Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh

The major landslide events that occurred in Chittagong City in 2007 and 2008 have caused the death of about 140 people and incurred a considerable amount of property loss.At least ten landslide events occurred during the period of 2000–2009, with mainly rainfall as the triggering factor.The critical...

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Main Authors: Khan, Younus Ahmed, Lateh, Habibah, Baten, Md Azizul, Kamil, Anton Abdulbasah
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Published: Springer International Publishing AG 2012
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Online Access:http://repo.uum.edu.my/12849/
http://dx.doi.org/10.1007/s12665-011-1483-0
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spelling my.uum.repo.128492014-12-18T03:43:26Z http://repo.uum.edu.my/12849/ Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh Khan, Younus Ahmed Lateh, Habibah Baten, Md Azizul Kamil, Anton Abdulbasah GB Physical geography The major landslide events that occurred in Chittagong City in 2007 and 2008 have caused the death of about 140 people and incurred a considerable amount of property loss.At least ten landslide events occurred during the period of 2000–2009, with mainly rainfall as the triggering factor.The critical rainfall condition of the landslide events was analyzed with Gumbel’s extreme value distribution using the historical rainfall–landslide data.The antecedent rainfalls were used for Gumbel’s distribution for the critical rainfall intensity–durations of each historical landslide event.Landslides were correlated with the monthly average as well as the percentile rank of monthly median rainfall. The regression relationship between 30 days of absolute antecedent rainfall intensity (I) and corresponding duration (D) of rainfall responsible for the landslides in the study area was found as I = −15.8ln(D) + 60.49.The calibrated antecedent rainfall analysis showed a relation between I and D as I = −40.5ln(D) + 162.5.The major recent landslide events were related to the extreme rainfall intensities (>40 mm/day) having short period of time (2–7 days).All the major landslide events occurred at much higher rainfall amount compared to the monthly average.However, these rainfall thresholds were statistically based and were not defined hydrological response of rainfall to the soil, as well as other geological conditions associated with slopes. Springer International Publishing AG 2012 Article PeerReviewed Khan, Younus Ahmed and Lateh, Habibah and Baten, Md Azizul and Kamil, Anton Abdulbasah (2012) Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh. Environmental Earth Sciences, 67 (1). pp. 97-106. ISSN 1866-6280 http://dx.doi.org/10.1007/s12665-011-1483-0 doi:10.1007/s12665-011-1483-0
institution Universiti Utara Malaysia
building UUM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Utara Malaysia
content_source UUM Institutionali Repository
url_provider http://repo.uum.edu.my/
topic GB Physical geography
spellingShingle GB Physical geography
Khan, Younus Ahmed
Lateh, Habibah
Baten, Md Azizul
Kamil, Anton Abdulbasah
Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
description The major landslide events that occurred in Chittagong City in 2007 and 2008 have caused the death of about 140 people and incurred a considerable amount of property loss.At least ten landslide events occurred during the period of 2000–2009, with mainly rainfall as the triggering factor.The critical rainfall condition of the landslide events was analyzed with Gumbel’s extreme value distribution using the historical rainfall–landslide data.The antecedent rainfalls were used for Gumbel’s distribution for the critical rainfall intensity–durations of each historical landslide event.Landslides were correlated with the monthly average as well as the percentile rank of monthly median rainfall. The regression relationship between 30 days of absolute antecedent rainfall intensity (I) and corresponding duration (D) of rainfall responsible for the landslides in the study area was found as I = −15.8ln(D) + 60.49.The calibrated antecedent rainfall analysis showed a relation between I and D as I = −40.5ln(D) + 162.5.The major recent landslide events were related to the extreme rainfall intensities (>40 mm/day) having short period of time (2–7 days).All the major landslide events occurred at much higher rainfall amount compared to the monthly average.However, these rainfall thresholds were statistically based and were not defined hydrological response of rainfall to the soil, as well as other geological conditions associated with slopes.
format Article
author Khan, Younus Ahmed
Lateh, Habibah
Baten, Md Azizul
Kamil, Anton Abdulbasah
author_facet Khan, Younus Ahmed
Lateh, Habibah
Baten, Md Azizul
Kamil, Anton Abdulbasah
author_sort Khan, Younus Ahmed
title Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
title_short Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
title_full Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
title_fullStr Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
title_full_unstemmed Critical antecedent rainfall conditions for shallow landslides in Chittagong City of Bangladesh
title_sort critical antecedent rainfall conditions for shallow landslides in chittagong city of bangladesh
publisher Springer International Publishing AG
publishDate 2012
url http://repo.uum.edu.my/12849/
http://dx.doi.org/10.1007/s12665-011-1483-0
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score 13.18916