Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment

Flooding appears to be increasing in Kelantan, Malaysia, in terms of frequency as well as magnitude. This is likely to be due to changes in precipitation, but may also be contributed to by land use change. The Mann-Kendall non-parametric method was used to test for trends in streamflow and precipita...

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Published in:International Journal of Climatology
Main Author: Adnan N.A.; Atkinson P.M.
Format: Article
Language:English
Published: 2011
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-79954582798&doi=10.1002%2fjoc.2112&partnerID=40&md5=95689c390be1c4d3b85939828a5ae1e5
id 2-s2.0-79954582798
spelling 2-s2.0-79954582798
Adnan N.A.; Atkinson P.M.
Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
2011
International Journal of Climatology
31
6
10.1002/joc.2112
https://www.scopus.com/inward/record.uri?eid=2-s2.0-79954582798&doi=10.1002%2fjoc.2112&partnerID=40&md5=95689c390be1c4d3b85939828a5ae1e5
Flooding appears to be increasing in Kelantan, Malaysia, in terms of frequency as well as magnitude. This is likely to be due to changes in precipitation, but may also be contributed to by land use change. The Mann-Kendall non-parametric method was used to test for trends in streamflow and precipitation at the 90% significance level. Several significant trends in streamflow were found for the upstream (River Galas) and downstream (River Kelantan) sub-catchments for all variables (annual, seasonal and monthly time-series). In particular, streamflow increased in all seasons in the upstream sub-catchment, but increased in the wet season and decreased in the dry season downstream. Several trends were also observed for precipitation. Precipitation trends were increasing in the wet season and decreasing in the dry season for both upstream and downstream sub-catchments. Analysis of land use change revealed that most changes occurred through conversion of forest to agricultural land (i.e. rubber and oil palm), predominantly in the upstream sub-catchment. The analysis suggests a clear association between streamflow change and precipitation change, but also reveals that land use change may be an important contributing factor, particularly in the upstream sub-catchment. © 2010 Royal Meteorological Society.

10970088
English
Article

author Adnan N.A.; Atkinson P.M.
spellingShingle Adnan N.A.; Atkinson P.M.
Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
author_facet Adnan N.A.; Atkinson P.M.
author_sort Adnan N.A.; Atkinson P.M.
title Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
title_short Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
title_full Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
title_fullStr Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
title_full_unstemmed Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
title_sort Exploring the impact of climate and land use changes on streamflow trends in a monsoon catchment
publishDate 2011
container_title International Journal of Climatology
container_volume 31
container_issue 6
doi_str_mv 10.1002/joc.2112
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-79954582798&doi=10.1002%2fjoc.2112&partnerID=40&md5=95689c390be1c4d3b85939828a5ae1e5
description Flooding appears to be increasing in Kelantan, Malaysia, in terms of frequency as well as magnitude. This is likely to be due to changes in precipitation, but may also be contributed to by land use change. The Mann-Kendall non-parametric method was used to test for trends in streamflow and precipitation at the 90% significance level. Several significant trends in streamflow were found for the upstream (River Galas) and downstream (River Kelantan) sub-catchments for all variables (annual, seasonal and monthly time-series). In particular, streamflow increased in all seasons in the upstream sub-catchment, but increased in the wet season and decreased in the dry season downstream. Several trends were also observed for precipitation. Precipitation trends were increasing in the wet season and decreasing in the dry season for both upstream and downstream sub-catchments. Analysis of land use change revealed that most changes occurred through conversion of forest to agricultural land (i.e. rubber and oil palm), predominantly in the upstream sub-catchment. The analysis suggests a clear association between streamflow change and precipitation change, but also reveals that land use change may be an important contributing factor, particularly in the upstream sub-catchment. © 2010 Royal Meteorological Society.
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