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Agricultural Drought Indices - US Department of Agriculture

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In Australia, an approach was developed that would capture a multitude <strong>of</strong> agricultural drought<br />

assessment methods to assist drought declarations, especially drought exceptional circumstances.<br />

This approach was pursued through the National <strong>Agricultural</strong> Monitoring System (NAMS) and<br />

appeared to contain all the requirements that would deliver scientific objectivity into the agricultural<br />

drought assessment process. Indeed, a science advisory group was included which would<br />

oversee that the “best indices and production models in Australia” (whether for rainfed cereals,<br />

pastures, or irrigated systems) were employed in order to help overcome disputes within the<br />

scientific community and between various scientific institutions regarding drought status. It is not<br />

known why NAMS has recently been discontinued.<br />

Valuable assessments have been made in Australia that show that when various drought indices<br />

are compared, especially for grazing enterprise purposes, in respect to rainfall, soil moisture,<br />

pasture growth, animal liveweight, and generated income, they will generally all identify the major<br />

droughts in the relevant regions <strong>of</strong> Australia (Stafford-Smith and McKeon 1998).<br />

However, Stafford-Smith and McKeon (1998) point out these measures may well differ in respect<br />

to ranking the more contentious droughts in which affected farmers may be very sensitive in<br />

eligibility for associated “exceptional drought” assistance (severe droughts <strong>of</strong> a 1 in 20 to 25 year<br />

occurrence). As individual grazing properties in Australia can be relatively large, these<br />

assessments on drought status will be also “dependent on assumptions about soil types and<br />

pasture condition which are quite specific to individual properties” (Stafford-Smith 2003).<br />

On the other hand, more straightforward, easily calculated drought indices and measures that are<br />

based on just rainfall or soil moisture and which can be calculated on a more universal manner<br />

appear, unfortunately, to be less closely aligned with issues <strong>of</strong> farmer hardship in Australia and<br />

maybe less relevant to application for assessment <strong>of</strong> exceptional drought assistance, to which<br />

drought indices in Australia are inexorably applied.<br />

Indeed, it has been noted that a single national measure (index) <strong>of</strong> exceptional and extreme<br />

drought is “likely to create inequity between regions” (Stafford-Smith 2003). This is especially the<br />

case <strong>of</strong> a country as large as Australia in that the timing and pattern <strong>of</strong> drought declarations is<br />

likely to differ between regions and types <strong>of</strong> agricultural land use (Stafford- Smith 2003, White and<br />

Walcott 2009).<br />

In a similar manner to that employed by Keating and Meinke (1998) in respect to assessment <strong>of</strong><br />

agricultural drought for cereal cropping enterprises, Stafford-Smith and McKeon (1998) emphasize<br />

the need for an integrated index for application but focused on pastoral enterprise drought<br />

assessment. They applied 100-year pasture growth and animal liveweight-gain simulations (using<br />

the GRASP simulation model for pasture production) in relation to the monitoring, assessment, and<br />

declaration <strong>of</strong> droughts in Australia and recommended a form <strong>of</strong> an integrative index since<br />

information on soil moisture and pasture growth noticeably give differing results from a rainfall<br />

index alone (Stafford-Smith and McKeon 1998, White and Walcott 2009).<br />

Utilization <strong>of</strong> “Common” Single <strong>Agricultural</strong> <strong>Drought</strong> <strong>Indices</strong><br />

To an Australian agronomist, drought tends to be defined as below-average rainfall that restricts<br />

typical plant growth for agricultural production. On the other hand, measurements <strong>of</strong> amounts <strong>of</strong><br />

rainfall expressed as deciles are rarely questioned by drought relief agencies in terms <strong>of</strong><br />

recognition <strong>of</strong> meteorological drought, unless a dispute on the density <strong>of</strong> rainfall gauges is raised.<br />

However, because <strong>of</strong> the widely varying nature <strong>of</strong> soils, crops, and pasture species, disputes may<br />

be initiated by farmers or different assessment agencies (usually state agencies) with other<br />

drought assessment agencies (usually federal agencies) over “which is the more reliable crop or<br />

pasture model to apply as an index in agricultural drought assessment,” especially if state<br />

governments provide their own scientific inputs, which may be at odds or even in competition for<br />

notoriety with federally produced scientific inputs—such has been the nature <strong>of</strong> state-federal<br />

politics in Australia and competition or even jealousy between scientific agencies and individuals.<br />

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