Show simple item record

dc.contributor.authorChappell, Adrianen_US
dc.contributor.authorMcTainsh, Granten_US
dc.contributor.authorStrong, Craigen_US
dc.date.accessioned2017-05-03T11:22:07Z
dc.date.available2017-05-03T11:22:07Z
dc.date.issued2003en_US
dc.date.modified2009-10-01T05:51:19Z
dc.identifier.issn01979337en_US
dc.identifier.doi10.1002/esp.463en_AU
dc.identifier.urihttp://hdl.handle.net/10072/5972
dc.description.abstractLittle is known about the spatial and temporal scales of variation in aeolian processes. Studies that aim to investigate surface erodibility often sample aeolian sediment transport at the nodes of a regular grid of arbitrary size. Few aeolian transport investigations have the resources to obtain sufficient samples to produce reliable models for mapping the spatial variation of transport. This study reports the use of an innovative nested strategy for sampling multiple spatial scales simultaneously using 40 sediment samplers. Reliable models of the spatial variation in aeolian sediment transport were produced and used for ordinary punctual kriging and stochastic simulated annealing to produce maps for several wind erosion events over a 25 km2 playa in western Queensland, Australia. The results support the existence of a highly dynamic wind erosion system that was responding to possibly cyclic variation in the availability of material and fluctuations in wind energy. The spatial scale of transport was considerably larger than the small scale expected of the factors controlling surface erodibility. Thus, it appears that transport cannot be used as a surrogate of erodibility at the scale of this investigation. Simulation maps of transport provided considerably more information than those from kriging about the variability in aeolian sediment transport and its possible controlling factors. The proposed optimal sampling strategy involves a nested approach using ca 50 samplers.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherJohn Wiley and Sons Ltd.en_US
dc.publisher.placeUnited Kingdomen_US
dc.publisher.urihttp://www3.interscience.wiley.com/journal/117935722/grouphome/home.htmlen_AU
dc.relation.ispartofpagefrom567en_US
dc.relation.ispartofpageto585en_US
dc.relation.ispartofedition2003en_US
dc.relation.ispartofjournalEarth Surface Processes and Landformsen_US
dc.relation.ispartofvolume28en_US
dc.subject.fieldofresearchcode260114en_US
dc.titleUsing geostatistics to elucidate temporal change in the spatial variation of aeolian sediment transporten_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.rights.copyrightCopyright 2003 John Wiley & Sons, Ltd. Self-archiving of the author-manuscript version is not yet supported by this publisher. Please refer to the journal link for access to the definitive, published version or contact the author for more information.en_AU
gro.date.issued2003
gro.hasfulltextNo Full Text


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

  • Journal articles
    Contains articles published by Griffith authors in scholarly journals.

Show simple item record