Articles

Catchment-Coast Interactions of the Asian Region: APN Recent Research Topics

Expand
  • Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing 210093,China

Received date: 2006-02-07

  Revised date: 2006-06-15

  Online published: 2006-07-15

Abstract

Across the Asia-Pacific region, coastal areas are highly varied in the status of water, sediment, nutrient, and pollutant discharges from catchments. Such changes are mainly caused by extremely intense human activities in the catchment basins, ranging from construction of numerous dams to the large scale utilization of chemical fertilisers, and, to less extent, by climate and sea level changes. The nature of catchment-coast interactions means that changes of material fluxes will result in morphological, environmental, and ecosystem changes in the catchment areas, estuaries, and adjacent coastal waters. In order to improve management of regional development under the changed conditions of the catchment-coast system, it is proposed that research should: (1) define the various changes quantitatively, on the basis of in situ monitoring and measurements; (2) understand the basic processes and mechanisms that are responsible for the changes; (3) develop new methods and techniques for the prediction of future changes, in terms of both trends and magnitude of fluctuations; and (4) apply the findings obtained from these studies to future catchment-coast development and management practices. Recently, a workshop was organized by APN (Asian Pacific Network for Global Change Research) to discuss about future research topics for the region. Following the workshop, the author completed a document for suggestions of future research directions within the study area of “Catchment-Coast Interactions”. The present contribution is a short summary of the document.

Cite this article

Gao Shu . Catchment-Coast Interactions of the Asian Region: APN Recent Research Topics[J]. Advances in Earth Science, 2006 , 21(7) : 680 -686 . DOI: 10.11867/j.issn.1001-8166.2006.07.0680

References

[1] Loicz Ipo. Land-Ocean Interactions in the Coastal Zone Science Plan and Implementation Strategy (IGBP Report 51 / IHDP Report 18) [M]. Stockholm: IGBP Secretariat,2005.

[2] Crossland C J, Kremer H H, Lindeboon H J, et al, eds. Coastal Fluxes in the Anthropocene [C]. Berlin: Springer-Verlag, 2005.

[3] Salomons W. European Catchments: Catchment Changes and Their Impact on the Coast[M]. Amsterdam: Institute for Environmental Studies, 2004.

[4] Margins Office. NSF Margins Program Science Plan 2004[M]. New York: Columbia University, 2003.

[5] Milliman J, Syvistski J P M. Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers[J]. Journal of Geology, 1992, 100:525-544.

[6] Gao S. Catchment-coastal interaction in the Asia-Pacific region[C]Harvey N, ed. APN Coastal Zone Management Synthesis. Amsterdam: Springer-Verlag, 2006:65-90.

[7] Milliman J, Farnsworth K L, Albertin C S. Flux and fate of fluvial sediments leaving large islands in the East Indies[J]. Journal of Sea Research, 1999, 41: 97-107.

[8] World Commission on Dams. Dams and Development:A New Framework for Decision-making[M]. London:Earthscan,2000.

[9] Jian-an Sheng, An-zheng Liao. Erosion control in South China[J]. Catena, 1997, 29(2):211-221.

[10] Ahmad T, Khanna P P, Chakrapani G J, et al. Geochemical characteristics of water and sediment of the Indus River, Trans-Himalaya, India: Constraints on weathering and erosion[J]. Journal of Southeast Asian Earth Sciences, 1998, 16:333-346.

[11] Gao S. Modeling the limit of the Changjiang River delta growth[J]. Geomorphology, 2006, in press.

[12] Yang S L, Belkin I M, Belkina A I, et al. Delta response to decline in sediment supply from the Yangtze River: Evidence of the recent four decades and expectations for the next half-century[J]. Estuarine, Coastal and Shelf Science, 2003, 57:689-699.

[13] Dyer K R. Estuaries: A Physical Introduction (2nd edition)[M]. Chichester:John Wiley, 1997.

[14] Lewis R. Dispersion in Estuaries and Coastal Waters[M]. Chichester:John Wiley, 1997.

[15] Paola C. Quantitative models of sedimentary basin filling[J]. Sedimentology, 2000, 47 (suppl. 1):121-178.

[16] Gao S, Jia J J. Accumulation of fine-grained sediment and organic carbon in a small tidal basin: Yuehu, Shandong Peninsula, China[J]. Regional Environmental Change, 2004, 4:63-69.

[17] De Vriend H J, Capobianco M, Chesher T, et al. Approaches to long-term modeling of coastal morphology: A review[J]. Coastal Engineering, 1993, 21:225-269.

[18] Owens P N, Walling D E, Leeks G J L. Tracing fluvial suspended sediment sources in the catchment of the River Tweed, Scotland, using composite fingerprints and a numerical mixing model[C]Foster I D L, ed. Tracers in Geomorphology.Chichester:John Wiley, 2000:291-308.

[19] Bhandari S, Maurya D M, Chamyal L S.Late Pleistocene alluvial plain sedimentation in Lower Narmada Valley, Western India: Palaeoenvironmental implications[J]. Journal of Asian Earth Sciences,2005,24:433-444.

[20] Mitsch W J, Gosselink J G. Wetlands (3rd edition)[M]. New York:John Wiley, 2000.

[21] Kathiresan K, Bingham B L. Biology of mangroves and mangrove ecosystems[J]. Advances in Marine Biology,2001, 40:83-251.

[22] Coles S L, Brown B E. Coral bleaching capacity for acclimatization and adaptation[J]. Advances in Marine Biology,2003, 46:183-223.

Options
Outlines

/