, Vol.14 (3), p.1235-1240 |
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description | This study analyzed the size of 172 rainfall-induced landslides in Taiwan during 2006–2012. Comparing the landslide size with rainfall conditions, this study found that large and deep landslides usually occurred due to long-duration and moderate-intensity rainfall (11.5–31.0 mm/h; 26.5–62.5 h), whereas small and shallow landslides occurred in a wide range of rainfall intensity and duration (8.5–31.0 mm/h; 4.0–62.5 h). This observation is ascribable to the fact that large and deep landslides need a high ground water level caused by a prolonged rainfall. Concerning the area of landslides, their frequency–area distribution correlates well with a power law relation having an exponent of −1.1 ± 0.07, over the range 6.3 × 10
2
to 3.1 × 10
6
m
2
. The slope of the power law relation for the size–frequency distribution of landslides in Taiwan is lower than those for other areas around the world. This indicates that for the same total area or total number of landslides, the proportion of large landslides is higher in Taiwan than in other areas. |
doi_str_mv | 10.1007/s10346-016-0790-7 |
format | Article |
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2
to 3.1 × 10
6
m
2
. The slope of the power law relation for the size–frequency distribution of landslides in Taiwan is lower than those for other areas around the world. This indicates that for the same total area or total number of landslides, the proportion of large landslides is higher in Taiwan than in other areas.</description><identifier>ISSN: 1612-510X</identifier><identifier>EISSN: 1612-5118</identifier><identifier>DOI: 10.1007/s10346-016-0790-7</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Agriculture ; Area ; Civil Engineering ; Distribution ; Duration ; Earth and Environmental Science ; Earth Sciences ; Frequency distribution ; Geography ; Groundwater ; Groundwater levels ; Landslides ; Landslides & mudslides ; Natural Hazards ; Power law ; Rain ; Rainfall ; Rainfall intensity ; Technical Note ; Water levels</subject><ispartof>Landslides, 2017-06, Vol.14 (3), p.1235-1240</ispartof><rights>Springer-Verlag Berlin Heidelberg 2016</rights><rights>Landslides is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a405t-71983996a7d215691da7a538d61399474cb3c9050a5b5a6032ebff291c36d93e3</citedby><cites>FETCH-LOGICAL-a405t-71983996a7d215691da7a538d61399474cb3c9050a5b5a6032ebff291c36d93e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10346-016-0790-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10346-016-0790-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Chen, Chi-Wen</creatorcontrib><creatorcontrib>Oguchi, Takashi</creatorcontrib><creatorcontrib>Hayakawa, Yuichi S.</creatorcontrib><creatorcontrib>Saito, Hitoshi</creatorcontrib><creatorcontrib>Chen, Hongey</creatorcontrib><title>Relationship between landslide size and rainfall conditions in Taiwan</title><title>Landslides</title><addtitle>Landslides</addtitle><description>This study analyzed the size of 172 rainfall-induced landslides in Taiwan during 2006–2012. Comparing the landslide size with rainfall conditions, this study found that large and deep landslides usually occurred due to long-duration and moderate-intensity rainfall (11.5–31.0 mm/h; 26.5–62.5 h), whereas small and shallow landslides occurred in a wide range of rainfall intensity and duration (8.5–31.0 mm/h; 4.0–62.5 h). This observation is ascribable to the fact that large and deep landslides need a high ground water level caused by a prolonged rainfall. Concerning the area of landslides, their frequency–area distribution correlates well with a power law relation having an exponent of −1.1 ± 0.07, over the range 6.3 × 10
2
to 3.1 × 10
6
m
2
. The slope of the power law relation for the size–frequency distribution of landslides in Taiwan is lower than those for other areas around the world. This indicates that for the same total area or total number of landslides, the proportion of large landslides is higher in Taiwan than in other areas.