Grant H. McTainsh

ORCID: 0000-0001-9181-877X
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About
Contact & Profiles
Research Areas
  • Aeolian processes and effects
  • Atmospheric chemistry and aerosols
  • Atmospheric aerosols and clouds
  • Soil erosion and sediment transport
  • Geology and Paleoclimatology Research
  • Air Quality and Health Impacts
  • Atmospheric and Environmental Gas Dynamics
  • Marine and coastal ecosystems
  • Geological formations and processes
  • Hydrology and Sediment Transport Processes
  • Biocrusts and Microbial Ecology
  • Soil Geostatistics and Mapping
  • Air Quality Monitoring and Forecasting
  • Particle Dynamics in Fluid Flows
  • Fire effects on ecosystems
  • Marine Biology and Ecology Research
  • Radioactivity and Radon Measurements
  • Vehicle emissions and performance
  • Aerosol Filtration and Electrostatic Precipitation
  • Climate Change and Health Impacts
  • Rangeland and Wildlife Management
  • Geological and Geophysical Studies
  • Impact of Light on Environment and Health
  • Soil Carbon and Nitrogen Dynamics
  • Geochemistry and Geologic Mapping

Griffith University
2010-2019

Centre for Remote Health
2008-2009

Loughborough University
2003

Macquarie University
1980

Over the past 10 to 15 years there has been a rising interest in interactions between aeolian and fluvial processes from geomorphologists sedimentologists. This reflects recognition of limitations reductionist perspective examining single process systems understanding landform landscape development. paper focuses on rise aeolian-fluvial interaction research dryland environments. We first explore background contemporary situation then review existing at global/regional local scales. From this...

10.1191/0309133303pp386ra article EN Progress in Physical Geography Earth and Environment 2003-12-01

We present a simple theoretical land-surface classification that can be used to determine the location and temporal behaviour of preferential sources terrestrial dust emissions.The also provides information about likely nature sediments, their erodibility likelihood they will generate emissions under given conditions.The scheme is based on dual notions geomorphic type connectivity between units.We demonstrate map potential modern-day in Chihuahuan Desert, Lake Eyre Basin Taklamakan.Through...

10.1029/2011jf002061 article EN Journal of Geophysical Research Atmospheres 2011-10-11

The spatial and temporal variability of dust emissions from different surfaces in the Lake Eyre Basin, Australia is determined using MODIS data. For 2003–6 sources 529 plumes were classified: overall 37% originated areas aeolian deposits, 30% alluvial deposits floodplains 29% ephemeral lakes or playas. At this sub‐basin scale, relative importance source geomorphologies varied primarily response to sediment supply availability was not related transport capacity, suggesting Basin a...

10.1029/2008gl033928 article EN Geophysical Research Letters 2008-08-01

10.1016/j.geomorph.2006.07.028 article EN Geomorphology 2006-11-02

During late 2002 and early 2003, southern Australia was in the grip of drought experienced one its most active dust storm seasons last 40 years with large plumes frequently advected over adjacent Southern Ocean. We use meteorological records activity, satellite ocean color, aerosol optical depth data transport modeling to investigate deposition mineral from regions correlate it biological response phytoplankton standing stock as measured by chlorophyll a concentration 5 degree latitude bands...

10.1029/2009gb003541 article EN Global Biogeochemical Cycles 2010-04-29

Field experiments using a sand particle counter and an optical clarified the links between saltation dust emission under wet weakly crusted conditions in fallow field previously cultivated with wheat Australia. A crust was formed by impact of raindroplets after small precipitation events. little soil moisture enhanced strengths aggregation even though dried. Dust concentration proportional to friction wind velocity, but proportionality dependent on ground surface conditions, such as...

10.1029/2008jd009955 article EN Journal of Geophysical Research Atmospheres 2008-12-27

Around 30% of oceanic waters are high nitrate low chlorophyll (HNLC) where iron levels limit algal growth. HNLC have mainly been studied using shipboard and lab experiments. Since 1997, remote‐sensing phytoplankton via SeaWiFS Ocean Color has permitted monitoring the constancy this “HNLC condition,” i.e., spatial homogeneity temporal variability over annual cycles. These trends can be exploited, as episodic inputs should conspicuous by subsequent expression iron‐elevated stocks. Subantarctic...

10.1029/2002gb002020 article EN Global Biogeochemical Cycles 2004-02-24

10.1016/0277-3791(89)90039-5 article EN Quaternary Science Reviews 1989-01-01

Abstract Using meteorological records (1957–1984) in Australia, formal definitions are proposed of four types dust event: storms, blowing dust, whirls, and haze. Australia‐wide maps the extent these event presented.

10.1002/esp.3290120407 article EN Earth Surface Processes and Landforms 1987-07-01

Dust is an important vector for iron supply to the ocean, which subsequently impacts ocean productivity, atmospheric CO 2 concentrations, and hence global climate. Here, we synthesize processes influencing biogeochemistry of Australian dust compare them with those from other Southern Hemisphere sources. Our observations range soil physical properties abrasion cloud chamber chemistry experiments storms their dispersion deposition. We then present satellite impact episodic deposition events on...

10.1029/2007gc001813 article EN Geochemistry Geophysics Geosystems 2008-03-01

Abstract Soil carbon stores amount to 54% of the terrestrial pool and twice atmospheric pool, but soil organic ( SOC ) can be transient. There is an ongoing debate about whether soils are a net source or sink carbon, understanding role aeolian processes in erosion, transport deposition rudimentary. The impacts erosion by wind on global budget, its importance for accounting remain largely unknown. Current losses based assumption that content eroded material same as parent soils. However,...

10.1111/j.1365-2486.2012.02780.x article EN Global Change Biology 2012-07-11

Dust transported by Southern Hemisphere mid-latitude westerly winds from Australia and deposited in the Tasman Sea shows no evidence for stronger during last glacial maximum (LGM), compared to Holocene. Features of particle-size distributions dust do, however, indicate enhanced dry deposition LGM changing rainfall scavenging deglaciation early Holocene as climate ameliorated. From these results it appears that activation desert dunefields over 40% was result a reduction stabilizing...

10.1006/qres.1999.2084 article EN Quaternary Research 1999-11-01
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