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amplitude of precipitation is realistic, but most models tend to start moist convection prematurely over land (Dai, 2006; Wang et al., 2011a). Many CMIP5 models also have peak precipitation several hours too early compared to surface observations and TRMM satellite observations (Figure 9.30). The hottest product st patricks day irish celtic full printing bedding set This and the so-called ‘drizzling bias’ can have large adverse impacts on surface evaporation and runoff (Qian et al., 2006). Over the ocean, models often rain too frequently and underestimated the diurnal amplitude (Stephens et al., 2010). It has also been suggested that a weak diurnal cycle of surface air temperature is produced over the ocean because of a lack of diurnal variations in SST (Bernie et al., 2008), and most models have dif culty with this due to coarse vertical resolution and coupling frequency (Dai and Trenberth, 2004; Danaba-soglu et al., 2006).
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