Estimated anthropogenic global warming is currently increasing at 0.2°C per decade and will likely reach 1.5°C between 2030 and 2050 (Pishva et al., 2020). As a result, the evapotranspiration rate is enhanced and therefore increases the likelihood of drought stress in plants (Yang et al., 2010). Drought frequency and intensity in drylands is projected to increase from 1% to 30% by 2100 (Dai, 2013). Globally, about one-third of the land area is affected by drought (Pishva et al., 2020). It is a major threat and the most unpredictable constraint, causing considerable adverse effects on crop production worldwide (Anjum et al., 2017;Hussain et al., 2018).These effects include a variety of plant functional and biochemical disorders, such as reduction in the rate of carbon uptake and turgor, increased oxidative damage, changes in leaf gas exchange, activity of enzymes and ion balance, resulting in impaired development, growth