2003
DOI: 10.1175/1520-0450(2003)042<1107:dvopwo>2.0.co;2
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Diurnal Variation of Precipitable Water over a Mountainous Area of Sumatra Island

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Cited by 84 publications
(77 citation statements)
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“…Mixed (or mixing) layer development by strong solar heating has been reported by observational studies (Wu et al 2003;Hadi et al 2000;Hashiguchi et al 1996) and modeling study (Sasaki et al 2004). Murata et al (2006) suggested that a mixed layer develops when synoptic-scale SCCs move to the east of Sumatra, because cloud cover decreases and solar heating increases.…”
Section: Relative Humiditymentioning
confidence: 83%
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“…Mixed (or mixing) layer development by strong solar heating has been reported by observational studies (Wu et al 2003;Hadi et al 2000;Hashiguchi et al 1996) and modeling study (Sasaki et al 2004). Murata et al (2006) suggested that a mixed layer develops when synoptic-scale SCCs move to the east of Sumatra, because cloud cover decreases and solar heating increases.…”
Section: Relative Humiditymentioning
confidence: 83%
“…Below the enhanced stability layer at 2.5-3.5 km, a weakened stability layer (dy/dz of smaller 3 K km À1 ) appeared after 7 May. A mixed layer which develops over the land region of the Indonesian Maritime Continent by strong solar heating were studied by Sasaki et al (2004), Wu et al (2003), Hadi et al (2000), and Hashiguchi et al (1996). Murata et al (2006) suggested that a mixed layer develops when synoptic-scale SCC moves to the east of Sumatra, because cloud cover decreases and solar heating increases at that time.…”
Section: Temperaturementioning
confidence: 99%
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“…However, due to the relatively coarse horizontal resolution of the models, it was noted that the climate change signal could quite possibly manifest itself differently at smaller scales-particularly for relatively small island countries which are crudely (if at all) represented on model grids with horizontal resolutions of the order of several hundred kilometers. The existence of (unresolved by models) large mountain peaks and valleys can introduce local circulations such as mountain and valley breezes, katabatic winds, and rain shadow effects, while detailed coastal boundaries and contrasting land surface types can also be important in shaping diurnal cycles of rainfall [Holland and Keenan, 1980;Liberti et al, 2001;Wu et al, 2003;Mori et al, 2004;Byon and Lim, 2005;Sakurai et al, 2005;Biasutti et al, 2012]. This is particularly true in the case of New Guinea where rainfall varies considerably over relatively small scales [Zhou and Wang, 2006].…”
Section: Introductionmentioning
confidence: 99%
“…Previous and ongoing studies using these instruments, as well as intensive rawinsonde soundings and satellite observations, have revealed several unique and interesting characteristics of precipitating cloud systems over this region, such as a diurnal land-sea rainfall peak and cloud cluster migrations Sakurai et al 2005), diurnal variations in precipitable water associated with local circulations (Wu et al 2003;Sasaki et al 2004), multi-scale interactions of convections and vertical wind variations associated with intraseasonal variation/oscillation (ISV/ISO; Seto et al 2004;Shibagaki et al 2006a), and type classifications of precipitating clouds and associated DSD variations (Renggono et al 2001;Kozu et al 2005). The VWP characteristics of precipitating cloud systems, however, have not yet been studied at sufficient temporal and spatial resolutions over this region or other tropical regions; this is despite the importance of VWPs in the dynamical and thermodynamical processes of precipitating clouds and in interactions with surrounding environments through latent heat releasing processes.…”
Section: Introductionmentioning
confidence: 99%