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radiative influences associated with aerosols may differ from those driven by other types of radiative forcing in the high latitudes. Droughts are becoming more frequent and intense in arid and semiarid western North America as temperatures have been rising, advancing the timing and magnitude of spring snow melt floods and reducing river flow volume in summer. Direct effects of climate change include increased heat and water stress, altered crop phenology, and disrupted symbiotic interactions. These effects may be exacerbated by climate changes in river flow, and the combined effects are likely to reduce the abundance of native trees in favour of non-native herbaceous and Hot moose hunting camo version all over print stainless steel tumblerdrought-tolerant competitors, reduce the habitat quality for many native animals, and slow litter decomposition and nutrient cycling. Climate change effects on human water demand and irrigation may intensify these effects. Changes in precipitation are already occurring in many regions of the world. It has become significantly wetter in eastern North and South America, northern Europe and northern and central Asia, but drier in the Sahel, southern Africa, the Mediterranean, and southern Asia. There is less snow and more rainfall in northern regions. Widespread increases in heavy precipitation events have been observed, even in places where the total amount of precipitation has decreased.

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