https://www.sciencedirect.com/science/article/pii/S2212094719302385

Could crop albedo modification reduce regional warming over Australia?

Jatin Kala, Annette L.Hirsch

Abstract

Climate observations and projections for Australia show an increase in warm
temperature extremes, including the frequency, duration and intensity of
heatwaves. Recent global scale studies have suggested that agricultural
land-use management options, such as increasing crop albedo, could reducing
local warming. Australia has approximately 3,727,210 km2 of cropland
agricultural land-use, the majority of which is in southwest Western
Australia and southeast Australia. This presents a potential opportunity to
reduce regional warming via crop albedo enhancement. We use a regional
climate model at 10 km resolution, to show that crop albedo enhancement of
up to 0.1 could reduce monthly mean daily maximum temperatures by −1.0 °C
to −1.2 °C, and monthly highest maximum temperatures by up to −1.4 °C to
−1.6 °C during the cropping season. This cooling is approximately 3 times
higher over Australia than global climate models predict. We highlight
stronger cooling over southwest Western Australia as compared to southeast
Australia, the opposite to global model studies which poorly resolve
southwestern agricultural regions. The regional cooling was driven by a
reduction in surface net shortwave radiation leading to a decrease in both
sensible and latent heat flux of up to 50 W m−2 and 20 W m−2 respectively,
when albedo is increased by up to 0.1. There were no cloud feedbacks or
effects on precipitation. Our results highlight the importance of using
regional climate models at a sufficiently high spatial resolution when
investigating agricultural land-use management to reduce regional warming.

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