Maps of the evolution of the Irrawaddy delta region, Myanmar, since 1850

We present a time series of coastline change for the Irrawaddy delta region of Myanmar using the earliest available navigation chart from 1850, and a set of topographic maps and satellite imagery dating from 1913 to 2006.

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    Data record related to this publication Maps of the evolution of the Irrawaddy delta region, Myanmar, since 1850
    Data Publication title Maps of the evolution of the Irrawaddy delta region, Myanmar, since 1850
  • Description

    We present a time series of coastline change for the Irrawaddy delta region of Myanmar using the earliest available navigation chart from 1850, and a set of topographic maps and satellite imagery dating from 1913 to 2006.

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    • Descriptor

      Despite the large sediment load delivered annually to the gulf by the Irrawaddy and Salween Rivers, the coastline has been largely stable for 156 years, advancing at an average rate of no more than 0.34 km per century since 1925. The long-term average rate of increase in land area across the study area between 1925 and 2006 is 4.2 km2/year, but this masks a period of more rapid accumulation between 1925 and 1989 (8.7 km2/year), followed by a period of net erosion at a rate of 13 km2/year until 2006. Less than 9% of the sediment load delivered to the study region by the Irrawaddy, Salween and Sittoung Rivers has contributed to the observed progradation, with the remainder being exported into the Gulf of Martaban to depths below low tide level, or filling any accommodation space created due to subsidence or sea level rise. In contrast to many deltas worldwide, we suggest that the coastline encompassing the Irrawaddy delta and the Salween River is more or less in equilibrium, and that sediment deposition currently balances subsidence and sea level rise. Myanmar has fewer large dams relative to its Asian neighbours, and the Salween is currently undammed. This is forecast to change in the next 5–10 years with extensive damming projects on the mainstem of the Salween under consideration or construction, and the sediment retention will cause losses in sediment supply to the Gulf of Martaban, and retreat of the delta. This could impact the densely populated delta region and Yangon, and further exacerbate the impacts of extreme events such as Cyclone Nargis in 2008.

    • Descriptor type Full
    • Descriptor

      Dataset contains 3 maps in pdf format.

    • Descriptor type Note
    • Descriptor
    • Descriptor type Full
  • Data type dataset
  • Keywords
    • Burma (Myanmar)
    • irrawaddy delta
    • Sediment flux
    • coastal sedimentation
    • salween
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  • Research themes
    Tropical Ecosystems, Conservation and Climate Change
    People and Societies in the Tropics
    FoR Codes (*)
    • 040310 - Sedimentology (040310)
    SEO Codes
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    Temporal (time) coverage
  • Start Date 1925/01/01
  • End Date 2006/01/01
  • Time Period
    Spatial (location) coverage
  • Locations
    Data Locations

    Type Location Notes
    Physical Location School of Earth and Environmental Science, James Cook University, PO Box 6811, Cairns, Qld 4870, AUSTRALIA, Phone Main Office: +61 7 4042 1211, Fax General: +61 7 4042 1284
    Attachment Maps_evolution_Irrawaddy_delta_region_Myanmar_since_1850.zip
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    Access conditions Open: free access under license
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    Citation Bird, Michael; Hedley, Peter J.; Robinson, Ruth A. J. (2012): Maps of the evolution of the Irrawaddy delta region, Myanmar, since 1850. James Cook University.