Aridity index Sample Clauses

Aridity index.Β The aridity index map shows moisture availability for potential growth of reference vegetation ignoring the impact of soil condition to absorb and retain water (Figure 11). The aridity index value is higher for more humid environments and lower for more arid environments. Precipitation and temperature data were obtained from the WorldClim dataset and mean annual evapotranspiration (MAE) was estimated based upon modelling of evapotranspiration (PET) (Xxxxxx X. Xxxxx, Xxxxxxxx, Xxxxxx, & Xxxxxxx, 2008). The aridity index was created by the Consultative Group on International Agricultural Research - Consortium for Spatial Information (CGIAR-CSI). This index is at a resolution of 30-arc seconds, or approximately 1 kilometer at the equator. Aridity is typically expressed as a function of precipitation, PET and temperature (X X Xxxxx, Xxxxxxxx, Xxx Xxxxxxxx, & Xxxxxx, 2006). The aridity index is used to calculate precipitation deficit over the ability of the atmosphere to remove water through evapo- transpiration processes (Xxxxxx X. Xxxxx et al., 2008). The equation used to calculate and map the aridity index is: π΄π‘Ÿπ‘–π‘‘π‘–π‘‘π‘¦ 𝐼𝑛𝑑𝑒π‘₯ (𝐴𝐼) = π‘€π‘’π‘Žπ‘› π‘Žπ‘›π‘›π‘’π‘Žπ‘™ π‘π‘Ÿπ‘’π‘π‘–π‘π‘–π‘‘π‘Žπ‘‘π‘–π‘œπ‘› (𝑀𝐴𝑃) π‘€π‘’π‘Žπ‘› π‘Žπ‘›π‘›π‘’π‘Žπ‘™ π‘’π‘£π‘Žπ‘π‘œπ‘‘π‘Ÿπ‘Žπ‘›π‘ π‘π‘–π‘Ÿπ‘Žπ‘‘π‘–π‘œπ‘› (𝑀𝐴𝐸)
Sample 1

Related to Aridity index

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