</description><subject>Agriculture</subject><subject>Area</subject><subject>Civil Engineering</subject><subject>Distribution</subject><subject>Duration</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Frequency distribution</subject><subject>Geography</subject><subject>Groundwater</subject><subject>Groundwater levels</subject><subject>Landslides</subject><subject>Landslides & mudslides</subject><subject>Natural Hazards</subject><subject>Power law</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Rainfall intensity</subject><subject>Technical Note</subject><subject>Water levels</subject><issn>1612-510X</issn><issn>1612-5118</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kE1LxDAQhoMouK7-AG8Bz9WZpGmaoyzrBywIsoK3kLapZqlpTbos-uvNWhEvHob5ep8ZeAk5R7hEAHkVEXheZIAppIJMHpAZFsgygVge_tbwfExOYtwAMAVczcjy0XZmdL2Pr26glR131nraGd_EzjWWRvdpaepoMM63puto3fvGfRPUebo2bmf8KTlKu2jPfvKcPN0s14u7bPVwe7-4XmUmBzFmElXJlSqMbBiKQmFjpBG8bApM41zmdcVrBQKMqIQpgDNbtS1TWPOiUdzyObmY7g6hf9_aOOpNvw0-vdRYKlWyUpSYVDip6tDHGGyrh-DeTPjQCHrvlp7c0sktvXdLy8SwiYlJ619s-HP5X-gLA8VryA</recordid><startdate>20170601</startdate><enddate>20170601</enddate><creator>Chen, Chi-Wen</creator><creator>Oguchi, Takashi</creator><creator>Hayakawa, Yuichi S.</creator><creator>Saito, Hitoshi</creator><creator>Chen, Hongey</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20170601</creationdate><title>Relationship between landslide size and rainfall conditions in Taiwan</title><author>Chen, Chi-Wen ; Oguchi, Takashi ; Hayakawa, Yuichi S. ; Saito, Hitoshi ; Chen, Hongey</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a405t-71983996a7d215691da7a538d61399474cb3c9050a5b5a6032ebff291c36d93e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Agriculture</topic><topic>Area</topic><topic>Civil Engineering</topic><topic>Distribution</topic><topic>Duration</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Frequency distribution</topic><topic>Geography</topic><topic>Groundwater</topic><topic>Groundwater levels</topic><topic>Landslides</topic><topic>Landslides & mudslides</topic><topic>Natural Hazards</topic><topic>Power law</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Rainfall intensity</topic><topic>Technical Note</topic><topic>Water levels</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chen, Chi-Wen</creatorcontrib><creatorcontrib>Oguchi, Takashi</creatorcontrib><creatorcontrib>Hayakawa, Yuichi S.</creatorcontrib><creatorcontrib>Saito, Hitoshi</creatorcontrib><creatorcontrib>Chen, Hongey</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Science Journals</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Landslides</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Chi-Wen</au><au>Oguchi, Takashi</au><au>Hayakawa, Yuichi S.</au><au>Saito, Hitoshi</au><au>Chen, Hongey</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationship between landslide size and rainfall conditions in Taiwan</atitle><jtitle>Landslides</jtitle><stitle>Landslides</stitle><date>2017-06-01</date><risdate>2017</risdate><volume>14</volume><issue>3</issue><spage>1235</spage><epage>1240</epage><pages>1235-1240</pages><issn>1612-510X</issn><eissn>1612-5118</eissn><abstract>This study analyzed the size of 172 rainfall-induced landslides in Taiwan during 2006–2012. Comparing the landslide size with rainfall conditions, this study found that large and deep landslides usually occurred due to long-duration and moderate-intensity rainfall (11.5–31.0 mm/h; 26.5–62.5 h), whereas small and shallow landslides occurred in a wide range of rainfall intensity and duration (8.5–31.0 mm/h; 4.0–62.5 h). This observation is ascribable to the fact that large and deep landslides need a high ground water level caused by a prolonged rainfall. Concerning the area of landslides, their frequency–area distribution correlates well with a power law relation having an exponent of −1.1 ± 0.07, over the range 6.3 × 10
2
to 3.1 × 10
6
m
2
. The slope of the power law relation for the size–frequency distribution of landslides in Taiwan is lower than those for other areas around the world. This indicates that for the same total area or total number of landslides, the proportion of large landslides is higher in Taiwan than in other areas.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10346-016-0790-7</doi><tpages>6</tpages></addata></record> |
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subjects | Agriculture Area Civil Engineering Distribution Duration Earth and Environmental Science Earth Sciences Frequency distribution Geography Groundwater Groundwater levels Landslides Landslides & mudslides Natural Hazards Power law Rain Rainfall Rainfall intensity Technical Note Water levels |
title | Relationship between landslide size and rainfall conditions in Taiwan |
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